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Water Resources

Well T28S, R1E, Sec. 32, SW SW SE, Action: Constructed

Location Info
Owner: Farney, Jerry Status: Constructed
Location: T28S, R1E, Sec. 32, SW SW SE County: Sedgwick
Directions: 620 E Grand, Haysville
Latitude: 37.5653139 Longitude: -97.3415972 Datum NAD 27
Latitude: 37.565331 Longitude: -97.3419202 Datum NAD 83
Longitude and latitude calculated by Survey from township-range-section-quarter calls. Only good to within the quarter call accuracy.
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General Info
Well Depth: 20 ft. Elevation: ft.
Static Water Level: 13.5 ft. Est. Yield: gpm.
Comp. Date: 12-Dec-1989 Well Use: Monitoring well/observation/piezometer
DWR Applic. #: Other ID:
Driller Info
Driller: HWS Consulting Group Inc. License #: 471
Scanned Form
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Chemical Sample Submitted?: No
Water Well disinfected?:
Ground water encountered: 13 ft. , 0 ft. , 0 ft.
Pump test data: Well water was 0 ft after 0 hours pumping 0 gpm
Casing Info
Casing Type: PVC
Casing Joints:
Diam: 2 in. to 20 ft
Diam: 0 in. to 0 ft
Diam: 0 in. to 0 ft
Casing height above land surface: in
Casing Weight: lbs/ft
Wall thickness or gauge no.:
Screen and Perforation Info
Screen Type: PVC Screen Openings: Mill slot
Screen-perforated intervals From: 10 ft to 20 ft
From: 0 ft to 0 ft
From: 0 ft to 0 ft
Gravel pack intervals From: ft to ft
Grout Info
Grout used: From: 0 to 6 ft
From: 0 to 0 ft
From: 0 to 0 ft
Source of Possible Contamination
Source: OTHER
Direction from well: Distance: 0 ft
Lithologic Log
(Log data entered by KGS.)
From: 0 ft. to 5 ft. silty clay, dark brown, mottled, medium plasticity, 5-10% gravel
From: 5 ft. to 7 ft. sandy clay, 30-40% fine sand, 5-10% gravel, light brown, low plasticity
From: 7 ft. to 11 ft. very fine sand, gray staining, clay seams, well sorted, non plasticity
From: 11 ft. to 13 ft. very fine sand, gray staining, clay seams, well sorted, non plasticity, moist
From: 13 ft. to 16 ft. sand, slightly more coarse, 5% gravel, saturated, poorly sorted, stained
From: 16 ft. to 20 ft. sand, slightly more coarse, 5% gravel, saturated, poorly sorted, staining less prominent

Kansas Geological Survey
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