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Allen Sorenson: <br />Well, the ability to watch those and catch those sources and if you can do it systematically <br />through tank inventories and things like that, that'll work. <br />Harry Posey: <br />I'm not sure that you guys have looked at the most recent submittals from American Soda. <br />They produced a monitoring plan, I believe in April. If you haven't looked at that, I think <br />you ought to take a look at it because I think it really does represent a collective effort to <br />come up with a primary list. <br />Jerry Daub: <br />Is this what you're talking about? Mine's dated April 22. I've seen an April 4 on the draft <br />version. I've seen so many versions of this thing that I'm not sure what they're doing, to be <br />quite honest. <br />Paul Daggett: <br />This one's dated May 10. This is the final one. There's a lot of changes. The April 22 one <br />says final, but there were some changes. <br />Jerry Daub: <br />Would you be able to get us a copy of that, Paul? <br />Paul Daggett: <br />It's going to be in the final EIS. <br />Jerry Daub: <br />That may not be out for a couple of years!!! <br />Paul Daggett: <br />We'll get you one before that. <br />Harry Posey: <br />One of the things it points out is that there's rough water down there. There is a fair bit of <br />information in there. If you think that a person has to drink that water and eliminate any <br />fears. Possibly some of that water goes right to your drinking water well. I know you're not <br />situated like that, but if you think like that, then you start looking at the water parameters. <br />You imagine a situation where dissolution zone water makes it's way up into the aquifer, by <br />whatever mechanism, then analyzing most of these parameters down at the low parts of the <br />building ranges starts to make sense. <br />Jerry Daub: <br />We know that the water does come from the dissolution surface up to and throughout the <br />Mahogany Zone. Alkali Flats is a perfect example of that. It comes up through major joints, <br />fractures and faults and it's happening today under natural conditions. That's one of the <br />reasons why the TDS in Piceance Creek is so high at the mouth of the Piceance and at the <br />White River. That, and the fact that there's a lot of tail water from the irrigation that's <br />coming back into the stream. Most of the water that I know of that is consumptive out in the <br />27 <br />