Dakota Aquifer Program--Subsurface Hydrology
Optical-fiber temperature logging
Figure 3
Figure 3. Difference of interval gradients resulting
from comparison of two sets of unsmoothed logging data obtained in
Smokyhill borehole: A, gradient interval 1 m; B, gradient interval
2 m; C, gradient interval 5 m; D, gradient interval 10 m.
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Start of Hydrology Section
Kansas Geological Survey, Dakota Aquifer Program
Updated Sept. 30, 1996
Scientific comments to P. Allen Macfarlane
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URL=http://www.kgs.ku.edu/Dakota/vol1/hydro/DTSfig3.htm