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

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.

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

Whitman_Douglas_1989.tif (427195 kB)
Refraction Depth Sections for Lines 1 thru 4

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Thesis Location

 
COinS