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Introduction

Geography

Geology

Ground Water

Water Bearing Formations

Well Records

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Table 6

Table 6--Physical properties of samples of the Ogallala formation from the measured section in sec. 30, T. 5 S., R. 32 W., Rawlins County. By Ada Swineford and Carrie B. Thurber.

No. of bed in measured section Mechanical analysis (percent by weight) Coefficient of permeability* Percent soluble in dilute HCl
Coarse gravel (larger than 4.0 mm) Medium gravel (4.0-2.0 mm) Fine gravel (2.0-1.0 mm) Coarse sand (1.0-0.5 mm) Medium sand (0.5-0.25 mm) Fine sand (0.5-0.25 mm) Very fine sand (0.125-0.062) Silt and clay (less than 0.062 mm)
9 2.0 5.6 9.2 11.7 17.2 16.4 16.0 21.9 107 9.3
7   0.1 0.5 3.6 25.1 36.9 18.2 15.6 154 9.4
5 0.2 2.0 4.3 11.1 24.1 31.8 18.4 8.0 172 4.2
4 0.6 4.5 9.5 16.1 28.1 27.0 10.8 3.3   38.1
3 5.4 4.3 12.1 27.2 33.1 15.2 2.2 0.4 609 1.9
2   tr. 1.6 11.4 30.5 36.5 11.4 8.4   23.4
1     0.1 5.5 20.3 26.8 19.2 28.1 107 3.0
* Gallons of water a day, at 60 deg. F., that is conducted laterally through each mile of water-bearing bed under investigation (measured at right angles to the direction of the flow), for each foot of thickness of the bed and for each foot per mile of of hydraulic gradient.

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  Kansas Geological Survey, Thomas County Geohydrology
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Web version Nov. 2001. Original publication date Dec. 1945.
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