Foster S S D, Chilton P J
British Geological Survey, Wallingford, Oxfordshire OX10 8BB, UK.
Philos Trans R Soc Lond B Biol Sci. 2003 Dec 29;358(1440):1957-72. doi: 10.1098/rstb.2003.1380.
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.
人类对地下水资源的开发利用可追溯到最早的文明时期,但大规模的资源开发在很大程度上仅限于过去50年。尽管这一现象在全球范围内存在,但本文重点关注发展中国家以地下水为基础的经济,在过去20年里,加速的资源开发带来了重大的社会和经济效益。这是因为地下水在城市供水和农村生计(包括灌溉农业)中发挥着重要作用。然而,资源开发带来的经济效益很少再投资于地下水管理,人们开始对含水层退化和资源可持续性感到担忧。本文面向广大读者,对含水层退化的三个半独立方面的机制和意义进行了综述。这三个方面分别是:(i)含水层储量的消耗及其对地下水可利用性、陆地和水生生态系统的影响;(ii)由各种不同的诱导水力扰动和土壤分异过程引起的地下水盐渍化;(iii)含水层对与城市发展和农业集约化相关的土地利用和废水排放造成的污染的脆弱性。在全球范围内,用于评估含水层退化状况的数据可靠性存疑、覆盖范围不足且汇编质量差。不得不借助“典型例子”以及对可能经历类似地下水需求和地下污染物负荷条件的类似水文地质环境范围的假设。得出的结论是:(i)含水层退化远不止是一个局部问题,因为20世纪下半叶许多快速社会经济发展的资源基础的可持续性在相当广泛的地理范围内受到威胁;(ii)迫切需要对地下水资源和质量保护进行重大(且早就应该进行)的投资。这些投资包括适当的制度安排、需求侧管理、供给侧增强和污染控制。