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to ensure responsible use of the irrigation systemsto preventover - abstraction of groundwater
the funnel - shaped water tableresultingfrom groundwater over abstraction
Induced recharge from nearby surface water bodies ( such as rivers , lakesresultingfrom groundwater abstraction
datum subsidence of several metres(passive) caused bygroundwater abstraction
hydraulically connected surface water resourcesresultingfrom groundwater abstraction
Flow conditions are preventing the surface water body maintaining or achieving the target status class and the reduction in river flow in the surface water body concerned (resulting solelyfrom groundwater abstraction
potential impactsresultingfrom groundwater abstraction
the state fed(passive) led bygroundwater abstraction technology
a reduction of the quality and quantity of water ,resultingfrom groundwater abstraction
Member States and groundwater abstraction volumes(passive) are set bygroundwater abstraction limits
the occurrence of land subsidence(passive) caused bythe occurrence of land subsidence
the future land subsidence(passive) caused bythe future land subsidence
problems of quality degradation , excessive drawdown of groundwater levels , land subsidence , reduction of spring and baseflows or degradation of groundwater - dependent ecosystemshas causedproblems of quality degradation , excessive drawdown of groundwater levels , land subsidence , reduction of spring and baseflows or degradation of groundwater - dependent ecosystems
groundwater - related subsidence.[17may triggergroundwater - related subsidence.[17
groundwater - related subsidence.[19may triggergroundwater - related subsidence.[19
difficulties of caliber degradation , over the top drawdown of groundwater degrees , land subsidence , aid of spring and baseflows or degradation of groundwater - dependent ecosystemshas prompteddifficulties of caliber degradation , over the top drawdown of groundwater degrees , land subsidence , aid of spring and baseflows or degradation of groundwater - dependent ecosystems
saline groundwater to reach about 10 km inland from the coastline and led to land subsidence at a rate of 2 to 34 centimeters per year ( cm / yr ) in east Jakartahas causedsaline groundwater to reach about 10 km inland from the coastline and led to land subsidence at a rate of 2 to 34 centimeters per year ( cm / yr ) in east Jakarta
a decline in the aquifer levels , which not only increases costs for water pumping , but water pumping is also directly linked with the degradation of the water quality due to higher concentration of natural and man - made contaminants in the remaining reservecausesa decline in the aquifer levels , which not only increases costs for water pumping , but water pumping is also directly linked with the degradation of the water quality due to higher concentration of natural and man - made contaminants in the remaining reserve
streamflow depletion ... understanding the hydraulic connectivity between streams and aquifers is critical to effectively manage water resources for societal needs and ecological conservationcan causestreamflow depletion ... understanding the hydraulic connectivity between streams and aquifers is critical to effectively manage water resources for societal needs and ecological conservation
to decline in groundwater levels within aquifers and drying up or causing severe flow reduction in riverscan leadto decline in groundwater levels within aquifers and drying up or causing severe flow reduction in rivers
The simulated drawdown(passive) caused byThe simulated drawdown
to enhanced vertical displacement of salt water or the so - called well upconing phenomenonleadingto enhanced vertical displacement of salt water or the so - called well upconing phenomenon
10.17014 / ijog.4.3.177 - 188 http://dx.doi.org/10.17014/ijog.vol4no3.20093Significant groundwater level drawdown(passive) caused by10.17014 / ijog.4.3.177 - 188 http://dx.doi.org/10.17014/ijog.vol4no3.20093Significant groundwater level drawdown
a base flow reduction of 5 - 28 % ( Hendriks et al . ... in review[4 ... even though the density of groundwater abstraction points for spray irrigation in these catchments is relatively low compared to some sandy catchments in the province of Noord - Brabant that show stream discharge reductions of 22 % to 56 % due to intensive spray irrigation ( > 6 irrigation points per km 2 ) ( De Louw , 2000[5have causeda base flow reduction of 5 - 28 % ( Hendriks et al . ... in review[4 ... even though the density of groundwater abstraction points for spray irrigation in these catchments is relatively low compared to some sandy catchments in the province of Noord - Brabant that show stream discharge reductions of 22 % to 56 % due to intensive spray irrigation ( > 6 irrigation points per km 2 ) ( De Louw , 2000[5
to pumping and changes in flow directions below the surface andleadsto pumping and changes in flow directions below the surface and
aquifer depletion(passive) caused byaquifer depletion
in saline ( saltwater ) intrusionresultingin saline ( saltwater ) intrusion
senior water uses(passive) caused bysenior water uses
crop damage(passive) caused bycrop damage
the site(passive) may have been caused bythe site
from a reduction in water consumption compared with the resent past ( Mandilaras and Voudouris , 2001has resultedfrom a reduction in water consumption compared with the resent past ( Mandilaras and Voudouris , 2001
a drop in the water table ( 34.64 - 60 metres below surfacealso causeda drop in the water table ( 34.64 - 60 metres below surface
to a reduction in pore water pressure by draining water from the poresleadsto a reduction in pore water pressure by draining water from the pores
overpumping of the aquifersto preventoverpumping of the aquifers
a greater increase in the vulnerability to seawater intrusion for a low - lying coastal aquifer than sea - level risecould causea greater increase in the vulnerability to seawater intrusion for a low - lying coastal aquifer than sea - level rise
to streamflow Il - Moon Chungacontributingto streamflow Il - Moon Chunga
an external diseconomy in the form of declining groundwater levelscausesan external diseconomy in the form of declining groundwater levels
in a decline of groundwater levels and a dramatic increase in salinity through both lateral seawater intrusion and shallow salinization from irrigationhas resultedin a decline of groundwater levels and a dramatic increase in salinity through both lateral seawater intrusion and shallow salinization from irrigation
river and wetland degradationdoes causeriver and wetland degradation
to Musimcheon streamcontributingto Musimcheon stream
aquifer - system compaction(passive) caused byaquifer - system compaction
depletion of groundwater storage until a new dynamic equilibrium is establishedcausesdepletion of groundwater storage until a new dynamic equilibrium is established
increasing global population and strain on surface water resources , which in many ways are more sensitive to climate change than groundwater , saline intrusion(passive) caused byincreasing global population and strain on surface water resources , which in many ways are more sensitive to climate change than groundwater , saline intrusion
the environment(passive) caused bythe environment
to more depressed river flows during a droughtleadingto more depressed river flows during a drought
in decreasing groundwater levels and sea water intrusion phenomenonresultingin decreasing groundwater levels and sea water intrusion phenomenon
to drinking water crisis especially during the premonsoon periodleadingto drinking water crisis especially during the premonsoon period
a cone of depression in the source aquifer and the subsequent reinjection results in mounding in the destination aquifercausesa cone of depression in the source aquifer and the subsequent reinjection results in mounding in the destination aquifer
to groundwater resource depletioncan resultto groundwater resource depletion
out in WAT - RM-11 ( SEPA 2010ais ... setout in WAT - RM-11 ( SEPA 2010a