Crack coalescence in granite

Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Civil and Environmental Engineering, 2008.

Bibliographic Details
Main Author: Miller, James Thomas, Ph. D. Massachusetts Institute of Technology
Other Authors: Herbert H. Einstein.
Format: Thesis
Language:eng
Published: Massachusetts Institute of Technology 2009
Subjects:
Online Access:http://hdl.handle.net/1721.1/47771
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author Miller, James Thomas, Ph. D. Massachusetts Institute of Technology
author2 Herbert H. Einstein.
author_facet Herbert H. Einstein.
Miller, James Thomas, Ph. D. Massachusetts Institute of Technology
author_sort Miller, James Thomas, Ph. D. Massachusetts Institute of Technology
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description Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Civil and Environmental Engineering, 2008.
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spelling mit-1721.1/477712019-04-12T13:52:02Z Crack coalescence in granite Miller, James Thomas, Ph. D. Massachusetts Institute of Technology Herbert H. Einstein. 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 (S.M.)--Massachusetts Institute of Technology, Dept. of Civil and Environmental Engineering, 2008. Includes bibliographical references. This thesis experimentally investigates crack coalescence in prismatic Barre Granite specimens with two pre-cut, open flaws under uniaxial compression. Using a high-speed video system, crack initiation, propagation, and coalescence are observed. Flaw geometries are chosen to allow one to compare the results with those of studies in other materials as well as to better understand fracturing and coalescence processes. Specifically, the effect of ligament length (L), flaw inclination angle (p3), and bridging angle (a) on coalescence is investigated. The same crack types as in other materials are observed. Coalescence patterns observed fit into a previously developed framework (for molded gypsum and Carrara marble) with the exception of one new coalescence pattern. Crack processes and coalescence patterns suggest a more tensile behavior as grain size increases from gypsum to marble to granite. Similar to previous work in marble and granite, white patches are observed during compression tests. These white patches can be categorized as either diffuse or linear, with linear white patches further subdivided into two more types, namely boundary-following and through-going. The white patches are essentially process zones. The effect of water pressure on coalescence pattern is also investigated. Flaw water pressure is seen to affect coalescence in granite, although further work is needed. by James Thomas Miller. S.M. 2009-10-01T15:40:58Z 2009-10-01T15:40:58Z 2008 2008 Thesis http://hdl.handle.net/1721.1/47771 428976146 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 474 p. application/pdf Massachusetts Institute of Technology
spellingShingle Civil and Environmental Engineering.
Miller, James Thomas, Ph. D. Massachusetts Institute of Technology
Crack coalescence in granite
title Crack coalescence in granite
title_full Crack coalescence in granite
title_fullStr Crack coalescence in granite
title_full_unstemmed Crack coalescence in granite
title_short Crack coalescence in granite
title_sort crack coalescence in granite
topic Civil and Environmental Engineering.
url http://hdl.handle.net/1721.1/47771
work_keys_str_mv AT millerjamesthomasphdmassachusettsinstituteoftechnology crackcoalescenceingranite