Groundwater: the processes and global significance of aquifer degradation
The exploitation of groundwater resources for human use dates from the earliest civilizations, but massive resource development has been largely restricted to the past 50 years. Although global in scope, the emphasis of this paper is on groundwater-based economies in a developing nation context, whe...
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Veröffentlicht in: | Philosophical transactions of the Royal Society of London. Series B. Biological sciences 2003-12, Vol.358 (1440), p.1957-1972 |
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container_end_page | 1972 |
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container_issue | 1440 |
container_start_page | 1957 |
container_title | Philosophical transactions of the Royal Society of London. Series B. Biological sciences |
container_volume | 358 |
creator | Foster, S. S. D. Chilton, P. J. |
description | The exploitation of groundwater resources for human use dates from the earliest civilizations, but massive resource development has been largely restricted to the past 50 years. Although global in scope, the emphasis of this paper is on groundwater-based economies in a developing nation context, where accelerated resource development has brought major social and economic benefits over the past 20 years. This results from groundwater's significant role in urban water supply and in rural livelihoods, including irrigated agriculture. However, little of the economic benefit of resource development has been reinvested in groundwater management, and concerns about aquifer degradation and resource sustainability began to arise. A general review, for a broad-based audience, is given of the mechanisms and significance of three semi-independent facets of aquifer degradation. These are (i) depletion of aquifer storage and its effects on groundwater availability, terrestrial and aquatic ecosystems; (ii) groundwater salinization arising from various different processes of induced hydraulic disturbance and soil fractionation; and (iii) vulnerability of aquifers to pollution from land-use and effluent discharge practices related to both urban development and agricultural intensification. Globally, data with which to assess the status of aquifer degradation are of questionable reliability, inadequate coverage and poor compilation. Recourse has to be made to 'type examples' and assumptions about the extension of similar hydrogeological settings likely to be experiencing similar conditions of groundwater demand and subsurface contaminant load. It is concluded that (i) aquifer degradation is much more than a localized problem because the sustainability of the resource base for much of the rapid socio-economic development of the second half of the twentieth century is threatened on quite a widespread geographical basis; and (ii) major (and long overdue) investments in groundwater resource and quality protection are urgently needed. These investments include appropriate institutional provisions, demand-side management, supply-side enhancement and pollution control. |
doi_str_mv | 10.1098/rstb.2003.1380 |
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S. D. ; Chilton, P. J.</creator><contributor>Folke, C. ; Falkenmark, M. ; Falkenmark, M. ; Folke, C.</contributor><creatorcontrib>Foster, S. S. D. ; Chilton, P. J. ; Folke, C. ; Falkenmark, M. ; Falkenmark, M. ; Folke, C.</creatorcontrib><description>The exploitation of groundwater resources for human use dates from the earliest civilizations, but massive resource development has been largely restricted to the past 50 years. Although global in scope, the emphasis of this paper is on groundwater-based economies in a developing nation context, where accelerated resource development has brought major social and economic benefits over the past 20 years. This results from groundwater's significant role in urban water supply and in rural livelihoods, including irrigated agriculture. However, little of the economic benefit of resource development has been reinvested in groundwater management, and concerns about aquifer degradation and resource sustainability began to arise. A general review, for a broad-based audience, is given of the mechanisms and significance of three semi-independent facets of aquifer degradation. These are (i) depletion of aquifer storage and its effects on groundwater availability, terrestrial and aquatic ecosystems; (ii) groundwater salinization arising from various different processes of induced hydraulic disturbance and soil fractionation; and (iii) vulnerability of aquifers to pollution from land-use and effluent discharge practices related to both urban development and agricultural intensification. Globally, data with which to assess the status of aquifer degradation are of questionable reliability, inadequate coverage and poor compilation. Recourse has to be made to 'type examples' and assumptions about the extension of similar hydrogeological settings likely to be experiencing similar conditions of groundwater demand and subsurface contaminant load. It is concluded that (i) aquifer degradation is much more than a localized problem because the sustainability of the resource base for much of the rapid socio-economic development of the second half of the twentieth century is threatened on quite a widespread geographical basis; and (ii) major (and long overdue) investments in groundwater resource and quality protection are urgently needed. 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S. D.</creatorcontrib><creatorcontrib>Chilton, P. J.</creatorcontrib><title>Groundwater: the processes and global significance of aquifer degradation</title><title>Philosophical transactions of the Royal Society of London. Series B. Biological sciences</title><addtitle>Philos Trans R Soc Lond B Biol Sci</addtitle><description>The exploitation of groundwater resources for human use dates from the earliest civilizations, but massive resource development has been largely restricted to the past 50 years. Although global in scope, the emphasis of this paper is on groundwater-based economies in a developing nation context, where accelerated resource development has brought major social and economic benefits over the past 20 years. This results from groundwater's significant role in urban water supply and in rural livelihoods, including irrigated agriculture. However, little of the economic benefit of resource development has been reinvested in groundwater management, and concerns about aquifer degradation and resource sustainability began to arise. A general review, for a broad-based audience, is given of the mechanisms and significance of three semi-independent facets of aquifer degradation. These are (i) depletion of aquifer storage and its effects on groundwater availability, terrestrial and aquatic ecosystems; (ii) groundwater salinization arising from various different processes of induced hydraulic disturbance and soil fractionation; and (iii) vulnerability of aquifers to pollution from land-use and effluent discharge practices related to both urban development and agricultural intensification. Globally, data with which to assess the status of aquifer degradation are of questionable reliability, inadequate coverage and poor compilation. Recourse has to be made to 'type examples' and assumptions about the extension of similar hydrogeological settings likely to be experiencing similar conditions of groundwater demand and subsurface contaminant load. It is concluded that (i) aquifer degradation is much more than a localized problem because the sustainability of the resource base for much of the rapid socio-economic development of the second half of the twentieth century is threatened on quite a widespread geographical basis; and (ii) major (and long overdue) investments in groundwater resource and quality protection are urgently needed. These investments include appropriate institutional provisions, demand-side management, supply-side enhancement and pollution control.</description><subject>Aquifer Degradation</subject><subject>Aquifers</subject><subject>Conservation of Natural Resources</subject><subject>Economic resources</subject><subject>Fresh Water</subject><subject>Geography</subject><subject>Groundwater</subject><subject>Groundwater contamination</subject><subject>Groundwater Pollution</subject><subject>Groundwater recharge</subject><subject>Human Activities</subject><subject>Irrigation</subject><subject>Models, Theoretical</subject><subject>Plant Transpiration - physiology</subject><subject>Resource Depletion</subject><subject>Resource Protection</subject><subject>Soil - analysis</subject><subject>Soil pollution</subject><subject>Surface water</subject><subject>Sustainable agriculture</subject><subject>Water Movements</subject><subject>Water Pollution</subject><subject>Water resources</subject><subject>Water Supply</subject><issn>0962-8436</issn><issn>1471-2970</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2003</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><recordid>eNp9ks1v1DAQxSMEokvhygmhnLhlseP4iwMq9IuKIgQUriPHcXa9ZOOtnbRd_nqczWphhejJsuY3M-89O0meYzTFSIrXPnTlNEeITDER6EEywQXHWS45ephMkGR5JgrCDpInISwQQpLy4nFyEKFccIknycW5d31b3arO-DdpNzfpyjttQjAhVW2VzhpXqiYNdtba2mrVapO6OlXXva2NTysz86pSnXXt0-RRrZpgnm3Pw-T72enV8Yfs8vP5xfG7y0xzSbqMMlJxjkrFkZG8KqqyUExgLmtGac0p44KysmCaGqoVEjnRkhS5kBWiuESaHCZvx7mrvlyaSpu286qBlbdL5dfglIX9SmvnMHM3gJkk0XUc8Go7wLvr3oQOljZo0zSqNa4PgKXkAgkZwekIau9C8KbeLcEIhvRhSB-G9GFIPza8_FvaH3wbdwTCCHi3jhk5bU23hoXrfRuv8PXb1fu4Hd0QKiwuCgRIEIwYEYTDL7va7BsAiADYEHoDG2xfx7-yyH1b_2vmxdi1CJ3zOy-E0qipiOVsLNvQmbtdWfmfwDjhFH6IAj59PEFfTsgZsMjjkZ_b2fzWegN7auJlFdcPvjaOcPypsefo3p5BsHZtFx96vxPqvolfoqrJb91j-LI</recordid><startdate>20031229</startdate><enddate>20031229</enddate><creator>Foster, S. 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These are (i) depletion of aquifer storage and its effects on groundwater availability, terrestrial and aquatic ecosystems; (ii) groundwater salinization arising from various different processes of induced hydraulic disturbance and soil fractionation; and (iii) vulnerability of aquifers to pollution from land-use and effluent discharge practices related to both urban development and agricultural intensification. Globally, data with which to assess the status of aquifer degradation are of questionable reliability, inadequate coverage and poor compilation. Recourse has to be made to 'type examples' and assumptions about the extension of similar hydrogeological settings likely to be experiencing similar conditions of groundwater demand and subsurface contaminant load. It is concluded that (i) aquifer degradation is much more than a localized problem because the sustainability of the resource base for much of the rapid socio-economic development of the second half of the twentieth century is threatened on quite a widespread geographical basis; and (ii) major (and long overdue) investments in groundwater resource and quality protection are urgently needed. These investments include appropriate institutional provisions, demand-side management, supply-side enhancement and pollution control.</abstract><cop>England</cop><pub>The Royal Society</pub><pmid>14728791</pmid><doi>10.1098/rstb.2003.1380</doi><tpages>16</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Aquifer Degradation Aquifers Conservation of Natural Resources Economic resources Fresh Water Geography Groundwater Groundwater contamination Groundwater Pollution Groundwater recharge Human Activities Irrigation Models, Theoretical Plant Transpiration - physiology Resource Depletion Resource Protection Soil - analysis Soil pollution Surface water Sustainable agriculture Water Movements Water Pollution Water resources Water Supply |
title | Groundwater: the processes and global significance of aquifer degradation |
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