The mechanisms involved during the desaturation process of a porous matrix

Thesis (Ph.D.)--Massachusetts Institute of Technology, Dept. of Civil and Environmental Engineering, 2000.

Bibliographic Details
Main Author: Sjoblom, Kurt J. (Kurt John), 1965-
Other Authors: John T. Germaine.
Format: Thesis
Language:eng
Published: Massachusetts Institute of Technology 2006
Subjects:
Online Access:http://hdl.handle.net/1721.1/29890
_version_ 1826202813697359872
author Sjoblom, Kurt J. (Kurt John), 1965-
author2 John T. Germaine.
author_facet John T. Germaine.
Sjoblom, Kurt J. (Kurt John), 1965-
author_sort Sjoblom, Kurt J. (Kurt John), 1965-
collection MIT
description Thesis (Ph.D.)--Massachusetts Institute of Technology, Dept. of Civil and Environmental Engineering, 2000.
first_indexed 2024-09-23T12:19:09Z
format Thesis
id mit-1721.1/29890
institution Massachusetts Institute of Technology
language eng
last_indexed 2024-09-23T12:19:09Z
publishDate 2006
publisher Massachusetts Institute of Technology
record_format dspace
spelling mit-1721.1/298902019-04-12T21:50:46Z The mechanisms involved during the desaturation process of a porous matrix Sjoblom, Kurt J. (Kurt John), 1965- John T. Germaine. Massachusetts Institute of Technology. Dept. of Civil and Environmental Engineering. Massachusetts Institute of Technology. Dept. of Civil and Environmental Engineering. Civil and Environmental Engineering. Thesis (Ph.D.)--Massachusetts Institute of Technology, Dept. of Civil and Environmental Engineering, 2000. Includes bibliographical references (p. 247-253). Traditionally, soil mechanics deals with soil in either of two states, saturated or dry. The effective stress concept proposed by Terzaghi has proven to be valid for soils in either of these states. However, when the water or air phase becomes large enough, the soil no longer behaves as two-phase system and the third phase must be considered. Unsaturated soil behavior has been argued to be a function of negative pore pressure or matric suction. All the unsaturated soil behavioral issues contain a single underlying question; what is the nature of soil suction? Nature refers to the physical phenomenon that generates soil suction and changes with environmental factors. The goal of this work is to provide an understanding of the generation of soil suction. Examining the drying process of porous material gave perspective into the development of negative pressures. The drying material was modeled by a regular packed matrix of equal diameter spheres. Configuring the water into the geometric shape of pendular rings simulated the water held in the matrix. A predictive model was then developed relating the water content of the matrix to the associated tension in the water. The model was tested using a unique measurement technique to determine a continuous drying curve of a porous material. The technique required the development of a tensiometer capable of directly measuring the high negative pressures. Glass beads of narrow distribution provided insight into the behavior of the drying pendular rings. It was determined that the actual tension to initiate draining is much greater than that predicted by the largest pendular ring. This reduced size of ring was also observed by a series of photographs of drying spheres. The information gained was then used to predict the tension of draining (or air entry pressure, AEP) for natural materials. Three types of soils were tested to validate this prediction. Finally, a literature search was done to obtain data for a wide variety of soils. The literature data provided a means to refine the prediction by relating the grain size distribution of the soil to the AEP. by Kurt J. Sjoblom. Ph.D. 2006-03-24T18:00:27Z 2006-03-24T18:00:27Z 2000 2000 Thesis http://hdl.handle.net/1721.1/29890 48245212 eng M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission. http://dspace.mit.edu/handle/1721.1/7582 334 p. 12668635 bytes 12714457 bytes application/pdf application/pdf application/pdf Massachusetts Institute of Technology
spellingShingle Civil and Environmental Engineering.
Sjoblom, Kurt J. (Kurt John), 1965-
The mechanisms involved during the desaturation process of a porous matrix
title The mechanisms involved during the desaturation process of a porous matrix
title_full The mechanisms involved during the desaturation process of a porous matrix
title_fullStr The mechanisms involved during the desaturation process of a porous matrix
title_full_unstemmed The mechanisms involved during the desaturation process of a porous matrix
title_short The mechanisms involved during the desaturation process of a porous matrix
title_sort mechanisms involved during the desaturation process of a porous matrix
topic Civil and Environmental Engineering.
url http://hdl.handle.net/1721.1/29890
work_keys_str_mv AT sjoblomkurtjkurtjohn1965 themechanismsinvolvedduringthedesaturationprocessofaporousmatrix
AT sjoblomkurtjkurtjohn1965 mechanismsinvolvedduringthedesaturationprocessofaporousmatrix