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1.
湖北省钟祥市汉江河谷平原区浅层孔隙水的脆弱性评价 总被引：1，自引：1，他引：0
以MAPGIS为工作平台,以地下水类型、盖层岩性、地下水埋深为评价指标,利用国际上广泛应用的GOD模型开展了湖北省钟祥市第四系浅层孔隙水的脆弱性评价.研究结果表明:区内浅层孔隙水的脆弱性评分值在0～0.7间,其中极低脆弱性区(评分值=0～0.1)、低脆弱性区(评分值= 0.1～0.3)、中等脆弱性区(评分值=0.3～0.5)、高脆弱性区(评分值=0.5～0.7)和极高脆弱性区(评分值=0.7~10.0)的面积分别占评价区总面积的0.3 %,0.0 %,64.1 %,35.6 %,0. 0 %.换言之,钟祥市汉江河谷平原区浅层孔隙水总体上具有中等脆弱性和高脆弱性,且脆弱性最高的地段几乎全部分布在汉江沿岸.为解决钟祥市工农业发展带来的高污染风险性与地下水具有较高脆弱性这一对明显的矛盾,应加强汉江河谷平原区的地下水资源的管理工作. 相似文献
2.
Sensitivity analysis for the EPIK method of vulnerability assessment in a small karstic aquifer, southern Belgium 总被引：5，自引：0，他引：5
Applying the EPIK parametric method, a vulnerability assessment has been made for a small karstic groundwater system in southern
Belgium. The aquifer is a karstified limestone of Devonian age. A map of intrinsic vulnerability of the aquifer and of the
local water-supply system shows three vulnerability areas. A parameter-balance study and a sensitivity analysis were performed
to evaluate the influence of single parameters on aquifer-vulnerability assessment using the EPIK method. This approach provides
a methodology for the evaluation of vulnerability mapping and for more reliable interpretation of vulnerability indices for
karst groundwater resources.
Received, March 1999/Revised, December 1999, February 2000/Accepted, February 2000 相似文献
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4.
Groundwater vulnerability assessment and sensitivity analysis in Nong Rua, Khon Kaen, Thailand, using a GIS-based SINTACS model 总被引：2，自引：0，他引：2
The SINTACS approach was used to evaluate intrinsic groundwater vulnerability within Nong Rua District, Khon Kaen Province, Thailand. The approach is based on seven environmental variables prepared in the form of GIS data layers. These variables are depth to water level, infiltration capacity, unsaturated zone, soil type, aquifer media, hydraulic conductivity, and slope. The resulting vulnerability map depicts the spatial extent of six classes of vulnerability ranging from very low to extremely high. High and moderate level classes of vulnerability dominated most of the study area. The northwestern, southwestern and central parts of the study area fell under the very high and extremely high vulnerability levels according to this approach. These regions displayed characteristics that indicated their vulnerability such as a high infiltration rate, coarse-texture soil, and shallow depth to groundwater. The statistical correlation coefficient between the nitrate concentration in 87 wells and the SINTACS vulnerability levels was 0.51. Both map removal and single variable sensitivity analyses were performed to observe the influence of specific variables on the model result. The result of this study is useful for guiding strategic planning of groundwater quality management. 相似文献
5.
Ruslan Melian Nicolai Myrlian Alexander Gouriev Constantin Moraru Frank Radstake 《Hydrogeology Journal》1999,7(2):188-196
This paper describes the results of a groundwater quality assessment conducted in two pilot areas, Balatina and Carpineni,
in the Republic of Moldova. Shallow groundwater is the main source of drinking water in rural areas, but reliable data on
its quality are currently insufficient for developing rural water-supply systems with standard designs. The main components
of the study included a field sampling program (including pesticides), an evaluation of the reliability of existing drinking-water
data, an analysis of land use and groundwater-pollution risks using GIS, and the formulation of recommendations to reduce
risks for public health.
Microbiological, nitrate, and selenium contamination are most serious in the villages. These contaminants should be given
priority in addressing drinking-water aspects for rural water-supply development in the two pilot areas. Pollution occurs
mainly due to poor sanitary conditions. In a few shallow wells, traces of selected pesticides were observed, but the effect
of these levels of pesticides on public health is still unclear.
Limited resources of shallow groundwater of good quality occur outside the villages. Additional pilot studies should be implemented
to prove the technical and institutional feasibility of developing and protecting these resources.
Received, September 1997 Revised, September 1998 Accepted, March 1999 相似文献
6.
大型新生代断陷盆地的浅层地下水的脆弱性评价——以山西太原盆地为例 总被引：3，自引：1，他引：2
为开展山西太原盆地的地下水环境保护工作,在GIS平台上利用DRASTIC模型采用地下水位埋深、含水层净补给量、含水层介质、土壤介质、地形、包气带、水力传导系数7个指标评价了盆地浅层孔隙地下水的脆弱性.结果表明:太原市与介休市是盆地内地下水脆弱性最高的地区,同时也是山西省工农业最发达的地区.为解决工农业发展带来的高污染风险性与地下水环境脆弱性这一对明显的矛盾,应加强以上地区的地下水污染防治工作,在开展工作时应坚持"以预防为主,防、治结合"的原则. 相似文献
7.
南水北调工程是优化我国水资源配置、解决北方水资源短缺问题的重大举措。由于南水北调中线工程的调蓄作用,河南省受水地区水源结构的改变对主要的供水水源第四系地下水资源势必造成一定的影响。论文在建立河南平原地下水流数值模型的基础上,按照受水区的分配水量相应压采各城市的浅层地下水开采量,模拟预测南水北调中线工程实施后第四系地下水流系统的演化趋势。预测结果表明: 河南平原受水区浅层地下水位都得到了不同程度的恢复,到2010年,郑州市、新乡市、濮阳市漏斗中心水位相比南水北调中线工程实施前（2007年1月1日）将分别提高6.64m,8.15m和4.15m,很大程度上减轻了地下水的开采压力,有效地恢复了地下水位降落漏斗,缓解了当地水资源的供需矛盾; 但是由于农业灌溉超量开采地下水,河南平原中部和东部的非受水区浅层地下水位仍持续下降; 南部尽管不在受水区范围内,但是供水水源主要来自地表水,所以浅层地下水位无明显变化。结合前人的供需水量预测结果,到2010年,南水北调中线工程分配给受水区的水量与受水区的需水量基本持平。 相似文献
8.
Combining rough sets and GIS techniques to assess aquifer vulnerability characteristics in the semi-arid South Texas 总被引：1，自引：0，他引：1
The coastal semi-arid region of South Texas is undergoing significant growth causing an enormous burden on its limited water
resources. Understanding regional-scale vulnerability of this resource is important for sustainable water resources management
and land use development. In this study, DRASTIC methodology is integrated with an information-analytic technique called rough
sets to understand groundwater vulnerability characteristics in 18 different counties of South Texas. The rough set theory
provides three useful metrics: the strength factor which depicts how vulnerability characteristics occur over the area; the
certainty factor computes the relative probabilities for various vulnerability states within a county and the coverage factor
which elucidates the fraction of a specific vulnerability state present in each county. The coupling of rough sets with GIS
is particularly advantageous to cluster counties exhibiting similar vulnerability characteristics and to obtain other related
insights. The application of the approach indicates that the groundwater vulnerability exhibits greater variability along
the coast than in the interior sections of the area. The shallow aquifer in Aransas, DeWitt, Goliad and Gonzales counties
is the most vulnerable, while the aquifer in Duval, Jim Wells, Karnes, Live Oak, Nueces and San Patricio is less vulnerable.
This approach should prove useful to regional planners and environmental managers entrusted with the protection of groundwater
resources. 相似文献
9.
Zbynek Hrkal 《Hydrogeology Journal》2001,9(4):348-357
The area of the Jizerské Mountains in the northern part of the Czech Republic is known to have suffered from heavy acid atmospheric
deposition which has led to mass extinction of the forest cover in apical parts of the mountains and to degradation of groundwater
quality. A methodology for construction of groundwater vulnerability maps, using a Geographical Information System (GIS),
has been developed as a tool for protecting the groundwater resources.
The maps were constructed by using four subsidiary layers, each of which reflects a particular parameter that governs acidification.
The factors that determine vulnerability are: (1) elevation above sea level, (2) morphology of the terrain, (3) areal extent
and type of vegetation cover, and (4) lithology of the aquifer. A step-wise analysis and application of the data in each of
the layers was accomplished to compare changes in the quality of groundwaters, and to obtain the best weighting factors for
the individual parameters. Changes in alkalinity of the groundwater during the last 30 years were used as a test criterion.
The vulnerability map should be a valuable tool to identify and outline areas most vulnerable to acidification and also areas
considered for reforestation.
Electronic Publication 相似文献
10.
基于GIS的黄河三角洲地下水开发适宜性评价模型 总被引：4，自引：0，他引：4
本文运用地理信息系统（GIS）技术，建立了黄河三角洲地区浅层地下水开发适宜性综合评价模型。评价模型考虑了浅层地下水补给，含水层导水性和储水性，地下水水质，土地利用以及地下水开采对环境影响等多方面因素，模型评价结果为地下水开发适宜性等级分区图。模型评价成果为黄河三角洲地区浅层地下水资源规划和开发利用提供了科学依据。 相似文献
11.
河南平原浅层地下水年龄 总被引：1，自引：0，他引：1
利用3H法和CFCs法对河南平原第四系浅层地下水年龄进行计算,为河南平原浅层地下水可更新能力评价和水循环的研究提供依据。结果表明：2种方法计算出的年龄拟合误差较小（2 a）,均可代表河南平原浅层地下水年龄。总体上,河南平原浅层地下水主要为近50 a以来补给的现代水。太行山、伏牛山、大别山山前地区以及开封西部的黄河两岸等地区浅层地下水年龄均小于30 a,并且顺着地下水流向年龄逐渐增大。从山前地区和黄河两岸至平原区,浅层地下水开采潜力逐渐减小。总体上:平原北部地下水系统地下水年龄较小,地下水循环交替较快;平原南部地下水系统次之;平原中部地下水系统地下水年龄最大,地下水循环交替最慢。 相似文献
12.
Water resources in New Zealand are not evenly distributed across the country which makes it difficult to adequately allocate the use of water resources in every basin. Groundwater is a fundamental water resource in New Zealand for agricultural, industrial and domestic use. Detailed knowledge regarding groundwater recharge potential is a pre-requisite for sustainable groundwater management, including the assessment of its vulnerability to contamination by pollutants. In this study, a comprehensive GIS approach was used to map the potential groundwater recharge zones across New Zealand. National data sets of lithology, slope, aspect, land use, soil drainage and drainage density were converted to raster data sets with a spatial resolution of 500 m × 500 m and superimposed to derive groundwater potential zones. The resultant maps demonstrate that the potential is low in urban and mountainous areas, such as the Southern Alps, whereas the highest potential can be found in regions with large lakes and in the lower elevation plains areas, where Quaternary sediments prevail. The resulting maps can be used to identify areas of high nutrient leaching in zones where high groundwater recharge potential exists. 相似文献
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14.
Groundwater Systems and Resources in the Ordos Basin, China 总被引：1，自引：1，他引：0
HOU Guangcai LIANG Yongping SU Xiaosi ZHAO Zhenghong TAO Zhengping YIN Lihe YANG Yuncheng WANG Xiaoyong 《《地质学报》英文版》2008,82(5)
The Ordos Basin is a large-scale sedimentary basin in northwestern China.The hydrostratigraphic units from bottom to top are pre-Cambrian metamorphic rocks,Lower Paleozoic carbonate rocks,Upper Paleozoic to Mesozoic clastic rocks and Cenozoic deposits.The total thickness is up to 6000 m.Three groundwater systems are present in the Ordos Basin,based on the geological settings,i.e.the karst groundwater system,the Cretaceous clastic groundwater system and the Quaternary groundwater system.This paper describes systematically the groundwater flow patterns of each system and overall assessment of groundwater resources. 相似文献
15.
Robert Mokrik Vytautas Juodkazis Anicetas Štuopis Jonas Mažeika 《Hydrogeology Journal》2014,22(4):925-941
A steady-state groundwater flow model of three Quaternary intertill aquifers in the eastern part of Lithuania has been compiled. The distinction of separate modelled layers is based on hydraulic and isotope-hydrochemistry data criteria. 3H data were used to estimate the corrected groundwater age and were coupled with a groundwater-flow-dynamics model of the Quaternary aquifer system along a cross-section flow pathway from the Baltic Upland recharge area in eastern Lithuania towards the discharge area in the lowlands near the city of Kaunas in central Lithuania. The bicarbonate content in groundwater (214–462 mg/l) increases downgradient towards the lowland area. The other major constituents and total dissolved solids (TDS) have a trend analogous to the bicarbonate. The 14C activity of dissolved inorganic carbon (DIC) in the groundwater ranges from 41.4 to 85.7 pMC. With aquifer-system depth, active precipitation of aqueous solution takes place by dissolving minerals of calcite and dolomite and leakage of “old” groundwater from lower aquifers; the process is also traced by lower 14C and 3H activities and by more positive δ18O values in lowland areas. 相似文献
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17.
Groundwater Systems and Resources in the Ordos Basin,China 总被引：7，自引：0，他引：7
HOU Guangcai LIANG Yongping SU Xiaosi ZHAO Zhenghong TAO Zhengping YIN Lihe YANG Yuncheng WANG Xiaoyong 《《地质学报》英文版》2008,82(5):1061-1069
The Ordos Basin is a large-scale sedimentary basin in northwestern China. The hydrostratigraphic units from bottom to top are pre-Cambrian metamorphic rocks, Lower Paleozoic carbonate rocks, Upper Paleozoic to Mesozoic clastic rocks and Cenozoic deposits. The total thickness is up to 6000 m. Three groundwater systems are present in the Ordos Basin, based on the geological settings, i.e. the karst groundwater system, the Cretaceous clastic groundwater system and the Quaternary groundwater system. This paper describes systematically the groundwater flow patterns of each system and overall assessment of groundwater resources. 相似文献
18.
以内蒙古呼和浩特市平原区地下水系统为例,采用传统DRASTIC方法和同位素3H浓度、3H与14C测年的新方法划分了不同的地下水系统防污性能区,开展了地下水系统防污性评价方法研究。研究结果表明,DRASTIC方法评价结果显示了浅层地下水系统对来自垂向上污染物的固有防御能力;同位素方法评价结果反映了浅、深层含水层系统对来自补给区污染物的防御能力。并且文中指出了两种评价方法各自具有优、缺点。最后指出应根据区域水文地质条件、地下水开发利用现状,以及城市发展规划,采取DRSTIC和同位素辅助方法综合区划地下水系统的防污性能,为环境管理和决策者划分地下水源保护区,制定地下水保护措施提供科学依据。 相似文献
19.
Road salt is pervasively used throughout Canada and in other cold regions during winter. For cities relying exclusively on groundwater, it is important to plan and minimize the application of salt accordingly to mitigate the adverse effects of high chloride concentrations in water supply aquifers. The use of geospatial data (road network, land use, Quaternary and bedrock geology, average annual recharge, water-table depth, soil distribution, topography) in the DRASTIC methodology provides an efficient way of distinguishing salt-vulnerable areas associated with groundwater supply wells, to aid in the implementation of appropriate management practices for road salt application in urban areas. This research presents a GIS-based methodology to accomplish a vulnerability analysis for 12 municipal water supply wells within the City of Guelph, Ontario, Canada. The chloride application density (CAD) value at each supply well is calculated and related to the measured groundwater chloride concentrations and further combined with soil media and aquifer vadose- and saturated-zone properties used in DRASTIC. This combined approach, CAD-DRASTIC, is more accurate than existing groundwater vulnerability mapping methods and can be used by municipalities and other water managers to further improve groundwater protection related to road salt application. 相似文献
20.
滹滏平原地下水系统脆弱性最佳地下水水位埋深探讨 总被引：4，自引：2，他引：2
笔者以滹滏平原为研究区, 采用统计分析的方法, 分析了地下水防污性与地下水资源脆弱性随地下水位埋深之间的变化关系。结果表明, 当地下水位埋深增大时, 地下水防污性增强的地区, 地下水资源脆弱性也增高;通过二者之间变化关系, 认为受地下水位埋深制约及地下水位埋深对二者的不同影响, 存在使地下水系统脆弱性最佳的地下水位埋深区间;通过地下水位埋深对地下水防污性与地下水资源脆弱性影响及其制约关系, 确定滹滏平原淡水区和咸水区地下水系统脆弱性最佳地下水位埋深分别为27~30 m和15~19 m。 相似文献