WEBVTT 00:00:00.000 --> 00:00:00.000 First speaker this afternoon is Andrea. Yeah, we're on off. There we go. Yeah. 00:00:00.000 --> 00:00:00.000 She works at the USGS as a research hydrologist. And she focuses on, 00:00:00.000 --> 00:00:00.000 Exposure fake transport P fast manages a P fast research lab. That's the Eastern Ecological Science Center and, has the Bachelor's degree from Brown and a PhD from Harvard. 00:00:00.000 --> 00:00:00.000 And she's going to talk with us today about an effort to assess P fast occurrence and background concentrations in hamster soils. 00:00:00.000 --> 00:00:00.000 Thank you. 00:00:00.000 --> 00:00:00.000 Alright, thank you very much. So today I was asked to talk a little bit about our work looking at what we're calling anthropogenic background concentrations in New Hampshire. 00:00:00.000 --> 00:00:00.000 Soils. And so the majority of the talk will focus on that work and then I'll transition and talk a little bit about what the USGS is doing more broadly. 00:00:00.000 --> 00:00:00.000 Looking at groundwater concentrations of PEFASs doing more broadly, looking at groundwater concentrations of P. 00:00:00.000 --> 00:00:00.000 Fass using a groundwater concentrations of PFASs doing more broadly, looking at groundwater concentrations of PFAS using a very simple, very similar sampling design is what we and then finally I'll just conclude with a note about the work that my laboratory does, which is located just an hours drive from here. 00:00:00.000 --> 00:00:00.000 So. 00:00:00.000 --> 00:00:00.000 You need to be stuck. 00:00:00.000 --> 00:00:00.000 Oh, there it goes. Alright. Alright, so of course this work was done in collaboration with, many different people from the USGS, primarily Leos Antangelo, Sidney Ballach, and Joe, and then we did this work in close collaboration with the New Hampshire Department of Environmental Services, Jeffrey Marts, and then we did this work in close collaboration with the New Hampshire Department of Environmental 00:00:00.000 --> 00:00:00.000 Services, Jeffrey Marts, Kate Amos Lesser and Anthony Druin. 00:00:00.000 --> 00:00:00.000 And of course, many other people contributed to this project. So, let's just take a step back and talk about what anthropogenic P fast means. 00:00:00.000 --> 00:00:00.000 So when we talk about background concentrations, background for P fast should really be 0 or close to 0. 00:00:00.000 --> 00:00:00.000 You know, it's primarily a human made compound. And so background should be 0. But realistically, we've all seen that there's P fast and rain, there's P fast in the atmosphere, there's PFAS, it seems everywhere. 00:00:00.000 --> 00:00:00.000 And so I'm terming this anthropogenically fast background for the purpose of this talk. 00:00:00.000 --> 00:00:00.000 And that is what we were trying to understand for the state of New Hampshire. So New Hampshire, was required to set their soil remediation standard rulemaking and initiate that by November first, 2,023. 00:00:00.000 --> 00:00:00.000 You'll note that that was last week, which they did for PFNA, PFOS, and PFHXS. 00:00:00.000 --> 00:00:00.000 And so they came to the USGS asking for support because they needed a lot of information in order to do this. 00:00:00.000 --> 00:00:00.000 And so they came to the USGS asking for support because they needed a lot of information in order to do this rulemaking process. 00:00:00.000 --> 00:00:00.000 They've evaluated or could evaluate several 5 different components and that includes direct contact risk-based soil concentrations, bleaching base soil concentrations, background soil concentrations, which is the main focus of this talk. 00:00:00.000 --> 00:00:00.000 Ceiling concentrations and practical quantification limits. I'm not going to delve into any more details on how they've done this process, but I just wanted to mention that this work was directly translated into, rulemaking by New Hampshire DES, which has been a really exciting process to be part of. So. 00:00:00.000 --> 00:00:00.000 This study is part of a larger project with the state of New Hampshire. The first component was to characterize an propaganda PFAS throughout the entire state of New Hampshire in areas specifically not known to be impacted by local PFAS sources. 00:00:00.000 --> 00:00:00.000 And that is because a lot of work to date has been focused on hotspots, places where we know that PFS has been released. 00:00:00.000 --> 00:00:00.000 But with the declining Mcl's proposed MCLs, and, and statewide regulations, it's become more important to understand what is background in our environment. 00:00:00.000 --> 00:00:00.000 I think it's really important not just for soils like we're talking about here, but for groundwater, for surface waters, for atmospheric contributions because when we go to a site and we get a P fast detection. 00:00:00.000 --> 00:00:00.000 At what point does that mean that there's actually a local source or are we just looking at this anthropogenic background? 00:00:00.000 --> 00:00:00.000 And that's becoming really critical to understand. So the second part of this project was extensive laboratory experiments to understand partitioning. 00:00:00.000 --> 00:00:00.000 We did batch experiments, column experiments. We looked at pH and ionic strength effects. We evaluated soils and biosolids all from the state of New Hampshire. 00:00:00.000 --> 00:00:00.000 We looked at adsorption versus desorption, literally hundreds of samples we evaluated in the lab to better understand partitioning within the state. 00:00:00.000 --> 00:00:00.000 And then we also did a field investigation at 2 different sites. One was a biosolids impacted site, which is on an active farm where they have deposited biosolids for several decades. 00:00:00.000 --> 00:00:00.000 And then the second site was a fire training area, which many of us have come worked on one of those with And so this is just to mention that this is part of a larger study. 00:00:00.000 --> 00:00:00.000 And the part that I'm talking about today, which was of interest to this crowd was mostly the anthropogenic background in the soils. 00:00:00.000 --> 00:00:00.000 So how do we, develop an effective study design? For soil assessment? There are a lot of resources and I think Nikki pointed out some of them this morning that can be used to draw from ITRC as a good example for our state of Michigan. 00:00:00.000 --> 00:00:00.000 There are a lot of resources available now. When we started the study in 2020, there weren't quite so many resources available. 00:00:00.000 --> 00:00:00.000 And so I'll walk through some of the things that we considered when we did the study design and it closely matches what the recommendations are on line that you see these days. 00:00:00.000 --> 00:00:00.000 The most important thing is to consider your study goals of course. How are these data going to be used? 00:00:00.000 --> 00:00:00.000 What questions are you trying to answer that will dictate how your study design is set up? Do those data need to be compared to other data? 00:00:00.000 --> 00:00:00.000 In our case, the state of Vermont and Maine both also conducted soil studies and so we wanted to be able to compare our results to theirs. 00:00:00.000 --> 00:00:00.000 Although our design was was quite a bit different. The sample network design, what scale are we looking at? 00:00:00.000 --> 00:00:00.000 In this case, statewide. The number of sites for statistical significance, if you'd like to stratify your data in any way, look at different soil types. 00:00:00.000 --> 00:00:00.000 Or different land uses having enough statistical power in order to do that. And then I'll just group site selection and restrictions on location. 00:00:00.000 --> 00:00:00.000 So how do you define what an optimal site is for sampling? And if you're looking at a small area, this might be pretty self-explanatory. 00:00:00.000 --> 00:00:00.000 You want to sample that particular area for a statewide study. There are a lot of considerations. What do we consider to be an acceptable location to look at anthropogenic background? 00:00:00.000 --> 00:00:00.000 And I'll get into that. And then for soil sampling discrete or composite samples are 2 very different types of sampling and both have their advantages and disadvantages to considering whether or not you want a more homogeneous picture or you do want those discreet samples that are not composited. 00:00:00.000 --> 00:00:00.000 Is very important sampling depths how you're going to actually process your sample. And then this was mentioned also this morning, you know, what other type of supporting data is necessary. 00:00:00.000 --> 00:00:00.000 Organic carbon, pH, medals, you name it. Potentially there are ways to leverage other emerging contaminants of concern along with the study that you're executing. 00:00:00.000 --> 00:00:00.000 You know, we oftentimes have concern along with the study that you're executing. We oftentimes have blinders on because we're focused on PFAS and I'm absolutely guilty of this as well, but there's a lot out there. 00:00:00.000 --> 00:00:00.000 And so if we're going to do a statewide study. It's potentially advantageous to leverage resources to better understand other things as well. 00:00:00.000 --> 00:00:00.000 And like was described in excellent detail this morning, lab. And field QA QC and. And reporting limits, which was a big issue for us in 2,020. 00:00:00.000 --> 00:00:00.000 So our study goal is jumping right into our specific study was again to look at anthropogenic P fast concentrations in soil shallow soil across the state of New Hampshire. 00:00:00.000 --> 00:00:00.000 In order to do that, we limited our sampling to lands that were classified as forested, troubling, herbaceous, barren, or wetlands. 00:00:00.000 --> 00:00:00.000 So that means we excluded anything that was developed land. Agricultural lands and waters obviously. We also placed a 500 meter buffer around any parcels that had known or potential be fast contamination. 00:00:00.000 --> 00:00:00.000 And we were lucky because the New Hampshire had excellent documentation of all sorts of sites and facilities where they knew KEEPS was being emitted or likely to be omitted. 00:00:00.000 --> 00:00:00.000 Those are all those orange dots that you see across the state. And so that eliminated things like airports, waste water treatment plants, fire training areas, landfills, places we know that have 00:00:00.000 --> 00:00:00.000 One of the most important aspects of our study design was to employ this method called stratified equal area random sampling and what this does is it minimizes the bias and it provides equal statewide coverage. 00:00:00.000 --> 00:00:00.000 And so the way that it works is we gridded the state of New Hampshire up into 100 equal area grid cells. 00:00:00.000 --> 00:00:00.000 And then within those grid cells, there was 1 point randomly selected from each grid cell from which we took a sample. 00:00:00.000 --> 00:00:00.000 So that minimizes bias. It provides statewide coverage. It's also incredibly inconvenient. 00:00:00.000 --> 00:00:00.000 And so when we did this, you know, we knew this going in. It was going to be a challenge identifying at those random sites who the property owners are, how we're going to get there. 00:00:00.000 --> 00:00:00.000 For those who are not familiar with New Hampshire, the southern portion of the state is relatively populated. 00:00:00.000 --> 00:00:00.000 The northern portion of the state is basically forest. And so those random points were oftentimes, you know, in the middle of that country, impossible to get to. 00:00:00.000 --> 00:00:00.000 And so we of course had to get to somewhere accessible. But this was this was our design. It was not convenient. 00:00:00.000 --> 00:00:00.000 It was not easy, but it does minimize bias. 00:00:00.000 --> 00:00:00.000 So at all 100 of our locations, we did sample from 0 to 6 inches in depth. 00:00:00.000 --> 00:00:00.000 And that was to compare directly to Vermont and main concentrations. Who also conducted a study looking from 0 to 6 inches in depth at 50 of these locations we went further to look from 6 to 12 inches in depth to better understand migration of PFAS through the shallow soil to the subsurface and then at 6 locations we did a profile down to 36 inches. 00:00:00.000 --> 00:00:00.000 We analyzed for 36 different P fast compounds. Tapa, the total oxidizable precursor assay, which was nicely talked about earlier. 00:00:00.000 --> 00:00:00.000 We did that at 50 of our locations all from 0 to 6 inches in depth. And then we measured pH, total organic carbon protein. 00:00:00.000 --> 00:00:00.000 Given that there is recent research looking at protein as a, as a sorption mechanism essentially for PFAS. 00:00:00.000 --> 00:00:00.000 Percent moisture and then we did a visual classification of the soils. 00:00:00.000 --> 00:00:00.000 So we cleared our land surface of leafletter, sticks, and so forth. We use D fast free sampling equipment, primarily stainless steel, everything, stainless steel trials, bowls, auguras. 00:00:00.000 --> 00:00:00.000 And then, samples. Up the, at the target location. We're collected from 3 nearby locations and then composited and homogeneized within Restala Stale Bowl. 00:00:00.000 --> 00:00:00.000 We cleaned off our equipment between samples without using any methanol and that actually was incredibly effective. We were able to brush off loose soil, rinse with DI water, scrub with Liquinox with the eye water and then did a very thorough DI water rinse and then finally a P fast-free LCMS grade water branch that was also key fast-free. 00:00:00.000 --> 00:00:00.000 And with all of that rinsing and rinsing and more rinsing, we were all of that rinsing and rinsing and more rinsing, we were able to achieve a clean sampling equipment without generating a lot of methanol waste. 00:00:00.000 --> 00:00:00.000 That we would have to transport across the state. 00:00:00.000 --> 00:00:00.000 Okay, so we did collect 22 equipment blanks. We actually collected a lot more than that. We measure 22 equipment blanks and those were measured for PFAS, TAPA and TOC. 00:00:00.000 --> 00:00:00.000 The way that we took blanks for soil was actually a water blank in which we put the we Essentially, put the water over all of our sampling. 00:00:00.000 --> 00:00:00.000 Equipment measured the water volume so we knew exactly how much mass we were dealing with and send that off for aqueous analysis then we could convert that back to a massive PFAS in case of any detections. 00:00:00.000 --> 00:00:00.000 We did source solution blanks and then several sets of replicates and, 20 sets of matrix spike matrix like duplicates. 00:00:00.000 --> 00:00:00.000 To ensure quality control. 00:00:00.000 --> 00:00:00.000 So, Equipment Blank concentrations were really minimal. And if any, if they were ever detected, they were determined to be unlikely to impact any sample results. 00:00:00.000 --> 00:00:00.000 We had bigger questions about method blank detections that came back from the contracts lab. And, we decided to censor the data if it was less than 5 times the method blind detection and that resulted primarily in censoring of PFBS, which seems to be a problem for the laboratory and some minor instances of one PFHXA and 5 6 to FDS samples. 00:00:00.000 --> 00:00:00.000 The duplicate RPD was, surprisingly good considering how a non homogeneous, or, it's less than 25% for all compounds except for all compounds except for all compounds except for PFTRDA which was less than 25% for all compounds except for PFTRDA which was 27%. 00:00:00.000 --> 00:00:00.000 30% are within those 2 dashashed blue lines. Generally, we see really excellent recoveries across the board. 00:00:00.000 --> 00:00:00.000 I've highlighted a few. Where we see some deviations. These are important to keep in mind and keep track of that because they can provide negative or positive bias. 00:00:00.000 --> 00:00:00.000 In your sample interpretation, Luckily those compounds didn't seem to be particularly important to our study. 00:00:00.000 --> 00:00:00.000 But you know these it's really important to look at the QC data and look at it really closely because if you think you have a non detect but all of your recoveries are 50% you know, it leads to a negative bias. 00:00:00.000 --> 00:00:00.000 So it's important to keep this in mind. 00:00:00.000 --> 00:00:00.000 Okay, so getting to some of the results. What we're looking at here is again compounds on the X-axis arranged in the same way. 00:00:00.000 --> 00:00:00.000 And then, the number of samples all the way up to 100 samples from across the state. Samples that were less than MDL are shown with the gray bars and then in orange are detections with a J flag so that means that they were in between the method detection limit and the recording limit. 00:00:00.000 --> 00:00:00.000 And then detections with no J-flag. In other words, they're above the recording limit or in blue. 00:00:00.000 --> 00:00:00.000 You can see right off the bat that primarily we're seeing a large range of carboxylate compounds and PFOS. 00:00:00.000 --> 00:00:00.000 So, looking at this another way, if we pause the detection frequency on the x-axis here, we have the number of per fluorocarbons. 00:00:00.000 --> 00:00:00.000 And so that means that PEFOSA is 7 and PFOS is 8. And we have detection frequency on the y-axis and we see an orange are the carboxylic acids. 00:00:00.000 --> 00:00:00.000 The closed symbols are 0 to 6 inches and the open symbols are 6 to 12 inch depth samples in blue we have the same for the And so we see for the Ker Box slits that we have a wide range of carboxylic compounds with eye detection frequencies across the state. 00:00:00.000 --> 00:00:00.000 And keep in mind these samples are from Natural quote unquote land use as much as we could. And oftentimes in very forested remote areas, when we look at cellphones, we see that there is this zigzag pattern and that we also see in our groundwater data the USGS has from eastern United States and actually beyond that as well we see the zigzag pattern where the even 00:00:00.000 --> 00:00:00.000 chain length compounds have much much higher detection frequencies than the odd chain length compounds and that likely reflects manufacturing history. 00:00:00.000 --> 00:00:00.000 When we look at detection frequency of other compounds, they're generally much lower than the the PSAA and so I've put those in a table here on the right. 00:00:00.000 --> 00:00:00.000 Which you can review if you're interested. 00:00:00.000 --> 00:00:00.000 So looking at the concentrations of PFAS, we're looking here. The purple again is the carboxylates, the blue or the soft names at the end. 00:00:00.000 --> 00:00:00.000 And then that green bar that you see is Gen X HF PO DA. I just want to point out that the concentrations on this plot are on a log scale. 00:00:00.000 --> 00:00:00.000 And so those are incredibly low concentrations of Gen X. I think it was oftentimes a judgment call whether or not those were real detect or not. 00:00:00.000 --> 00:00:00.000 So treat that data with caution. The other compounds we see of course that PEPOS and PEFOSA are highest in concentration. 00:00:00.000 --> 00:00:00.000 For PFOS it was about 0 point 9 6 nanograms per gram meeting concentration across the state of New Hampshire. 00:00:00.000 --> 00:00:00.000 I've put the common laboratory reporting limit as one nanograms per leader and those of you who are a student might point out that that is no longer true from 1,633. 00:00:00.000 --> 00:00:00.000 It was true at the time we started this 20 this study in 2,02016 33 did not exist yet and that was the reporting limit we were typically given from various laboratories. 00:00:00.000 --> 00:00:00.000 And so we had to work with the laboratories. They actually were able to reduce their detection limits substantially, which is excellent because as you can see, most of our data would have fallen below it. 00:00:00.000 --> 00:00:00.000 And so that was that was really important for the study to be successful. The median MDL, because the MVL varied by day by batch of samples that we sent. 00:00:00.000 --> 00:00:00.000 And also by, by sample itself, the NDL. Median is plotted as those blue lines just to give you a sense of where the data is falling. 00:00:00.000 --> 00:00:00.000 The most, one important point that I should make is that, across the state of New Hampshire every single 0 to 6 and 6 to 12 inch soil sample that we collected had the technical P fast within it was mentioned earlier that other more global soil studies have also found similar, results. 00:00:00.000 --> 00:00:00.000 So we're looking. Very forested places and yet we still see. Substantial, you fast concentrations. 00:00:00.000 --> 00:00:00.000 Visually, this is what the sum of P fast looks like in the state of New Hampshire. 00:00:00.000 --> 00:00:00.000 There are 2 plots here. The first one on the left is showing nanograms per gram of the sum of 35 different PFAS. 00:00:00.000 --> 00:00:00.000 We did drop one compound PF ODA because of core recoveries. And then on the right we see the sum of 35 PFAS as well in Pico Moles program. 00:00:00.000 --> 00:00:00.000 I only show that to point out that really if we're gonna look at songs we should do it on a molar basis, but we've all been trained for PFFs to think in nanograms per leader and nanograms per gram. 00:00:00.000 --> 00:00:00.000 So I've given in and we're gonna use manograms for grand nanograms per leader for the rest of this talk. 00:00:00.000 --> 00:00:00.000 But the distribution does not change very much as you can see. 00:00:00.000 --> 00:00:00.000 When we split this up and start looking at different compounds and different trends on the left we see PSCAs, the sum of 12 PSCA compounds. 00:00:00.000 --> 00:00:00.000 And on the right, the sum of 8 PFSAs. The scales are the same between the 2 figures and we see that there are much higher concentrations for the sum of PFCAs than there are for PF essays and those PF essays are almost completely dominated by PS OS specifically. 00:00:00.000 --> 00:00:00.000 When we look at PEFOA and PFOS, we start seeing very different trends across the state. 00:00:00.000 --> 00:00:00.000 Pefoa, you can see that there's a higher concentration of higher detections in the southern portion of the state. 00:00:00.000 --> 00:00:00.000 There is a note, first of all, there's higher population density in the southern portion of the state. 00:00:00.000 --> 00:00:00.000 And second of all, there is a known large emitter for atmospheric, key fast in the southern part of the state. 00:00:00.000 --> 00:00:00.000 It's unknown how much they contribute to that PFS. Pfoa, total load there, but we do see a statistically significant increase in PE concentrations in the southern part of the state. 00:00:00.000 --> 00:00:00.000 Key Foss on the other hand is much more broadly distributed. You see high concentrations even in the north. 00:00:00.000 --> 00:00:00.000 And we see very, very strong correlations between PFOS and organic carbon. Hey, in the soils. 00:00:00.000 --> 00:00:00.000 Tapa was somewhat surprising for me. I've done a lot of work on DOD sites and looking at at and fire training areas. 00:00:00.000 --> 00:00:00.000 Vermont is plotted in green and the main study is plotted in purple and we can see that generally New Hampshire had much higher concentrations of P fast across the board. 00:00:00.000 --> 00:00:00.000 And, why this is, I think, is a probably nuanced question, that we don't necessarily have the answers to. 00:00:00.000 --> 00:00:00.000 New Hampshire is more popular populated to start with. Or has higher population densities at least. 00:00:00.000 --> 00:00:00.000 I think there are questions about atmospheric transport and load that we don't know the answers to to really fully say why this is occurring. 00:00:00.000 --> 00:00:00.000 We do see a statistically significant. A decrease in soil concentrations as we move deeper into the soil profile. 00:00:00.000 --> 00:00:00.000 So the 6 to 12 inch samples are generally lowering concentration for all compounds. As we move deeper in the soil profile. 00:00:00.000 --> 00:00:00.000 We can see. This also with those 6 sites where we went down to 36 inches when we when we could get it without hitting the water table. 00:00:00.000 --> 00:00:00.000 And so you can see here that typically P fast concentrations decreased with depth below the land surface. 00:00:00.000 --> 00:00:00.000 Okay, so let's talk about what this means. So As has been pointed out, you know, P fast. 00:00:00.000 --> 00:00:00.000 Is fairly prevalent in our soils as we see in New Hampshire and it really leads to this discussion about what that means. 00:00:00.000 --> 00:00:00.000 So I think we have this massive PFAS. So I think we have this massive PFAS soil reservoir that's sitting in our soil surface and this has been proposed in the literature as well over the last couple of years. 00:00:00.000 --> 00:00:00.000 If we do some back of the envelope calculations and we assume that median concentration of PFOS is point 9 6 nanograms per gram as we determine from our study and a soil dry bulk density of one gram per centimeter cube which is very low and a New Hampshire land area that includes all land use types we can calculate that we have 3,400 So to put that into 00:00:00.000 --> 00:00:00.000 context, that's enough PFOS to contaminate over 7,000 years of domestic water use in New Hampshire at a concentration of 4 nanograms per leader that proposed MCL. 00:00:00.000 --> 00:00:00.000 So that's a totally unrealistic scenario I'd like to point out that's not actually what's happening right because it depends on where the water is coming from and and assumes that you have leeching in exactly 4 nanograms per leader. 00:00:00.000 --> 00:00:00.000 It's not a realistic estimate. It just provides some context of how much 3,400 kg means. 00:00:00.000 --> 00:00:00.000 And that assumes, you know, 79.7 million gallons per day. Used in New Hampshire for domestic uses and that includes drinking and food prep and bathing and washing and so forth. 00:00:00.000 --> 00:00:00.000 So starts to put into context how much PFOS and that's just for PEPOS, how much POSS we're talking about. 00:00:00.000 --> 00:00:00.000 So I'm not going to delve into some of them more interpretive aspects of the study and we are still working on that. 00:00:00.000 --> 00:00:00.000 But we do have statistically significant correlations. Using Spearman Row. Positive correlations using Spearman Roe. 00:00:00.000 --> 00:00:00.000 Positive correlations for protein and. Positive correlations for protein and TOC, positive correlations for protein and TOC, as has been found in many studies, negative correlations for pro team and TOC, as has been found in many studies, negative correlations for pro team and TOC, as has been found in many studies, negative correlations with PH and negative correlation with latitude as we talked about specifically for 00:00:00.000 --> 00:00:00.000 the PSCAs like we showed with PEFFA having a higher concentration in the southern portion of the state. 00:00:00.000 --> 00:00:00.000 So I'm going to quickly summarize this and then move on to some of the other work that the USGS is doing. 00:00:00.000 --> 00:00:00.000 But the main takeaways of this New Hampshire background, anthropogenic background study was the use of an equal area grid approach that minimized sampling bias and also provided statewide coverage. 00:00:00.000 --> 00:00:00.000 It, it was not convenient, but it does provide a more robust set of data. 00:00:00.000 --> 00:00:00.000 Pfas were detected in every single 0 to 6 and 6 to 12 inch sample. We have a reservoir of PFAS that is stuck with in the soils and potentially could slowly leach out over time. 00:00:00.000 --> 00:00:00.000 And, we, we find that concentrations typically decrease with depths in the soil, which indicates retention in the top layers. 00:00:00.000 --> 00:00:00.000 Topper results were surprisingly low. Which I think is good news and we are still working on data analysis. 00:00:00.000 --> 00:00:00.000 So, just to bring this, back into context, that was one part of this larger study with. 00:00:00.000 --> 00:00:00.000 Hampshire. We are also still working on interpreting all of our laboratory experimental data, the column experiments, the batch experiments and so forth and our field studies as well. 00:00:00.000 --> 00:00:00.000 I wanted to point out that we also have a pilot study that is now looking at the we also have a pilot study that is now looking at the bleaching potential into shallow groundwater that is now looking at the bleaching potential into shallow groundwater that is now looking at the bleaching potential into shallow ground water. 00:00:00.000 --> 00:00:00.000 So we know that there's P fast in the soil, that is now looking at the bleaching potential into shallow ground water. 00:00:00.000 --> 00:00:00.000 So we know that there's P fast in the soil, but and we know and we' about ready to publish those results as well. 00:00:00.000 --> 00:00:00.000 Okay, so, switching tracks somewhat, but this is related in the sense that the same equal area design that we use for our New Hampshire study was actually taken from a broader groundwater network that the USGS has and they use the same equal area stratified equilibrium grid approach in order to do a well selection to understand detection frequencies of contaminants and principal aquifers across the United States. 00:00:00.000 --> 00:00:00.000 And so in 2,019, the USGS started adding PFAS sampling to the National Water Quality Network for groundwater. 00:00:00.000 --> 00:00:00.000 And also the California groundwater ambient monitoring assessments program. That's the Gamma program. 00:00:00.000 --> 00:00:00.000 Both of these networks do provide long-term consistent and comparable information on groundwater quality. They've been sampled for many, many things for many, many years besides P fast. 00:00:00.000 --> 00:00:00.000 Just in 2019, we added be fast to the mix. And they provide information on our, the nation's ground water quality and the trends over time. 00:00:00.000 --> 00:00:00.000 So the idea is that these networks are sampled on a ten-year cycle in order to understand changes in quality. 00:00:00.000 --> 00:00:00.000 So in 2019, you can see on the map there, we had samples primarily from the East Coast networks. 00:00:00.000 --> 00:00:00.000 We published a paper in 22, and we are working on a follow-up paper with data all the way from 2019 to 23 which includes all of those purple dots that you see there. 00:00:00.000 --> 00:00:00.000 So the national water quality network. Is composed of 82 networks, each with 20 to 30 wells approximately and the depths are targeting the zone used for drinking water and they also target specific land uses. 00:00:00.000 --> 00:00:00.000 So usually targeting one of those 2 things like urban land use or agricultural land use. They're sampled on a 10 year cycle in order to evaluate the cattle scale trends. 00:00:00.000 --> 00:00:00.000 Likewise, the California Gamma program. Is has a similar network design which allows us to sort of mesh that data together. 00:00:00.000 --> 00:00:00.000 And they're also specifically looking at networks for drinking water supply statewide. And so in, 22, we published a paper where we said, okay, we have all this groundwater data. 00:00:00.000 --> 00:00:00.000 It's collected using our equal area approach. We're not targeting specific sources. We are we are just looking at the landscape and looking at what's in our ground water. And so we decided to build a model. 00:00:00.000 --> 00:00:00.000 We ended up using a business regression tree model to better understand what variables are driving whether or not we see P fast occurrence in groundwater. 00:00:00.000 --> 00:00:00.000 And so we compared 57 different potential predictor variables and you can see a long list of them on the screen here, but generally they included geochemical conditions, hydrologic position and this included Tritium, which is a tracer for groundwater age, well depths, landscape sources, which we were able to leverage the work that the EPA had done with their analytical 00:00:00.000 --> 00:00:00.000 toolbox. Or PFAS toolbox. And then we looked at urban land use, natural land use, agricultural land use and so forth. 00:00:00.000 --> 00:00:00.000 And so our model, found that the most important predictors of P fast occurrence in groundwater was the number one predictor was tritium which is a tracer for groundwater age and tritium concentrations coincide with chemical weapons testing in 1,953 which is around the same time period that PFAS started being widely used and likely emitted into the environment. 00:00:00.000 --> 00:00:00.000 And so we have a fairly good tracer of whether or not we think we're going to have key fast in our sample is whether or not it's modern groundwater. 00:00:00.000 --> 00:00:00.000 The second most important picture you can see is distance from the near its fire training area and then things like urban land use are further down on the list. 00:00:00.000 --> 00:00:00.000 We can look at partial dependence. So for example, on the x-axis here, we see urban land use and as you'd increase urban land use you have a greater probability of a fee fast detection. 00:00:00.000 --> 00:00:00.000 So as we can see here, this model did a really good job at predicting a P fast occurrence. 00:00:00.000 --> 00:00:00.000 We weren't quite ready to actually use it to predict the areas where we hadn't sampled yet, but with the incoming data that we have since 2,019 we are now revisiting that and we are currently building a model that is using only mapable factors to try and predict EFASa crashes across the Conas. 00:00:00.000 --> 00:00:00.000 And so we're only using mapable factors, things like land use. And different sources of P fast because otherwise we wouldn't be able to predict the unknown locations. 00:00:00.000 --> 00:00:00.000 And so that is what we are currently working on. And it's all based on this equal area red design. 00:00:00.000 --> 00:00:00.000 Run a B fast laboratory. It's only an hour from here if anybody wants to stop by. 00:00:00.000 --> 00:00:00.000 It's at the Eastern Ecological Science Center and Carneas built West Virginia. We have a high-resolution mas spectrometer. 00:00:00.000 --> 00:00:00.000 We do both targeted and non-targeted analysis. With a variety of matrices and we can work with very very small sample volumes. 00:00:00.000 --> 00:00:00.000 We are a research laboratory so we're not regulatory. We are really designed to help with research. 00:00:00.000 --> 00:00:00.000 Deal with those weird samples that you don't know what to do with and how to measure, we'll work with them. 00:00:00.000 --> 00:00:00.000 And there you see my other lab group members, Zach Hopkins, David Wanlow and work in Begs. 00:00:00.000 --> 00:00:00.000 So happy to talk about that if anybody's curious. So hopefully we have a few minutes for questions. 00:00:00.000 --> 00:00:00.000 Thanks. 00:00:00.000 --> 00:00:00.000 Great, anyone in the room? 00:00:00.000 --> 00:00:00.000 Okay, I believe we hope. I see a question in the room. Go ahead. 00:00:00.000 --> 00:00:00.000 There's a question here. You got the mic right there. 00:00:00.000 --> 00:00:00.000 Okay, great presentation. The findings that you presented were pretty stark when you consider like for So the ground water protection criteria are less than your median concentrations for P. 00:00:00.000 --> 00:00:00.000 So it really does seem like your recommendation to better understand. The nature of groundwater impacts is imperative, right? 00:00:00.000 --> 00:00:00.000 We've got pervasive soil impacts above a potential. So the groundwater pathway criterion. 00:00:00.000 --> 00:00:00.000 And, you know, the question of background now is going to become Uber complicated. 00:00:00.000 --> 00:00:00.000 I agree. That's a great impact. I think it really, it's becoming really critical. 00:00:00.000 --> 00:00:00.000 That we better understand what's happening in this anthropogenic background that we better understand what's happening in this anthropogenic background scenario. 00:00:00.000 --> 00:00:00.000 We've done so much incredible work looking at hotspots and you know where we know key pass were released but you know it's and this is You know, we know P faster and polar bears and in the oceans, but these concentrations are they're not they're not in substantial and and I think that it really warrants a lot more research on the topic. 00:00:00.000 --> 00:00:00.000 Absolutely. 00:00:00.000 --> 00:00:00.000 So I just, maybe it's a very small point, but you showed, our bias recoveries for both. 00:00:00.000 --> 00:00:00.000 And I was just gonna ask to do if you had idea of what the cause might be. You know, so. 00:00:00.000 --> 00:00:00.000 I'd probably say we this is probably a question for the contract laboratory. I was following EPA method. 00:00:00.000 --> 00:00:00.000 5 37.1 modified and I know EPA absolutely hits it when I say modified EPA. 00:00:00.000 --> 00:00:00.000 37.1 modified and I know EPA absolutely hits it when I say modified EPA 5 37.1. 00:00:00.000 --> 00:00:00.000 But From an analytical perspective, FAFSA is hard, right? Because FAFSA also has this sort of weird transition. 00:00:00.000 --> 00:00:00.000 There's no qualifier ion in many cases. Qualifier ions were not used for P fast or POSIT quantification and so there could be some bias. 00:00:00.000 --> 00:00:00.000 And we're not used for PEPS or POSTA quantification. And so there could be some bias from that. 00:00:00.000 --> 00:00:00.000 Okay. 00:00:00.000 --> 00:00:00.000 Craig, define arcadis just to follow up to Joe's question on, significance to, you know, potential impacts to background or groundwater. 00:00:00.000 --> 00:00:00.000 What, what do you think this has to do? With our concept of background load and surface water. I'm thinking about overland flow, overland flow, storm water driven impacts, you know, this very diffuse. 00:00:00.000 --> 00:00:00.000 Shallow soil impact. Right. Is, is there a need for background surface water and storm water, attributed to, this source? 00:00:00.000 --> 00:00:00.000 Right. I okay, so I don't know if I'm supposed to repeat the question, but I wasn't doing that, but the question was whether or not we should be looking more at a background or genetic background concentrations of storm water or overland flow and surface waters and I think the answer is yeah we probably should. 00:00:00.000 --> 00:00:00.000 The USGS did start doing some sampling of streams and rivers across the US. 00:00:00.000 --> 00:00:00.000 Just this past summer to better understand what's in our surface waters but You know, I think there's an incredible amount of work to be done on that. 00:00:00.000 --> 00:00:00.000 And I think, you know, there was. Talk about the, groundwater surface water interactions. 00:00:00.000 --> 00:00:00.000 I think that becomes really important because everything from what I've seen from my work is that anything that has sort of what we call modern groundwater or water that's interacted with the atmosphere has the potential to have P fast and and sometimes at significant concentrations. 00:00:00.000 --> 00:00:00.000 And so how that all interacts, I think, is. Wildly not. Well characterized at this point. 00:00:00.000 --> 00:00:00.000 I'm a 00:00:00.000 --> 00:00:00.000 Hmm. Okay. Yeah. 00:00:00.000 --> 00:00:00.000 Of the Hey. Oh. It's a Hello. Yeah, Yep, great, great comments. 00:00:00.000 --> 00:00:00.000 Okay, the first question was. Our assumption here of a soil dry bulk density of one grand percent in meter cube and I've, you know, that's a very low value as was just pointed out and I 100% agree that is a very low value. 00:00:00.000 --> 00:00:00.000 We were doing a conservative estimate. So that is the only I found the lowest value I could across the literature and I use that. 00:00:00.000 --> 00:00:00.000 So that's the only reason we chose one. And then the second, comment was about the 7,000 years and what assumptions went into this calculation. 00:00:00.000 --> 00:00:00.000 And again, I will repeat that this is not a realistic calculation. It's just meant to show if you looked at 3,400 kg of PFOS and soil and you just happened to distribute all of that peakos into water at exactly 4 nanograms per liter, which we can all agree is unrealistic. 00:00:00.000 --> 00:00:00.000 How much water are we talking about being contaminated? Just to put into perspective. So, 100% agree. 00:00:00.000 --> 00:00:00.000 It is not a realistic calculation. It's just meant to put things into context. Yeah. 00:00:00.000 --> 00:00:00.000 We have an online question. The online questioner asks, did you consider air emitters outside of the state where prevailing winds could transport PFAS into the study area. 00:00:00.000 --> 00:00:00.000 Yes. So great question and, the answer is that we would need to do an entire study on atmospheric deposition, which comes to one of my favorite points to talk about these days, which is that we really need that. 00:00:00.000 --> 00:00:00.000 And yes, so we, were looking at the soil, which is, you know, obviously linked to the atmosphere. 00:00:00.000 --> 00:00:00.000 We did not do a full atmospheric study. I think that that would be fantastic and I would love to be part of that. 00:00:00.000 --> 00:00:00.000 And ideally also beyond just New Hampshire but nationwide. Yes. Okay. 00:00:00.000 --> 00:00:00.000 Thank you. 00:00:00.000 --> 00:00:00.000 So our next speaker is not with us. She is online, I believe. Is that correct? She is. 00:00:00.000 --> 00:00:00.000 All right, it is Rebecca Higgins from the Minnesota Pollution Control Agency. 00:00:00.000 --> 00:00:00.000 He is a senior. They didn't see there and currently serves as co-chair of the ITRC. 00:00:00.000 --> 00:00:00.000 And President-elect with the, so, Groundwater Association. Her current role is a state regulator. 00:00:00.000 --> 00:00:00.000 She provides technical oversight. Free pass investigations in East. Under a 7, 3 m, 2018 settlement and another 3, super fund size. 00:00:00.000 --> 00:00:00.000 This is work that we are focused on because we have over 1,400, wells that are residential and municipal supply wells that have health advisories. 00:00:00.000 --> 00:00:00.000 And treatment on them for PFAS impacts in particular. And so the area that I'm going to be talking about is really in the upper portion of that inset box there blown out for you. 00:00:00.000 --> 00:00:00.000 And this is something special called the Project 1,007 Area. It was a singular line item in the settlement and, this is a infrastructure project installed in the late eightys. 00:00:00.000 --> 00:00:00.000 Basically a large flood control or storm water conveyance system installed to drain flood waters that were prevalently flooding homes as you can see in this picture provided by our watershed district that was really a problem back in the late eightys and so we've been understanding that while it was doing its job back in the late eightys. 00:00:00.000 --> 00:00:00.000 And so we've been understanding that while it was doing its job effectively to mitigate flood waters in the area and save homes from flooding. 00:00:00.000 --> 00:00:00.000 It also was conveying just as a conveyed water key fast. So, where water moves and P fast exists, hence P fast movement occurs to a greater degree. 00:00:00.000 --> 00:00:00.000 So today this area is greater than a hundred 20 square miles in size. Roughly speaking. And at the time I originally put the slide back together. 00:00:00.000 --> 00:00:00.000 And at the time I originally put the slide back together. And at the time I originally put this slide back together, we had a monitoring well network, speaking. 00:00:00.000 --> 00:00:00.000 And at the time I originally put the slide back together, we had a monitoring well network that was a result of this settlement work together we had a monitoring well network that was a result of this settlement work that was over 90 wells and I can fast forward now to say that's over I think it's a hundred plus now that we have for just monitoring in the system and you'll understand why that has grown over the time that we've been doing this work since the 2018 settlement but 00:00:00.000 --> 00:00:00.000 we also have not just monitoring wells across this broad area but we also have not just monitoring wells across this broad area but we also have not just monitoring wells across this broad area but we also have a number of surface water sample locations that we do continuously monitor in terms of characterization. 00:00:00.000 --> 00:00:00.000 And not just give you just yet another project to understand that there's P fast everywhere, but to really give you a better understanding of how you can, throw everything plus the kitchen sink at a project and find, that you, some of our hunches, I think maybe as hydrogeologists, we have a lot of hunches that we have to put into our work initially, but that we can really demonstrate through robust 00:00:00.000 --> 00:00:00.000 science that, it is really defensible and, worthwhile to go through those efforts. 00:00:00.000 --> 00:00:00.000 So that's what I hope to share with you. And I'll just start by mentioning very quickly that again, this was a singular line item in the in the conveyance of what was then called PSCs in the environment. 00:00:00.000 --> 00:00:00.000 So, bit of a data terminology, but one of the things that is special about this project is the fact that it is special in its terminology because it was attorneys at the time working under the NRDA settlement language, negotiating language that they felt was spinning. 00:00:00.000 --> 00:00:00.000 So some of the language that we were working with during this investigation process was unique to it and we have since grown not only the MS and its outcomes but also we've had to translate this now into much more circular direct, for a Larry's, for our jargon. 00:00:00.000 --> 00:00:00.000 So our process language has changed quite a bit as we've gone along. But we were given this onus underneath the settlement. 00:00:00.000 --> 00:00:00.000 So we were told to conduct a source assessment, as well as the feasibility study. But in the interim, we, felt it was, absolutely necessary to conduct near term actions as they were called at that time. 00:00:00.000 --> 00:00:00.000 Also known synonymously for those of us in the remedial area as interim corrective actions, to, try, to, do, what, we, could, to, stop, or, slow, the, spread, up, So, if you are a process person and you really like to think about the project management aspects of this, this was an extraordinary effort, over the past 4 plus 00:00:00.000 --> 00:00:00.000 years, to understand all that with all that goes into, you know, 70 years worth of P fast movement in the environment. 00:00:00.000 --> 00:00:00.000 So we conducted surface water investigation, sediment investigation, groundwater. We built out our own numeric model, which I'll tell you about later. 00:00:00.000 --> 00:00:00.000 And then we have a special project called a multi-benefit well array evaluation, which again is the topic for today, but it is a major component of our work, to get at that larger regional groundwater impact, evaluation and potential for, slowing the spread of PFAS. 00:00:00.000 --> 00:00:00.000 And then we've also conducted lastly on the right hand side there. It shows you the, water pilot study. 00:00:00.000 --> 00:00:00.000 And I'll just touch on that briefly. All of those built into those goals on the left hand side of identifying where treatment options are available for us for any one of these different media and whether or not those treatment options are even applicable at the scale that we're talking about. 00:00:00.000 --> 00:00:00.000 And then recommend to our co-trustees of the settlement dollars being 850 million dollars. 00:00:00.000 --> 00:00:00.000 That has been allocated to the larger drinking water protection, issue in the East Metro, whether or not these are appropriate, types of actions with the exception of some maybe some other places in the country. 00:00:00.000 --> 00:00:00.000 But as far as I know, it's maybe the oldest disposal site anywhere in the world, for P fast impacts emanating from at least, this, 3 M particular industrial waste material. 00:00:00.000 --> 00:00:00.000 And this was basically, you know, what we what they used to do, many, many decades ago, which was to fill the swamp, with waste material. 00:00:00.000 --> 00:00:00.000 A waste holler had property. It was, you know, largely made up of a wetland area and they quite literally filled the swamp with industrial waste along with other ways from other sources but in particular this was a receiving area for waste that still to the day emanates P fast masks off of it. 00:00:00.000 --> 00:00:00.000 So, remedial activities were in part related and conducted out there in the eightys. And then a shallow pump up, groundwater system was installed and fast forwarding to today. 00:00:00.000 --> 00:00:00.000 We understand that the conveyance of the surface water pathway is one that it has to be really an utmost focus of our work because it still does convey P fast mask through the site and down gradient. 00:00:00.000 --> 00:00:00.000 Unfortunately that Oakdale disposal site is also a hydrologic. Unfortunate reality and that's that it has a groundwater divide not just on site there but also nearby in multiple different aquifers than multiple different vertical, pathways and allows peak fast mass to spread in multiple directions in multiple areas across the larger regional context. 00:00:00.000 --> 00:00:00.000 We have a secondary service area called the Washington County landfill and the lower half of your screen that accepted P fast containing waste and then was closed in the seventies. 00:00:00.000 --> 00:00:00.000 Later there was a number of efforts to deal with other issues. The site, and it may be just aided in our understanding that you can exacerbate a problem by inadvertent activities such as a pipe being left open to a drain affluent for a number of years directly to a the project 1,007 conduit which then was a direct connection to surface water. 00:00:00.000 --> 00:00:00.000 Again, exacerbating the spread of P fast throughout the region. And so since then, of course, that pipe was turned off. 00:00:00.000 --> 00:00:00.000 That landfill has been since picked up and put literally replaced onto a triple liner. And so that waste material itself doesn't necessarily aid in in additional mass to the subsurface however the impacts once as we know into the environment continue to spread. 00:00:00.000 --> 00:00:00.000 So I guess this is really just to take a big step back and to give everybody maybe just a second to understand how much and how far PFAS can spread over the decades. 00:00:00.000 --> 00:00:00.000 When you have a well, hydrologically connected system. You can expect that these impacts unless otherwise mitigated have the freedom to spread as far as they can in the environment will allow and this just gives you a gross understanding of. 00:00:00.000 --> 00:00:00.000 Our depictions of the overall contaminant blooms as they sit in the East Metro. 00:00:00.000 --> 00:00:00.000 Not all of these are necessarily P fast. Dominated areas. However, the one that we're particularly talking about right now is this upper portion and that's this this area which now goes from the Mississippi River on the west side over to the Sankra River on the east side spinning as again many miles and distance as the crow flies west to east but also then you can see the effect of larger regional groundwater divides 00:00:00.000 --> 00:00:00.000 and I'll touch on many other aspects to the spread of this. P fast mass. But in the meanwhile, we do want to talk about what we can do to understand the transport mechanisms and just characterize our impacts better. 00:00:00.000 --> 00:00:00.000 This mass should have been flowing to the southwest versus Mississippi. And that we could have had some complicating factors in between the 2 primary source areas, but that we should generally expect things to be, you know, somewhat well. 00:00:00.000 --> 00:00:00.000 Characterized in terms of extent magnitude. Fast forwarding to 21 a couple of years ago we depicted this same or similar type of map. 00:00:00.000 --> 00:00:00.000 And we wanted to give an understanding to not only our co-trustees, but our public work groups that are very intimately partnered with us as the state to try to make the best decisions for these resources in the long term. 00:00:00.000 --> 00:00:00.000 And you can see that dash line going down the middle map there depicts the major regional groundwater divide for the area. 00:00:00.000 --> 00:00:00.000 However, we found sub regional divides throughout these multiple different, vertical aquifer, units that are exacerbating the spread of P fast in multiple directions. 00:00:00.000 --> 00:00:00.000 And then directly affected by major pumping centers and impacting ultimately many different thousands of residents in the area. 00:00:00.000 --> 00:00:00.000 So we have these 2 primary areas and we've understood now if you took all of those aquifers and put them into one layer it would you know change our map significantly at the end of the day but it's really important to note that as you can pay this information to the public it's, it's, it's our job really as geologists to make this. 00:00:00.000 --> 00:00:00.000 You know somewhat playing language and somewhat understandable that we do not have all information in hand despite years and many many dollars spent on this effort. 00:00:00.000 --> 00:00:00.000 We do have data gaps that remain and that we do understand that that is something we need to continue forward pushing forward to understand that you know you it's one thing to get a generalized understanding and make interpolations about these plumes, but it's a whole other thing to really explain this to the public that we are never necessarily completely satisfied. 00:00:00.000 --> 00:00:00.000 With a monitoring network, even as big and as robust as we have in hand, there are gaps because aquifer by aquifer in this case the parity chain is is really just, still lacking some, very important components of characterization. 00:00:00.000 --> 00:00:00.000 So although we like to share what we have as we go, we always have to be acknowledging that we're not completely done and you know that's that's just important to get context and always make sure that people understand we don't have all of the information in hand at any one time. 00:00:00.000 --> 00:00:00.000 We don't have all of the information in hand at any one time. To make sure that people understand we don't have all of the information in hand at any one time. 00:00:00.000 --> 00:00:00.000 And particularly as it pertains to PEPAS, right? So one of the things I'd like to make sure that I always send people home with no matter how technically adapt they are is just this fundamental principle that our surface water and groundwater connections and that conveyance is really important to characterize at the outset that it is not just a groundwater problem. 00:00:00.000 --> 00:00:00.000 It is not just a small source area problem. It is a regional investigation when you're looking at a source area that is anything but just recent in its spill or recent in its release. 00:00:00.000 --> 00:00:00.000 We're talking about a very large area that has surface water conveyance and that will continue to be conveying surface water with PFAS impacts because once out of the gate, that horse is not returning and surface water with P fast impacts because once out of the gate, that of course is not returning and, certainly the secondary source mass areas as you've heard others talk about, is so directly related to things like organic, 00:00:00.000 --> 00:00:00.000 And then really changing those geometries of the plumes and the stability of those plumes once deeper into those. 00:00:00.000 --> 00:00:00.000 You know, researchers aquifers that, you know, I think most of us would acknowledge the You know are not always going to, you know, horizontally stay as they should and very much complicated by larger regional situations and in this case we have a remnant from the mid continental rift that has left us with a large fracture zone to the eastern portion of this system that has only exacerbated 00:00:00.000 --> 00:00:00.000 the spread through those vertical pathways. So we're not just talking about, you know, those kind of small localized glacial impacts that can. 00:00:00.000 --> 00:00:00.000 Affect your characterization but also then larger regional geologic aspects that complicate matters. Even more. 00:00:00.000 --> 00:00:00.000 So that goes without saying that it's a complex picture and I think we all would agree with that. 00:00:00.000 --> 00:00:00.000 But I would like to give you a few examples really quickly and I'm gonna go through these quickly, but bear with me. 00:00:00.000 --> 00:00:00.000 I'd like to share with you as much as I can. So a few examples of some of the more interesting aspects I think that we've been able to deploy in this investigation and what might be useful to your investigations as you go forward. 00:00:00.000 --> 00:00:00.000 And so one of the most valuable aspects of I think our monitoring well installations have been downhill geophysics work that we've been able to do using rotary air rotary drilling of course and then really deploying as much as we could and bringing to bear the full brunt of the partnerships and the expertise of our partners. 00:00:00.000 --> 00:00:00.000 In this work. So the Minnesota Geological Survey coming to bear with their expertise and and tooling out in this work was really really wonderful. 00:00:00.000 --> 00:00:00.000 We deployed video logging of course to get the standard, you know, 4 whole side walls and all those wonderful visuals that we could understand as well as fracture patterns, flow directions, etc, as you would normally expect to get from that type of work. 00:00:00.000 --> 00:00:00.000 But then really saying, well, what else should we know about the area that we don't we don't already have from our County atlases and while though we have a wonderful recent, fresh County atlas update from our geological survey, we said let's just throw everything in the kitchen. 00:00:00.000 --> 00:00:00.000 Sink at this because we need to understand these pathways better, particularly because of the breadth of these plum spread. 00:00:00.000 --> 00:00:00.000 So we put everything out there, gamelogs, calipers, EM flow meters, and multi-parameter e-logs allowing for us to understand better all of these changes through the vertical profile to really get at what where we should be targeting our monitoring well sets. 00:00:00.000 --> 00:00:00.000 So this was very helpful right at the gate. We took a groundwater and soil sampling strategy that allowed us to use vertical aqua for profiling in order to set those wells at the right depth. 00:00:00.000 --> 00:00:00.000 And although I won't go through all of these bullets, it really is getting at the idea that we could use iterative in field analysis as well as then back-end visuals and analytical data coupled together to target our best, our best well sets so that we have well nests throughout the region, not just singular wells here and there. 00:00:00.000 --> 00:00:00.000 And also making sure that we were adequately characterizing the P fast impacts because early on we weren't necessarily sure. 00:00:00.000 --> 00:00:00.000 What type of mixture we have. We had a good guess, but it was really, really nailing down what type of mixture we were looking at and we wanted to make sure that these wellness were appropriately installed to adequately characterize that work. 00:00:00.000 --> 00:00:00.000 So pads forwarding, using a number of analytical tools, our primary, analysis throughout this process and throughout this investigation has been access SGS's MLA 1 10 method for multiple media and being able to use that consistently across the entire region and be able to use that through these wonderful wellness that were installed across a broad area for different geological purposes. 00:00:00.000 --> 00:00:00.000 We're able to bring all of that analytical information to bear and had another partner come in in this case for this example, the second example. 00:00:00.000 --> 00:00:00.000 It was to do some statistical analysis from the University of California, Berkeley through basically just taking our data sets that we already had in hand, but taking it well beyond, standard just percentage distribution and, standard, but taking it well beyond, standard, just percentage distribution and, standard breakdowns of our mixture. 00:00:00.000 --> 00:00:00.000 What was our, just percentage distribution and, standard breakdowns of our mixture and, standard breakdowns of our mixture. What was our P fast soup? 00:00:00.000 --> 00:00:00.000 What was our recipe that we were looking at. What was our P fast soup? What was our recipe that we were looking at? 00:00:00.000 --> 00:00:00.000 We were able to, hand this off to Berkeley and they were looking at, what was our recipe that we were looking at. 00:00:00.000 --> 00:00:00.000 We were able to, hand this off to Berkeley and they you know, mixing differently and at what depth we should be really looking at a potential opportunities then maybe in the future to mitigate spread or to understand where we could deploy effective. 00:00:00.000 --> 00:00:00.000 Remedial options of any variety. And I'll just say any writing because that's a different discussion. 00:00:00.000 --> 00:00:00.000 But, this really gave us not just an understanding of the groundwater picture, but also our surface water picture. 00:00:00.000 --> 00:00:00.000 And I mentioned that early on that it's not just about groundwater analysis. It's not just about small area, it's about getting well down gradient of where you think you might or should be looking. 00:00:00.000 --> 00:00:00.000 But these large-scale regional patterns of the allow us to understand better again where that mixing might be occurring or these signatures by grouping were aiding in our analysis. 00:00:00.000 --> 00:00:00.000 And we did this through not just that MLA 110 data, but also top assay. 00:00:00.000 --> 00:00:00.000 And now fast forwarding through today, we've taken what we've learned from this type of complex behavior and complex mixing from the surface to the subsurface and into our deeper aquifers. 00:00:00.000 --> 00:00:00.000 But we also have some really unexpected behavior and really the fate and transport parameters of these different mixtures as they've been out in the environment and well oxidized and well transformed as much as they possibly could be in the environment. 00:00:00.000 --> 00:00:00.000 Understanding that their behavior isn't always expected and particularly in these type of curse systems and in glacial systems watching how they've been moving and where they're mixing where they're not. 00:00:00.000 --> 00:00:00.000 Should we, you know, sort of take that opportunity to, maximize what remedial approaches could be appropriate for those constituents that might pose the greatest harm to human health. 00:00:00.000 --> 00:00:00.000 That type of theory and investigation and mindset has been going into this work. And then we've kind of grown that out from beyond just that again, beyond the one, the 1 10 analysis to top essay Toff and AOF as well. 00:00:00.000 --> 00:00:00.000 And, and then I'll pause before I move on and just say that. Again, this is a reiteration of the message that our signatures of the surface and in our surface waters and those statistics that we've looked at thus far don't always point to expected behaviors in some cases they do and in some cases they don't always point to expected behaviors. 00:00:00.000 --> 00:00:00.000 In some cases they do. And in some cases, they do. And in some cases, they do. And in some cases, they don't. 00:00:00.000 --> 00:00:00.000 They're again. In some cases, they do. And in some cases, they don't. 00:00:00.000 --> 00:00:00.000 They're again, once it's, they do and in some cases they don't. They're again, once it's just a constant message that P fast may or may not behave as expected in the environment. 00:00:00.000 --> 00:00:00.000 So, are may or may not behave as expected in the environment. So while I won't go into this detail, too deep, I just want to reiterate those main messages about using all of these types of statistical analyses and breakdowns to understand your own special mixture. 00:00:00.000 --> 00:00:00.000 Out as the toxicology comes down the pike. So effectively, communicating all of that out to internal and external audiences and partners and stakeholders is a really big part of our project and we try to make sure that what we're saying is understandable. 00:00:00.000 --> 00:00:00.000 At the end of the day. So building all of that out and understanding and probably taking more time than expected. 00:00:00.000 --> 00:00:00.000 I wanted to share quickly that a fate and transport model is really our goal, to be able to understand those mechanisms at play. 00:00:00.000 --> 00:00:00.000 So while we're taking all of those stats analysis and all the analytical over multiple years and a very robust monitoring network. 00:00:00.000 --> 00:00:00.000 We definitely want to make sure that we're able to use what tools we have for modeling all of that. 00:00:00.000 --> 00:00:00.000 So identifying not just our sources from secondary sources or commingling, but also understanding new hydrologic connections that we maybe didn't understand as well prior to the study and then any of those other migration pathways that have been exacerbated through the spread of peak fast and man-made conveyance systems like the project 1,007 quarter. 00:00:00.000 --> 00:00:00.000 And that's that storm water system. Where the pipe travels water, it also travels P fast. 00:00:00.000 --> 00:00:00.000 So understanding this in a numeric model standpoint. I wanna be able to share with you just some generalized findings. 00:00:00.000 --> 00:00:00.000 This, this is taking an, slightly earlier version of the model. We've advanced this since now. 00:00:00.000 --> 00:00:00.000 Or since then, this time, this is just showing you groundwater component of it. It is a surface water and ground water and groundwater integrated model. 00:00:00.000 --> 00:00:00.000 It is also going to integrate state and transport parameters so that it becomes transient. And we're building this out so that we can understand once it's in our deeper aquifers beyond the surface water units, not just the mass that's being spread, but also, where we might expect those, preferential pathways to be infected. 00:00:00.000 --> 00:00:00.000 From natural conveyance systems as well as large pumping centers in particular. That's what you're seeing represented here. 00:00:00.000 --> 00:00:00.000 This aerial photo is overlaid with our model boundary, that yellow line that thin yellow line going all the way from the Mississippi to the St. 00:00:00.000 --> 00:00:00.000 Louis River and then also these yellow boxes being major pumping centers for municipal supplies. And so understanding where we could expect this mixture of ours, which is one of the most transformed P fast mixtures. 00:00:00.000 --> 00:00:00.000 This is just modeling initially as groundwater molecules not as the PEFOS, but we have grown this since the time of this. 00:00:00.000 --> 00:00:00.000 Initial presentation. But understanding that over 30 years you could have this much spread and you could have. 00:00:00.000 --> 00:00:00.000 Directionally challenged. P fast, tortuous pathways is what comes to mind really. 00:00:00.000 --> 00:00:00.000 And so understanding where and how far this peak path might travel over 30 years, 50 years, and then a hundred years travel time. 00:00:00.000 --> 00:00:00.000 We could expect just traveling as a water molecule, not even as our specific P fast mixture. 00:00:00.000 --> 00:00:00.000 We can expect to see that treatment means will be not only present now but you know very much into the long term for our current and future generations and so multiple different aquifers in our case, 6 different aquifers are impacted. 00:00:00.000 --> 00:00:00.000 And so to that end, there's one other main message I want to send home with you and that is the last 2 slides here talking about the conveyance from surface water to deeper groundwater units and looking at this from in this case a leap frog three-dimensional transect across our area and really getting an understanding of those secondary source mass areas being as complex as our primary sort of series in some 00:00:00.000 --> 00:00:00.000 cases because where you have not only surface water spread, but wetland complexes to sell out that which is organically, adhered and absorbed and then, leaching over time. 00:00:00.000 --> 00:00:00.000 We do have this understanding that man-made and natural infiltration is going to be a major component of our characterization and if you take nothing else home from what I say today, I really hope it is that you go back and take a look at your areas of man-made infiltration systems wherever you are investigating. 00:00:00.000 --> 00:00:00.000 And you ask where have there been new developments or redevelopment installed and where should those infiltrating areas, whether natural or man-made, be exacerbating the spread because that's exactly what we see where we had areas with 3 small naturally occurring ponds, but beautiful homes developed around these areas, nice residential areas. 00:00:00.000 --> 00:00:00.000 Now those infiltration areas have been improved, enhanced, and are aiming at different goals to get water back into our aquifers. 00:00:00.000 --> 00:00:00.000 But where water is passing and P fast impacts exist, the P fast also travels. And so we now have larger, more exacerbated plumes because of these infiltration areas. 00:00:00.000 --> 00:00:00.000 And so from that standpoint, my characterization message to you today is just that you can't necessarily. 00:00:00.000 --> 00:00:00.000 Only look to our standard natural pathways, whether they're fractures, cast, surface water, creeks or lakes or ponds. 00:00:00.000 --> 00:00:00.000 You also need to be looking to man-made, influences on that and pumping influence, you know, of course as well. 00:00:00.000 --> 00:00:00.000 So with that, I will just, I always like to thank all the partners. Involved because it takes a great deal of effort, great deal of time, energy and expertise to bring all of this to bear and I'll take any questions you might have. 00:00:00.000 --> 00:00:00.000 Okay. 00:00:00.000 --> 00:00:00.000 Okay, so hopefully Rebecca, you can hear me. In the room, I And maybe. 00:00:00.000 --> 00:00:00.000 If not, I have online questions. So I'm gonna start with those. The first question, how are you integrating the groundwater modeling and surface water modeling together? 00:00:00.000 --> 00:00:00.000 They specifically ask what programs are you modeling these 2 mechanisms? 00:00:00.000 --> 00:00:00.000 Mike sheet. Yeah, we actually have the, developer of Mike she working, with, from DEI, I believe it is, working to develop the integrated model. 00:00:00.000 --> 00:00:00.000 So our modeling team from ecom has been to develop the integrated model. So our modeling team from ecom has been working directly with the Mike Shi developer to explicitly make sure that our model is representing that connection appropriately. 00:00:00.000 --> 00:00:00.000 Okay, I have another question. What factors are used to choose your fate and transport properties like partitioning? 00:00:00.000 --> 00:00:00.000 Given how specific. And therefore variable they can be. Do all modeled P fast have quote good values of these parameters? 00:00:00.000 --> 00:00:00.000 Request, which is why we've asked the manufacturer directly for that information. So we're explicitly getting not only published values for review or comparison, but also explicitly asking directly for under our regulatory authority for. 00:00:00.000 --> 00:00:00.000 Consent order work as well as the settlement for the manufacturers to provide for us. The fate and transport parameters, those physiochemical properties that will be most informative and accurate to our model. 00:00:00.000 --> 00:00:00.000 All right, another question. Do you know of any successful remediation projects? Since 2018. 00:00:00.000 --> 00:00:00.000 P fast remediation explicitly. You know, I think in the context of this type of project, nothing at this scale. 00:00:00.000 --> 00:00:00.000 Certainly, I know a great deal of effort, nothing at this scale, certainly. I know a great deal of effort. 00:00:00.000 --> 00:00:00.000 I know a great deal of efforts, going on in terms of pilot projects, nothing at this scale, certainly. 00:00:00.000 --> 00:00:00.000 I know a great deal of efforts, going on in terms of pilot projects, including a great deal of efforts, going on in terms of pilot projects, including our own. 00:00:00.000 --> 00:00:00.000 And that is aimed at initially surface water and groundwater, conveyance systems that are impacted right in this area. 00:00:00.000 --> 00:00:00.000 So we, have, purchased and deployed a phone fractionation unit and have been, I would say effectively using that bus far at our pilot study, for both surface water and groundwater, physical removal. 00:00:00.000 --> 00:00:00.000 And, then, as, a, secondary, step, in, that, treatment, train, approach, for, the, pilot, study, we performing as expected. 00:00:00.000 --> 00:00:00.000 Able to get even recently down to a non-detect for PEFola, in, 00:00:00.000 --> 00:00:00.000 All right, I don't see any other questions. So let's call. 00:00:00.000 --> 00:00:00.000 Hey, Rebecca, I think we'll just thank you one more time for the virtual presentation. 00:00:00.000 --> 00:00:00.000 And then I'll stop out the. 00:00:00.000 --> 00:00:00.000 Thank you. 00:00:27.000 --> 00:00:41.000 Variety of roles, since that time. Remedial project manager, brand coordinator, environmental engineer. 00:00:41.000 --> 00:00:50.000 Prior to that he worked with the Railroad Commission, Texas Railroad Commission is a geologist and he holds a BS, from Texas Tech. 00:00:50.000 --> 00:01:05.000 He's gonna talk with us about, the remedial investigation work that he and others have been doing at, the remedial investigation work that he and others have been doing at, Res Air Force Base outside. 00:01:05.000 --> 00:01:13.000 Hi everybody, Hopefully I'll be able to work this. It's past down. 00:01:13.000 --> 00:01:25.000 I think I'm here. 00:01:25.000 --> 00:01:38.000 I'm getting it. 00:01:38.000 --> 00:01:47.000 Okay. Alright, thank you. 00:01:47.000 --> 00:01:51.000 Okay. 00:01:51.000 --> 00:01:59.000 So we'll be talking about like a quick introduction and then overview. We'll be talking about, domestic well sampling that we did. 00:01:59.000 --> 00:02:16.000 At Reese and then the affected property assessment which is roughly an equivalent of a remedial investigation. However, we're working under a record regime under, at Reece under TCQ, Texas conditional environmental quality. 00:02:16.000 --> 00:02:22.000 Little bit about future actions and we'll have questions. 00:02:22.000 --> 00:02:29.000 So. Anyway, I work for the Air Force Several Engineer Center and that's headquarters in San Antonio. 00:02:29.000 --> 00:02:36.000 I'm in Lubbock. The division I work for is, the Brac division. 00:02:36.000 --> 00:02:42.000 And that's, handles all the bright places, and all 40 black bases across the United States. 00:02:42.000 --> 00:02:54.000 So. Cz, is the active side. So CIB is the So just a quick overview. 00:02:54.000 --> 00:03:03.000 And. 1970 roughly. Hey, Triple F started being used in the Air Force. 00:03:03.000 --> 00:03:09.000 It was pioneered at one of my bases. I managed at Shenude Air Force Base in Illinois. 00:03:09.000 --> 00:03:17.000 So at the fire training school there. So, in 1997, Res Air Force Base closed. 00:03:17.000 --> 00:03:27.000 And then in 2,016 we've conducted a preliminary assessment that identified 11 A triple F areas and one fire training area. 00:03:27.000 --> 00:03:37.000 And 2017, we also started a side inspection. That identified P fast and soil and groundwater at Reece. 00:03:37.000 --> 00:03:48.000 And then, 2017, as soon as we found out that we had a PFAS in the Ogala aquifer, which is a major drinking water source in the area. 00:03:48.000 --> 00:03:58.000 We started doing ongoing domestic or domestic well sampling and then we have been sampling and greeting since then. 00:03:58.000 --> 00:04:08.000 2019 through 2023. We conducted the effective property assessments under the record format. 00:04:08.000 --> 00:04:21.000 So start with drinking water mitigation. This is a big task that we had to do per policy and that started in about November of, 20. 00:04:21.000 --> 00:04:33.000 2829. First we conducted a drinking water well database search. And within 4 miles down gradient of the former base. 00:04:33.000 --> 00:04:40.000 And then we started sampling. Domestic wells and we started doing that November, 2017. 00:04:40.000 --> 00:04:47.000 We sampled 545 drinking water wells. Of which, today. 00:04:47.000 --> 00:04:59.000 266 private wells and 4 public wells exceeded 70 parts per trillion. In accordance with DOD policy and or TCQ PCLs. 00:04:59.000 --> 00:05:09.000 So we looked at both the 70 parts per trillion under the under the policy and anything that TCQ had issued protected concentration levels. 00:05:09.000 --> 00:05:21.000 Which are typically at 93 for something like PFHXS. And, there are 16 of those compounds that we had to look at as well. 00:05:21.000 --> 00:05:31.000 And then, immediately as since we got, sample results that indicated something was over those limits. 00:05:31.000 --> 00:05:48.000 We would provide bottled water to a resident. And then we'd start putting in point of entry treatment systems which treated all the water coming out of their well toward their house or whatever use they were using it for. 00:05:48.000 --> 00:05:52.000 So here's the figure of the impacted wells. Each one of those radius marks is a mile out from the former base. 00:05:52.000 --> 00:06:03.000 So you can see it's a pretty large area. They ended up being 266 wells, that are impacted. 00:06:03.000 --> 00:06:05.000 Those are all the red wells. And as you can see, we had groundwater that flowed in different directions from Reece. 00:06:05.000 --> 00:06:24.000 We also had different release areas at the former base. Which helped in that migration. In different directions. 00:06:24.000 --> 00:06:32.000 So when we started the effective property, 00:06:32.000 --> 00:06:46.000 The, regime was for us to, conduct the investigation. Reece was under a record permit. 00:06:46.000 --> 00:06:53.000 And we typically, the Air Force typically conducts their investigations under Cercla, but at least we were. 00:06:53.000 --> 00:07:02.000 Bound to this record permit we're conducting it under PCQ regulations. There, so. 00:07:02.000 --> 00:07:16.000 When we did this effective property assessment, that consisted of a conceptual site model. Media sampled included groundwater, soil, surface water, sediment, fish, mthick invertebrates, fat tissue, vegetable tissue. 00:07:16.000 --> 00:07:24.000 We conducted a human health risk assessment. And we did a tier 3 ended up doing a tier 3 human health risk assessment. 00:07:24.000 --> 00:07:32.000 Confission. And a screen level ecological risk assessment as well as a site specific ecological risk assessment. 00:07:32.000 --> 00:07:38.000 And part of the sampling we did for human health was a residential, vegetable gardens. 00:07:38.000 --> 00:07:49.000 Evaluation and we also did live seminar studies to evaluate solar groundwater migration. Hmm. 00:07:49.000 --> 00:07:58.000 Sorry conceptual site model, building that. We use. Environmental sequence stratigraphy. 00:07:58.000 --> 00:08:07.000 Our, contract was a ecom and, Ryan Samuels is here actually back here in the audience who helped with our CSM. 00:08:07.000 --> 00:08:13.000 He was our primary author of our CSM and he helped us. Devise our sampling scheme as we went along and conducting our investigation. 00:08:13.000 --> 00:08:39.000 So, anyway, the conceptual side model here's this is actually Reese. Has the faces and and the migration pathways but you know, a common CSM elements in the southwest include, groundwater where we've got limited precipitation. 00:08:39.000 --> 00:08:45.000 Lubbock area gets about 18 inches of rain per year on average. So, and then the water table is pretty deep. 00:08:45.000 --> 00:08:55.000 It's about a hundred 10 to a hundred 30 feet deep it's about a hundred 10 to a hundred 30 feet deep and then it's highly variable. 00:08:55.000 --> 00:09:01.000 Limited surface water. It's very flat there, flatest place on earth, I think. 00:09:01.000 --> 00:09:09.000 And it's got ply at what's called fly a light so those are just depressions that the ground the surface water flows to. 00:09:09.000 --> 00:09:22.000 And these, these don't really flow to streams in this immediate area. They, infiltrate in through those Water infiltrates through those buyer likes. 00:09:22.000 --> 00:09:29.000 So the pathways to ground water are often indirect and they're far removed from the source areas in some cases. 00:09:29.000 --> 00:09:42.000 And then there's preferential groundwater flows through course channel deposits. As the water migrates down to the groundwater. 00:09:42.000 --> 00:09:52.000 So, the groundwork, of our investigation. Our, and outcrops, study. 00:09:52.000 --> 00:10:02.000 Luckily we had a local quarry that was about a hundred Yeah, right to the ground the base of the Ogalala as a matter of fact. 00:10:02.000 --> 00:10:13.000 So we had a really good cross-section of Ogalala formation. To help us in our, understanding of the local Giology there. 00:10:13.000 --> 00:10:22.000 They did a preliminary CSM using environmental sequence. And then pre-investigation modeling. 00:10:22.000 --> 00:10:31.000 And all of this was built on previous investigations and cleanup we had done there at Reese over the last 25 years. 00:10:31.000 --> 00:10:41.000 Or TCE, we've gone through this entire cycle of investigating, installing remedies and remediating TCD. 00:10:41.000 --> 00:10:55.000 As a matter of fact, the TCE Plume was closed right about the time we started sampling and found out that we had P fast in the groundwater at the time. 00:10:55.000 --> 00:11:15.000 So another thing that, AECON did was pre-grilling projections with understanding what the geology was from the previous monitor wells that were installed and projecting what was already gonna be in the stratigraphy when we drill the new wells. 00:11:15.000 --> 00:11:30.000 So the groundwater monitoring network at Reese. Includes at a hundred 30 locations 299 nested monitoring wells and those are completed in the upper middle and lower portions of the Ogallala aquifers. 00:11:30.000 --> 00:11:43.000 We did Sonic drilling, with continuous cores, which helped considerably over the previous methods that we have been using in the forth. 00:11:43.000 --> 00:11:48.000 Okay, another important thing, I think you heard the same all day long pretty much. High resolution. 00:11:48.000 --> 00:12:02.000 Fill techniques, logging techniques. Our geologists were specifically trained by Ryan and other geologists in logging with this high resolution login techniques. 00:12:02.000 --> 00:12:17.000 And, it helped a lot in our understanding of The specific of the of the Ogalala here so Here's a couple of examples. 00:12:17.000 --> 00:12:30.000 This pre mobilization lithology data that we have here on the left is from monitor wells that were drill in the ninetys and they were logged as good as could be logged with the rotary drilling. 00:12:30.000 --> 00:12:53.000 And as you can see from the boxes here, there's a there's lithology that looks the same pretty much you know for the bottom part of the well that the new wells that were drilled with the well that the new wells that were drilled with the fine high resolution logging you can actually see lots of difference in the logging of those wells and those are really close by. 00:12:53.000 --> 00:13:08.000 From these other wells. Yeah. We can see the finding up sequence here on our. Sequence, that So what does that result in? 00:13:08.000 --> 00:13:28.000 Better interpretation of this particular key in the area, better understanding of the flow paths as well as the, the grain size and, you know, we even saw floodplain deposits that we hadn't seen before in some of these areas. 00:13:28.000 --> 00:13:42.000 So the So the oranges and yellows or the gravels and sands and the greens and the and the dark charcoal are very fine or grain sediments. 00:13:42.000 --> 00:13:56.000 So another thing that was important, as in this area, there are several. There are several floodplain deposits that acted as aqua fluids that prevented downward migration of contamination. 00:13:56.000 --> 00:14:19.000 So when we were installing the wells, we know, Ecom was doing this. They would ensure that the screen intervals that they installed We're not penetrating both the upper and lower portions of the course of grain materials that are sandwiched by this these floodplain deposits. 00:14:19.000 --> 00:14:30.000 So that prevented, you know, inaccurate. And understanding of the migration of the contaminants. 00:14:30.000 --> 00:14:48.000 So that was helpful. It also maintains the integrity of the clock. Refining. Confining layers and helps us to gather discrete groundwater elevation contain the concentration data. 00:14:48.000 --> 00:14:56.000 So another thing they did was, look at. Wells that had been drilled in the area. 00:14:56.000 --> 00:15:06.000 And, in combination of wells that we drill to get a good understanding of the top of the confining unit. 00:15:06.000 --> 00:15:13.000 So this is, this is one thing they do. They used, evaluated 3 over 3,000 points. 00:15:13.000 --> 00:15:23.000 And used. Over 2,000 points to get that understanding of that confining unit. 00:15:23.000 --> 00:15:34.000 So in the geologic, geologic, using environmental sequence stratigraphy. Here's a depiction of at the top. 00:15:34.000 --> 00:15:41.000 You can see as, we're looking at the groundwater flowing into this cross-section. 00:15:41.000 --> 00:15:53.000 Preferential flow through course screen, gravel grain channel deposits. And then fine grain flood plane deposits acting as barriers to groundwater flow. 00:15:53.000 --> 00:16:08.000 And also, on the right, preferential flow through course grain channel deposits. Understanding this environmental sequence is, important that you understand the depositional environment. 00:16:08.000 --> 00:16:28.000 So this is in the eastern, eastern side of the Rocky Mountains. It has the Rocky Mountains, the wedge there the Ogalala is part of that and understanding that deposition environment is important in understanding what's going on, CSM conceptual site model wise here. 00:16:28.000 --> 00:16:36.000 So we, we did that in general. We did also the top of bedrock, formation. 00:16:36.000 --> 00:16:46.000 Which is part of that understanding. And a can also develop faces maps for every 10 feet of the saturated interval. 00:16:46.000 --> 00:16:58.000 Which helped considerably in a more of a three-dimensional understanding. Of the, preferential flow pathways. 00:16:58.000 --> 00:17:11.000 So the highlights of the investigation. Lots of data collected over this area. The plumes were over 3 miles long, so, going 2 different directions. 00:17:11.000 --> 00:17:18.000 Our 1,300, soil samples, 749 groundwater samples. 00:17:18.000 --> 00:17:26.000 Surface water sediment fish That should be vegetables and produce. 77 samples. 00:17:26.000 --> 00:17:33.000 And then when we did the tier 2 and tier 3, sampling. Regime, we ended up plants, sampling fish. 00:17:33.000 --> 00:17:52.000 And vegetables and produce and benefit. Macro invertebrates so lots of sampling going on during this 3 year process of collecting this information and riding this, effective property assessment report. 00:17:52.000 --> 00:18:13.000 So some of the things we've done, you're kind of. Kind of see a 3 and through the day on some of this stuff, but the state of the science and it's helped us to understand the environment much better than it than 20 years ago when we we're doing the TCE investigations. 00:18:13.000 --> 00:18:21.000 So they did downhill geophysics, Sonic drilling, sled tests. Time series water level evaluations. 00:18:21.000 --> 00:18:35.000 We did biological field surveys lysimeter sampling and a conceptual shot model iterative updates every mobilization that we did. 00:18:35.000 --> 00:18:48.000 So the migration pathways based on the conceptual site model. This picnic like is a one of the pla lakes that was a major, source area. 00:18:48.000 --> 00:18:58.000 Of P fast migration into the groundwater because all of the surface drainage from the main part of the base drained into this picnic lake one way or another. 00:18:58.000 --> 00:19:06.000 There was an industrial grain line that went right down the flight line. And also are all the surface water drainage drained into that picnic lake. 00:19:06.000 --> 00:19:13.000 And, Anyway, there's several things to note here. Confining unit is the white below. 00:19:13.000 --> 00:19:21.000 That's the Cretaceous Duck Creek Shale. And limestone, alternating shell and limestone. 00:19:21.000 --> 00:19:29.000 So the color coding here is from, you know, dark to. The yellows, oranges, and purples. 00:19:29.000 --> 00:19:36.000 Are the more transmissive zones. So, You, you can only see this in cross-section, but imagine this is a meandering stream and things go in and out of the paper that out of the page here. 00:19:36.000 --> 00:19:50.000 So you can see the point bars. And the other, the other geological sequence, found the scriptigraphy here. 00:19:50.000 --> 00:20:06.000 So, we're gonna look. Next at a. A animation that shows the migration from picnic like down 00:20:06.000 --> 00:20:20.000 So this is P fast migrating to death via vertically connected channels. And the migration steeper than the observed downgrown down groundwater gradient. 00:20:20.000 --> 00:20:27.000 And then the consistent, water elevations were measured throughout the aquifer as you can see in the little, blue. 00:20:27.000 --> 00:20:38.000 Marks there. And there was very little vertical gradient observed here. 00:20:38.000 --> 00:20:49.000 So if I can make this simulation work. We'll see. This is the this is the model with this DVS I believe simulation that shows. 00:20:49.000 --> 00:20:59.000 The migration over 50 years since the BFAS was started being used at Reeze. 00:20:59.000 --> 00:21:08.000 So imagine some of this migration going in and out of the page as well. But these, eventually it gets into these, purple zones. 00:21:08.000 --> 00:21:24.000 With the most transmissive, which are the most transmissive zones. And, down gradient of all this, there are pumping centers with irrigation, large center pivot irrigation wells, approximately, 1,200 gallons a minute. 00:21:24.000 --> 00:21:35.000 Each and there are multiple ones of those down gradient of this. 00:21:35.000 --> 00:21:43.000 So I think we get the gist on that. That's about 50 years of migration. 00:21:43.000 --> 00:21:58.000 So here's a here's a map view of all of this pretty much the same area. And I'll push the animation on this as well. 00:21:58.000 --> 00:22:05.000 So this is calibrated to match our model. I mean, our model is calibrated to match what we're seeing in reality. 00:22:05.000 --> 00:22:13.000 Here. So it's, pretty similar to what we've seen. What we actually see out in the field. 00:22:13.000 --> 00:22:20.000 Some areas that I don't show, formerly had a pumping tree system that re-injected water. 00:22:20.000 --> 00:22:28.000 Into the aquifer and you can actually see that injection activity when we're treating TCE. 00:22:28.000 --> 00:22:41.000 We didn't focus on P fast and understand the fact that our carbon Creatment. Associated with our TCE may not have been sufficient. 00:22:41.000 --> 00:22:49.000 And treating the PFAS. So we could see where the re-injection areas where the PFAS was. 00:22:49.000 --> 00:22:58.000 Helped that system help spread the PFAS further than it would have gone otherwise. 00:22:58.000 --> 00:23:06.000 So conclusions. You know, building your program. It takes a lot of plant programming and planning. 00:23:06.000 --> 00:23:14.000 We went into a lot of effort and consulted with our consultants, a, and other folks. 00:23:14.000 --> 00:23:23.000 To understand kind of what needs to go into this, high definition. Understanding of the conceptual site model. 00:23:23.000 --> 00:23:40.000 And the environmental sequence trajectory that we we needed to put together to better understand. What was going on in the environment here of course we didn't do that only 5 years ago and not, anywhere near to that extent. 00:23:40.000 --> 00:23:51.000 So we did modeling. And, you know, throughout the process. Some initial modeling, lithological and groundwater using existing data. 00:23:51.000 --> 00:24:00.000 And then, the Hydro geological CSM using ESS to drive the investigation path forward at each mobilization. 00:24:00.000 --> 00:24:08.000 So we have like 5 mobilizations at each mobilization. We took the understanding of what was drill, what our wells. 00:24:08.000 --> 00:24:26.000 We're showing us geologically and data-wise P fast-wise to help us step out and to, drill the new set of wells and then we would build the CSM again to understand where we needed to go next. 00:24:26.000 --> 00:24:32.000 So we ended up with 5 iterations. That Reece doing this doing this work. 00:24:32.000 --> 00:24:42.000 It was a comprehensive reproach for the effective property assessment. Of course, you've got all, all your pieces that you've got to do for a remedial investigation. 00:24:42.000 --> 00:24:50.000 But we, did some predictive modeling up front. Did the high resolution logging and Sonic drilling. 00:24:50.000 --> 00:24:56.000 We did that downhill geophysics. Select test, lysimeters. 00:24:56.000 --> 00:25:05.000 We had some pretty good success with some of the lastimeters, but as you explained a while ago, you know, it's not, it's kind of hit or miss sometimes. 00:25:05.000 --> 00:25:15.000 Especially out in the West where you've got pretty arid conditions. And you're not, you're not gonna see some of the grass or water that you would up elsewhere. 00:25:15.000 --> 00:25:22.000 But we did get a couple of sites that we were able to do the lysimeter zone and get the tier 3 data to help us. 00:25:22.000 --> 00:25:37.000 In that investigation. We also did the ecological and human health risk assessments. And then, you know, one of the keys is that the modeling and conceptual site model are going to help us. 00:25:37.000 --> 00:25:47.000 Drive our remediation design. And the operations of that. That pump and treat or whatever we end up putting in. 00:25:47.000 --> 00:25:53.000 For our remediation over time. So that's an important thing. You can kind of. 00:25:53.000 --> 00:26:02.000 Think about the end. The overall process when you start developing these programs. 00:26:02.000 --> 00:26:09.000 And that's it for my presentation. 00:26:09.000 --> 00:26:12.000 Hmm. 00:26:12.000 --> 00:26:23.000 Again. In the room if you have any questions, see a hand up. 00:26:23.000 --> 00:26:32.000 So, I was just wondering if. Thought it all about sort of long-term storage and the sediments. 00:26:32.000 --> 00:26:42.000 And, you know, even if you were to pump this groundwater for an extended period of time, presumably there's PFAS that I've integrated themselves really deep in the sediment structures. 00:26:42.000 --> 00:26:50.000 And, how that's gonna sort of play out long term with reviation strategies. 00:26:50.000 --> 00:27:05.000 Okay. So I'm wondering about, about storage in the sentiments. And how the fast structures can integrate themselves from the sediment and beef in the grains. 00:27:05.000 --> 00:27:10.000 And even if you were to compat that water for a long period of time, they're slow leashing out of these sediments. 00:27:10.000 --> 00:27:18.000 And how that impacts Hi, fine. 00:27:18.000 --> 00:27:30.000 Hey, Yeah. Okay. With lowering DMC, how that might affect all term. 00:27:30.000 --> 00:27:39.000 We get. Those are the things that we're definitely thinking about. We'll think about in future because this phone team. 00:27:39.000 --> 00:27:53.000 Oh, the best. That's available technology. That might take your model of the mask, but we get to a point of the finished turn of that. 00:27:53.000 --> 00:28:04.000 So we're gonna be, to that to forward. Right. 00:28:04.000 --> 00:28:11.000 I have a question online. Which key fast species were shown in your animations? 00:28:11.000 --> 00:28:24.000 Which PEVAS species were shown in the animations? We saw, Yeah, I check suddenly. 00:28:24.000 --> 00:28:36.000 We're about 6. B fast saw. Yeah. Do you have any Right. 00:28:36.000 --> 00:28:52.000 Stations compared to You see if you. You know, there, CC, 2, are, or we'd possibly be both about 2. 00:28:52.000 --> 00:29:05.000 I'm like, So. And 00:29:05.000 --> 00:29:12.000 And then another online question. Where the POE systems comprised of GAC. 00:29:12.000 --> 00:29:19.000 We started. Yeah. Systems. Okay. 00:29:19.000 --> 00:29:31.000 It's all sacrificial gap, it's treating organics. And then, we found that. 00:29:31.000 --> 00:29:43.000 Getting time for all. Is that material? And it wasn't really buying anything. But we could use gas. 00:29:43.000 --> 00:29:53.000 Thanks, exclusively with that and if we're. Well, that. Both systems. 00:29:53.000 --> 00:30:01.000 Alright, thank you. Any questions in the room? 00:30:01.000 --> 00:30:19.000 Oh, I see where Mark got. One more question. I was wondering if, in your word that all evaluated, So the atmospheric transport of phone from fire training activities to nearby locations because it seems like that. 00:30:19.000 --> 00:30:39.000 Potentially a route that contaminates a larger area around what you might expect. And so I'm just curious if that's come up at all in your at Shinu, my base in Illinois, the wind blows there too, so. 00:30:39.000 --> 00:30:52.000 We, definitely have been looking into the nature and extent. We just started the, in the remedial investigation at my base at, in Illinois. 00:30:52.000 --> 00:31:03.000 So part of that will factor into that was that was the Air Force's firefighting school. And that's definitely gonna come and play there. 00:31:03.000 --> 00:31:18.000 We have not looked at atmospheric going out as far as, you know, several miles or anything like that, but we are going to look at least on the base to kind of see the extent of how that's affected. 00:31:18.000 --> 00:31:26.000 Yes.