Masters Theses
Abstract
"Soil is a material that has been formed through the influence of many different natural agencies. The engineer is not so much interested in how the soil was formed, but he does want to know the characteristics of the soil with respect to its use as a structural material. Therefore, the engineer is primarily interested in the physical properties of soils.
Much progress has been made during the past twenty five years in the study of Soil Mechanics, but even today there is a tendency among engineers to think of soil as just a mixture of clay, sand, silt and gravel. In designing a structure, if soil is one of the principal building materials or serves as the structure's base, the designer can prepare better plans, reduce the initial construction effort and make maintenance easier, by a knowledge of the physical properties of the soil.
It is generally believed that soils have five basic physical characteristics: Internal friction, cohesion, compressibility, elasticity, and capillarity. This paper is concerned directly with finding a simple method of determining the capillarity of a soil"--Preface, page iii.
Advisor(s)
Gevecker, Vernon A. C., 1909-1992
Department(s)
Civil, Architectural and Environmental Engineering
Degree Name
M.S. in Civil Engineering
Publisher
Missouri School of Mines and Metallurgy
Publication Date
1951
Pagination
vi, 40 pages
Note about bibliography
Includes bibliographical references (pages 38-39).
Rights
© 1951 Samuel P. Halcomb, All rights reserved.
Document Type
Thesis - Open Access
File Type
text
Language
English
Subject Headings
Soil moisture -- Mathematical modelsSoil mechanics -- Mathematical modelsSoils
Thesis Number
T 979
Print OCLC #
5985160
Electronic OCLC #
936362024
Recommended Citation
Halcomb, Samuel Payton, "The relationship between the centrifuge moisture equivalent and the vacuum moisture equivalent in soils" (1951). Masters Theses. 2991.
https://scholarsmine.mst.edu/masters_theses/2991