利用基于gis的方法确定地下水补给的保留盆地和渗透井区:案例研究:印度尼西亚南苏拉威西省班丹县

L. A. Devianto, Rusmawan Suwarman, A. Rohman, R. Iqbal
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引用次数: 2

摘要

目前,印尼政府在水部门面临的最大挑战是清洁水的供应和质量。造成水资源脆弱性的原因包括土地利用变化、人口快速增长、气候变化以及居住和农业活动。在本研究中,利用GIS作为确定地下水和地表水涵蓄盆地和入渗井区的工具。一些标准改编自参考资料,如SNI 03-2453-2002和马里兰州雨水设计手册。开发了几张坡度在8-30%之间的专题地图;粘土类型;水田、沼地、花园等开发截留流域的空地用地。而入渗井区则需要以地下水位标高大于3 m、岩石渗透率> 2 cm/hr、位于危险区外、无潜在污染为标准的专题图。利用地理信息系统(GIS)对万腾县含水层补给截留盆地和入渗井进行了研究。在此基础上,建立了6个专题图,并提出了保留池区和渗透井区建议。结果表明,在Uluere区(12.99 km2)、Eremerasa区(14.19 km2)、Sinoa区(14.33 km2)和Tompobulu区(18.22 km2)有可能形成保留盆地带。而渗透井区分布在Eremerasa (20.22 km2)、Tompobulu (40.68 km2)和Uluere (45.65 km2)地区。
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Determination of retention basin and infiltration well zone for groundwater recharge using GIS-based approach: Case study: Bantaeng regency, South Sulawesi, Indonesia
Currently, the biggest challenges of the Indonesian Government in water sector is the availability and quality of clean water. The causes of water vulnerability are land use change, rapid population growth, climate change, as well as residential and agricultural activities. In this study, GIS was utilized as tool for determining for retention basin and infiltration well zone as groundwater and surface water conservation. Several criteria were adapted from references such as SNI 03-2453-2002 and Maryland Storm water Design Manual. Several Thematic maps were developed which are slope between 8–30%; clay soil type; open space landuse as paddy field, moor, garden, etc. for developing retention basin zone. While infiltration well zone were needed thematic maps with water table elevation more than 3 m with rock permeability > 2 cm/hr that located outside of hazard zone as well as free of potential pollution as the criteria. Retention basin and infiltration well for aquifer recharge were studied in Bantaeng Regency using GIS tool. Several criteria were set up which allowed building six thematic map and resulting recommendation of retention basin zone as well as infiltration well zone. The results of retention basin zone potentially can be built in Uluere (12.99 km2), Eremerasa (14.19 km2), Sinoa (14.33 km2), and Tompobulu (18.22 km2) districts. While the infiltration well zone are within Eremerasa (20.22 km2) Tompobulu (40.68 km2) and Uluere (45.65 km2) districts.
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