Limit this search to....

Pore Scale Geochemical Processes
Contributor(s): Steefel, Carl (Editor), Emmanuel, Simon (Editor), Anovitz, Lawrence (Editor)
ISBN: 0939950960     ISBN-13: 9780939950966
Publisher: de Gruyter
OUR PRICE:   $47.50  
Product Type: Paperback - Other Formats
Published: November 2016
Qty:
Additional Information
BISAC Categories:
- Science | Earth Sciences - Mineralogy
Dewey: 549.2
LCCN: 2016304722
Series: Reviews in Mineralogy and Geochemistry
Physical Information: 1" H x 6.14" W x 9.21" (1.52 lbs) 495 pages
 
Descriptions, Reviews, Etc.
Publisher Description:
This RiMG (Reviews in Mineralogy & Geochemistry) volume includes contributions that review experimental, characterization, and modeling advances in our understanding of pore-scale geochemical processes. The volume had its origins in a special theme session at the 2015 Goldschmidt Conference in Prague. From a diversity of pore-scale topics that ranged from multi-scale characterization to modeling, this work summarizes the state-of-the-science in this subject. Topics include: modification of thermodynamics and kinetics in small pores. chemo-mechanical processes and how they affect porosity evolution in geological media. small angle neutron scattering (SANS) techniques. how isotopic gradients across fluid-mineral boundaries can develop and how these provide insight into pore-scale processes. Information on an important class of models referred to as "pore network" and much more. The material in this book is accessible for graduate students, researchers, and professionals in the earth, material, environmental, hydrological, and biological sciences. The pore scale is readily recognizable to geochemists, and yet in the past it has not received a great deal of attention as a distinct scale or environment that is associated with its own set of questions and challenges. Is the pore scale merely an environment in which smaller scale (molecular) processes aggregate, or are there emergent phenomena unique to this scale? Is it simply a finer-grained version of the "continuum" scale that is addressed in larger-scale models and interpretations? The scale is important because it accounts for the pore architecture within which such diverse processes as multi-mineral reaction networks, microbial community interaction, and transport play out, giving rise to new geochemical behavior that might not be understood or predicted by considering smaller or larger scales alone.