Investigasi Intrusi Air Asin di Kawasan Prospek Bijih Besi Pesisir Nusawungu Kabupaten Cilacap Jawa Tengah Berdasarkan Profil Resistivitas-2D

Sehah Sehah, Z. Irayani, Sukma Sewiji
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Abstract

ABSTRACT −Investigation of saltwater intrusion in Nusawungu Coastal area of Cilacap Regency based on the 2D-resistivity data has been done in April – Juni 2018. The resistivity data acquisition has been carried out using Wenner's configuration on four locations covering of the NWT-01, NWT-02, NWT-03, and NWT-04 with a length as 200 meters. The obtained result is the 2D-resistivity profile of subsurface rocks for each trajectory with a depth of about 30 meters. The rock resistivity values which obtained for each trajectory consists of the NWT-01 is 2.30 – 103.00 Ωm; the NWT-02 is 3.65 – 54.30 Ωm; the NWT-03 is 0.96 – 43.20 Ωm; and the NWT-04 is 2.33 – 70.80 Ωm. Based on the interpretation results, the deep aquifer in each trajectory with a resistivity value of 0.96 - 6.81 Ωm are estimated to be intruded by saltwater, while the shallow aquifers have not been significantly intruded by saltwater. Based on the testing results of the electrical conductivity (DHL) of several water samples taken from some wells around the NWT-01 to NWT-04 trajectory, it is known that all of the water is freshwater. Some well water samples have a rather high electrical conductivity value, such as the well A on the NWT-01 with a value of 740.0 μSi/cm and the well C on the NWT-03 with a value of 894.67 μSi/cm. This is thought to be due to the relatively high salt mineral content in the aquifer rocks.
基于二维阻力剖面的海水铁预报区酸性水入侵调查Nusaungu Seaborne Capacity Mid Reaction Cyclap Capacity
摘要/ ABSTRACT摘要:2018年4月至6月,利用二维电阻率数据对Cilacap Regency Nusawungu沿海地区的盐水入侵进行了调查。利用Wenner配置在NWT-01、NWT-02、NWT-03、NWT-04四个位置进行电阻率数据采集,长度为200米。得到的结果是每条深度约为30米的轨迹的地下岩石二维电阻率剖面。由NWT-01组成的每条轨迹的岩石电阻率值为2.30 ~ 103.00 Ωm;NWT-02为3.65 ~ 54.30 Ωm;NWT-03为0.96 ~ 43.20 Ωm;NWT-04为2.33 ~ 70.80 Ωm。根据解释结果,在电阻率值为0.96 ~ 6.81 Ωm的各轨迹上,估计深层含水层受盐水侵入,浅层含水层受盐水侵入不明显。根据对NWT-01至NWT-04轨道附近部分井的水样电导率(DHL)测试结果,可知该井的水均为淡水。部分井水电导率较高,如NWT-01的a井电导率为740.0 μSi/cm, NWT-03的C井电导率为894.67 μSi/cm。这被认为是由于含水层岩石中含盐量相对较高。
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