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Serpentinization is the change in mineralogy, usually of mafic and ultramafic rocks such as periodites and dunites, through the oxidation and hydrolysis of minerals (such as olivines), forming serpentine, brucite and magnetite. So calculate the value of the serpentinization reaction below

Serpentinization is the change in mineralogy, usually of mafic and ultramafic rocks such as periodites and dunites, through the oxidation and hydrolysis of minerals (such as olivines), forming serpentine, brucite and magnetite. So calculate the value of the serpentinization reaction below

Introduction to Chemical Engineering Thermodynamics
Introduction to Chemical Engineering Thermodynamics
8th Edition
ISBN:9781259696527
Author:J.M. Smith Termodinamica en ingenieria quimica, Hendrick C Van Ness, Michael Abbott, Mark Swihart
Publisher:J.M. Smith Termodinamica en ingenieria quimica, Hendrick C Van Ness, Michael Abbott, Mark Swihart
Chapter1: Introduction
Section: Chapter Questions
Problem 1.1P
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Serpentinization is the change in mineralogy, usually of mafic and ultramafic rocks such as periodites and dunites, through the oxidation and hydrolysis of minerals (such as olivines), forming serpentine, brucite and magnetite. So calculate the value of the serpentinization reaction below:

+ SiO2(aq) sílica aquosa 3 Mg2 SiO4(s) + 4 H2 0(1) → 2 Mg3 Siz Os(s)(OH)4(s) serpentina (crisotila) forsterita com base nas entalpias padrão de formação: Composto Mg2 SiO4(s) SiO2(aq) H20(I) Mg3 Siz Os (s)(OH)4(s) AH; (kJ mol-1) -2173,6 -876,9 -285,8 -4360,3
Transcribed Image Text:+ SiO2(aq) sílica aquosa 3 Mg2 SiO4(s) + 4 H2 0(1) → 2 Mg3 Siz Os(s)(OH)4(s) serpentina (crisotila) forsterita com base nas entalpias padrão de formação: Composto Mg2 SiO4(s) SiO2(aq) H20(I) Mg3 Siz Os (s)(OH)4(s) AH; (kJ mol-1) -2173,6 -876,9 -285,8 -4360,3
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