標(biāo)題: Titlebook: Clay Microstructure; Richard H. Bennett,Matthew H. Hulbert Book 1986 International Human Resources Development Corporation 1986 chemistry. [打印本頁(yè)] 作者: Braggart 時(shí)間: 2025-3-21 20:06
書目名稱Clay Microstructure影響因子(影響力)
書目名稱Clay Microstructure影響因子(影響力)學(xué)科排名
書目名稱Clay Microstructure網(wǎng)絡(luò)公開度
書目名稱Clay Microstructure網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Clay Microstructure被引頻次
書目名稱Clay Microstructure被引頻次學(xué)科排名
書目名稱Clay Microstructure年度引用
書目名稱Clay Microstructure年度引用學(xué)科排名
書目名稱Clay Microstructure讀者反饋
書目名稱Clay Microstructure讀者反饋學(xué)科排名
作者: declamation 時(shí)間: 2025-3-21 22:27
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作者: 橫條 時(shí)間: 2025-3-22 02:17
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 作者: Awning 時(shí)間: 2025-3-22 08:09 作者: 奴才 時(shí)間: 2025-3-22 11:05 作者: 四目在模仿 時(shí)間: 2025-3-22 15:36
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作者: 四目在模仿 時(shí)間: 2025-3-22 17:12 作者: 轉(zhuǎn)向 時(shí)間: 2025-3-23 00:20 作者: 殺菌劑 時(shí)間: 2025-3-23 05:05 作者: 不持續(xù)就爆 時(shí)間: 2025-3-23 07:18
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.作者: limber 時(shí)間: 2025-3-23 10:08
Geological Sciences Serieshttp://image.papertrans.cn/c/image/227264.jpg作者: CONE 時(shí)間: 2025-3-23 15:19 作者: 王得到 時(shí)間: 2025-3-23 20:35 作者: Bucket 時(shí)間: 2025-3-23 23:00
https://doi.org/10.5822/978-1-61091-893-0sediments. 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 devel作者: reperfusion 時(shí)間: 2025-3-24 05:10 作者: negotiable 時(shí)間: 2025-3-24 09:31 作者: 高度贊揚(yáng) 時(shí)間: 2025-3-24 12:15
Darlene Yee-Melichar,Emiko Takagi,Kristy Luiious important areas of research on clay microstructure. Only a few studies dealing with the fabric of natural sedimentary material have been reported, in contrast to numerous studies of laboratory prepared material. The only comprehensive studies of submarine sediment clay fabrics have been conduct作者: Invigorate 時(shí)間: 2025-3-24 17:37
Resilience in Childhood Disordersesses and events, and on the types of source material available, and on the environmental setting. These processes and factors produce primary and postdepositional sediment properties in time and space. The primary depositional properties include textures, mass physical and mechanical properties, an作者: 組裝 時(shí)間: 2025-3-24 22:42
The Connor–Davidson Resilience Scaleng 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作者: Irksome 時(shí)間: 2025-3-24 23:10
Physico-Chemical Interactions,ent of the theory of physico-chemical interactions has been reflected in reports of research on clay-water systems. Although keeping the current theory in mind simplifies review of research on clay fabric, we recognize that the theory surely will be altered as old ideas are refined on the basis of n作者: 夜晚 時(shí)間: 2025-3-25 04:12
Concepts of Clay Fabric, Goldschmidt (1926) proposed that clay properties are due to crystalline minerals enclosed by a film of adsorbed water molecules. He thought that the water molecules adhere to each other and to mineral grains due to their dipolar moment. Goldschmidt proposed that the flaky minerals of chemically sen作者: 優(yōu)雅 時(shí)間: 2025-3-25 07:34 作者: 不適 時(shí)間: 2025-3-25 12:58
Clay Fabric and Environment,re important in determining the fabric of the transported material and the freshly deposited sedimentary material. Deposited particles establish the primary properties of the sediment. Once deposited, postdepositional processes come into play. Postdepositional processes and effects can be grouped in作者: antedate 時(shí)間: 2025-3-25 19:14 作者: Camouflage 時(shí)間: 2025-3-25 21:43 作者: Palate 時(shí)間: 2025-3-26 00:20
Joseph G. Pickard,M. Denise King Goldschmidt (1926) proposed that clay properties are due to crystalline minerals enclosed by a film of adsorbed water molecules. He thought that the water molecules adhere to each other and to mineral grains due to their dipolar moment. Goldschmidt proposed that the flaky minerals of chemically sen作者: CANT 時(shí)間: 2025-3-26 06:14 作者: 摘要 時(shí)間: 2025-3-26 11:36 作者: affluent 時(shí)間: 2025-3-26 13:28 作者: 使饑餓 時(shí)間: 2025-3-26 17:28
Book 1986particle 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作者: 偏見(jiàn) 時(shí)間: 2025-3-26 21:54 作者: 蛙鳴聲 時(shí)間: 2025-3-27 03:11
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