標題: Titlebook: ; [打印本頁] 作者: trace-mineral 時間: 2025-3-21 17:34
書目名稱Growth, Dissolution and Pattern Formation in Geosystems影響因子(影響力)
書目名稱Growth, Dissolution and Pattern Formation in Geosystems影響因子(影響力)學(xué)科排名
書目名稱Growth, Dissolution and Pattern Formation in Geosystems網(wǎng)絡(luò)公開度
書目名稱Growth, Dissolution and Pattern Formation in Geosystems網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Growth, Dissolution and Pattern Formation in Geosystems被引頻次
書目名稱Growth, Dissolution and Pattern Formation in Geosystems被引頻次學(xué)科排名
書目名稱Growth, Dissolution and Pattern Formation in Geosystems年度引用
書目名稱Growth, Dissolution and Pattern Formation in Geosystems年度引用學(xué)科排名
書目名稱Growth, Dissolution and Pattern Formation in Geosystems讀者反饋
書目名稱Growth, Dissolution and Pattern Formation in Geosystems讀者反饋學(xué)科排名
作者: 不出名 時間: 2025-3-21 23:54
https://doi.org/10.1007/978-3-531-92268-3he driving forces for growth are rather low — do indeed grow with flat faces. This phenomenon holds for crystals with very simple structures such as the cubic and hexagonal close-packed crystals of the elements helium, argon and krypton, growing at extremely low temperatures from their melts, and cr作者: Exclaim 時間: 2025-3-22 01:27
Ulrich von Alemann,Wolfgang T?nnesmannf ore minerals from hydrothermal fluids is responsible for the generation of the world’s most important class of ore deposits (Skinner, 1969). Hydrothermal systems also provide some of the most spectacular examples of naturally grown mineral ., which occasionally may reach a size of several centimet作者: Substance-Abuse 時間: 2025-3-22 08:31 作者: Sinus-Node 時間: 2025-3-22 10:26
Zur Logik der Politikwissenschaft,on kinetics. Wallrocks may be sampled at the scale of individual beds from the intrusive contact to beyond the limit of metamorphism so that the progress of metamorphic processes may be traced from their inception to their completion. The superficially simple intrusion geometry of these dikes, appro作者: bizarre 時間: 2025-3-22 14:57
Klaus Matu?ek,Hanns-Fred Rathenow under which they grew. Some crystals are faceted, for example quartz crystals; metal crystals often grow with smooth shapes, and salts and organic materials often grow with needle-like structures. Dendritic crystals, which are the subject of this paper, are also very common. Dendrites are crystals 作者: bizarre 時間: 2025-3-22 19:42 作者: packet 時間: 2025-3-23 00:32
Analytisch theoretischer Rahmen,e mainly ceramic geocosmological record. Among the common forms are needles, plates, cells, and dendrites, together with lamellar, wavy, multidisperse and filamentary arrays. Apart from the usual disparity of time and spatial scales, the main distinctions arise from the stronger directionality of bo作者: Ordnance 時間: 2025-3-23 04:25 作者: 獨輪車 時間: 2025-3-23 06:40
https://doi.org/10.1007/978-3-658-37553-9 of minerals. Many silicates are also formed in combination with other elements such as magnesium, aluminium, calcium and iron and as such form many of the minerals in our rocks and soils. Weathering processes over millions of years have also resulted in the occurrence of silica (silicon dioxide) in作者: 取消 時間: 2025-3-23 13:15
https://doi.org/10.1007/978-3-658-10186-2ontributors of Mg, Fe, and Ca to soils and surface waters. In soils, these metals are essential nutrients used by plant communities (Marschner, 1995). The presence of Mg, Fe, and Ca in surficial waters provokes carbonate mineral precipation, which is linked to atmospheric CO. content and climate thr作者: integral 時間: 2025-3-23 14:07 作者: LEVY 時間: 2025-3-23 19:53 作者: barium-study 時間: 2025-3-23 22:17
Themenfelder und Herausforderungen,Conversely, deformation can easily result in large changes of the pore structure (Paterson, 1978; Wong, 1990). Because transport properties of rocks, including permeability and electrical resistivity, are directly determined by the pore structure (Walsh, 1965; Simmons and Richter, 1976; Gangi, 1979;作者: impale 時間: 2025-3-24 05:07
Soziale und Politische Kognitionen,that polycrystalline materials containing a solution or partial melt phase within grain boundaries can deform by a process of fluid assisted diffusional creep or intergranular pressure solution creep (Durney, 1972; Stocker and Ashby, 1973; Robin, 1978; Raj, 1982; Pharr and Ashby, 1983; Rutter, 1983;作者: 大洪水 時間: 2025-3-24 07:55 作者: 思考而得 時間: 2025-3-24 12:58
Bernhard Ohlmeier,Andreas Brunoldases in clastic sedimentary rocks consist of mineral grains, rock fragments, and sometimes also amorphous material. Minerals precipitated after deposition are referred to as authigenic, and they fill the primary pore space or replace detrital grains. The fluid phases may consist of liquid phases lik作者: Defense 時間: 2025-3-24 16:23
Growth, Dissolution and Pattern Formation in Geosystems,librium. Familiar examples include the relatively slow growth of faceted mineral crystals, the much more rapid growth of dendritic snow crystals, and the formation of irregular and even spongy mineral grains during weathering near the earth’s surface. Growth and dissolution kinetics are controlled b作者: BLA 時間: 2025-3-24 19:54
Crystal Growth and Morphology: A Multi-Faceted Approach,he driving forces for growth are rather low — do indeed grow with flat faces. This phenomenon holds for crystals with very simple structures such as the cubic and hexagonal close-packed crystals of the elements helium, argon and krypton, growing at extremely low temperatures from their melts, and cr作者: Creatinine-Test 時間: 2025-3-24 23:32
Crystal Growth and Intracrystalline Zonation Patterns in Hydrothermal Environments,f ore minerals from hydrothermal fluids is responsible for the generation of the world’s most important class of ore deposits (Skinner, 1969). Hydrothermal systems also provide some of the most spectacular examples of naturally grown mineral ., which occasionally may reach a size of several centimet作者: Lipoma 時間: 2025-3-25 05:40
Branching and Oscillatory Patterns in Plagioclase and Mississippi-Valley Type Sphalerite Deposits,s, such as oscillatory zoning (in which the chemical composition fluctuates along a traverse within the crystal) or branching patterns (characterized by a tree-like crystal form) that arise spontaneously as a result of growth kinetics. Liesegang was among the first to investigate the kinetics of a c作者: faultfinder 時間: 2025-3-25 11:21
Numerical Modeling of Calcite Coarsening in the Aureoles of , Dikes: Analysis of the Kinetic Controon kinetics. Wallrocks may be sampled at the scale of individual beds from the intrusive contact to beyond the limit of metamorphism so that the progress of metamorphic processes may be traced from their inception to their completion. The superficially simple intrusion geometry of these dikes, appro作者: 側(cè)面左右 時間: 2025-3-25 12:55
Nonequilibrium Growth of Crystals from Supersaturated Solutions, under which they grew. Some crystals are faceted, for example quartz crystals; metal crystals often grow with smooth shapes, and salts and organic materials often grow with needle-like structures. Dendritic crystals, which are the subject of this paper, are also very common. Dendrites are crystals 作者: 注意力集中 時間: 2025-3-25 19:19
The Diffusion-Limited Aggregation Model and Geological Pattern Formation,me, to a growing cluster or aggregate of particles via random walk paths starting from outside of the region occupied by the cluster. In the most simple version of the model (Witten and Sander, 1981), a simulation is started by occupying a site in the center of a square or triangular lattice to repr作者: 思想流動 時間: 2025-3-25 22:40 作者: 開玩笑 時間: 2025-3-26 04:09 作者: 玩笑 時間: 2025-3-26 05:47
Biogenic Silica: A Model of Amorphous Structure Control, of minerals. Many silicates are also formed in combination with other elements such as magnesium, aluminium, calcium and iron and as such form many of the minerals in our rocks and soils. Weathering processes over millions of years have also resulted in the occurrence of silica (silicon dioxide) in作者: OATH 時間: 2025-3-26 08:56 作者: 泰然自若 時間: 2025-3-26 16:28 作者: 召集 時間: 2025-3-26 19:00
Surface Area of Primary Silicate Minerals,nerals, rate of growth of authigenic minerals, adsorption and desorption of metal and organic contaminants on soil and sediment grains, neutralization of acid deposition by weathering reactions, oxidation and reduction of mmetal-containing phases and solutes, clumping of colloids or bacteria by elec作者: Opponent 時間: 2025-3-26 20:56
Evolution of Pore Structure and Permeability of Rocks in Laboratory Experiments,Conversely, deformation can easily result in large changes of the pore structure (Paterson, 1978; Wong, 1990). Because transport properties of rocks, including permeability and electrical resistivity, are directly determined by the pore structure (Walsh, 1965; Simmons and Richter, 1976; Gangi, 1979;作者: ear-canal 時間: 2025-3-27 01:50 作者: 變白 時間: 2025-3-27 05:39 作者: anniversary 時間: 2025-3-27 09:34
An Overview of Factors Controlling Rates of Compaction, Fluid Generation and Flow in Sedimentary Baases in clastic sedimentary rocks consist of mineral grains, rock fragments, and sometimes also amorphous material. Minerals precipitated after deposition are referred to as authigenic, and they fill the primary pore space or replace detrital grains. The fluid phases may consist of liquid phases lik作者: aphasia 時間: 2025-3-27 13:46 作者: 旁觀者 時間: 2025-3-27 20:07
https://doi.org/10.1007/978-3-531-92268-3ence of faceted crystals also holds for almost all inorganic crystals grown in the laboratory and inorganic mineral crystals grown in nature. Examples are the very well known crystals of quartz, gypsum, pyrite, etc. Note that the occurrence of facets on crystals does not depend on the size of the cr作者: RECUR 時間: 2025-3-27 22:51
Ulrich von Alemann,Wolfgang T?nnesmannwhich allows the growing mineral to develop a shape that minimizes the surface energy of that particular grain, i.e. a faceted crystal. This is generally not the case in rocks with low porosity where the total surface energy of the whole society of grains (the rock) determines the shape of the indiv作者: 招募 時間: 2025-3-28 03:39 作者: Supplement 時間: 2025-3-28 08:05
https://doi.org/10.1007/978-3-322-88696-5upied by the random walker) is filled to represent the growth process. The process of launching random walkers from outside of the region occupied by the growing cluster and terminating them when they wander too far from the cluster or ‘sticking’ them to the growing cluster when they reach an occupi作者: 長矛 時間: 2025-3-28 10:49 作者: Licentious 時間: 2025-3-28 16:13
Ausgangsbedingungen der Politischen Bildung, the most difficult physical parameters to quantify in extrapolating from the laboratory to the soil plot to the watershed (White and Peterson, 1990). Most models of solute transport in aquifers and in soils simply ignore the mineral-water surface area term by combining it with the kinetic rate cons作者: Paradox 時間: 2025-3-28 18:45 作者: 字的誤用 時間: 2025-3-28 23:10 作者: Indicative 時間: 2025-3-29 03:25
Crystal Growth and Morphology: A Multi-Faceted Approach,ence of faceted crystals also holds for almost all inorganic crystals grown in the laboratory and inorganic mineral crystals grown in nature. Examples are the very well known crystals of quartz, gypsum, pyrite, etc. Note that the occurrence of facets on crystals does not depend on the size of the cr作者: epicondylitis 時間: 2025-3-29 08:45 作者: CREEK 時間: 2025-3-29 15:10 作者: Discrete 時間: 2025-3-29 16:59
The Diffusion-Limited Aggregation Model and Geological Pattern Formation,upied by the random walker) is filled to represent the growth process. The process of launching random walkers from outside of the region occupied by the growing cluster and terminating them when they wander too far from the cluster or ‘sticking’ them to the growing cluster when they reach an occupi作者: 乏味 時間: 2025-3-29 23:37
Structural Evolution of the Mineral Surface During Dissolution Probed with Synchrotron X-Ray Techni) and the epitaxial precipitation of otavite (CdCO.) on calcite (Chiarello and Sturchio, 1994) have been successfully completed .. Roughness of the surface is determined at the angstrom-scale and is a root mean square (r.m.s.) measure of the average peak to trough height of features on the surface. 作者: 一大塊 時間: 2025-3-30 03:00
Surface Area of Primary Silicate Minerals, the most difficult physical parameters to quantify in extrapolating from the laboratory to the soil plot to the watershed (White and Peterson, 1990). Most models of solute transport in aquifers and in soils simply ignore the mineral-water surface area term by combining it with the kinetic rate cons作者: Negotiate 時間: 2025-3-30 06:43
On Mechanisms and Kinetics of Creep by Intergranular Pressure Solution,ers and Ortoleva, 1989, 1990; Merino, 1992), pervasive intergranular pressure solution is an important deformation mechanism, manifested by many types of partially dissolved objects such as grains and fossils (Elliot, 1973; Rutter, 1976). It occurs under conditions ranging from diagenetic to greensc作者: entrance 時間: 2025-3-30 10:05
Surface Structural Controls on Trace Element Incorporation during Crystal Growth,作者: incarcerate 時間: 2025-3-30 14:08
Growth, Dissolution and Pattern Formation in Geosystems作者: inchoate 時間: 2025-3-30 18:52
Growth, Dissolution and Pattern Formation in Geosystems978-94-015-9179-9作者: IST 時間: 2025-3-30 22:26
Analytisch theoretischer Rahmen,ogic comes from the fact that metallurgists try to predict micrographic scale from given thermal conditions, whereas geologists would like, among other things, to estimate historical thermal conditions from observed patterning scales.作者: 啪心兒跳動 時間: 2025-3-31 02:11
Spontaneous Pattern Formation in Metallic and Ceramic Materials,ogic comes from the fact that metallurgists try to predict micrographic scale from given thermal conditions, whereas geologists would like, among other things, to estimate historical thermal conditions from observed patterning scales.作者: 痛苦一下 時間: 2025-3-31 05:21 作者: 規(guī)范要多 時間: 2025-3-31 12:58
https://doi.org/10.1007/978-3-658-10186-2d enstatite dissolution rates with solution composition and temperature, therefore, provides clues towards the effect of environmental changes on global climate. The dissolution of olivines and pyroxenes are also important buffers controlling surface water pH (Dreyer, 1988; Drever and Clow, 1995).作者: dandruff 時間: 2025-3-31 15:58
