Geochemical and Biogeochemical Reaction ModelingThis book provides a comprehensive overview of reaction processes in the Earth's crust and on its surface, both in the laboratory and in the field. A clear exposition of the underlying equations and calculation techniques is balanced by a large number of fully worked examples. The book uses The Geochemist's Workbench® modeling software, developed by the author and already installed at over 1000 universities and research facilities worldwide. Since publication of the first edition, the field of reaction modeling has continued to grow and find increasingly broad application. In particular, the description of microbial activity, surface chemistry, and redox chemistry within reaction models has become broader and more rigorous. These areas are covered in detail in this new edition, which was originally published in 2007. This text is written for graduate students and academic researchers in the fields of geochemistry, environmental engineering, contaminant hydrology, geomicrobiology, and numerical modeling. |
From inside the book
Results 1-5 of 38
Page i
... find increasingly broad application. In particular, the description of microbial activity, surface chemistry, and redox chemistry within reaction models has become broader and more rigorous. Reaction models are commonly coupled to ...
... find increasingly broad application. In particular, the description of microbial activity, surface chemistry, and redox chemistry within reaction models has become broader and more rigorous. Reaction models are commonly coupled to ...
Page xvii
... find that the programs allow us to try fresh approaches to teaching aqueous geochemistry . Once a student can reliably balance reactions by hand , the task quickly becomes a chore . After calculating a few Eh - pH diagrams , what does ...
... find that the programs allow us to try fresh approaches to teaching aqueous geochemistry . Once a student can reliably balance reactions by hand , the task quickly becomes a chore . After calculating a few Eh - pH diagrams , what does ...
Page 1
... find solutions. The field of geochemical modeling has grown rapidly since the early 1960s, when the first attempt was made to predict by hand calculation the concentrations of dissolved species in seawater. Today's challenges might be ...
... find solutions. The field of geochemical modeling has grown rapidly since the early 1960s, when the first attempt was made to predict by hand calculation the concentrations of dissolved species in seawater. Today's challenges might be ...
Page 9
... find that the water is supersatu- rated with respect to one or more minerals. The calculation predicts that the water exists in a metastable state because the reactions to precipitate these minerals have not progressed to equilibrium ...
... find that the water is supersatu- rated with respect to one or more minerals. The calculation predicts that the water exists in a metastable state because the reactions to precipitate these minerals have not progressed to equilibrium ...
Page 11
... find if it is to follow a reaction path. By allowing supersaturated minerals to precipitate, accounting for any min- erals that dissolve as others precipitate, the model determines the stable mineral assemblage and corresponding fluid ...
... find if it is to follow a reaction path. By allowing supersaturated minerals to precipitate, accounting for any min- erals that dissolve as others precipitate, the model determines the stable mineral assemblage and corresponding fluid ...
Contents
7 | |
29 | |
Solving for the equilibrium state | 53 |
Changing the basis | 71 |
6 | 73 |
7 | 101 |
8 | 111 |
Sorption and ion exchange | 137 |
Reactive transport | 301 |
Hydrothermal fluids | 319 |
Geothermometry | 341 |
Evaporation | 357 |
Sediment diagenesis | 373 |
Kinetics of waterrock interaction | 387 |
Weathering | 405 |
Oxidation and reduction | 415 |
10 | 155 |
11 | 166 |
12 | 181 |
Mass transfer | 193 |
Polythermal fixed and sliding paths | 201 |
Geochemical buffers | 217 |
Kinetics of dissolution and precipitation | 231 |
Redox kinetics | 245 |
Microbial kinetics | 257 |
Stable isotopes | 269 |
Transport in flowing groundwater | 285 |
Waste injection wells | 427 |
Petroleum reservoirs | 435 |
Acid drainage | 449 |
Contamination and remediation | 461 |
Microbial communities | 471 |
Sources of modeling software | 485 |
Evaluating the HMW activity model | 491 |
Minerals in the LLNL database | 499 |
Nonlinear rate laws | 507 |
Index | 536 |
Other editions - View all
Common terms and phrases
acid activity coefficients albite anhydrite aqueous species aquifer assume basis species Bethke brine buffer Ca++ CaCC CaCO3 calcite calculation results carbonate CaSO4 CH3COO Chapter chemical CO2 fugacity component composition concentration cont’d contains Cosmochimica Acta cristobalite dispersion dissolution dissolved dolomite electron equilibrium constant example Fe++ ferric fluid fluorite formation free cm3 fugacity geochemical modeling geochemistry Geochimica et Cosmochimica governing equations groundwater groundwater flow HCO3 hematite hydrothermal initial ionic strength isotopic iteration kaolinite kinetic methanogens mg/kg Mg++ microbial minerals molal mole numbers muscovite NaCl oxidation oxygen precipitate predicted procedure produce pyrite quartz rate constant rate law rate_con react reactant reaction modeling reaction path reactive transport redox reactions saturation seawater sediment silica simulation SiO2 SiO2(aq solution sorbing sorption step sulfate sulfide supersaturated surface complexation swap temperature thermodynamic tridymite umolal undersaturated
Popular passages
Page 379 - ... present day because erosion has reduced the elevation of the basin's western margin. Paleohydrologic models calculated for the basin (Lee and Bethke, 1994) suggest that in the Eocene groundwater flowed eastward through the Lyons at an estimated discharge of about 1 m/yr. Flow in the Pennsylvania!! Fountain formation, a sandstone aquifer that underlies the Lyons and is separated from it by an aquitard complex, was more restricted because the formation grades into less permeable dolomites and evaporites...