Masters Theses
Abstract
"Fundamental aspects of thixotropic phenomena are described, and previous investigations of thixotropic behavior in soil systems are summarized. The complex nature of the thixotropic phenomena as well as its general occurrence in fine grained soils is described. As existing hypothesis for thixotropic behavior based on initial non-equilibrium conditions is examined. Experimental results, as determined from a testing program on the Putnam clay, verify this hypothesis. The rate and magnitude of thixotropic strength increases of the Putnam clay were determined. Shear strength determinations were made by the unconfined compression and laboratory vane shear tests. The results of the tests were compared and variations are explained. Results of the research program indicate that: 1) Water content is of primary importance in determining the rate of shear strength increase. 2) Aging leads to an increase in stiffness and ultimate strength. 3) Acquired sensitivity is greatest at small strains"--Abstract, page ii.
Advisor(s)
Armstrong, James C.
Committee Member(s)
Bolter, Ernst
Harbaugh, Terence E., 1935-1973
Department(s)
Civil, Architectural and Environmental Engineering
Degree Name
M.S. in Civil Engineering
Publisher
University of Missouri at Rolla
Publication Date
1968
Pagination
ix, 68 pages
Note about bibliography
Includes bibliographical references (page 38).
Rights
© 1968 John Arthur Mathes, All rights reserved.
Document Type
Thesis - Open Access
File Type
text
Language
English
Subject Headings
Clay soils -- TestingShear strength of soilsThixotropy
Thesis Number
T 2079
Print OCLC #
5994860
Electronic OCLC #
802288235
Recommended Citation
Mathes, John Arthur, "Thixotropic effects in a clay-water system" (1968). Masters Theses. 5219.
https://scholarsmine.mst.edu/masters_theses/5219