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Hydrogeological Mapping for Analyzing of Groundwater Conservation Zone in Sumowono Groundwater Basin, Central Java Province

机译:中爪哇省苏威地下水盆地地下水区盆地地下水区保守区的水文地质测绘

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摘要

Groundwater management at groundwater basins Sumowono needs to be done because of the increasing development of the area. This research is oriented to analyzing groundwater conditions, compiling groundwater conservation zones, and explaining conservation zones' suitability with spatial maps. The method used is mapping hydrogeological conditions such as surface observation of rock types, inventory of hydrogeological points of interest, knowing the patterns and directions of groundwater flow, groundwater utilization, and groundwater sampling to measure the degree of acidity and electrical conductivity. From the mapping results, it is found that the lithology is composed of tuffaceous sandstones and volcanic breccias. Based on the free groundwater table analysis, the free groundwater flow pattern follows the topographic slope, flowing from the high topography on the south and southeast sides to the low topography on the north side of the area. The utilization of groundwater is used for irrigation, domestic and fishery purposes. Measurement of groundwater samples' quality for the degree of acidity is between 5.32-7.98 while the electrical conductivity is between 36-550 µS / cm, and the level of damage due to groundwater utilization is included in the safe zone. The groundwater conservation zone consists of recharge areas and spring protection zones. The result of overlapping between the groundwater conservation zone and the spatial plan map shows suitability as a protection zone.
机译:在地下水盆地Sumowono需求地下水管理,因为该地区的不断发展来完成。这项研究是面向分析地下水状况,编制地下水保护区,并解释与空间地图保护区是否适合。所用的方法映射水文地质条件,例如岩石类型,兴趣点的水文地质的库存的表面观察,知道的模式和地下水流,地下水利用方向,和地下水采样测量酸度和导电性的程度。从映射结果,可以发现,岩性由凝灰质砂岩和火山角砾岩。基于自由地下水位分析,自由地下水流动模式遵循地形坡度,从南部和东南部双方在该地区的北侧地势低的地势高流动。地下水的利用,用于灌溉,生活和渔业的目的。地下水样品质量酸度的测量是5.32-7.98之间,而导电性是36-550μS/厘米之间,并且损坏的由于地下水利用的水平被包含在安全区。地下水保护区由补给区和泉保护区。地下水保护区和所述空间平面地图显示适合作为保护区之间的重叠的结果。

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