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-- v m s .. ...rf./l&;-,<.y"'*Ni-l'! ,s -j;,..., Site^l
Bedrock -
- Permian Dimkard Group - Shales, sandstones, siltstones, minor limestones
Alluvium
- Pleistocene "-, , 1 glacial outwash d&posits
f i- coaree sands and gravels
S- "^i&,: ?: predominant valley fill sediments
^'l^i^^^r,terrace levels in the river valley
i@|^^y:trl^ tfae center of the river valley (more fmes) during sub ^^^^""'^liiiygggradadonevents
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Modeled Stage of Ohio River "
- Previous model above normal pool elevation - 5N1^.';a|
- Revised to normal pool elevation (582 ft. above MSlJ^^^gi^
Recharge Rates
-- Previous model - 11 in./yr. across domain - Revised zonation based on surficial sediment distribution
Les were estimated and adjusted during calib
tirJIyor daily pumping rates from the DuPont, Lit
data available)
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Boundary Conditions
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- Previous model - north edge of domain ende^l
- Revised: Domain extended to cover entire Ohio River basin betwe^n'l-l
* No-flow boundaries coincide with bedrock divides
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Ohio Riverbed Conductance
Previous model - conductance based on very low K of riverbed '
-, .';;. 1-'
Revised:
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^^.i I^^^CoK^uctance based on riverbed K -10% of expected Kv of underly
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Primary Data Sources fei|
RFI Report, DuPont, 1999
-- lithologic data -- groimdwater elevation data -- aquifer testing data
Simard, 1989, Geologic History of the Lower Terraces Upper Ohio River Valley, West Virginia Geological Survey Open^
-- Lithology, thickness, and depositional history of the Ohio River alluvial. -- Historical low water levels of the Ohio River
and Mathes, 2001, Aquifer-Characteristics Data for W -Resources Investigations Report 01-4036
r^ixdtauKc conductivity data
ie'rates
Investigation Reports
laaag and Lubeck
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