Author: Texas A & M University. Department of Oceanography
Publisher:
ISBN:
Category : Electron microscopy
Languages : en
Pages : 232
Book Description
Sediment samples were taken from Gulf of Mexico cores. From these samples smaller ones were cut, freeze-dried and impregnated with Maraglas, an epoxy resin. Ultrathin sections of the impregnated samples were cut, and viewed in an electron microscope. Micrographs of the ultrathin sections revealed that the microstructures of most of the samples had a loose, open, random arrangement of particles. Differences in appearance of some of the microstructures are attributed to grain size variation, desiccation, remolding, and shearing of the sediment. Associated with this last factor is the formation of oriented domain structures. Variations among the samples in depth of burial, rate of deposition, and, particularly, clay mineralogy were generally small and resulted in no obvious differences in their microstructures. Cohesion, water content, and consolidation characteristics of samples were found to be generally indicative of the type of microstructure observed. Laboratory consolidation and desiccation of samples caused a 'collapse' of the microstructure and preferred, as well as non-preferred, orientation among the particles. Remolding of a sediment resulted in clumping of the particles, parallelism among the particles, and large voids. No evidence was observed in the micrographs which would substantiate the existence of a precipitated chemical cement. (Author).
Electron Microscopy Investigation of the Microstructure in Sediment Samples from the Gulf of Mexico
Author: Texas A & M University. Department of Oceanography
Publisher:
ISBN:
Category : Electron microscopy
Languages : en
Pages : 232
Book Description
Sediment samples were taken from Gulf of Mexico cores. From these samples smaller ones were cut, freeze-dried and impregnated with Maraglas, an epoxy resin. Ultrathin sections of the impregnated samples were cut, and viewed in an electron microscope. Micrographs of the ultrathin sections revealed that the microstructures of most of the samples had a loose, open, random arrangement of particles. Differences in appearance of some of the microstructures are attributed to grain size variation, desiccation, remolding, and shearing of the sediment. Associated with this last factor is the formation of oriented domain structures. Variations among the samples in depth of burial, rate of deposition, and, particularly, clay mineralogy were generally small and resulted in no obvious differences in their microstructures. Cohesion, water content, and consolidation characteristics of samples were found to be generally indicative of the type of microstructure observed. Laboratory consolidation and desiccation of samples caused a 'collapse' of the microstructure and preferred, as well as non-preferred, orientation among the particles. Remolding of a sediment resulted in clumping of the particles, parallelism among the particles, and large voids. No evidence was observed in the micrographs which would substantiate the existence of a precipitated chemical cement. (Author).
Publisher:
ISBN:
Category : Electron microscopy
Languages : en
Pages : 232
Book Description
Sediment samples were taken from Gulf of Mexico cores. From these samples smaller ones were cut, freeze-dried and impregnated with Maraglas, an epoxy resin. Ultrathin sections of the impregnated samples were cut, and viewed in an electron microscope. Micrographs of the ultrathin sections revealed that the microstructures of most of the samples had a loose, open, random arrangement of particles. Differences in appearance of some of the microstructures are attributed to grain size variation, desiccation, remolding, and shearing of the sediment. Associated with this last factor is the formation of oriented domain structures. Variations among the samples in depth of burial, rate of deposition, and, particularly, clay mineralogy were generally small and resulted in no obvious differences in their microstructures. Cohesion, water content, and consolidation characteristics of samples were found to be generally indicative of the type of microstructure observed. Laboratory consolidation and desiccation of samples caused a 'collapse' of the microstructure and preferred, as well as non-preferred, orientation among the particles. Remolding of a sediment resulted in clumping of the particles, parallelism among the particles, and large voids. No evidence was observed in the micrographs which would substantiate the existence of a precipitated chemical cement. (Author).
Microstructure of Fine-Grained Sediments
Author: W.A. Chiou
Publisher: Springer Science & Business Media
ISBN: 1461244285
Category : Science
Languages : en
Pages : 570
Book Description
Knowledge of basic clay microstructure is fundamental to an understanding of the physical, chemical, and mechanical properties of fine-grained sediments and rocks. This compilation of fifty-nine peer-reviewed papers examines clay microstructure in detail with comprehensive sections focusing on microstructure signatures, environmental processes, modeling, measurement techniques, and future research recommendations. Many of these topics are discussed in light of geological and engineering applications, such as hazardous waste disposal, construction techniques, and drilling programs. The field of clay microstructure is developing rapidly. The concepts, observations, and principles presented in this book will help stimulate new thought and be a "spring board" for exciting new research.
Publisher: Springer Science & Business Media
ISBN: 1461244285
Category : Science
Languages : en
Pages : 570
Book Description
Knowledge of basic clay microstructure is fundamental to an understanding of the physical, chemical, and mechanical properties of fine-grained sediments and rocks. This compilation of fifty-nine peer-reviewed papers examines clay microstructure in detail with comprehensive sections focusing on microstructure signatures, environmental processes, modeling, measurement techniques, and future research recommendations. Many of these topics are discussed in light of geological and engineering applications, such as hazardous waste disposal, construction techniques, and drilling programs. The field of clay microstructure is developing rapidly. The concepts, observations, and principles presented in this book will help stimulate new thought and be a "spring board" for exciting new research.
ESSA Professional Paper
Author: United States. National Oceanic and Atmospheric Administration
Publisher:
ISBN:
Category :
Languages : en
Pages : 472
Book Description
Publisher:
ISBN:
Category :
Languages : en
Pages : 472
Book Description
Cooperative Investigation of the Carribbean and Adjacent Regions: CICAR.: Bibliography on marine geology and geophysics
Author:
Publisher:
ISBN:
Category : Geophysics
Languages : en
Pages : 262
Book Description
Publisher:
ISBN:
Category : Geophysics
Languages : en
Pages : 262
Book Description
Collected Reprints
Author:
Publisher:
ISBN:
Category : Marine meteorology
Languages : en
Pages : 572
Book Description
Publisher:
ISBN:
Category : Marine meteorology
Languages : en
Pages : 572
Book Description
Clay Microstructure
Author: Richard Bennett
Publisher: Springer Science & Business Media
ISBN: 9400946848
Category : Science
Languages : en
Pages : 163
Book Description
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 scientific papers published before 1986 on physico-chemical interactions in fine grained sediments and on clay fabric. Since the development follows an intricate path, the current view of clay microstructure is summarized. This summary includes a discussion of the present state of knowledge, the observations made so far, and the facts that are now established.
Publisher: Springer Science & Business Media
ISBN: 9400946848
Category : Science
Languages : en
Pages : 163
Book Description
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 scientific papers published before 1986 on physico-chemical interactions in fine grained sediments and on clay fabric. Since the development follows an intricate path, the current view of clay microstructure is summarized. This summary includes a discussion of the present state of knowledge, the observations made so far, and the facts that are now established.
Geological Survey Bulletin
Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 1492
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 1492
Book Description
Electron Microscopy of Soils and Sediments
Author: Peter Smart
Publisher: Oxford University Press, USA
ISBN:
Category : Science
Languages : en
Pages : 296
Book Description
Concerned mainly with the preparation of samples and the interpretation of electron micrographs, whether of undisturbed samples, or of samples that have been deformed under laboratory conditions. The difficulties that arise in preparing undamaged samples for electron microscopy are discussed.
Publisher: Oxford University Press, USA
ISBN:
Category : Science
Languages : en
Pages : 296
Book Description
Concerned mainly with the preparation of samples and the interpretation of electron micrographs, whether of undisturbed samples, or of samples that have been deformed under laboratory conditions. The difficulties that arise in preparing undamaged samples for electron microscopy are discussed.
Abstracts of North American Geology
Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 1080
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 1080
Book Description
U.S. Government Research & Development Reports
Author:
Publisher:
ISBN:
Category : Science
Languages : en
Pages : 1184
Book Description
Publisher:
ISBN:
Category : Science
Languages : en
Pages : 1184
Book Description