Last week I posted an update on the Mississippi v. Memphis groundwater case. I learned from reporter Tom Charlier that folks from the University of Memphis had presented an alternative view on the flow system at a conference last year. A journal article is in preparation.
Brian Waldron of the University of Memphis was kind enough to send me a PDF of the Power Point he and Daniel Larsen presented at a conference in 2011. He gave me permission to post it (may take a while to download):
Download MS v Memphis Waldron_Larsen
They postulate that under proposed predevelopment conditions (shown below), the amount of groundwater that flowed from Mississippi into Shelby County, Tennessee (Memphis metropolitan area), was 141,725 cubic meters per day (about 37.4 MGD).
Under 2007 conditions, shown below, the amount flowing from Mississippi into Shelby County, Tennessee, was approximately 101,225 cubic meters per day (about 26.7 MGD).
So it looks like development has cost Tennessee groundwater, not Mississippi - about 40, 470 cubic meters per day (10.7 MGD). If this seems odd, remember - there is groundwater pumpage on the Mississippi side of the border.
So who's stealing from whom?
I am not in a position to evaluate their assumptions; I do they know they assumed a constant aquifer thickness (255 m or about 835 feet) and an average transmissivity of 2850 square meters per day (about 30,700 square feet per day). Use of an 'average' transmissivity suggests that spatially variable transmissivities were employed but I am unsure of that. It could simply mean that number is an average of all the values in the aquifer, and that single value was used in the flow calculations.
Curious to see what the blowback will be.
I will be anxious to see the journal article.
I think the fat lady has not yet sung - see today's quote.
"We are still evaluating our options with this." - Jan Schaefer, Mississippi Attorney General's office (email to Tom Charlier, April 2011)


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