Dakota Aquifer Program--Subsurface Hydrology
Optical-fiber temperature logging
Figure 4
Figure 4. Gradient difference obtained at 1 m
intervals in Smokyhlll borehole in comparison to gradient differences
smoothed by different running averages: A, unsmoothed; B, smoothed
by 2 m running average; C, smoothed by 5 m running average; D,
smoothed by 10 m running average.
Use the "Back" command of your browser to return to the page you were viewing.
Dakota Home ||
Start of Hydrology Section
Kansas Geological Survey, Dakota Aquifer Program
Updated Sept. 30, 1996
Scientific comments to P. Allen Macfarlane
Web comments to webadmin@kgs.ku.edu
URL=http://www.kgs.ku.edu/Dakota/vol1/hydro/DTSfig4.htm