利用三维电阻率分析识别印尼中爪哇三宝垄Simpang 5区无承压含水层

Warta Geologi Pub Date : 2020-12-31 DOI:10.7186/WG463202005
S. Supriyadi, Fianti Fianti, R DwiRizki, A. Setyawan, Ronaldo Talapessy
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引用次数: 0

摘要

水是地球的独特属性,对每一个生物都非常重要。地下水的存在只占地球上总水量(海洋、河流、湖泊、极地冰、雨水)的0.61%。本研究的目的是通过二维和三维建模来确定含水层的位置和深度。研究方法为电阻率法,采用斯伦贝谢配置,根据勘察设计采集数据,坐标范围为X:436100, Y:9226880 ~ X:436680, Y:9227640,共7条线。模拟结果表明,目前该区地下水含水层电位呈低电阻率分布。估算了无承压含水层在新邦5区北部至东部的扩展。这可以从同步第一行到第六行的数据看出。但是第7行数据的模式与其他行不同。在这条线上不容易识别地下水盆地的存在。这可能是由于七号线的位置位于Ciputra Mall、Horison Hotel和tologorejo Hospital等耗水量较大的地区,因此地下水条件较差。这可能会导致地面下沉等情况。基于模型的解释结果表明,在边界地下水深度端部变化的情况下,可能存在10 ~ 15 m深度的无承压含水层。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Identification Of Unconfined Aquifer Using 3D Resistivity Analysis At Simpang 5 Area, Semarang, Central Java, Indonesia
Water is a unique property of the Earth and very important to every living organism. The existence of groundwater is only 0.61% of the total water on earth (oceans, rivers, lakes, polar ice, rain). The purpose of this research is to determine the location and depth of the aquifer by using 2D and 3D modeling. The method of research is resistivity method using Schlumberger configuration, where data is collected according to the survey design with coordinate ranging from X:436100, Y:9226880 to X:436680, Y:9227640, and covered by 7 lines. The modeling results indicate that the present groundwater aquifer potential has low resistivity distribution in this area. The spreading of unconfined aquifer is estimated on the north side to the east of Simpang 5 area. This can be seen from syncing the data of line one to six. But the data on line seven is of different patterns with other lines. The existence of groundwater basin is not easily identified on this line. This may be due to the location of Line Seven being located in the area of Ciputra Mall, Horison Hotel and Tlogorejo Hospital with higher consumption of water, thus the decrease in groundwater condition. This may cause conditions such as land subsidence. The results of interpretation based on the modeling show the possibility of an unconfined aquifer with groundwater level at 10-15 m depth with varied end of border groundwater depth.
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