Results 301 to 310 of about 264,999 (349)
Some of the next articles are maybe not open access.
1996
Buffers are reactions that at least temporarily resist change to some aspect of a Fluid’s chemistry. A pH buffer, for example, holds pH to an approximately constant value, opposing processes that would otherwise drive the solution acid or alkaline.
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Buffers are reactions that at least temporarily resist change to some aspect of a Fluid’s chemistry. A pH buffer, for example, holds pH to an approximately constant value, opposing processes that would otherwise drive the solution acid or alkaline.
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1996
To this point we have measured reaction progress parametrically in terms of the reaction progress variable ξ, which is dimensionless. When in Chapter 11 we reacted feldspar with water, for example, we tied reaction progress to the amount of feldspar that had reacted and expressed our results along that coordinate.
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To this point we have measured reaction progress parametrically in terms of the reaction progress variable ξ, which is dimensionless. When in Chapter 11 we reacted feldspar with water, for example, we tied reaction progress to the amount of feldspar that had reacted and expressed our results along that coordinate.
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The processing methods of geochemical exploration data: past, present, and future
Applied Geochemistry, 2021Renguang Zuo
exaly
1994
Abstract The usefulness of geochemical modeling in diagenesis lies in the ability to analyze processes that cannot be measured directly in the laboratory, either due to the time element (slow kinetics) or, more typically, metastable equilibria.
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Abstract The usefulness of geochemical modeling in diagenesis lies in the ability to analyze processes that cannot be measured directly in the laboratory, either due to the time element (slow kinetics) or, more typically, metastable equilibria.
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Geochemical rate models: an introduction to geochemical kinetics
Choice Reviews Online, 2014openaire +1 more source