Masters Theses
Abstract
“Discrete recharge of a karst aquifer occurs from a losing portion of the Dry Fork River, Phelps County, Missouri, as shown by refraction seismology, self-potential surveys, and dye tracing results. The discrete losing zone is best defined by a streaming potential anomaly of -15 millivolts. Water moves from the river, through coarse alluvial deposits, into fracture-controlled solution features in the underlying bedrock, as determined from the shape of the SP anomaly.
The average hydraulic conductivity of the riverbed deposits is 0.10 m/s as determined by dye tracing. In the vicinity of the losing zone, a vertical flow path into bedrock solutional features is preferred over the downstream path to lower portions of the stream channel. In the recharge area, bedrock underlies the unconsolidated alluvium at depths of 9 to 12 meters”--Abstract, page ii.
Advisor(s)
Gerald B. Rupert, 1930-2016
Committee Member(s)
Charles E. Corry
Charles J. Haas
Department(s)
Geosciences and Geological and Petroleum Engineering
Degree Name
M.S. in Geology and Geophysics
Publisher
University of Missouri--Rolla
Publication Date
Summer 1989
Pagination
vi, 95 pages, map
Note about bibliography
Includes bibliographical references (pages 40-41).
Geographic Coverage
Phelps County, Missouri
Rights
© 1989 Douglas Wendel Whitman, All rights reserved.
Document Type
Thesis - Restricted Access
File Type
text
Language
English
Thesis Number
T 5916
Print OCLC #
20860370
Recommended Citation
Whitman, Douglas Wendel, "Geophysical investigations in a losing stream valley, Phelps County, Missouri" (1989). Masters Theses. 790.
https://scholarsmine.mst.edu/masters_theses/790
Refraction Depth Sections for Lines 1 thru 4
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Comments
One plate, folded in the back pocket of the manuscript, is provided here as a supplemental file. Due to its large size, this file may take more time to download.
This research project was supported in part by the U.S. Department of Interior and a Sigma-Xi Grant-in-Aid of Research.