Note: Page numbers followed by f and t indicate figures and tables.
airborne LiDAR106.
See also geodetic surveys
alluvial220
alluvial fan220
alluvium220
altitude220
ancillary/anecdotal information83.
See also geothermal area identification and monitoring
anisotropic220
aquifer45, 220
artificial recharge of164–166
confined220
skeleton55
storage coefficients63
unconfined220.
See also aquifer-system compaction; subsidence analysis and simulation; subsidence processes
aquifer mechanics and land subsidence55
stress causing aquifer-system compaction65–73
stress–strain relationship in susceptible aquifer systems73–77
subsurface-fluid withdrawal55
theory of aquifer-system compaction55–65
aquifer-system compaction45, 47, 56, 165
aquitard drainage model56
dimensionless time factor65
effective stress58–59
excess pore water56
hydrodynamic consolidation theory58, 64–65
idealized aquifer system56, 57
fload change on aquitards56
modeling135
skeleton of aquifer system55
theory55
time constant for doubly draining aquitard65
unconsolidated heterogeneous aquifer system57.
See also aquifer mechanics and land subsidence; aquifer-system compressibility and storage
aquifer-system compressibility and storage59
effective stress changes60
skeletal and fluid storage coefficient63–64
skeletal compressibility60
skeletal elastic storage coefficient76, 77
specific storage60–61, 62–63
storage coefficients63
volume skeletal compressibility59–60.
See also aquifer-system compaction; stress–strain relationship
aquitard45, 220–221
compressibility45.
See also subsidence processes
aquitard drainage model56, 136, 137
fcompaction simulation142–145, 144
f, 145
fDarcy–Gersevanov law140, 142
Darcy's law139
diffusion equation for transient flow141
features of MODFLOW-based subsidence models145
tgroundwater flow theory138–142
Interbed Storage Package, version 1143
MODFLOW143
one-dimensional consolidation137
one-dimensional model143
prediction138.
See also aquifer-system compaction; subsidence analysis and simulation
area of Daqing49.
See also compaction by fluid extraction
artesian221
Atterberg limits182
Atterberg limits and indexes197–202
effect of clay content on LL for core holes200
ffrom core hole 14/13–11D1198
t–199
tunified soil classification plasticity201
f.
See also laboratory analysis results
bench mark221
“blackbox” models.
See empirical methods
cable-casing friction97
carbonate221
casing-collar logging104–105.
See also subsurface measurement techniques
centralizers97.
See also extensometry
clay content–subsidence relation129–130.
See also quasi-theoretical approach
coefficient of:compressibility209
horizontal permeability190
permeability224.
See saturated hydraulic conductivity
vertical permeability191
volume compressibility209, 211
collar counting104.
See also subsurface measurement techniques
compaction56, 221
residual221.
See also aquifer-system compaction
compaction by fluid extraction46
area of Daqing49
deformation and ground failures47
earth fissures and surface faults47
extraction of pore fluids46–47
geothermal fluids49
groundwater47–48
hydrocarbons48
land subsidence in Wairakei-Tauharo geothermal system50
fsubsurface-fluid withdrawal48
water of compaction48.
See also subsidence processes
composite logs179.
See also laboratory tests and field sampling standards
compressibility209
coefficient of209
coefficient of volume209, 211, 211
fconstrained modulus of elasticity209
laboratory virgin compression curve211
semilogarithmic plot of void ratio211
total subsidence210.
See also laboratory analysis results
confining unit221
consolidation56, 183–186, 202, 221
alternate procedures184
coefficient of184
coefficient of consolidation and LL207
fcoefficients of consolidation estimation206
comparison of methods of compression index206
fcompression index184
compression index estimation203–205
computed compression indexes205
tconsolidation characteristics and LLs207–208
correlation of compression indexes206
LL and compression index204
fone-dimensional consolidometer specimen container183
fprinciples of137
saturated hydraulic conductivity186
soil classification effect207
stress–strain analysis from185
ftest curves202
void ratio–load curves205.
See also aquifer-system compaction; laboratory analysis methods
constitutive models150–151.
See also subsidence analysis and simulation
constrained modulus of elasticity209.
See also compressibility
continuous GPS (CGPS)86
Continuously Operating Reference Stations (CORS)86
conventional groundwater flow theory135, 138–142.
See also aquitard drainage model; subsidence analysis and simulation
conversion table227–229
core221
corollary effects29
Daqing49.
See also compaction by fluid extraction
Darcy–Gersevanov law140, 142, 146–147.
See also aquitard drainage model; poroelasticity model
Darcy's law139
debris flow222
deformation47, 222
elastic222
inelastic222.
See also compaction by fluid extraction
depth–porosity model130–135.
See also quasi-theoretical approach
differential leveling86–89.
See also ground-based geodetic surveys
differential LiDAR (Dif-LiDAR)102
digital elevation models (DEMs)107
dimensionless time factor65.
See also aquifer-system compaction
discharge222
displacement model109.
See also geodetic surveys
drawdown222
dynamic stresses71–73.
See also stress causing aquifer-system compaction
earth excavation equipment179
earth fissures47.
See also compaction by fluid extraction
effective stress67, 68, 77
changes60
principle of58–59, 68
f.
See also stress causing aquifer-system compaction; stress–strain relationship
elasticity, constrained modulus of209.
See also compressibility
elevation222
empirical methods121–122.
See also subsidence analysis and simulation
eustasy222
evaporite222
extensometry92, 93
fabandoned oil-test holes98
borehole extensometer types95
cable and pipe extensometers95–101
cable extensometer100
centralizers97
constructed in converted oil-test hole98
counterweighted pipe extensometers101
evaluating cable and pipe extensometers100
extensometer records102
free-pipe extensometers101
gross compaction95
horizontal94
recording borehole extensometer installations96
fsingle and double pipe borehole extensometers94–95
slip joints101
subsurface bench mark92
teeter bar96
telescopic extensometer101–102
wells to measure water levels and compaction99
f.
See also ground-based geodetic surveys
Fen-Wei Faulted Basin (FWB)28
field sampling173.
See also laboratory tests and field sampling standards
flow222
Geertsma's coefficient of uniaxial compaction152.
See also subsidence model types
geodetic surveys106
airborne LiDAR106
displacement model109
factors in airborne-LiDAR mapping107
land subsidence and aquifer-system compaction110
fLiDAR107–108
PSI generalized velocity map111
fspace-based geodetic techniques107
synthetic aperture radar interferometry108–112.
See also geothermal area identification and monitoring
geostatic stresses66–67.
See also stress causing aquifer-system compaction
geothermal222
geothermal area identification and monitoring83
airborne and spaced-based geodetic surveys106–112
ancillary/anecdotal information83
ground-based geodetic surveys86
horizontal displacement112
identifying groundwater basins83–84
manual for surface monitoring86
methods of measuring aquifer compaction and subsidence85
treference networks for horizontal and vertical geodetic control85–86
sufficiently stable84
geothermal fluids49.
See also compaction by fluid extraction
glacioisostasy222
global positioning system (GPS)86, 89, 102
strengths of90.
See also ground-based geodetic surveys
granular displacement model (GDM)150
ground-based geodetic surveys86
differential leveling86–87
extensometry92–102
geodetic network to measure historical subsidence91
fglobal positioning system89–91
horizontal GPS displacement vectors superimposed on InSAR imagery92
fland-surface change measuring techniques91
monitoring network87
near-surface deposits88
network of level lines in San Jose subsidence area89
fprecise differential leveling87–89
strengths of GPS90
subsurface measurement techniques104–106
tripod-mounted LiDAR102–104.
See also geothermal area identification and monitoring
ground failures47.
See also compaction by fluid extraction
groundwater47–48
basin identification83–84
withdrawal46
withdrawal reduction164.
See also compaction by fluid extraction; geothermal area identification and monitoring; subsidence processes
groundwater flow theory, conventional135, 138–142.
See also aquitard drainage model; subsidence analysis and simulation
Guidebook to Studies of Land Subsidence due to Ground-Water Withdrawal1
half-space model153
f, 154.
See also subsidence model types
“Height Modernization” program86
heterogeneous222
high accuracy reference networks (HARNs)86
homogeneous223
horizontal displacement112.
See also geothermal area identification and monitoring
horizontal permeability coefficient190.
See also hydraulic conductivity
hydraulic conductivity (permeability)180–181, 190, 191, 223
consolidation test summaries192
t–194
thorizontal permeability coefficient190
range in permeability of samples in core holes195
fvertical hydraulic conductivity and texture196
fvertical permeability coefficient191.
See also laboratory analysis results; saturated hydraulic conductivity
hydraulic gradient223
hydraulic head, total222
hydrocarbons48.
See also compaction by fluid extraction
hydrocompaction50–52, 223.
See also subsidence processes
hydrodynamic consolidation theory58, 64–65.
See also aquifer-system compaction
hydrostatic pressure224
hydrostatic stresses66–67.
See also stress causing aquifer-system compaction
illite223
inclinometers106.
See also subsurface measurement techniques
inertial measurement unit (IMU)107
interbed223
Interbed Storage Package, version 1 (IBS1)143
interferometric synthetic aperture radar (InSAR)107, 108
International Association of Hydrological Sciences (IAHS)4
International Hydrological Programme (IHP)3
isothermal223
isotropic223
kaolinite223
karst223
laboratory analysis methods179
Atterberg limits182
consolidation183–186
hydraulic conductivity180–181
moisture content181
particle-size classes180
tparticle-size distribution180
porosity and void ratio181
specific gravity of solids181
unit weight181.
See also laboratory tests and field sampling standards
laboratory analysis results186
Atterberg limits and indexes197–202
compressibility209–212
consolidation202–208
hydraulic conductivity190–196
moisture content208–209
particle-size distribution186–190
pore volume208
soil-engineering and hydrogeologic terms and concepts208
specific gravity, unit weight, and porosity196–197
virgin compression curve211.
See also laboratory tests and field sampling standards
laboratory tests and field sampling standards173
composite logs of core holes179
field sampling173
general need of tests173
methods of laboratory analysis179–186
properties core hole samples174
t–178
tresults of laboratory analyses186
lacustrine223
land subsidence1, 2–4, 224
attributed to groundwater extraction6
t–14
tcause of1
international database29
locations16
t–27
tmagnitude and areal extent of15
foccurrence and history of4
principal areas of known global5
fproblems resulting from29–30
selected areas of15
fland-surface change measurement techniques91.
See also ground-based geodetic surveys
light detection and ranging (LiDAR)87, 107–108.
See also geodetic surveys
linear poroelasticity theory135.
See also subsidence analysis and simulation; “line-of-sight”
(LOS)109
liquid limit (LL)182
load.
See stress
model121
MODFLOW143.
See also aquitard drainage model
moisture content208–209.
See also laboratory analysis results; water—content
montmorillonite45, 224.
See also subsidence processes
National Geodetic Survey (NGS)86
National Geodetic Vertical Datum of 1929 (NGVD 1929)86
National Oceanic and Atmospheric Administration (NOAA)87
National Spatial Reference System (NSRS)86
near-surface deposits88.
See also ground-based geodetic surveys
network monitoring87.
See also ground-based geodetic surveys
nonsteady flow.
See unsteady flow
North American Datum of 1927 (NAD27)86
North American Datum of 1983 (NAD83)85
North American Vertical Datum of 1988 (NAVD88)85
North China Plain (NCP)2, 28
notations and symbols215–219
odometer test.
See uniaxial consolidation test
one-dimensional model143.
See also aquitard drainage model
particle-size distribution180, 186
curves for core hole 14/13–11D1186
fparticle-size classes180
tfor samples tested for consolidation187
t–189
tsediment classification triangles190
statistical measures190.
See also laboratory analysis results
permafrost224
permanent scatterer interferometry.
See persistent-scatterer interferometry
permeability.
See hydraulic conductivity; saturated hydraulic conductivity
permeability intrinsic224
permeability coefficient224
horizontal190
vertical191.
See also hydraulic conductivity
persistent-scatterer interferometry (PSI)108
plasticity index (PI)182
plastic limits (PLs)182
pore pressure, excess224
pore volume208.
See also laboratory analysis results
poroelasticity model145
changes in groundwater storage147
coupling term of pressure head149
Darcy–Gersevanov Law146–147
derivation of groundwater flow equations146
poroelasticity theory146–149
simulation149–150
theory146–149
volume strain rate148.
See also subsidence analysis and simulation
porosity181, 196–197, 224.
See also laboratory analysis results
pressure, hydrostatic224
principles of consolidation137
quality assurance/quality control (QA/QC)107
quasi-theoretical approach122
annual land subsidence and corresponding discharge126
fchange in altitude at BM9536 and BM9537129
fclay content–subsidence relation129–130
cumulative oil, gross-liquid, and net-liquid production124
fcumulative volumes of subsidence and pumpage127
fdecrease of porosity with depth131
fdepth–porosity model130–135
expression for rate of subsidence122
leakage rate and volumetric subsidence rate126
fpercent clay and subsidence131
fratio of subsidence to head decline127–129, 130
frelation for subsidence124
specific storage for inelastic compaction134
fsubsidence as function of liquid extraction123–127
Wadachi's model122–123
water-level decline and land subsidence128
f.
See also subsidence analysis and simulation
radioactive-marker logging105.
See also subsurface measurement techniques
radioactive marker technique (RMT)105
real-time networks (RTNs)86
recharge224
satellite synthetic aperture radar (SAR)108
saturated hydraulic conductivity (coefficient of permeability)180
sediment elevation tables (SETs)88
seepage stress71.
See also stress causing aquifer-system compaction
semilogarithmic plot of void ratio211.
See also compressibility
smectite.
See montmorillonite
space-based geodetic techniques107.
See also geodetic surveys
specific discharge224
specific gravity196–197
of solids181.
See also laboratory analysis methods; laboratory analysis results
specific storage224
specific yield225
static stresses66–71.
See also stress causing aquifer-system compaction
steady flow222
storage225
storage coefficient225
strain225
stress225, 226
applied225
effective225
geostatic225
hydrostatic225
preconsolidation226
total226
yield226
stress causing aquifer-system compaction65
computed stresses at two depth horizons70
tdynamic stresses71–73
effective stress67, 68
effective stress principle68
fgeostatic and hydrostatic stresses66–67
measured and computed hydraulic properties73
tnonsteady flow in doubly-draining aquitard72
fproperties used to compute stresses69
tseepage stress71
static stresses66–71
types of65–66.
See also aquifer mechanics and land subsidence
stress–strain relationship73
aquifer-system skeletal elastic storage coefficient76, 77
change in applied stress, compaction, and74
f, 75
compressibilities of clays and sands77–78
effective stresses77
elastic storage and compressibility parameters76
ratio of inelastic storage coefficient and initial aggregate thickness77
stress–strain analysis74–77
stress–strain curves74.
See also aquifer mechanics and land subsidence
subjacent deposits88
subsidence.
See land subsidence
subsidence analysis and simulation121
analysis and simulation of aquifer-system compaction135
analysis of subsidence-prone areas121
aquifer-system compaction modeling135
aquitard drainage model136–145, 137
fconstitutive models150–151
conventional groundwater flow theory135
empirical methods121–122
linear poroelasticity theory135
methods121
poroelasticity model145–150
quasi-theoretical approach122–135
simplifications of aquifer-system properties136
subsidence model types151–154
theoretical approach135
subsidence mitigation163
aquifer-system compaction165
artificial recharge of aquifer systems164–166
in china166
in Italy166–167
in Japan168
in United States168–169
subsidence model types151
Geertsma's coefficient of uniaxial compaction152
half-space model153
f, 154
influence of material within unpumped overburden152–154
simple subsidence estimates151–152
tension center model154
theoretical techniques151.
See also subsidence analysis and simulation
subsidence processes45
aquifers45
aquifer-system compaction45, 47
aquitard compressibility45
aquitards45
compaction by fluid extraction46–50
groundwater withdrawal46
hydrocompaction50–52
montmorillonite45
underground voids46
subsidence-prone area analysis121.
See also subsidence analysis and simulation
subsurface-fluid withdrawal55.
See also aquifer mechanics and land subsidence
subsurface measurement techniques104
casing-collar logging104–105
collar counting104
inclinometers106
observation well in Niigata106
fradioactive-marker logging105.
See also ground-based geodetic surveys
surface faults47.
See also compaction by fluid extraction
synthetic aperture radar interferometry108–112.
See also geodetic surveys
teeter bar96.
See also extensometry
tension center model154.
See also subsidence model types
Terzaghi's theory of one-dimensional consolidation137.
See also aquitard drainage model
tests, general need of173
theodolite86
transmissivity226
tripod light detection and ranging (T-LiDAR)102
Dif-LiDAR102–104
imagery of geothermal transmission line103
f.
See also ground-based geodetic surveys
unconsolidated heterogeneous aquifer system57.
See also aquifer-system compaction
underground voids46.
See also subsidence processes
uniaxial consolidation test (odometer test)210
United Nations Educational, Scientific and Cultural Organization (UNESCO)3
unit weight181, 196–197, 226.
See also laboratory analysis results
unsteady flow222
uplift226
virgin compression curve211.
See also compressibility
void ratio181, 226.
See also laboratory analysis methods
volume compressibility coefficient209, 211.
See also compressibility
volumetric-flask method181
Wadachi's model122–123.
See also quasi-theoretical approach
water:content181
table226.
See also laboratory analysis methods
Yangtze River Delta (YRD)15