利用垂直电测深和Dar Zarrouk参数对印度尼西亚马鲁古雷伊图地区地下水水质的调查

Samsul Bahri, Aditya Ramadhan, None Zulfiah
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引用次数: 0

摘要

本研究的目的是基于垂直电测深(VES)数据和Dar-Zarrouk参数分析,获取含水层保护能力、透光率、含水层厚度等含水层质量相关信息。研究区位于安汶市雷赫图区,共有8个测量点。马鲁古安汶片的地质图则包括雷伊图地区。安汶片由晚上新世—全新世岩性组成,主要为安汶火山岩、礁灰岩和冲积矿床。利用电测深法获取岩石电阻率测量值和层厚信息,并利用IP2WIN软件进行分析。基于VES数据,利用Dar-Zarrouk参数识别含水层属性。该参数包括纵向电导、传递电阻、纵向电阻率和传递电阻率。采用纵向单位电导评价含水层的保护能力等级,传递阻力有利于分析岩石类型和含水层的透过率。根据Dark-Zarrouk参数,其纵向电导S范围为0.0278 ~ 5.1213 mho,防护能力为中等~良好。高S值是由于观测点粘土层较厚所致。该区域横向阻力(T)也足够高,如果与含水层透水率相关,则该区域属于透水率较好的含水层,特别是在2、5、6、7、8层。如果与岩层对比,灰岩和火山岩区比冲积沉积层区有更好的透射率。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Investigation of Groundwater Quality using Vertical Electrical Sounding and Dar Zarrouk Parameter in Leihitu, Maluku, Indonesia
The goal of this research is to obtain information related to aquifer quality, including aquifer protection capacity, transmissivity, and aquifer thickness based on vertical electrical sounding (VES) data and Dar-Zarrouk parameter analysis. The research area is located in Leihitu District, Ambon with 8 measurement points. The Leihitu region is included in the geological map of the Ambon sheet, Maluku, which consists of Late Pliocene - Holocene lithology, specifically Ambon volcanic rocks, reef limestones, and alluvial deposits. The rock resistivity measurements and layer thickness information were obtained using the VES method and analyzed with IP2WIN software. Based on VES data, aquifer properties were identified using Dar-Zarrouk parameters. That parameter consisted of longitudinal conductance, transfer resistance, longitudinal resistivity, and transfer resistivity. Longitudinal unit conductance is applied to evaluate the protective capacity class of the aquifer, the transfer resistance is beneficial for analyzing rock type and aquifer transmissivity. Based on the Dark-Zarrouk parameters, the longitudinal conductance (S) ranged from 0.0278 to 5.1213 mho and was classified as moderate to good protective capacity. The high S value results from a thick layer of clay at the observation point. This area also has a high enough transverse resistance (T) and then if related to aquifer transmissivity, this area is classified as a good transmissivity aquifer, especially at VES 2, VES 5, VES 6, VES 7, and VES 8. If correlated to rock formations, areas with limestone and volcanic rocks have better transmissivity than areas with alluvial deposits.
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