作者: bronchiole 時間: 2025-3-21 21:40 作者: 落葉劑 時間: 2025-3-22 02:08 作者: 他很靈活 時間: 2025-3-22 06:07
,Abkürzungen und Formelzeichnen,f time and space, most such processes are not accessible to direct observation, but they can be reconstructed by deciphering the physicochemical frameworks of formation of rocks and mineral deposits which formed in response to them. Supposing the observed mineral assemblage preserved in a rock recor作者: forthy 時間: 2025-3-22 09:51 作者: Painstaking 時間: 2025-3-22 13:04 作者: Mobile 時間: 2025-3-22 18:32
,L?ndergruppen und Entwicklungspfade, without a pure fluid or a fluid mixture. Yet another subject, which can be handled at the present stage, is the derivation of an internally consistent thermodynamic database, which is indispensable for obtaining a geologically reliable phase diagram. However, the computation of the phase relations 作者: OREX 時間: 2025-3-22 22:56 作者: ENNUI 時間: 2025-3-23 04:48
https://doi.org/10.1007/978-3-642-77665-6t is also geologically relevant, because the natural fluids are mixtures of a number of species including H.O, CO., CH., etc. The computation of the mixed-volatile equilibria demands that the thermodynamic properties of the fluid mixtures be known. Accordingly, research work on the equations of stat作者: 高度贊揚 時間: 2025-3-23 06:27 作者: 蝕刻術(shù) 時間: 2025-3-23 13:46 作者: dapper 時間: 2025-3-23 15:19 作者: Cardioversion 時間: 2025-3-23 18:16 作者: 傳染 時間: 2025-3-24 01:11
978-3-540-53215-6Springer-Verlag Berlin Heidelberg 1991作者: 混雜人 時間: 2025-3-24 04:33 作者: Flavouring 時間: 2025-3-24 09:27
Measurement, Evaluation, and Tabulation of Thermodynamic Properties,ia. Thermodynamic data tables, in vogue today, fall into two categories. The first of these seeks to deal with ., drawing heavily on calorimetric (and a few electrochemical cell) measurements. The compilation of thermodynamic data of minerals and related substances by Robie et al. (1979) belongs to 作者: 伴隨而來 時間: 2025-3-24 14:05 作者: Harpoon 時間: 2025-3-24 16:38 作者: 畸形 時間: 2025-3-24 22:48 作者: NOVA 時間: 2025-3-24 23:43
Phase Relations Among End-Member Solids and a Binary Fluid Mixture,t is also geologically relevant, because the natural fluids are mixtures of a number of species including H.O, CO., CH., etc. The computation of the mixed-volatile equilibria demands that the thermodynamic properties of the fluid mixtures be known. Accordingly, research work on the equations of stat作者: Acetabulum 時間: 2025-3-25 06:16
Derivation of an Internally Consistent Thermodynamic Dataset by Mathematical Programming,amic dataset based . on calorimetry seldom allows computation of phase diagrams sufficiently accurate for geochemical applications. Nevertheless, calorimetry is, and will remain, the fundamental source of thermodynamic data, even if such data need to be fine-tuned for further use. The preceding chap作者: 嚴(yán)厲批評 時間: 2025-3-25 08:30 作者: infantile 時間: 2025-3-25 11:45
Phase Equilibria Involving Nonideal Solutions and Outlines of Geothermometry and Geobarometry,l potentials of the components in any phase, solid or fluid, are readily computed at any pressure, temperature, and composition. The knowledge of the chemical potentials sets the stage for the computation of phase diagrams comprising nonideal solutions. A phase diagram predicted from thermodynamic d作者: avulsion 時間: 2025-3-25 17:22
Phase Relations Among End-Member Solids and a Binary Fluid Mixture,e of the fluid mixtures of relevance to geochemistry has been a centerpiece of activity for about a decade (Holloway 1977; Jacobs and Kerrick 1981a,b; Kerrick and Jacobs 1981; Bowers and Helgeson 1983; Saxena and Fei 1988). The availability of these data has promoted our ability to predict mixed-volatile reactions with confidence.作者: 艦旗 時間: 2025-3-25 22:15
Thermodynamics of Crystalline Solutions,s. Our treatment focuses on the thermodynamics of simple crystalline solutions (defined below). Its extension to complex crystalline solutions will be somewhat cursory, and order-disorder phenomena, observed in numerous minerals, will be barely touched. Readers interested in such topics may find the monograph by Ganguly and Saxena (1987) helpful.作者: ABYSS 時間: 2025-3-26 00:46
,Abkürzungen und Formelzeichnen,of their equilibration. What thermodynamics cannot do is to tell us how long a quenched mineral assemblage is likely to survive once it is outside its field of stability, or what the mechanism of a certain mineral reaction will be. Such questions — geologically of equal importance — can be answered by kinetics, a subject not treated in this book.作者: 進(jìn)步 時間: 2025-3-26 07:09 作者: 危機 時間: 2025-3-26 09:25 作者: HACK 時間: 2025-3-26 16:38
Derivation of an Internally Consistent Thermodynamic Dataset by Mathematical Programming,etry must give us a thermodynamic dataset best suited to accomplish our goal of computing precise phase diagrams. A thermodynamic dataset, compatible with calorimetry and reaction reversals alike, is called an internally consistent thermodynamic dataset.作者: CANON 時間: 2025-3-26 19:30 作者: Expertise 時間: 2025-3-26 21:46
,L?ndergruppen und Entwicklungspfade,t thermodynamic database, which is indispensable for obtaining a geologically reliable phase diagram. However, the computation of the phase relations involving crystalline solutions, a topic of fundamental interest to geology, must be deferred until the thermodynamics of crystalline solutions is introduced in Chapter 8.作者: 浮雕 時間: 2025-3-27 04:43
https://doi.org/10.1007/978-3-322-93473-4multicomponent systems (Chap. 9). The objective of this chapter is to calculate phase relations between mineral end-members and a pure fluid, such as water or oxygen. Other fluids will be amenable to treatment in an analogous manner.作者: crescendo 時間: 2025-3-27 07:13
Phase Relations among End-Member Solids,t thermodynamic database, which is indispensable for obtaining a geologically reliable phase diagram. However, the computation of the phase relations involving crystalline solutions, a topic of fundamental interest to geology, must be deferred until the thermodynamics of crystalline solutions is introduced in Chapter 8.作者: 阻止 時間: 2025-3-27 11:34 作者: 偽證 時間: 2025-3-27 16:39
https://doi.org/10.1007/978-3-642-77665-6e of the fluid mixtures of relevance to geochemistry has been a centerpiece of activity for about a decade (Holloway 1977; Jacobs and Kerrick 1981a,b; Kerrick and Jacobs 1981; Bowers and Helgeson 1983; Saxena and Fei 1988). The availability of these data has promoted our ability to predict mixed-volatile reactions with confidence.作者: 革新 時間: 2025-3-27 21:22 作者: 束縛 時間: 2025-3-27 22:34 作者: 暖昧關(guān)系 時間: 2025-3-28 05:01
Konzepte fuzzybasierter Leitkomponenten,es in those three chapters will reveal to us the perils of depending exclusively on such data, and urge us to develop the internally consistent thermodynamic database, which is achieved by a simultaneous treatment of the calorimetric . phase equilibria measurements. One of the methods of deriving in作者: synovitis 時間: 2025-3-28 09:19 作者: induct 時間: 2025-3-28 12:23 作者: JEER 時間: 2025-3-28 17:26
Phase Equilibria Involving Nonideal Solutions and Outlines of Geothermometry and Geobarometry,ct the condition of equilibrium. The extraction of the temperature of equilibration is geothermometry; geobarometry is the calculation of the pressure of equilibrium for any assemblage. Because the T and P of solid-solid reactions are independent of the activity or fugacity of fluids prevalent durin作者: fiscal 時間: 2025-3-28 21:17 作者: 文字 時間: 2025-3-29 00:40
as helped put mineralogy and petrology on a firm quantitative basis. In the wake of these developments, academic curricula now require the students of geology to take a course in basic thermodynamics, traditionally offered by the departments of chemistry. Building on that foundation, a supplementary course is978-3-540-53215-6978-3-662-02716-5作者: 生意行為 時間: 2025-3-29 07:07
10樓作者: 用肘 時間: 2025-3-29 08:42
10樓作者: minimal 時間: 2025-3-29 14:26
10樓
