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9783540241959

Groundwater Geochemistry

by ; ;
  • ISBN13:

    9783540241959

  • ISBN10:

    3540241957

  • Edition: CD
  • Format: Hardcover
  • Copyright: 2005-04-15
  • Publisher: Springer Verlag
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Supplemental Materials

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Summary

The 2nd edition of "Groundwater Geochemistry a?? A practical guide to modeling of natural and contaminated aquatic systems" remains the comprehensive text book offering beginners and advanced modellers alike a minimum theoretical background and a strong focus on the practical solution of geochemical modeling with PHREEQC. The new edition covers the possibility to use PITZER equation and the CD music concept within the new version of PHREEQC. Examples for reactive transport use PHREEQCA's 1d features with multicomponent diffusion as well as PHAST with the graphical user interface GoPhast on 2d and 3d examples. Implementing uncertainties of thermodynamically data is addressed by means of the program Ljungskile. As in the 1st edition, detailed descriptions on how to solve each problem step by step guide the user from basic to more and more advanced hydrogeochemical modelling.

Author Biography

Broder J. Merkel was offered the chair of hydrogeology at the Technische Universitat Bergakademie Freiberg in 1993.

Table of Contents

Theoretical Background
1(66)
Equilibrium reactions
1(48)
Introduction
1(3)
Thermodynamic fundamentals
4(1)
Mass action law
4(2)
Gibbs free energy
6(1)
Gibbs phase rule
7(1)
Activity
8(1)
Ionic strength
8(2)
Calculation of activity coefficient
10(1)
Theory of ion dissociation
10(2)
Theory of ion interaction
12(2)
Theories of ion dissociation and ion interaction
14(3)
Interactions at the liquid-gaseous phase boundary
17(1)
Henry-Law
17(1)
Interactions at the liquid-solid phase boundary
18(1)
Dissolution and precipitation
18(1)
Solubility product
18(2)
Saturation index
20(2)
Limiting mineral phases
22(2)
Sorption
24(1)
Hydrophobic /hydrophilic substances
24(1)
Ion exchange
24(6)
Mathematical description of the sorption
30(4)
Interactions in the liquid phase
34(1)
Complexation
34(2)
Redox processes
36(1)
Measurement of the redox potential
36(1)
Calculation of the redox potential
37(4)
Presentation in predominance diagrams
41(4)
Redox buffer
45(1)
Significance of redox reactions
46(3)
Kinetics
49(8)
Kinetics of various chemical processes
49(1)
Half-life
49(1)
Kinetics of mineral dissolution
50(1)
Calculation of the reaction rate
51(1)
Subsequent reactions
52(1)
Parallel reactions
53(1)
Controlling factors on the reaction rate
53(2)
Empiric approaches for kinetically controlled reactions
55(2)
Reactive mass transport
57(10)
Introduction
57(1)
Flow models
57(1)
Transport models
57(1)
Definition
57(1)
Idealized transport conditions
58(2)
Real transport conditions
60(1)
Exchange within double-porosity aquifers
61(2)
Numerical methods of transport modeling
63(1)
Finite-difference / finite-element method
63(2)
Coupled methods
65(2)
Hydrogeochemical Modeling Programs
67(44)
General
67(17)
Geochemical algorithms
67(2)
Programs based on minimizing free energy
69(1)
Programs based on equilibrium constants
70(1)
PHREEQC
70(2)
EQ 3/6
72(1)
Comparison PHREEQC - EQ 3/6
73(3)
Thermodynamic data sets
76(1)
General
76(2)
Structure of thermodynamic data sets
78(2)
Problems and sources of error in geochemical modeling
80(4)
Use of PHREEQC
84(27)
Structure of PHREEQC under the Windows surface
84(1)
Input
85(8)
Thermodynamic data
93(1)
Output
94(1)
Grid
95(1)
Chart
95(1)
Introductory Examples for PHREEQC Modeling
95(1)
Equilibrium reactions
95(1)
Example 1: Standard output -- seawater analysis
96(2)
Example 2 equilibrium -- solution of gypsum
98(1)
Introductory examples for kinetics
99(1)
Defining reaction rates
100(3)
Basic within PHREEQC
103(3)
Introductory example for reactive mass transport
106(5)
Exercises
111(32)
Equilibrium reactions
112(18)
Groundwater - Lithosphere
112(1)
Standard-output well analysis
112(1)
Equilibrium reaction - solubility of gypsum
113(1)
Disequilibrium reaction - solubility of gypsum
113(1)
Temperature dependency of gypsum solubility in well water
113(1)
Temperature dependency of gypsum solubility in distilled water
113(1)
Temperature and P(CO2) dependent calcite solubility
113(1)
Calcite precipitation and dolomite dissolution
114(1)
Calcite solubility in an open and a closed system
114(1)
Pyrite weathering
114(2)
Atmosphere -- Groundwater -- Lithosphere
116(1)
Precipitation under the influence of soil CO2
116(1)
Buffering systems in the soil
116(1)
Mineral precipitates at hot sulfur springs
117(1)
Formation of stalactites in karst caves
117(1)
Evaporation
118(1)
Groundwater
119(1)
The pE-pH diagram for the system iron
119(3)
The Fe pE-pH diagram considering carbon and sulfur
122(1)
The pH dependency of uranium species
122(1)
Origin of groundwater
123(1)
Origin of spring water
124(1)
Pumping of fossil groundwater in arid regions
125(2)
Salt water / fresh water interface
127(1)
Anthropogenic use of groundwater
127(1)
Sampling: Ca titration with EDTA
127(1)
Carbonic acid aggressiveness
128(1)
Water treatment by aeration - well water
128(1)
Water treatment by aeration - sulfur spring
128(1)
Mixing of waters
129(1)
Rehabilitation of groundwater
129(1)
Reduction of nitrate with methanol
129(1)
Fe(0) barriers
130(1)
Increase in pH through a calcite barrier
130(1)
Reaction kinetics
130(7)
Pyrite weathering
130(1)
Quartz-feldspar-dissolution
131(1)
Degradation of organic matter within the aquifer on reduction of redox sensitive elements (Fe, As, U, Cu, Mn, S)
132(1)
Degradation of tritium in the unsaturated zone
133(4)
Reactive transport
137(6)
Lysimeter
137(1)
Karst spring discharge
137(1)
Karstification (corrosion along a karst fracture)
138(1)
The pH increase of an acid mine water
139(1)
In-situ leaching
140(3)
Solutions
143(42)
Equilibrium reactions
143(25)
Groundwater-Lithosphere
143(1)
Standard-output well analysis
143(2)
Equilibrium reaction-solubility of gypsum
145(1)
Disequilibrium reaction -- solubility of gypsum
146(1)
Temperature dependency of gypsumsolubility in well water
146(1)
Temperature dependency of gypsum solubility in distilled water
146(1)
Temperature and P(CO2) dependent calcite solubility
147(1)
Calcite precipitation and dolomite dissolution
148(1)
Comparison of the calcite solubility in an open and a closed system
149(1)
Pyrite weathering
150(2)
Atmosphere-Groundwater-Lithosphere
152(1)
Precipitation under the influence of soil CO2
152(1)
Buffering systems in the soil
152(1)
Mineral precipitations at hot sulfur springs
152(1)
Formation of stalactites in karst caves
153(1)
Evaporation
154(1)
Groundwater
155(1)
The pE-pH diagram for the system iron
155(1)
The Fe pE-pH diagram considering carbon and sulfur
156(1)
The pH dependency of uranium species
157(2)
Origin of groundwater
159(1)
Origin of spring water
159(1)
Pumping of fossil groundwater in arid regions
159(1)
Salt water / fresh water interface
160(1)
Anthropogenic use of groundwater
161(1)
Sampling: Ca titration with EDTA
161(1)
Carbonic acid aggressiveness
162(1)
Water treatment by aeration - well water
162(1)
Water treatment by aeration - sulfur spring
162(2)
Mixing of waters
164(1)
Rehabilitation of groundwater
165(1)
Reduction of nitrate with methanol
165(1)
Fe(0) barriers
166(1)
Increase in pH through a calcite barrier
167(1)
Reaction kinetics
168(8)
Pyrite weathering
168(3)
Quartz-feldspar-dissolution
171(1)
Degradation of organic matter within the aquifer on reduction of redox sensitive elements (Fe, As, U, Cu, Mn, S)
172(3)
Degradation of tritium in the unsaturated zone
175(1)
Reactive transport
176(9)
Lysimeter
176(1)
Karst spring discharge
176(2)
Karstification (corrosion along a karst fracture)
178(1)
The pH increase of an acid mine water
179(2)
In-situ leaching
181(4)
References 185(6)
Index 191

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