{"title":"印度尼西亚中爪哇省三宝垄市沿海地区地下水研究中的稳定同位素 18O 和 2H 以及钠吸附比 (SAR) 分析","authors":"T. Putranto, N. Susanto, D. Pangestuti","doi":"10.15244/pjoes/183077","DOIUrl":null,"url":null,"abstract":"Water is the most important basic need for sustaining life, and groundwater remains the primary source of this need in the coastal area of Semarang City. This indicates that the recharge of the source must be monitored as an important part of water resource management. Therefore, this study aimed to determine the origin of groundwater through the analysis of stable isotopes 18 O and 2 H, as well as the calculation of the sodium adsorption ratio (SAR) in Semarang City. The purpose is to determine the origin of deep wells and the quality of water for irrigation. The methods used in this study included hydrogeological mapping, testing groundwater samples, and the analysis of stable isotopes 18 O and 2 H. Semarang City was located in an area with geological components, including the Alluvium and Damar Formation, as well as geological structures such as rectification. Chemical parameter testing was carried out by comparing the SAR aspect of 30 samples with their electrical conductivity (EC). From the analysis of stable isotopes 18 O and 2 H, most of the samples were obtained from deep groundwater, while 1 was found in shallow aquifers. Furthermore, the stable isotope composition of 29 samples still followed the Global Meteoric Water Line (GMWL), indicating that they were obtained from global rainwater and had experienced mixing.","PeriodicalId":510399,"journal":{"name":"Polish Journal of Environmental Studies","volume":"11 17","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-04-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Analysis of Stable Isotopes 18O and 2H and Sodium\\nAdsorption Ratio (SAR) for Groundwater Studies\\nin Coastal Area in Semarang City, Central Java\\nProvince Indonesia\",\"authors\":\"T. Putranto, N. Susanto, D. Pangestuti\",\"doi\":\"10.15244/pjoes/183077\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Water is the most important basic need for sustaining life, and groundwater remains the primary source of this need in the coastal area of Semarang City. This indicates that the recharge of the source must be monitored as an important part of water resource management. Therefore, this study aimed to determine the origin of groundwater through the analysis of stable isotopes 18 O and 2 H, as well as the calculation of the sodium adsorption ratio (SAR) in Semarang City. The purpose is to determine the origin of deep wells and the quality of water for irrigation. The methods used in this study included hydrogeological mapping, testing groundwater samples, and the analysis of stable isotopes 18 O and 2 H. Semarang City was located in an area with geological components, including the Alluvium and Damar Formation, as well as geological structures such as rectification. Chemical parameter testing was carried out by comparing the SAR aspect of 30 samples with their electrical conductivity (EC). From the analysis of stable isotopes 18 O and 2 H, most of the samples were obtained from deep groundwater, while 1 was found in shallow aquifers. Furthermore, the stable isotope composition of 29 samples still followed the Global Meteoric Water Line (GMWL), indicating that they were obtained from global rainwater and had experienced mixing.\",\"PeriodicalId\":510399,\"journal\":{\"name\":\"Polish Journal of Environmental Studies\",\"volume\":\"11 17\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2024-04-11\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Polish Journal of Environmental Studies\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.15244/pjoes/183077\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Polish Journal of Environmental Studies","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.15244/pjoes/183077","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
摘要
水是维持生命最重要的基本需求,而地下水仍然是三宝垄市沿海地区满足这一需求的主要来源。这表明,作为水资源管理的重要组成部分,必须对水源的补给情况进行监测。因此,本研究旨在通过分析稳定同位素 18 O 和 2 H 以及计算钠吸附率 (SAR) 来确定三宝垄市地下水的来源。目的是确定深井的来源和灌溉用水的质量。本研究采用的方法包括水文地质测绘、地下水样本测试以及稳定同位素 18 O 和 2 H 分析。三宝垄市位于一个地质成分包括冲积层和达玛地层以及整流等地质结构的地区。通过比较 30 个样本的 SAR 值和导电率(EC),进行了化学参数测试。从稳定同位素 18 O 和 2 H 的分析结果来看,大部分样本来自深层地下水,1 个样本来自浅层含水层。此外,29 个样本的稳定同位素组成仍然遵循全球陨落水线(GMWL),表明这些样本取自全球雨水并经历过混合。
Analysis of Stable Isotopes 18O and 2H and Sodium
Adsorption Ratio (SAR) for Groundwater Studies
in Coastal Area in Semarang City, Central Java
Province Indonesia
Water is the most important basic need for sustaining life, and groundwater remains the primary source of this need in the coastal area of Semarang City. This indicates that the recharge of the source must be monitored as an important part of water resource management. Therefore, this study aimed to determine the origin of groundwater through the analysis of stable isotopes 18 O and 2 H, as well as the calculation of the sodium adsorption ratio (SAR) in Semarang City. The purpose is to determine the origin of deep wells and the quality of water for irrigation. The methods used in this study included hydrogeological mapping, testing groundwater samples, and the analysis of stable isotopes 18 O and 2 H. Semarang City was located in an area with geological components, including the Alluvium and Damar Formation, as well as geological structures such as rectification. Chemical parameter testing was carried out by comparing the SAR aspect of 30 samples with their electrical conductivity (EC). From the analysis of stable isotopes 18 O and 2 H, most of the samples were obtained from deep groundwater, while 1 was found in shallow aquifers. Furthermore, the stable isotope composition of 29 samples still followed the Global Meteoric Water Line (GMWL), indicating that they were obtained from global rainwater and had experienced mixing.