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Application of Spatial Analysis for Delineating Groundwater Recharge Zone for Industrial Usage in Tanah Bumbu Regency, South Borneo/Indonesia

机译:空间分析在Tanah Bumbu Regency,South Borneo / Indonesia中划分地下水充电区的应用

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Population growtli in Tanah Bumbu Regency South Borneo Province is causing increased water demand. To fulfil the water needs, the government provides an ahernative water resource by using groundwater as a source of fresh water. The objective of this research is to delineate the groundwater recharge zone. The methods were hydrogeological mapping and spatial analysis approach to delineate the groundwater recharge zone. There were six parameters applied in the research, i.e. hydraulic conductivity, rainfall, slope, soil cover, water table depth, and electrical conductivity. The varies of hydraulic conductivity are 45 m/day (sandstone), 0.94 m/day (limestone), 0.49 m/day (alluvium) and 0.2 m/day (serpentimte). Rainfall has a range from 2,106 to 2,403 mm/year. There are several types of soil cover which are gravel, sand pebbles and clay sandstones. The slopes are varying from below 5° to 40°. The groundwater depth is varying from below 5 m to 10 m depth. Furthermore, the electrical conductivity of groundwater samples has a value around 14.9-1,477 μS/cm. Overlying all parameters in spatial analysis resulted in the recharge area spread in the north, centre, and northwest of the study area.
机译:塔赫·伯巴州南北京省的人口Growtli导致水需求增加。为了满足水需求,政府通过使用地下水作为淡水来源提供敏感的水资源。本研究的目的是描绘地下水补给区。该方法是水文地质测绘和空间分析方法,用于描绘地下水充电区。研究中有六个参数,即液压导电,降雨,斜坡,土壤覆盖,水台深度和导电性。液压导电性的变化为45米/天(砂岩),0.94米/天(石灰石),0.49米/天(胰岛素)和0.2米/天(Serpentimte)。降雨量的范围为2,106至2,403毫米/年。有几种类型的土覆盖物是砾石,砂卵石和粘土砂岩。斜坡从低于5°至40°变化。地下水深度从低于5米至10米的深度变化。此外,地下水样品的电导率具有约14.9-1,477μs/ cm的值。覆盖空间分析中的所有参数导致研究区域的北部,中心和西北地区的充电区域。

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