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Titlebook: Clay Microstructure; Richard H. Bennett,Matthew H. Hulbert Book 1986 International Human Resources Development Corporation 1986 chemistry.

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发表于 2025-3-21 20:06:50 | 显示全部楼层 |阅读模式
书目名称Clay Microstructure
编辑Richard H. Bennett,Matthew H. Hulbert
视频videohttp://file.papertrans.cn/228/227264/227264.mp4
丛书名称Geological Sciences Series
图书封面Titlebook: Clay Microstructure;  Richard H. Bennett,Matthew H. Hulbert Book 1986 International Human Resources Development Corporation 1986 chemistry.
描述Plan of Review This review of clay microstructure is aimed at the diverse group of professionals who share an interest in the properties of fine-grained minerals in sediments. During the last several decades, members of this group have included geologists, soil scientists, soil engineers, engineering geologists, and ceramics scientists. More recently, it has included significant numbers of marine geologists and other engineers. Each of the disciplines has developed special techniques for investigating properties of clay sediments that have proven to be fruitful in answering questions of central interest. Knowledge of clay microstructure-the fabric of a sediment and the physico­ chemical interactions between its components-is fundamental to all these disciplines (Mitchell 1956; Lambe 1958a; Foster and De 1971). Clay fabric refers to the spatial distribution, orientations, and particle-to-particle relations of the solid particles (generally those less than 3. 9 /Lm in size) of sediment. Physico-chemical interac­ tions are expressions of the forces between the particles. In this review, we trace the historical development of under­ standing clay microstructure by discussing key scient
出版日期Book 1986
关键词chemistry; clays; electron microscopy; environment; mineral; mineral resources; economic geology
版次1
doihttps://doi.org/10.1007/978-94-009-4684-2
isbn_softcover978-94-010-8582-3
isbn_ebook978-94-009-4684-2
copyrightInternational Human Resources Development Corporation 1986
The information of publication is updating

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发表于 2025-3-21 22:27:25 | 显示全部楼层
Physico-Chemical Interactions,se forces, gravity is important in settling aggregates and consolidating sediment masses. There have been numerous investigations of physico-chemical interactions in clay systems, and interested readers are referred to Mysels (1959), Grimshaw (1971), van Olphen (1977), and Yarin and Cross (1979). In
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Concepts of Clay Fabric,angement of soil particles and the bonding of cohesive soils. As early as 1908, Sorby alluded to the importance of clay particle arrangement during settling and consolidation. Terzaghi proposed that clay minerals stick to each other at points of contact, with forces sufficiently strong to construct
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Summary,ng of clay microstructure promises to be fruitful. Direct application of the results of many laboratory studies of clay microstructure to natural sediments and to clayey materials of commercial interest is commonly impeded by the much larger degree of variability in real systems than in laboratory s
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Introduction,ines (Mitchell 1956; Lambe 1958a; Foster and De 1971). . refers to the spatial distribution, orientations, and particle-to-particle relations of the solid particles (generally those less than 3.9 .m in size) of sediment. . are expressions of the forces between the particles.
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