Webster County Groundwater Impact Committee

Photo Gallery on Ethanol Plant Site


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Map source: www.dnr.mo.gov/env/wpp/ watersheds/info/ws-11010002.htm
 
Map source: cares.missouri.edu
 
Map source: cares.missouri.edu
Proposed ethanol plant site is in James River Basin Watershed, east of Rogersville, MO.

 
  The proposed ethanol plant site is a 252-acre property northeast of the junction of U.S. Highway 60 and Porter Crossing Road. The approximate location is the NEĽ of Section 15, Township 28N, Range 19W in Webster County, MO.   The proposed site straddles the school district and fire protection district boundaries of Rogersville and Fordland, MO.
         

Map source: cares.missouri.edu
 
Map source: dnr.missouri.gov/env/
wrc/docs/WR59.pdf
 
Map source: ims.missouri.edu/berm
 
Soils at the proposed site are wet-natured due to a restrictive layer approximately two feet below the surface.   Annual precipitation map of Missouri   Wind rose data recorded at the nearby Springfield, MO, Regional Airport shows the predominant wind direction for April through September will be from the south-southeast toward the north-northwest.
         

Diagram source: extension.missouri.edu/
explore/ envqual/eq0401.htm
 
Map source:
www.dnr.mo.gov/env/wrc/
springsandcaves.htm#Losing
 
Map source:www.dnr.mo.gov/env/wrc/
springsandcaves.htm#Sinkholes
Limestone deposits may provide high pollution potential in the Ozarks.   “Losing streams” leak water underground in unpredictable directions with little or no filtering.   Sinkholes are direct conduits for surface water to travel underground
         

Source: Missouri Department of Natural Resources 
 
Photo credit: Bob Schultheis
 
Map source: cares.missouri.edu
Karst (soluble limestone) topography of the Ozarks is among the most fragile and susceptible to pollution in the U.S.
 
  Surface water can move unfiltered and rapidly underground through solution channels and sinkholes on the Ozarks landscape.
 
  The proposed wells, capable of pumping 2,000 gallons per minute, would likely have a 2-mile radius of impact on groundwater levels in neighboring wells.
 
         

Map source: Missouri Department of Natural Resources-Southwest Regional Office 
   
Data source: www.oseda.missouri.edu/cgi-bin/countypage?29225
The Ozark aquifer consists of several water-bearing rock formations with no confining layers to separate them. The Davis Formation is below the Potosi Formation, and separates the low-yield Derby-Doerun dolomites from the Ozark aquifer.

 

 

Pumping a high-capacity deep well, over time, can draw water away from shallower wells, requiring these wells to  be deepened, need pumps lowered, or need new deeper more costly wells drilled.

 

  The expected population growth in Webster County through 2010

 

         

Last revised: 2006-11-17