Author(s)/Editor(s): Yung Ming Cheng, Henry Wong, Chin Leo, C. K. Lau | Size: 12 MB | Format:PDF | Quality:Original preprint | Publisher: Bentham Science Publishers | Year: 2016 | pages: 410| ISBN: 9781681083049
Introduction
Upper and Lower Bound Approaches
Slip Line, Limit Equilibrium and Limit Analysis Methods
Numerical Methods --
Finite Element and Distinct Element Methods
Numerical Techniques for Solution of Stability Problems
Applications of Plasticity Theory and Limit Analysis to the Bearing Capacity of Shallow Foundations
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Author(s)/Editor(s): John N. Cernica | Size: 19.48 MB | Format:PDF | Quality:Scanner | Publisher: John Wiley & Sons, Inc. | Year: 1995 | pages: 504 | ISBN: 978-0-471-30887-4
Combines a thorough theoretical presentation with the practical aspects of foundation design. The first three chapters offer a condensed version of the basic elements of soil mechanics. The remaining chapters deal with the design of diverse types of foundation components, retaining rock structures and site improvement.
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"The third revised edition offers exhaustive information regarding
concepts, processes and fundamental principles of forest hydrology.
This publication discusses functional properties, distributions of
water, forests and precipitation, humidity, runoff, soils and
sedimentation and also research approaches in the forest and water. In
addition, the watershed management and practical applications in forest
hydrology and water recourse managements are also discussed in this
book."
βNachrichten, Neue Publikationen,2013
Praise for the First Edition
A textbook for most forest hydrology courses should not only cover topics on forest impacts on water but also provide the basics of water properties, movement, and storage in the atmosphere, soil matrix, and surface water bodies. Putting both major topic areas in one manageable textbook requires trade-offs that do not dilute either subject area too much, but rather skillfully blend the two together. Mingteh Chang has done just that in writing this book.
βRichard C. Schultz, Professor of Forest Hydrology and Ecology, Iowa State University, in Forest Science, Vol. 49, No. 2
The book can be used as a text for students in agriculture, forestry, and land-resources management, and as a reference for foresters, rangers, geographers, watershed managers, biologists, agriculturalists, environmentalists, policy makers, engineers, and others who may need such background in their professions.
βFalhry A. Assaad, Consultant, Geologist, and Data Analyst
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Standard Penetration Test Proceures and the Effect on Sands of Overburden Pressure, relative Density, Ageing and Overconsolidation
Author(s): A. W. Skempton
Published By:Geotechnique
Published Year:1986
Size: 1.70 MB
Quality:Scanner(OCR)
Abstract: Granted that good site control is exercised in carrying out the standard penetration test the energy delivered
to the sampler, and therefore the blow count obtained in any given sand deposit at a particular effective overburden pressure, can still vary to a significant extent depending on the method of releasing the hammer, on the type of anvil and on the length of rods (if less than 10 m).
For consistency it is essential to correct the observed blow count N to the value which would have been measured using a specified rod energy.
A recommended value, which should be recognized internationally, is 60% of the free-fall energy of the standard hammer weight and drop.
The corrected blow count is then designated as N 60 and the normalized value (N 1)60 at unit effective pressure ( 1 kg/cm 2 or 100 kPa) may be regarded as a basic characteristic of the sand.
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Geotechnical Design of Retaining Walls - Limit State Analysis in geotechnical Engineering - The Collapse of Diaphragm Walls Retaining Clay - The Strength and Dilatancy of Sands
Author(s): M. D. Bolton
Size: 3.36 MB
Quality:Scanner(OCR)
Abstract: Collection of M. D. Bolton's geotechnical research papers.
It includes "The Strength and Dilatancy of Sands" paper (1986).
.... "Extensive data of the strength and dilatancy of 17 sands in axisymmetric or plane strain at different densities and confining pressures are collated. The critical state angle
of shearing resistance of soil which is shearing at constant
volume is principally a function of mineralogy and can readily be determined experimentally within a margin of about 1 Β°, being roughly 33Β° for quartz and 40Β° for feldspar" ....
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