Fundamental of Groundwater Hydrology Ted Way
Fundamental of Groundwater Hydrology
Ted Way
OutlineHydrologic cycleAquifersBasic groundwater equationsWell drilling and completionGroundwater level and velocityDefinition of key hydrologic parametersGroundwater/surface water interactionHydrologic testsSurface water monitoring/event samplingGround water problems
體積 百分比
OutlineHydrologic cycleAquifersBasic groundwater equationsWell drilling and completionGroundwater level and velocityDefinition of key hydrologic parametersGroundwater/surface water interactionHydrologic testsSurface water monitoring/event samplingGround water problems
Precipitation
Infiltration
Recharge
OutlineHydrologic cycleAquifersBasic groundwater equationsWell drilling and completionGroundwater level and velocityDefinition of key hydrologic parametersGroundwater/surface water interactionHydrologic testsSurface water monitoring/event samplingGround water problems
http://groundwater.ucdavis.edu/Publications/Harter_FWQFS_8083.pdf
http://www.bnl.gov/erd/Groundwater/GWreport01Files/Final.pdf.web.files/Appendix%20B.pdf
OutlineHydrologic cycleAquifersBasic groundwater equationsWell drilling and completionGroundwater level and velocityDefinition of key hydrologic parametersGroundwater/surface water interactionHydrologic testsSurface water monitoring/event samplingGround water problems
dxdhKv
e
xx φ
−=
WthS
bhK
zhbK
yhbK
yxhbK
xhbK zzyyxyxx +
∂∂
=+∂∂
+∂∂
+∂∂
∂+
∂∂
'
'
2
2
2
22
2
2
2
Water level measurements Precipitation,Pumping records
Pumping tests
Geologic study(drilling, geophysical study)
Pumping tests
Basic Groundwater Equations
h = water level elevationb = aquifer thicknessW = precipitation, pumping ratesK = hydraulic conductivityS = storage coefficientV = groundwater velocityΦ = effective porosity
Outline
Hydrologic cycleAquifersBasic groundwater equationsWell drilling and completionGroundwater level and velocityDefinition of key hydrologic parametersGroundwater/surface water interactionHydrologic testsGround water problems
http://ga.water.usgs.gov/edu/earthgwwells.html
Fetter C.W.,1999, Contaminant Hydrogeology, Second Edition, Prentice Hall
Geologic Cross-Sections
Fetter C.W.,1999, Contaminant Hydrogeology, Second Edition, Prentice Hall
http://www.jains.com/Pipefittings/jain%20pvc%20well%20casing%20and%20screen%20pipes.htmhttp://www.enviroequip.com/sales/screenandcasing50mm.htmhttp://www.ajaycorp.com/upvc-pipes-strainers-casing.html
http://www.wma-minelife.com/uranium/insitu/insitufr.htm
http://water.usgs.gov/owq/pubs/wri/wri964233/wri964233.pdf
http://cgsweb.moeacgs.gov.tw/ehome/Index10.htm
http://water.usgs.gov/owq/pubs/wri/wri964233/wri964233.pdf
Purposes of Monitoring wells
Groundwater level →water level fluctuations,→water quantity→ground water flow direction
Pumping tests/slug tests→aquifer properties
Water quality→sampling→in-situ measurement
Purposes of Monitoring wells
Groundwater level →water level fluctuations,→water quantity→ground water flow direction
Pumping tests/slug tests→aquifer properties
Water quality→sampling→in-situ measurement
Water Level Measurement
http://www.stevenswater.com/catalog/products/chart_recorders/datasheet/type_f.pdf
http://www.geotechnical.net/groundwaterpumps.shtml http://www.solinst.com/Prod/Data/428.pdf
Sampling pumps Bailers
Water Sampling
Ground
Gravel pack
6m
6m
5m
36m
Cover
Fine quartz
12m Cement+5%Bentonite
6mBentonite
Screen
∇
3 to 5 casing volumesof water
OutlineHydrologic cycleAquifersBasic groundwater equationsWell drilling and completionGroundwater level and velocityDefinition of key hydrologic parametersGroundwater/surface water interactionHydrologic testsSurface water monitoring/event samplingGround water problems
http://imnh.isu.edu/digitalatlas/hydr/concepts/gwater/gwflow.htm
http://www.oregon.gov/DHS/ph/dwp/docs/gwater/grndwtr.pdf
Orange County, California
dxdhKv
e
xx φ
−=
WthS
bhK
zhbK
yhbK
yxhbK
xhbK zzyyxyxx +
∂∂
=+∂∂
+∂∂
+∂∂
∂+
∂∂
'
'
2
2
2
22
2
2
2
Water level measurements Precipitation,Pumping records
Pumping tests
Geologic study(drilling, geophysical study)
Pumping tests
Basic Groundwater Equations
h = water level elevationb = aquifer thicknessW = precipitation, pumping ratesK = hydraulic conductivityS = storage coefficientV = groundwater velocityΦ = effective porosity
OutlineHydrologic cycleAquifersBasic groundwater equationsWell drilling and completionGroundwater level and velocityDefinition of key hydrologic parametersGroundwater/surface water interactionHydrologic testsSurface water monitoring/event samplingGround water problems
K - Hydraulic Conductivity
Q
Q
L
v
Area A
hL
Darcy’s Law
French hydrologist Henry Darcy (1856)
Q ~ hL
Q ~ 1/L
Q ~ A
LhKAQ L=
Darcy’s Law
K = hydraulic conductivity
Lh
dldh L−=
dldhKAQ −=
dldhKv
eφ−=
hydraulic gradient
Φe = effective porosity
GravelCoarse sandMedium sandFine sandSiltTillClayMarine clayKarst LimestoneLimestoneSandstoneSiltstoneSaltAnhydriteShalePermeable basaltFractured bedrockWeathered graniteWeathered grabroBasaltCrystalline rock
Hydraulic Conductivity(m/sec)
10-14 10-13 10-12 10-11 10-10 10-9 10-8 10-7 10-6 10-5 10-4 10-3 10-2
Transmissivity(m2/sec)= Hydraulic conductivity(m/sec)x Aquifer thickness(m)
Darcy’s Law
Range of Values of Porosity
Unconsolidated deposits• Gravel 25-40%• Sand 25-50% • Silt 35-50%• Clay 40-70%Rocks • Fractured basalt 5-50%• Karst Limestone 5-50%• Sandstone 5-30%• Limestone,dolomite 0-20%• Shale 0-10%• Fractured crystalline rock 0-10%• Dense crystalline rock 0-5%
Effective Porosity
Clay and related materials 0 to 3%
Gravel, Sand, Gravel and Sand 25 to 35%
http://groundwater.orst.edu/under/images/permeabilityb.html
Gravel Sand Clay
Darcy’s Law
K = hydraulic conductivity
Lh
dldh L−=
dldhKv
eφ−=
hydraulic gradient
Φe = effective porosity
S – Storage Coefficient
http://flightline.highline.edu/cwhittington/G110/LectureNotes/WaterSystems.pdf
http://www.egr.msu.edu/igw/testing/Pumping%20near%20an%20impervious%20boundary.pdf
Storage Coefficient (Unconfined Aquifer)
Pump the well at a rate of 1 m3/minute for one day
Volumepumped = 1 m3/min x 1,440 minutes = 1,440 m3
Volumecone of depression = 14,400 m3
storage coefficient (S)= Volumepumped/Volumecone of depression= 1,440 m3/14,400 m3
= 10%= effective porosity = specific yield
pumping
cone ofdepression
initial water level
unconfinedaquifer
drainageeffect
Ranges of Values of Specific Yield
Material No. of analyses Range Arithmetic mean
Sandstone (fine) 47 0.02-0.40 0.21
Sandstone (medium) 10 0.12-0.41 0.27
Siltstone 13 0.01-0.33 0.12
Sand (fine) 287 0.01-0.46 0.33
Sand (medium) 297 0.16-0.46 0.32
Sand (coarse) 143 0.18-0.43 0.30
Gravel (fine) 33 0.13-0.40 0.28
Gravel (medium) 13 0.17-0.44 0.24
Gravel (coarse) 9 0.13-0.25 0.21
Silt 299 0.01-0.39 0.20
Clay 27 0.01-0.18 0.06
Limestone 32 0.00-0.36 0.14
From Morris and Johnson, 1967.
Storage Coefficient (Confined Aquifer)
storage coefficient (S)
= Volumepumped/Volumecone of depression
= 0.001 to 0.00001
= f(cm,cw)
∗ matrix compaction
∗ water expansion
initial water level
cone ofdepression
pumping
ConfinedAquifer
S = γb(α+φβ)
Ranges of Values of Specific Storage
Material Specific storage (m-1)
Loose sand 1.0x10-3 - 4.9x10-4
Dense sand 2.0x10-4 - 1.3x10-4
Dense sandy gravel 1.0x10-4 - 4.9x10-5
Plastic clay 2.0x10-2 - 2.6x10-3
Stiff clay 2.6x10-3 - 1.3x10-3
Medium-hard clay 1.3x10-3 - 9.2x10-4
Rock, fissured, jointed 6.9x10-5 - 3.3x10-6
Rock, sound Less than 3.3x10-6
i 19 2
solid
OutlineHydrologic cycleAquifersBasic groundwater equationsWell drilling and completionGroundwater level and velocityDefinition of key hydrologic parametersGroundwater/surface water interactionHydrologic testsSurface water monitoring/event samplingGround water problem
http://www.oregon.gov/DHS/ph/dwp/docs/gwater/grndwtr.pdf
http://www.hydrosphere.com/img/surface_water.jpg
http://ponce.sdsu.edu/groundwater_utilization_and_sustainability.html
Source: U.S. Geological Survey.Conceptual hydrological flow system in Georgia's coastal plains.
Base Flow
http://nevada.usgs.gov/wb/final/chapter5.pdf
http://pubs.usgs.gov/circ/circ1139/htdocs/natural_processes_of_ground.htm
http://nevada.usgs.gov/wb/final/chapter5.pdf
http://www.na.fs.fed.us/spfo/pubs/n_resource/wetlands/wetlands4_hydrology.htm
http://ga.water.usgs.gov/edu/graphics/piessw.gif
dxdhKv
e
xx φ
−=
WthS
bhK
zhbK
yhbK
yxhbK
xhbK zzyyxyxx +
∂∂
=+∂∂
+∂∂
+∂∂
∂+
∂∂
'
'
2
2
2
22
2
2
2
Measurement Precipitation recordPumping record
Pumping test
Geologic study(drilling, geophysical logs)
Pumping test
h = water level elevationb = aquifer thicknessW = precipitation, pumping ratesK = hydraulic conductivityS = storage coefficientV = groundwater velocityΦ = effective porosity
OutlineHydrologic cycleAquifersBasic groundwater equationsWell drilling and completionGroundwater level and velocityDefinition of key hydrologic parametersGroundwater/surface water interactionHydrologic testsSurface water monitoring/event samplingGround water problems
(1) Constant rate pumping test - T(K), S(multiple wells)
(2) Slug tests - T(K)
Aquifer Tests
Constant Rate Pumping Test
Q
Observation well Pumping well
bK
r
Q
http://www.if.uidaho.edu/~johnson/ifiwrri/radflow/radflow.html
drainage Static water level
Troll Troll
Pump
Computer
Generator
Valve Flow meter
Slug test
Computer
Static water level
Troll
(Slug test)
Static WL
(1)
Static WL
(2)
OutlineHydrologic cycleAquifersBasic groundwater equationsWell drilling and completionGroundwater level and velocityDefinition of key hydrologic parametersGroundwater/surface water interactionHydrologic testsSurface water monitoring/event samplingGround water problems
http://www.uwsp.edu/geo/faculty/ritter/geog101/textbook/fluvial_systems/channel_geometry_and_flow.html
http://nevada.usgs.gov/barcass/articles/Ely3.pdf
http://geology.com/articles/hydrograph.shtml
http://geology.com/articles/hydrograph.shtml
http://ga.water.usgs.gov/edu/measureflow.html
http://www.uwsp.edu/geo/faculty/ritter/geog101/textbook/fluvial_systems/channel_geometry_and_flow.html
http://ga.water.usgs.gov/edu/measureflow.html
http://ga.water.usgs.gov/edu/measureflow.html
http://ga.water.usgs.gov/edu/measureflow.html
http://www.who.int/water_sanitation_health/resourcesquality/wqmchap12.pdf
http://www.uwsp.edu/geo/faculty/ritter/geog101/textbook/fluvial_systems/channel_geometry_and_flow.html
60%
http://geology.com/articles/hydrograph.shtml
http://geology.com/articles/hydrograph.shtmlEvent monitoring schedule
Event Sampling
Every 5 data points
Or
W L Change ≧ 0.05M
0.00 3.50 109:52
-0.01 3.50 109:51
0.00 3.51 109:50
0.01 3.51 109:49
-0.02 3.50 109:48
-0.07 3.52 109:47
-0.07 3.59 109:46
-0.09 3.66 109:45
-0.09 3.75 109:44
-0.06 3.84 109:43
0.15 3.90 109:42
0.13 3.75 109:41
0.07 3.62 109:40
0.05 3.55 109:39
0.01 3.50 109:38
-0.01 3.49 109:37
0.00 3.50 109:36
0.01 3.50 109:35
0.01 3.49 109:34
0.01 3.48 109:33
-0.02 3.47 109:32
0.01 3.49 109:31
03.48 109:30
RecordWater Level Change (M)Water Level (M)Duration (mins)Time
http://ga.water.usgs.gov/edu/gageonbridge.html
http://www.lmnoeng.com/Weirs/RectangularWeir.htm
http://www.uwsp.edu/geo/faculty/ritter/geog101/textbook/fluvial_systems/channel_geometry_and_flow.html
Lab – TSS (Total Suspended Solids)
Turbidity
TSS
Log
Log
Turbidity TSS Amount of solids (erosion)Flow
OutlineHydrologic cycleAquifersBasic groundwater equationsWell drilling and completionGroundwater level and velocityDefinition of key hydrologic parametersGroundwater/surface water interactionHydrologic testsSurface water monitoring/event samplingGround water problems
Ground Water Problems
Quantity(over-pumping)Reduction in aquifer storageDeeper wells, more equipment costsSubsidenceSeawater Intrusion
Quality(contamination)Seawater intrusionPesticide, herbicideIndustrial wastesLandfillsSeptic tanks
Miami, Florida, USA
Chloride concentration (ppm)
水位
http://www.solinst.com/Res/papers/101C4Salt.html
http://www.unep.org/DEWA/water/groundwater/pdfs/Groundwater_33-84_SCREEN.pdf
http://flightline.highline.edu/cwhittington/G110/LectureNotes/WaterSystems.pdf
http://ponce.sdsu.edu/groundwater_utilization_and_sustainability.html
SubsidenceMaterial Compressibility (m2/N) -
medianCompressibility (m2/kg) -
medianClay 1.0E-07 1.0E-06Sand 1.0E-08 1.0E-07Gravel 1.0E-09 1.0E-08Jointed rock 1.0E-09 1.0E-08Competent rock 1.0E-10 1.0E-09
http://ga.water.usgs.gov/edu/earthgwlandsubside.html
This is a picture of the San Joaquin Valley southwest of Mendota in the agricultural area of California. Years and years of pumping ground water for irrigation has caused the land to drop. The top sign shows where the land surface was back in 1925! Compare that to where the man is standing (about 1977).
http://ponce.sdsu.edu/groundwater_utilization_and_sustainability.html
Source: U.S. Geological Survey (Circular 1182) Regions of the United States where land subsidence has been linked to groundwater pumping
http://www.sewrpc.org/watersupplystudy/pdfs/tr-43_chapter-06_preliminary_draft.pdf
http://www.azwater.gov/dwr/Content/Find_by_Program/Recharge/images/Sweet_Water_Recharge_Fac-Smaller_Aerial_Photo.jpg
http://seismo.berkeley.edu/~manga/chia_et_al2001.pdf
1:47am, September 21, 1999Chi Chi, Taiwan
ML 7.3 earthquake
http://www.answers.com/topic/geologic-fault
http://www.geologicresources.com/earthquake_seismic_waves.html
The focus is the point or center where the energy release starts.The epicenter is the point on the Earth's surface directly above the focus of the earthquake
The Mars Climate Observer, an US$125 millionspacecraft, apparently burned up as it was aboutto go into orbit around Mars on September 23, 1999.
The loss was largely blamed on an embarrassingfailure to convert measurements from feet and inches into metric units.
Thank You!