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GroundWater Science and Monitoring for the Western United States

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Title: GroundWater Science and Monitoring for the Western United States


1
Ground-Water Science and Monitoring for the
Western United States
  • Ground Water Management in the West
  • Western States Water Council
  • Amarillo, Texas
  • Dec. 3-5, 2003
  • Mark T. Anderson
  • Tucson, Arizona


2
Main Topics
  • Challenge of Western water availability
  • Value of long-term monitoring
  • Data collection programs and support for
    hydrologic models
  • Indicators of aquifer condition

3
Southwest Population Growth
South-western states include Arizona,
California, Colorado, Nevada, New Mexico, and
Utah. Source Campbell, Paul R., 1996
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T
E
E
F

N
I

,
E
C
Well D-15-13 22DCC2
A
Total depth 45 feet
F
R
U
S

D
N
A
L

W
O
L
Well D-15-13 23CCB2
E
Total depth 280 feet
100
B

R
E
120
T
A
W

140
O
T

H
T
P
E
D
8
Ground Water Declines in Arizona
Source USGS
9
Houston, Texas
Relation between water level trends and land
subsidence (modified from Kasmarek and others,
1997 Coplin and Galoway, 1999)
10
Ground Water Development
Arizona Ground-Water Withdrawals
  • 16 million water wells in US
  • 800,000 new boreholes/year
  • Source National Ground Water Association

11
Importance of Ground-Water to the West
Percentage of drinking water supplied by ground
water
  • 283,000 wells serve public supplies

12
Well Hydrographs
13
Longest Period of Record for a well in the United
States
Oahu, Hawaii
Continuous record since 1910
Observation Well
14
Initiation of Observation Well Networks in the
arid Southwest
15
Observation Wells by Volume of Ground Water
Pumped Units MGD
16
Improved Methods of Estimating GW Budget Terms
Recharge
  • Change in Storage
  • Recharge
  • Discharge
  • Pumpage

17
Middle Rio Grande Water Budget
0
0
18
Water Level Change in the High Plains Aquifer
(Predevelopment to 1997)
19
Getting Storage Change from Water levels
Volume of Aquifer Drained
X
Water Table After Pumping
Specific Yield
Aquifer Storage Change
20
Storage Change in the High Plains Aquifer (1987
to 1999)
21
Aquifer Storage Change Determined by Gravity
Tucson Basin, Arizona
Gravimeter
22
Tucson Basin Ground-Water BudgetDecember 1997 to
Spring 2001 RECHARGE GWout DS
From D. R. Pool, USGS
23
Tucson Basin Aquifer Storage Change
24
http//www.csr.utexas.edu/grace/
25
Unlocking Our Future Toward a New National
Science Policy
  • House Science Committee revisited the Vannevar
    Bush Doctrine in 1998 to define the Post-Cold War
    agenda for science.
  • New role for science is to support environmental
    decision-making.

26
Summary
  • Systematic data collection important to assess
    trends and calibrate models
  • Improvements in all budget components is
    desirable but water use and storage change yield
    most return
  • Other indicators of aquifer condition in
    addition to water levels are needed

27
Questions?
28
The Hydrologic Cycle
29
Reservoir Contents for the Southwest
Data from Bureau of Reclamation
30
Basin-wide Hydrologic Budgets
  • Many Communities in Arizona are dependent on
    Ground Water drawn from Storage
  • Water also needed to sustain riparian ecosystems

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33
Upper Santa Cruz Basin near Tucson
34
Sustaining Riparian Ecosystems
35
History of Reservoir Construction
36
Well with the longest Period of Record in the
United Kingdom
Chilgrove House well
Continuous record since 1836 160 yrs of record
37
The Nile RiverContinuous record of river stage
from 840 to 1970 AD 1100 years
Calibration of the Nile Rivers Stages
from Dooge 1988
Rhoda Gage, Egypt
38
Systematic streamflow gaging began in 1889 on the
Rio Grande at Embudo, New Mexico
Photo of site in 1889 from USGS Professional
Paper-778
39
Well Hydrographs
40
Active streamflow stations
7,000 Nationwide 3,400 in Western States
41
Cumulative Volume of Water Artificially Recharged
in Arizona
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