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1-20 OF 108 RESULTS FOR
Nernst distribution law
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Journal Article
The use of thermodynamic excess functions in the Nernst distribution law; discussion and reply
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 October 1979
American Mineralogist (1979) 64 (9-10): 1122–1130.
... and constraints in applications of the Nernst distribution law to crystalline solutions. It is concluded that a strict accounting for the effects of crystal structure is required for a rigorous thermodynamic assessment of equilibria between coexisting, mutually-soluble crystalline solutions with different...
Journal Article
The use of thermodynamic excess functions in the Nernst distribution law
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 February 1978
American Mineralogist (1978) 63 (1-2): 83–86.
...N. B. Holst Abstract The Nernst distribution law, which is used by many authors in geology as the theoretical basis of geothermometry and trace-component distribution, is derived using excess functions. It is demonstrated that the free-energy term in the Nernst equation, as it is applied in many...
Journal Article
Disequilibrium Precipitation of Molluscan Skeletal Material and Its Implications Regarding the Use of Trace Elements in Fossil Shells as Paleoecological Indicators
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 March 1965
AAPG Bulletin (1965) 49 (3): 343.
... element distributions in other marine mollusks, indicates that molluscan skeletal material is not precipitated at equilibrium with coexisting sea water. Calculations demonstrate that the partitioning of minor elements between carbonate and sea water does not follow the Nernst distribution law...
Journal Article
Ca-Sr fractionation between zoisite, lawsonite, and aqueous fluids: An experimental study at 2.0 and 4.0 GPa/400 to 800 °C
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 May 2013
American Mineralogist (2013) 98 (5-6): 955–965.
... values of Δμ 0 = −9 kJ/mol and W Sr-Ca law Cmcm = 10 kJ/mol for orthorhombic and Δμ 0 = −10 kJ/mol and W Sr-Ca law P 21 /m = 11 kJ/mol for monoclinic lawsonite. Calculated Nernst distribution coefficients for the studied 1 M (Ca,Sr)Cl 2 aqueous fluids are D Sr zo-af = 2.8 ± 0.7 for zoisite at 2 GPa/600...
Journal Article
Subsolidus hydrogen partitioning between nominally anhydrous minerals in garnet-bearing peridotite
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 September 2017
American Mineralogist (2017) 102 (9): 1822–1831.
... concentration ratios are interpreted as mineral-to-mineral hydrogen partition coefficients (i.e., Nernst's law) for a garnet-peridotite assemblage. It yields, based on mineral-specific infrared calibrations, D Opx/Ol = 5 ± 1, D Cpx/Ol = 10 ± 2, and D Cpx/Opx = 1.9 ± 0.4. While D Cpx/Opx is in agreement (within...
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Calculated Sr-concentrations in coexisting zoisite and aqueous fluid ( a ) ...
in Ca-Sr fractionation between zoisite, lawsonite, and aqueous fluids: An experimental study at 2.0 and 4.0 GPa/400 to 800 °C
> American Mineralogist
Published: 01 May 2013
. The slope of these fits yields the Nernst distribution coefficients D Sr min−af with D Sr zo−af = 2.8 ± 0.7 and D Sr law−af = 0.6 ± 0.2.
Journal Article
Section 1. Introduction
Journal: Geochemical Perspectives
Publisher: European Association for Geochemistry
Published: 01 October 2016
Geochemical Perspectives (2016) 5 (2): 148–152.
...John H. Jones The Nernst partition coefficient D, which is wt. % concentration of element i in one phase normalised to the weight concentration of i in another phase ( Nernst, 1891 ). Typically, the numerator of this quotient will be a solid phase (α) and the denominator will be a liquid...
Journal Article
REVIEW AND COMPARISON OF SIMPLE TRANSFER AND EXCHANGE EQUILIBRIA
Journal: The Canadian Mineralogist
Publisher: Mineralogical Association of Canada
Published: 01 August 2005
The Canadian Mineralogist (2005) 43 (4): 1349–1354.
... element), quotient (12) becomes very nearly equal to the ratio X fs / X hd , which forms one expression of the Nernst distribution law ( Nernst 1904 ). The orthopyroxene – Ca pyroxene exchange equilibrium can be represented by a distribution diagram in which X fs is plotted against X hd...
Journal Article
Reactive Transport at the Crossroads
Publisher: Mineralogical Society of America
Published: 01 September 2019
Reviews in Mineralogy and Geochemistry (2019) 85 (1): 1–26.
... diffusion coefficients are the same (in which case Fick's Law is recovered if no ionic strength gradients are present). The Nernst–Planck equation has now been implemented in a number of reactive transport codes, including FLOTRAN, CrunchFlow, MIN3P, and PHREEQc ( Steefel et al. 2015 ). It was used...
Journal Article
Characterizing Unsaturated Diffusion in Porous Tuff Gravel
Journal: Vadose Zone Journal
Publisher: Soil Science Society of America
Published: 01 November 2004
Vadose Zone Journal (2004) 3 (4): 1425–1438.
... decrease in volumetric water content (cell basis). This is consistent with the unique behavior of water distribution in porous tuff, as discussed above. Extending the application of the Nernst–Einstein equation to diffusion in unsaturated porous media requires several assumptions. We first must...
Journal Article
2. THERMODYNAMICS AND THE KINETICS OF THERMOBAROMETRY: OVERVIEW
Journal: Geochemical Perspectives
Publisher: European Association for Geochemistry
Published: 01 April 2021
Geochemical Perspectives (2021) 10 (1): 31–40.
... (2.2) or its equivalent using wt. %, is known as the Nernst distribution law. Thus, a Roozeboom plot of the dilute species i (obeying Henry’s law) should define a line with constant slope and zero intercept. Figure 2.1c , which is reproduced from Kretz ( 1959 ), shows that the Nernst distribution...
Journal Article
HEATING Fe OXIDE-RICH SOILS INCREASES THE DISSOLUTION RATE OF METALS
Journal: Clays and Clay Minerals
Publisher: Clay Minerals Society
Published: 01 April 2006
Clays and Clay Minerals (2006) 54 (2): 165–175.
... Fe oxides follows more closely the modified Nernst equation ( Kabai, 1973 ) (Figure 4b , Table 3 ) than the cube root law (Figure 4a ). Hence, the cube root law will not be discussed further in this publication. Figure 4. Dissolution curves for samples derived from sample E2 by magnetic...
Journal Article
On charge accumulation in heterogeneous porous rocks under the influence of an external electric field
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 11 July 2013
Geophysics (2013) 78 (4): D271–D291.
...A. Revil ABSTRACT Electric polarization is described as the sum of charge accumulations (free charge density) and orientation of polar molecules such as those of bound and free water molecules (bound charge polarization). Charge accumulation in porous materials cannot be described with Ohm’s law...
Journal Article
Reactive Transport Modeling of Coupled Processes in Nanoporous Media
Publisher: Mineralogical Society of America
Published: 01 September 2019
Reviews in Mineralogy and Geochemistry (2019) 85 (1): 75–109.
... and dark gray are pore/solid mixtures and solids, respectively. C: Pore-width distribution obtained from a combination of bulk and microscopic characterization techniques. [Figure modified from Tournassat et al. (2016b) .] [email protected] ; [email protected] [email protected]...
Includes: Supplemental Content
Journal Article
THE URANINITE–PYRITE ASSOCIATION, A SENSITIVE INDICATOR OF CHANGES IN PALEOFLUID COMPOSITION: AN EXAMPLE FROM THE OHŘE (EGER) GRABEN, BOHEMIAN MASSIF, CZECH REPUBLIC
Journal: The Canadian Mineralogist
Publisher: Mineralogical Association of Canada
Published: 01 October 2008
The Canadian Mineralogist (2008) 46 (5): 1159–1172.
..., the distribution of a trace element A (in this study, arsenic and lead) and a major element M (in our case, uranium) between the fluid and the precipitating solid phase can be described by Nernst’s law: \batchmode \documentclass[fleqn,10pt,legalpaper]{article} \usepackage{amssymb} \usepackage{amsfonts...
Journal Article
Electrical conductivity of albite at high temperatures and high pressures
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 November 2011
American Mineralogist (2011) 96 (11-12): 1821–1827.
... bonded sodium cations, the dominant charge carriers, migrate into interstitial sites within the feldspar aluminosilicate framework. The Na diffusivity inferred from electrical conductivity of albite in this study using the Nernst-Einstein relation is consistent with that of previous studies on natural...
Journal Article
Mechanistic 3D finite-difference simulation of borehole spontaneous potential measurements
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 30 April 2020
Geophysics (2020) 85 (4): D105–D119.
...Joshua Bautista-Anguiano; Carlos Torres-Verdín; Joachim Strobel ABSTRACT The quantitative interpretation of borehole spontaneous potential (SP) measurements via Nernst’s equation often relies on limiting assumptions such as shallow mud-filtrate invasion, negligible streaming potentials, and uniform...
Journal Article
INDEX
Journal: Geochemical Perspectives
Publisher: European Association for Geochemistry
Published: 01 April 2021
Geochemical Perspectives (2021) 10 (1): 141–144.
... Nernst distribution 35, 49 Scott, Robert 46 GEOCHEMICAL PERSPECTIVES | J I B A M I T R A G A N G U LY 143 Seifert, Fritz 52, 135, 138 U Sharp, Zachary 89, 100, 138 Sikkim 58, 81, 89-91, 93, 131, 133 Urey, Harold 37, 38, 39, 51, 99, 139 Skinner, Brian 68, 138 solutions W ideal 32, 34, 40, 46, 71...
Journal Article
Aqueous Solubility of Zn Incorporated into Mg-Al-Layered Double Hydroxides
Journal: Clays and Clay Minerals
Publisher: Clay Minerals Society
Published: 01 February 2022
Clays and Clay Minerals (2022) 70 (1): 34–47.
... distribution law: 9 X Zn - LDH / 1 - X Zn - LDH = D Zn + / MgOH + 12 χ Zn , aq = Zn + / Zn + + MgOH + and: where the Berthelot–Nernst distribution coefficient D is given by: 10 D...
Includes: Supplemental Content
Journal Article
Ionic Transport in Nano-Porous Clays with Consideration of Electrostatic Effects
Publisher: Mineralogical Society of America
Published: 01 January 2015
Reviews in Mineralogy and Geochemistry (2015) 80 (1): 287–329.
...Christophe Tournassat; Carl I. Steefel (5) ∂ φ c i ∂ t = ∂ ∂ x ( D e , i ∂ c i ∂ x ) . The quantification of adsorption processes is commonly translated into distribution ratio values, Rd (L·kg −1 ): (7) R d i...
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