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Field and laboratory experimental study of water infiltration in cracked soil /Kwong, Chin Pang. January 2009 (has links)
Includes bibliographical references (p. 202-209).
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High resolution geophysical techniques for small-scale soil model testingLee, Jong-Sub, January 2003 (has links) (PDF)
Thesis (Ph. D.)--School of Civil and Environmental Engineering, Georgia Institute of Technology, 2004. Directed by J. Carlos Santamarina. / Includes bibliographical references (leaves 266-279).
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Field and laboratory study of an unsaturated expansive soil associated with rain-induced slope instability /Zhan, Liangtong. January 2003 (has links)
Thesis (Ph. D.)--Hong Kong University of Science and Technology, 2003. / Includes bibliographical references (leaves 471-490). Also available in electronic version. Access restricted to campus users.
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An experimental study of vertical infiltration into undisturbed residual soils /Tse, Siu-hung. January 1980 (has links)
Thesis (M. Phil.)--University of Hong Kong, 1981.
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The behaviour of Hong Kong residual soil as fill material.Ng, Wai-ying, Betty, January 1978 (has links)
Thesis (M. Phil.)--University of Hong Kong, 1979.
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The influence of spatial variability on the geotechnical design properties of a stiff, overconsolidated clay.Jaksa, Mark B January 1995 (has links)
The research presented in this thesis focuses on the spatial variability of the Keswick and Hindmarsh Clays within the Adelaide city area. Keswick Clay is locally significant since many of Adelaide's multi-storey buildings are founded directly on it, and internationally significant, since it has been shown by Cox (1970), that this clay exhibits remarkably similar properties to those of the well-documented London Clay. The assessment of the small-scale variability of the undrained shear strength of these clays is based on measurements obtained using the electrical cone penetration test (CPT), and a micro-computer based data acquisition system, designed specifically for this study. A significant feature of the data acquisition system is that it enables measurements to be obtained at intervals of 5 mm, both reliably and efficiently. The development of the data acquisition system is discussed, and the accuracy of its measurements is examined. The small-scale variability of the undrained shear strength of the Keswick Clay is based on more than 200 vertical CPTs, performed within an area of 50 X 50 metres at a site located in the Adelaide city area. The CPTs were spaced at lateral intervals varying between 0.5 and 5 metres, with each vertical CPT extending to a typical depth of 5 metres. In addition, the small-scale horizontal spatial variability of the Keswick Clay is examined using an electrical cone penetrometer driven horizontally into the face of an embankment, again located within the Adelaide city area. The accuracy of the CPT measurements is examined, and discussion is given of the shortcomings associated with a commonly used technique, by Baecher (1982), for estimating the random measurement error associated with various test procedures. The assessment of the large-scale spatial variability of the undrained shear strength of the Keswick and Hindmarsh Clays is founded on a data base of geotechnical engineering properties, compiled from a number of consulting engineering practices and government instrumentalities. The data base, known as KESWICK, contains approximately 160 site investigations, 380 boreholes, and 10,140 measurements obtained from a number of different laboratory and in situ tests. In addition, KESWICK is used to establish generalised trends and bounds, associated with the various geotechnical engineering design properties contained within the data base. The techniques of random field theory and geostatistics are used to quantify, model and predict the spatial variability of the Keswick and Hindmarsh Clays. These techniques are compared with one another in order to assess the suitability and shortcomings of each, when applied to the study of the spatial variability of geotechnical engineering materials. Furthermore, a number of specifically-written computer programs, which were developed to enable the various spatial variability analyses to be performed, are discussed. It is demonstrated that the lateral undrained shear strength of the Keswick Clay, within the Adelaide city area, exhibits a nested structure; that is, one which is the compound effect of several genetic sources of spatial variation. In addition, it is shown that this nested structure can be adequately modelled by means of a spherical semivariogram model. The nested structure is used, together with the kriging estimation process, to provide preliminary estimates of the undrained shear strength of the Keswick Clay, within the Adelaide city area. The analyses demonstrate that the nested model and the kriging process provide a useful facility for generating preliminary estimates of the strength of the clay. Finally, the significance of the spatial variability of the undrained shear strength of clay soils is examined, with reference to the design of embankments and pile foundations. It is demonstrated that the correlation distance can greatly influence the design of each of these geotechnical systems. / Thesis (Ph.D.)--Dept. of Civil and Environmental Engineering, 1995.
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Use of soil texture analyses to predict fracturing in glacial tills and other unconsolidated materialsKim, Eun Kyoung, January 2007 (has links)
Thesis (Ph. D.)--Ohio State University, 2007. / Title from first page of PDF file. Includes bibliographical references (p. 145-156).
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Aluminium-Spezies im Boden und ihre Mobilität /Schmid, Susanne. January 1989 (has links)
Thesis (doctoral)--Universität-Gesamthochschule-Duisburg, 1989. / Includes bibliographical references (p. 256-272).
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The effective hydraulic conductivity of unsaturated layered sandsHarvey, Donald John, January 1989 (has links) (PDF)
Thesis (M.S. - Hydrology and Water Resources)--University of Arizona, 1989. / Includes bibliographical references (leaves 114-118).
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Depth of soil in the Goss-Gasconade rock outcrop complex in Callaway County, Missouri, using the Soil Land Inference Model (SoLIM) a thesis presented to the Department of Geology and Geography in candidacy for the degree of Master of Science /Verbrugge, Lydia. January 2006 (has links)
Thesis (M.S.)--Northwest Missouri State University, 2006. / The full text of the thesis is included in the pdf file. Title from title screen of full text.pdf file (viewed on January 25, 2008) Includes bibliographical references.
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