text: Multiphase fluid flow and subsequent geochemical transport invariably saturated fractured rocks: 1. Approaches - Digital Library
  Reactive fluid flow and geochemical transport in unsaturated fractured rocks has received increasing attention for studies of contaminant transport, groundwater quality, waste disposal, acid mine drainage remediation, mineral deposits, sedimentary diagenesis, and fluid-rock interactions in hydrothermal systems. This paper presents methods for modeling geochemical systems that emphasize: (1) involvement of the gas phase in addition to liquid and solid phases in fluid flow, mass transport and chemical reactions, (2) treatment of physically and chemically heterogeneous and fractured rocks, (3) the effect of heat on fluid flow and reaction properties and processes, and (4) the kinetics of fluid-rock interaction. The physical ... continued below
  Xu, Tianfu & Pruess, Karsten August 8, 2000.
  Report No.: LBNL--45507
  DOI: 10.2172/926879 | External Link
  Office of Scientific & Technical Information Report Number: 926879
  Archival Resource Key: ark:/67531/metadc902822
  Xu, Tianfu & Pruess, Karsten. Multiphase fluid flow and subsequent geochemical transport invariably saturated fractured rocks: 1. Approaches, report, August 8, 2000; Berkeley, California. (digital.library.unt.edu/ark:/67531/metadc902822/: accessed January 17, 2019), University of North Texas Libraries, Digital Library, digital.library.unt.edu; crediting UNT Libraries Government Documents Department.