標(biāo)題: Titlebook: Geochemistry of Colloid Systems; For Earth Scientists Shmuel Yariv,Harold Cross Book 1979 Springer-Verlag Berlin Heidelberg 1979 Geochemie. [打印本頁] 作者: Roosevelt 時(shí)間: 2025-3-21 18:59
書目名稱Geochemistry of Colloid Systems影響因子(影響力)
書目名稱Geochemistry of Colloid Systems影響因子(影響力)學(xué)科排名
書目名稱Geochemistry of Colloid Systems網(wǎng)絡(luò)公開度
書目名稱Geochemistry of Colloid Systems網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Geochemistry of Colloid Systems被引頻次
書目名稱Geochemistry of Colloid Systems被引頻次學(xué)科排名
書目名稱Geochemistry of Colloid Systems年度引用
書目名稱Geochemistry of Colloid Systems年度引用學(xué)科排名
書目名稱Geochemistry of Colloid Systems讀者反饋
書目名稱Geochemistry of Colloid Systems讀者反饋學(xué)科排名
作者: 乳汁 時(shí)間: 2025-3-21 23:21
- chemistry, soil science, and oceanography. So that specialists interested in certain sections may find their subjects comprehensively covered, a few topics are dealt with in more than one chapter so that readers may ignore sections not especially of interest to them. However the chapters more fully treating978-3-642-67043-5978-3-642-67041-1作者: squander 時(shí)間: 2025-3-22 00:55
Introduction, for illumination. Consequently particles smaller than about a few hundred nm in diameter are submicroscopic. Colloid systems in which a liquid is the dispersing medium appear to form true solutions. These solutions pass unchanged through ordinary filter paper. The classical science of colloids deal作者: 整頓 時(shí)間: 2025-3-22 08:05
Die Interferenz der R?ntgenstrahlen for illumination. Consequently particles smaller than about a few hundred nm in diameter are submicroscopic. Colloid systems in which a liquid is the dispersing medium appear to form true solutions. These solutions pass unchanged through ordinary filter paper. The classical science of colloids deal作者: gentle 時(shí)間: 2025-3-22 11:03 作者: HUSH 時(shí)間: 2025-3-22 16:37
Some Geologic Colloid Systems,rated oxides and hydroxides, mainly of Si, Fe, Mn, and Al, and some organic macromolecules are responsible for most colloid properties of geologic systems that constitute the sedimentary cycle. The clay minerals, which generally comprise the greater part of the colloid fraction, are so-called from t作者: HUSH 時(shí)間: 2025-3-22 20:09 作者: Feckless 時(shí)間: 2025-3-22 23:30 作者: paradigm 時(shí)間: 2025-3-23 02:17 作者: FEAS 時(shí)間: 2025-3-23 07:16
Colloid Geochemistry of Clay Minerals,s. Although electro-neutrality in the bulk is maintained, these minerals have localized point-sites of high and low electric charges, either positive or negative. On a macroscale, the silicate unit layers are almost always negatively charged and the regions where the metallic exchangeable cations ar作者: insincerity 時(shí)間: 2025-3-23 12:11
Rheology of Colloid Systems,cated in Figure 9.1 as the “reference plane”. A tangential force is applied at the top surface of the unit volume, which results in movement of the top layer in the direction of the applied force. The stacked layers slide one above the other by equal relative amounts to each other. The result is tha作者: 協(xié)定 時(shí)間: 2025-3-23 14:02
Colloid Geochemistry of Argillaceous Sediments,es of clay minerals, namely, their very small particle size and their high surface energy, are recognizable in the physical and chemical reactions that take place after the particles have settled out (pages 395–396).作者: 南極 時(shí)間: 2025-3-23 18:59
978-3-642-67043-5Springer-Verlag Berlin Heidelberg 1979作者: exhibit 時(shí)間: 2025-3-24 02:13 作者: 清晰 時(shí)間: 2025-3-24 06:04
,Entstehung der Internet-?konomie,The adhesion between two particles is the result of factors such as (a) chemical and nonchemical bond formation, which may be at or away from the particle—particle interface, and (b) creation and release of mechanical strains and stresses at and around that interface. The area of contact between the two particles is called the ..作者: 失望昨天 時(shí)間: 2025-3-24 09:16
Formation of Aqueous Solutions and Suspensions of Hydrophobic Colloids,The two general ways in which suspensions are formed are by building up of particles from molecular or atomic units, or by breaking down particles of macroscopic dimensions, termed respectively condensation and dispersion. Both phenomena will be discussed in this chapter.作者: 嚴(yán)厲批評(píng) 時(shí)間: 2025-3-24 14:38 作者: 要求比…更好 時(shí)間: 2025-3-24 16:43
https://doi.org/10.1007/978-3-642-67041-1Geochemie; Kolloidchemie; Systems; atmosphere; desert; diagenesis; environment; geochemistry; geology; minera作者: jabber 時(shí)間: 2025-3-24 21:15
Die Interferenz der R?ntgenstrahlens the science of colloids was concerned mainly with the description of the behavior of very small particles. The classical definition of a colloid system described the disperse phase as being comprised of particles or macromolecules smaller than 1000 nm in diameter, but larger than 1 nm. Particles s作者: 營養(yǎng) 時(shí)間: 2025-3-25 02:25 作者: Expertise 時(shí)間: 2025-3-25 05:23 作者: Torrid 時(shí)間: 2025-3-25 11:26 作者: 引水渠 時(shí)間: 2025-3-25 12:22 作者: 陶器 時(shí)間: 2025-3-25 16:45
Vorwort Der European Communication Council,s. Although electro-neutrality in the bulk is maintained, these minerals have localized point-sites of high and low electric charges, either positive or negative. On a macroscale, the silicate unit layers are almost always negatively charged and the regions where the metallic exchangeable cations ar作者: maladorit 時(shí)間: 2025-3-25 20:30
Hans Jürgen Kleinsteuber dipl. pol.cated in Figure 9.1 as the “reference plane”. A tangential force is applied at the top surface of the unit volume, which results in movement of the top layer in the direction of the applied force. The stacked layers slide one above the other by equal relative amounts to each other. The result is tha作者: Ingrained 時(shí)間: 2025-3-26 02:29
Die Intrakapsulare Starextraktiones of clay minerals, namely, their very small particle size and their high surface energy, are recognizable in the physical and chemical reactions that take place after the particles have settled out (pages 395–396).作者: Enteropathic 時(shí)間: 2025-3-26 07:50
Die Intrakapsulare Starextraktiones of clay minerals, namely, their very small particle size and their high surface energy, are recognizable in the physical and chemical reactions that take place after the particles have settled out (pages 395–396).作者: 預(yù)防注射 時(shí)間: 2025-3-26 12:21
Colloid Geochemistry of Argillaceous Sediments,es of clay minerals, namely, their very small particle size and their high surface energy, are recognizable in the physical and chemical reactions that take place after the particles have settled out (pages 395–396).作者: 修正案 時(shí)間: 2025-3-26 15:57 作者: 不可思議 時(shí)間: 2025-3-26 20:29
Hans Jürgen Kleinsteuber dipl. pol.is the distance of the layer from the “reference plane”. This velocity gradient is called . (or simply .), and is measured in reciprocal seconds (m s. · m. = s.). The applied tangential force is called . (or simply .) and is indicated by τ. The stress is measured in dynes/cm. or in newtons/m..作者: annexation 時(shí)間: 2025-3-26 23:14
Some Geologic Colloid Systems,y deposits contain well-defined crystalline particles, most clay minerals occur as particles too small to be resolved by the ordinary microscope. Furthermore, a wide distribution of particle sizes is frequently present.作者: 哄騙 時(shí)間: 2025-3-27 02:11 作者: achlorhydria 時(shí)間: 2025-3-27 08:22 作者: Infuriate 時(shí)間: 2025-3-27 09:40 作者: 平項(xiàng)山 時(shí)間: 2025-3-27 16:54 作者: obviate 時(shí)間: 2025-3-27 18:59 作者: 隱藏 時(shí)間: 2025-3-27 21:58
avior of colloids have been contributed by them. Barring a few notable exceptions, only in the last decade have geochemists applied colloid science in their research and in this period much work has been published. It seemed to the authors that it would be useful at this stage to attempt to summariz作者: Lice692 時(shí)間: 2025-3-28 05:57
https://doi.org/10.1007/978-3-663-09727-3for thermodynamic treatment of surfaces was established in the last century by Gibbs, who published a considerable contribution to the field in 1878. His work still forms the basis of modern thermodynamics (Gibbs, 1928).作者: 美色花錢 時(shí)間: 2025-3-28 09:39 作者: 失誤 時(shí)間: 2025-3-28 10:40
Physical Chemistry of Surfaces,for thermodynamic treatment of surfaces was established in the last century by Gibbs, who published a considerable contribution to the field in 1878. His work still forms the basis of modern thermodynamics (Gibbs, 1928).作者: Canopy 時(shí)間: 2025-3-28 14:52
Surface Coatings on Rocks and Grains of Minerals,atoms from the core of the crystal to the surface resulting from abrasion and collision between solids in dry systems; (4) biologic activity, which is, however, outside the scope of this review and will not be considered.作者: 組成 時(shí)間: 2025-3-28 18:54 作者: Enervate 時(shí)間: 2025-3-29 01:20
Floya Anthias,Maria Kontos,Feiwel Kupferberg,Gabriella Lazaridis,Suzanne Mason,Skevos Papaioannou,Wa作者: 植物學(xué) 時(shí)間: 2025-3-29 04:14
