Environmental Isotopes in the Hydrological Cycle
Principles and Applications
VOLUME I: INTRODUCTION - THEORY, METHODS, REVIEW
by Willem G Mook, Centre for Isotope Research, Groningen
Contributing Author
J.J.de Vries, Free University, Amsterdam
CONTENTS
1 THE GLOBAL CYCLE OF WATER 1
1.1 Introduction 1
1.2 The hydrosphere 2
1.2.1 Origin of water on earth 2
1.2.2 The hydro-tectonic cycle 2
1.2.3 Distribution of water over the various reservoirs 4
1.3 The global water budget 6
1.4 Components of the hydrological cycle 7
1.4.1 Evaporation 7
1.4.2 Precipitation and atmospheric circulation 9
1.4.3 Discharge from the continents 11
1.4.4 Groundwater 13
1.4.5 Continental water surplus and water use 16
1.5 The hydrosphere and global change 16
1.5.1 Climatic change 16
1.5.2 The human factor 19
1.5.2.1 Irrigation 21
1.5.2.2 Wetland drainage 21
1.5.2.3 Ground cover damage 21
1.5.2.4 Deforestation 21
1.5.2.5 Interbasin diversion 22
1.5.2.6 Streamflow management 22
1.5.2.7 Land use changes 22
1.6 Isotopes in the hydrological cycle 23
2 ATOMIC SYSTEMATICS AND NUCLEAR STRUCTURE 25
2.1 Atomic structure and periodic table of the elements 25
2.2 Structure of the atomic nucleus 26
2.3 Stable and radioactive isotopes 27
2.4 Mass and energy 28
3 ABUNDANCE AND FRACTIONATION OF STABLE ISOTOPES 31
3.1 Isotope ratios and concentrations 31
3.2 Isotope fractionation 31
3.3 Kinetic and equilibrium isotope fractionation 34
3.4 Theoretical background of equilibrium fractionation 39
3.5 Fractionation by diffusion 43
3.6 Relation between atomic and molecular isotope ratios 44
3.7 Relation between fractionations for three isotopic molecules 45
4 ABUNDANCE VARIATIONS BY NATURAL PROCESSES 49
4.1 Use of d values and isotope references 49
4.2 Tracer concentration, amount of tracer 52
4.3 Mixing of reservoirs with different isotopic composition 53
4.3.1 Mixing of reservoirs of the same compound 53
4.3.1.1 Isotopic dilution analysis 55
4.3.2 Mixing of reservoirs of different compounds 56
4.4 Isotopic changes in Rayleigh processes 57
4.4.1 Reservoir with one sink 57
4.4.2 Reservoir with two sinks 60
4.4.3 Reservoir with one source and one sink, as a function of time 61
4.4.4 Reservoir with one source and one sink, as a function of mass 64
4.4.5 Reservoir with two sources and sinks, with and without fractionation 64
5 RADIONUCLIDE DECAY AND PRODUCTION 67
5.1 Nuclear instability 67
5.2 Nuclear decay and radiation 68
5.2.1 Negatron decay 68
5.2.2 Positron decay 68
5.2.3 Electron capture 69
5.2.4 Alpha decay 69
5.2.5 Spontaneous and induced fission, neutron emission 71
5.3 Recoil by radioactive decay 71
5.4 Nuclear reactions 72
5.4.1 Natural production 72
5.4.2 Anthropogenic releases of radionuclides 73
6 EQUATIONS OF RADIOACTIVE DECAY AND GROWTH 75
6.1 Law of radioactive decay 75
6.2 Half-life and mean life 77
6.3 Activity, specific activity and radionuclide concentration 77
6.4 Mixture of independent radioactivities 78
6.5 Branching decay 78
6.6 Radioactive decay series 79
6.6.1 Secular equilibrium 81
6.6.2 Transient equilibrium 82
6.6.3 No-equilibrium 83
6.7 Accumulation of stable daughter product 85
6.8 Radioactive growth 86
7 NATURAL ABUNDANCE OF THE STABLE ISOTOPES OF C, O AND H 89
7.1 Stable carbon isotopes 90
7.1.1 The natural abundance 90
7.1.2 Carbon isotope fractionations 91
7.1.3 Reporting 13C variations and the 13C standard 96
7.1.4 Survey of natural 13C variations 96
7.1.4.1 Atmospheric CO2 96
7.1.4.2 Seawater and marine carbonate 98
7.1.4.3 Vegetation and soil CO2 98
7.1.4.4 Fossil fuel 98
7.1.4.5. Global carbon cycle 99
7.1.4.6 Groundwater and riverwater 100
7.2 Stable oxygen isotopes 101
7.2.1 The natural abundance 101
7.2.2 Oxygen isotope fractionations 103
7.2.3 Reporting 18O variations and the18O standards 107
7.2.4 Survey of natural 18O variations 110
7.2.4.1 Seawater 110
7.2.4.2 Precipitation 110
7.2.4.3 Surface water 113
7.2.5 Climatic variations 113
7.3 Relation between 13C and 18O variations in H2O, HCO3-, and CO32- 115
7.4 Stable hydrogen isotopes 117
7.4.1 The natural abundance 117
7.4.2 Hydrogen isotope fractionations 117
7.4.3 Reporting 2H variations and the 2H standard 118
7.4.4 Survey of natural 2H variations 120
7.5 Relation between 2H and 18O variations in water 120
8 NATURAL ABUNDANCE OF RADIOACTIVE ISOTOPES 125
8.1 The radioactive carbon isotope 125
8.1.1 Origin of 14C, decay and half-life 125
8.1.2 Reporting 14C variations and the 14C standard 126
8.1.3 Survey of natural 14C variations 129
8.1.3.1 Atmospheric CO2 129
8.1.3.2 Vegetation and soils 130
8.1.3.3 Seawater and marine carbonate 130
8.1.3.4 Groundwater 131
8.1.4 14C age determination 132
8.1.5 Dating groundwater 134
8.1.5.1 Dating groundwater with DIC 134
8.1.5.1.1 The origin of 14C in DIC 134
8.1.5.1.2 The chemical/isotopic mass balance 135
8.1.5.1.3 Isotopic exchange in an open system 136
8.1.5.2 Dating groundwater with DOC 136
8.2 Relation between 13C and 14C variations 137
8.3 The radioactive hydrogen isotope 138
8.3.1 Origin of 3H, decay and half-life 138
8.3.2 Reporting 3H activities and the 3H standard 138
8.3.3 Survey of natural 3H variations 139
8.4 Comparison of 3H and 14C variations 140
8.4.1 Relation between 3H and 14C in the atmosphere 140
8.4.2 Relation between 3H and 14C in groundwater 141
9 CHEMISTRY OF CARBONIC ACID IN WATER 143
9.1 Introduction 143
9.2 Carbonic acid equilibria 144
9.3 The equilibrium constants 146
9.3.1 Ideal solutions 147
9.3.2 Seawater 148
9.3.3 Brackish water 148
9.4 Carbonic acid concentrations 155
9.5 Examples for closed and open systems 156
9.5.1 Comparison of freshwater and seawater exposed to the atmosphere 156
9.5.1.1 For freshwater 157
9.5.1.2 For seawater 158
9.5.2 System open for CO2 escape and CaCO3 formation 159
9.5.2.1 Starting conditions 159
9.5.2.2 Escape of CO2 160
9.5.2.3 Precipitation of CaCO3 161
9.5.3 System exposed to CO2 in the presence of CaCO3 161
9.5.4 Closed system, mixing of freshwater and seawater 163
10 WATER SAMPLING AND LABORATORY TREATMENT 167
10.1 Water sampling and storage 167
10.1.1 Sampling bottles 167
10.1.2 General field practice 168
10.1.3 Precipitation 168
10.1.4 Surface water 169
10.1.5 Unsaturated zone waters 169
10.1.6 Groundwater 170
10.1.7 Geothermal waters 170
10.2 Laboratory treatment of water samples 170
10.2.1 The 18O/16O analysis of water 171
10.2.1.1 Equilibration with CO2 for mass spectrometric analysis 171
10.2.1.2 Other methods 172
10.2.2 The 2H/1H analysis of water 173
10.2.2.1 Reduction of H2O to H2 for mass spectrometric analysis 173
10.2.2.2 Other methods 173
10.2.3 The 3H analysis of water 174
10.2.3.1 Water purification 174
10.2.3.2 3H enrichment 175
10.2.3.3 Preparation of gas for PGC of 3H 175
10.2.4 The 14C analysis of dissolved inorganic carbon 176
10.2.4.1 In the field 176
10.2.4.2 In the laboratory 177
10.2.5 The 13C/12C analysis of dissolved inorganic carbon 177
11 MEASURING TECHNIQUES 179
11.1 Mass spectrometry for stable isotopes 179
11.1.1 Physical principle 179
11.2 Reporting stable isotope abundance ratios 181
11.2.1 Measurement of 2H/1H in H2 182
11.2.2 Measurement of 15N/14N in N2 183
11.2.3 Measurement of 13C/12C and 18O/16O in CO2 184
11.2.3.1 Comparison with machine reference 184
11.2.3.2 Calibration 184
11.2.3.3 Isotopic corrections 186
11.2.3.4 18O correction for water-CO2 equilibration 188
11.2.3.5 Normalisation 188
11.2.4 Measurement of 18O/16O and 17O/16O in O2 190
11.3 Radiometry for radioactive isotopes 191
11.3.1 Gas counters 191
11.3.1.1 Ionisation chamber 192
11.3.1.2 Proportional counter 193
11.3.1.3 Geiger Müller counter 193
11.3.1.4 Counter operation 193
11.3.2 Liquid scintillation spectrometer 195
11.3.2.1 Physical principle 195
11.3.2.2 Counter operation 196
11.4 Mass spectrometry for low-abundance isotopes 197
11.4.1 Principle and application of AMS 197
11.5 Reporting 14C activities and concentrations 199
11.5.1 The choice of variables 199
11.5.2 The standardisation 201
11.5.2.1 The question of isotope fractionation 201
11.5.2.2 The question of radioactive decay 202
11.5.2.3 Definition of the 14C standard activity 202
11.5.3 Final definitions 203
11.5.4 Special cases 204
11.5.4.1 Hydrology 204
11.5.4.2 Oceanography and atmospheric research 205
11.5.4.3 Geochemistry 206
11.5.4.4 Enhanced 14C radioactivity 208
11.5.4.5 14C ages 211
11.5.5 Summary 211
12 NATURAL ISOTOPES OF ELEMENTS OTHER THAN H, C, O 213
12.1 Helium 214
12.1.1 Origin and characteristics 215
12.1.2 Experimental and technical aspects 215
12.1.3 Sources of 3He 215
12.1.4 Natural abundance 216
12.1.5 Applications 216
12.1.5.1 Principle of 3H/3He dating 216
12.1.5.2 Mass spectrometric measurement of 3H through 3He 216
12.2 Lithium 217
12.2.1 Natural abundance 217
12.2.2 Experimental and technical aspects 217
12.2.3 Applications 217
12.3 Beryllium 218
12.3.1 Origin and characteristics 218
12.3.2 Experimental and technical aspects 218
12.3.3 Natural abundance 218
12.3.4 Applications 219
12.4 Boron 219
12.4.1 Natural abundance 219
12.4.2 Experimental and technical aspects 219
12.4.3 Applications 219
12.5 Nitrogen 220
12.5.1 Experimental and technical aspects 220
12.5.2 Natural abundance and isotope fractionation 220
12.5.3 Applications 221
12.5.4 18O/16O in nitrate 221
12.6 Aluminium 222
12.6.1 Origin and characteristics 222
12.6.2 Experimental and technical aspects 222
12.6.3 Natural abundance 222
12.6.4 Applications 223
12.7 Silicon 223
12.7.1 Origin and characteristics 223
12.7.2 Natural abundance 224
12.7.3 Experimental and technical aspects 224
12.7.4 Applications 224
12.8 Sulphur 224
12.8.1 Experimental and technical aspects 225
12.8.2 Natural abundance 226
12.8.3 Applications 226
12.9 Chlorine 226
12.9.1 Radioactive 36Cl 226
12.9.1.1 Origin and characteristics 226
12.9.1.2 Experimental and technical aspects 227
12.9.1.3 Abundance in nature 228
12.9.1.4 Applications 228
12.9.1.4.1 Dating old water 228
12.9.1.4.2 Infiltration of young water 229
12.9.2 Stable 35Cl and 37Cl 229
12.9.2.1 Natural abundance and applications 229
12.9.2.2 Experimental and technical aspects 229
12.10 Argon 230
12.10.1 Origin and characteristics 230
12.10.2 Experimental and technical aspects 231
12.10.3 Natural abundance 231
12.10.4 Applications 231
12.11 Krypton 231
12.11.1 Origin and characteristics 231
12.11.2 Experimental and technical aspects 232
12.11.3 Natural abundance 233
12.11.4 Applications 233
12.12 Iodine 233
12.12.1 Origin and characteristics 233
12.12.2 Experimental and technical aspects 234
12.12.3 Natural abundance 234
12.12.4 Applications 234
12.13 Decay series 235
12.14 The uranium series 237
12.14.1 238U/234U 237
12.14.2 230Th - 234U dating 238
12.14.3 226Ra and 222Rn 238
12.14.4 210Pb 238
12.14.5 Experimental and technical aspects 239
12.15 The actinium series 239
12.16 The thorium series 239
13 ERRORS, MEANS AND FITS 243
13.1 Errors 243
13.2 Precision and accuracy 243
13.2.1 Definitions 243
13.2.2 Significant figures and digits 244
13.2.3 Uncertainties 245
13.3 Instrumental uncertainties 246
13.3.1 Mean values 246
13.3.2 Distribution of data 246
13.3.3 Standard deviation 248
13.3.3.1 Precision of data 248
13.3.3.2 Precision of the mean 249
13.4 Statistical uncertainties 250
13.5 Error propagation 251
13.5.1 Standard deviation 251
13.5.2 Weighted mean 252
13.6 Least-squares fit 253
13.6.1 Fit to a straight line 253
13.6.2 Fit to non-linear curves 254
13.7 Chi-square test 255
REFERENCES 257
LITERATURE 263
IAEA PUBLICATIONS 265
CONSTANTS 268
SYMBOLS AND UNITS 269
SUBJECT INDEX 271
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