MDEQ FORM #4 – SUSCEPTIBILITY ASSESSMENT Please use one form for each ground
water source (well or spring) Well Construction InformationDate well constructed:
__________________________________________________________ Drilled: rotary
Dug: hand If no well log is available, other records may be
substituted as documentation construction.
Other construction Average Pumping Rate:________________ (gpm)
Explain how this rate was determined:______ |
Wellhead InformationDepth to top of well screen (circle one) <20 ft
20 – 50 ft
50 – 100 ft
100 – 200 ft
>100 ft Coarse setting includes: predominant sand and gravel materials in unsaturated zone above aquifer. Depth to groundwater (circle one) <20 ft 20 – 50 ft 50 – 100 ft 100 – 200 ft >100 ft Well head elevation
_____________________________(height above mean sea level) (check one) ________ no evidence of confining layer ________ evidence of confining layer and < 20 ft piezometric head ________ evidence of confining layer and > 20 ft piezometric head ________ no well log available Thickness of each confining layer:
______________________________________________ in well house
well head
__________________________ ________ <18
ft, no waiver obtained |
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Regional Water Quality Information (check
appropriate lines): Source Specific Water Quality Records (check
appropriate lines): If any
contaminants have been detected in you system please provide
details__________________ Weighted Hydraulic Conductivity Calculation
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Z(total)_____________________________
Total Zi/Ki _______________
Kw = Z(total) ¸
=
Total Zi/Ki _______________________
1.
From Bouwer, H., 1978, Groundwater Hydrology. McGraw-Hill Book
Company, 480 p.
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FIGURE 1 – TRANSVERSE POTENTIAL1 (Hydrogeologic Characteristics Related to Water Movement to the Aquifer) Depth (feet) to the Aquifer
1. A Transverse Potential of 1 = low potential for water movement, 10 = high 2.
Kw =
Z (total) ¸ where Z(total) = total thickness of n layers, Z1, Z2….Zn represent individual thickness of layers 1 through n. K1, K2….Kn represent permeabilities of layers 1 through n. Permeabilities should be in units compatible with thickness, i. e., ft/sec if thickness in feet. Final value should be converted to gallons/day/ft2 for use in matrix. For example, if thickness is in feet, permeabilities in feet/second, multiply the result from the formula above by 646,340 to convert to gal/day/ft2.
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FIGURE
2 – INFILTRATION POTENTIAL1 (Relating Water Availability to Transverse Potential) Hydraulic Surplus2 (inches)
1.
An infiltration potential of 10 indicates a high probability that
the combined availability of water (hydraulic surplus) and geologic
conditions (transverse potential) will lead to water from the surface
reaching the aquifer. A score
of 1 indicates a low probability.
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FIGURE 3 – MOBILITY POTENTIAL2 ORGANIC
CHEMICAL_______________________________________________________ Organic Matter Score2
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