Science, Volume 296, Issues 5574-5577M. King, 2002 |
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Page 1985
... groundwater is not readily apparent , except where discharge is focused at springs or where recharge enters sinkholes . Yet groundwater flow and storage are continually changing in response to human and climatic stresses . Wise ...
... groundwater is not readily apparent , except where discharge is focused at springs or where recharge enters sinkholes . Yet groundwater flow and storage are continually changing in response to human and climatic stresses . Wise ...
Page 1988
... groundwater commonly is referred to as the hyporheic zone , although the transition between groundwater and surface water represents a hydrologic continuum , preventing a precise separation . Compaction progresses steadily despite water ...
... groundwater commonly is referred to as the hyporheic zone , although the transition between groundwater and surface water represents a hydrologic continuum , preventing a precise separation . Compaction progresses steadily despite water ...
Page 1989
... groundwater and surface water also are used to provide information on location and amount of re- charge ( 56 ) and discharge ( 57 ) , and these data enable indirect determination of geother- mal properties of groundwater flow systems ...
... groundwater and surface water also are used to provide information on location and amount of re- charge ( 56 ) and discharge ( 57 ) , and these data enable indirect determination of geother- mal properties of groundwater flow systems ...
Contents
Four Weeks of FREE Access Beginning 31 | 1923 |
The speed at which some | 2021 |
MOULIN | 2093 |
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