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2 edition of Thermodynamic properties of minerals and related substances at 298.15 K and 1 bar (10? pascals) pressure and at higher temperatures found in the catalog.

Thermodynamic properties of minerals and related substances at 298.15 K and 1 bar (10? pascals) pressure and at higher temperatures

Richard A. Robie

Thermodynamic properties of minerals and related substances at 298.15 K and 1 bar (10? pascals) pressure and at higher temperatures

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  • 8 Currently reading

Published by U.S. Dept. of the Interior, Geological Survey in Washington .
Written in English

    Subjects:
  • Minerals -- Tables.,
  • Thermodynamics -- Tables.

  • Edition Notes

    Includes bibliographical references (p. 428-446) and indexes.

    Statementby Richard A. Robie, Bruce S. Hemingway and James R. Fisher.
    GenreTables.
    SeriesGeological Survey bulletin -- 1452
    ContributionsHemingway, Bruce S., Fisher, James R. 1940-
    Classifications
    LC ClassificationsQE75 .B9 no. 1452, QE366.8 .B9 no. 1452
    The Physical Object
    Pagination456 p. ;
    Number of Pages456
    ID Numbers
    Open LibraryOL22608239M

      The databases of alkaline and alkaline earth sulfate solubilities in water at various temperatures were created using experimental data from the publications over about the last two centuries. and Fisher, J. R., Thermodynamic Properties of Minerals and Related Substances at K and 1 bar ( Pascals) Pressure and Higher Temperatures, Cited by: 6.


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Thermodynamic properties of minerals and related substances at 298.15 K and 1 bar (10? pascals) pressure and at higher temperatures by Richard A. Robie Download PDF EPUB FB2

@article{osti_, title = {Thermodynamic properties of minerals and related substances at 15 K and 1 bar (10/sup 5/ pascals) pressure and at higher temperatures}, author = {Robie, R.A. and Hemingway, B.S. and Fisher, J.R.}, abstractNote = {Selected values for the entropy (S/sup 0/), molar volume (v/sup 0/), and for the enthalpy and Gibbs free energy of formation .H/sub f.

Get this from a library. Thermodynamic properties of minerals and related substances at K and 1 bar (10⁵ pascals) pressure and at higher temperatures. [Richard A Robie; Bruce S Hemingway; James R Fisher; Geological Survey (U.S.)] -- A summary of the thermodynamic data for minerals at K together with calculated values for functions at temperatures up to 1, K.

Get this from a library. Thermodynamic properties of minerals and related substances at K and 1 bar (10⁵ pascals) pressure and at higher temperatures.

[Richard A Robie; Bruce S Hemingway; James R Fisher; Geological Survey (U.S.)] -- A summary of the thermodynamic data for minerals at K together with calculated values for the functions CP̊, T ̦[delta]Hf̊, T ̦[delta]Gf̊, T.

38 rows  Similar Items. Thermodynamic properties of minerals and related substances at K. Buy Thermodynamic Properties of Minerals and Related Substances at K and 1 Bar (10 Pascals Pressure and at Higher Temperatures) on FREE SHIPPING on qualified orders.

Book Review: Thermodynamic properties of minerals and related substances at k and 1 bar (10 5 pascals) pressure and at higher temperatures. Robie, B. Hemingway and J. Fisher, U.S. Geological Survey Bulletin, pp.

$Cited by: 7. Open Library is an open, editable library catalog, building towards a web page for every book ever published. Thermodynamic properties of minerals and related substances at K and 1 bar (10p5s by Richard A.

Robie,Dept. of the Interior, U.S. Geological Survey, For sale by the Supt. of Docs., U.S. G.P.O. edition, in English - Repr Pages: Robie, R.A. and Hemingway, B.S. () Thermodynamic Properties of Minerals and Related Substances at K and 1 Bar Pressure and at Higher Temperatures.

U.S. Geol. Survey, Washington DC, Bulletin Thermodynamic Properties of Minerals and Related Substances at K and 1 Bar ( Pascals) Pressure and at Higher Temperatures By RICHARD A.

RoBIE, BRuc•: S. HEMINGWAY, R. FisHER DEPARTMENT OF THE INTERIOR. Download the eBook Thermodynamic Properties of Minerals and Related Substances at K and 1 Bar ( Pascals) Pressure and at Higher Temperatures in PDF or EPUB format and read it directly on your mobile phone, computer or any device. Abstract.

A thermochemical study of natural apophyllite-group minerals, fluorapophyllite-(K) KCa 4 [Si 8 O 20]F ⋅ 8H 2 O (Maharashtra, India) (I) and hydroxyapophyllite-(K) KCa 4 [Si 8 O 20]OH ⋅ 8H 2 O (Norilsk, Russia) (II), was carried out on a high-temperature heat-flux Tian-Calvet Setaram (France) microcalorimeter using the melt solution calorimetry : L.

Ogorodova, L. Melchakova, M. Vigasina, Yu. Gritsenko, D. Ksenofontov, I. Bryzga. R. Robie and B. Hemingway, “Thermodynamic Properties of Minerals and Related Substances at K and 1 Bar (10 5 Pascals) Pressure and at Higher Temperatures,” U.S.

Geol. Surv. Bull, No. ().Cited by: 6. The book is divided into five parts that discuss structure and bonding within minerals; mineral physics and optical properties; modes of mineral formation and thermodynamics; mineral groups within the context of mineral-forming environments; and the application of mineralogy for the exploitation of metal deposits, gems, and by: Selected values for the entropy (So), molar volume (Vo), and for the enthalpy and Gibbs energy of formation (ΔfHo and ΔfGo) are given for 50 reference elements, 55 sulfides, 93 oxides and.

Six thermodynamic compilations that include the thermodynamic properties for baryte, free barium and sulfate ions at standard conditions (1 bar, K and assuming unit activity and 1 molal ionic strength) are summarized in Table 1 (all uncertainties in this work are reported with two standard deviations).

All these data sets were derived from experimental and theoretical studies, where the Cited by: 3. Thermodynamic properties can be derived from equilibrium achieved under high-temperature (HT) and high-pressure (HP) conditions (Holland and Powell, ; Vidal et al., ).This process has many advantages, such as a drastic decrease in the time required to reach equilibrium; it avoids analyzing the composition of an aqueous phase and makes it easier to reach equilibrium from reversal.

Thermodynamic data. Thermodynamic data is usually presented as a table or chart of function values for one mole of a substance (or in the case of the steam tables, one kg).

A thermodynamic datafile is a set of equation parameters from which the numerical data values can be calculated. Tables and datafiles are usually presented at a standard pressure of 1 bar or 1 atm, but in the case of steam. Shareable Link. Use the link below to share a full-text version of this article with your friends and colleagues.

Learn more. Improving Internal Consistency of Standard State Thermodynamic Data for Sulfate Ion, Portlandite, Gypsum, Barite, Celestine, and Associated Ions mi nerals and related substances at K Author: Darrell Kirk Nordstrom.

Thermodynamic Properties of Minerals and Related Substances at K and 1 bar (10⁵ Pascals) Pressure and at Higher Temperatures Thermophysical Properties of Carbon Dioxide QDC1 V (Geisel 1 Author: Teri Vogel.

The quantum-chemical calculations over the temperature range of 10– K resulted in obtaining the values of the following thermodynamic functions of the mineral: the heat capacity ( J mol −1 K −1 at K) and enthalpy change ( J mol −1 at K). Calculation of thermodynamic properties of celestine by LADYCited by: 4.

Calcium titanate is an inorganic compound with the chemical formula Ca Ti O 3. As a mineral, it is called perovskite, named after Russian mineralogist, L. Perovski (). It is a colourless, diamagnetic solid, although the mineral is often coloured owing to ance: white powder.

Evaluation of irreversible reactions in geochemical processes involving minerals and aqueous solutions – I. Thermodynamic relations. Geochimica et Cosmochimica Acta, 32, – Helgeson, H.C.

().Cited by: Dielectric properties of water and Debye-Hueckel parameters to °C and 1 kbar: Journal of Physical Chemistry, v.

83, p. Carpenter, A.B.,Origin and chemical evolution of brines in sedimentary basins: Oklahoma Geological Survey Circu p.

Choose the system as 1 mol of air, contained in an imaginary frictionless piston/cylinder arrangement. For R= J mol-1K, C V = C P =J mol-1 K-1 The initial and final conditions of the air are identical with those of Ex.1, where the molar volumes are given as: V 1 = V 2 =m3 Moreover, since the initial and finalFile Size: KB.

Row 1. Molar mass of species, density at K, ΔH° formS° and the upper temperature limit for the file. Row 2. Number of C p equations required. Here, three because of three species phases.

Row 3. Values of the five parameters for the first C p equation; temperature limit for the equation. Row 4. Stability of AuCl 2 − from 25 to °C at Pressures to bar and Consequences for Hydrothermal Gold Mobilization.

by Alexander V. Zotov, B.S. Thermodynamic Properties of Minerals and Related Substances at K and 1 bar (10 5 Pascals) Cited by: 6. Abstract. Earth scientists in search of thermodynamic data are faced with questions as to the quality and reliability of their finds.

Analysis of the currently available thermodynamic data bases for minerals reveals discrepancies of form and of contents, both of which complicate the quality differences render comparisons of properties among different data bases cumbersome at Cited by: A relevant research effort is devoted to the synthesis and characterization of phases belonging to the ternary system Cu–Sn–S, mainly for their possible applications in semiconductor technology.

Among all ternary phases, kuramite, Cu3SnS4, mohite, Cu2SnS3, and Cu4Sn7S16 have attracted the highest interest. Numerous studies were carried out claiming for the description of new phases in the Cited by: 6.

Thermodynamic properties of minerals and related substances at K and 1 bar (10⁵ pascals) pressure and at higher temperatures [] Robie, Richard A., Washington: U.S. G.P.O. ; Denver, CO: For sale by U.S. Geological Survey, Information Services, The thermodynamic properties of schoepite and metaschoepite were obtained by means of theoretical solid-state methods as a function of temperature.

Since the values of these properties for schoepite have not been measured experimentally, they were predicted. The computed thermodynamic functions of metaschoepite were in excellent agreement with the experimental by: 8.

Robie R. A., Hemingway B. Thermodynamic Properties of Minerals and Related Substances at 15 K and 1 bar ( Pascals) Pressure and at Higher Temperatures. USGS Geol. Survey Bulletin Lothenbach B., Winnefeld, F. Thermodynamic modelling of the hydration of Portland. Thermodynamic properties of minerals and related substances at K and 1 bar (10⁵ pascals) pressure and at higher temperatures Published Other Authors: '; “.

K'\n Superscript ° K. Superscript SER Equilibrium constant for the formation of the compounds from their elements in conventional reference states Conventional standard state — 1 bar, temperature of interest, most stable form of the element at that temperature of interest Standard Element Reference State — 1 bar, K, most stable.

Thermodynamic Properties of Minerals and Related Substances at K and 1 Bar ( Pascals) Pressure and at Higher Temperatures. Robie R.A., Hemingway B.S., Fisher J.R. Language: english. File: PDF, MB.

Post a Review You can write a book review and share your experiences. Other readers will always be interested in your opinion of. The standard state of a substance does not have to exist in nature: for example, it is possible to calculate values for steam at K and 10 5 Pa, although steam does not exist (as a gas) under these conditions.

The advantage of this practice is that tables of thermodynamic properties prepared in this way are self-consistent. R.A. Robie, B.S. Hemingway, J.R. Fisher: Thermodynamic Properties of Minerals and Related Substances at K and 1 bar ( Pascals) Pressure and at Higher Temperatures, US Geol.

Surv. Bul. () p. [28]. The basis of thermodynamic theory [] is known since the end of the nineteenth century, and the fundamental developments carried out in the twentieth century have established this theory as a self-contained system of thermodynamic calculations are mainly used for the description of the changes of state associated with the transfer of matter and energy and are an indispensable part Cited by: 3.

Template:Cleanup {{#invoke:Sidebar |collapsible | bodyclass = plainlist | titlestyle = padding-bottomem;border-bottom:1px solid #aaa; | title = Thermodynamics. Rard, J. and Archer, D. “ Isopiestic investigation of the osmotic and activity coefficients of aqueous NaBr and the solubility of NaBr2H 2 O(cr) at K: Thermodynamic properties of the NaBr + H 2 O system over wide ranges of temperature and pressure,” J.

Chem. Eng. D – ().Cited by: 6. This book is intended to serve as a text for an introductory course in geochemistry for undergraduate/graduate students with at least an elementary-level background in earth sciences, chemistry, and mathematics. ( K, 1 bar) thermodynamic data table and a listing of answers to selected chapter-end questions.

Additional resources for.Geotermobarometría: Referencias [Introducción] J. R. () Thermodynamic properties of minerals and related substances at K and 1 bar (10 5 pascals) pressure and at higher temperatures. U.S. Geological Survey Bulletin,p.Thermodynamic Properties of Minerals and Related Substances at K and 1 Bar (10 5 Pascals) Pressure and at Higher Temperatures.

Washington, D. C.: U. .