印度西孟加拉邦purba medinipur盐碱易发地区的地下水位现状

S. Chakraborty, Subhasish Das
{"title":"印度西孟加拉邦purba medinipur盐碱易发地区的地下水位现状","authors":"S. Chakraborty, Subhasish Das","doi":"10.26480/cic.01.2020.09.13","DOIUrl":null,"url":null,"abstract":"Received 26 October 2020 Accepted 27 November 2020 Available online 03 December 2020 Accurate estimate of groundwater budgeting requires accurate identification of the locations containing freshwater especially if the concerned area is saline prone. Current trends everywhere show that surface water available is low due to low amount of rainfall and other reasons. People are more inclined to use groundwater for irrigation use, domestic use and industrial purpose. According to Ghyben-Herzberg principle, if the groundwater level declines one unit then the seawater intrusion will intrude around forty units towards the inland areas. Therefore the depth interface between the freshwater and saline water will also be shifted towards the inland. For this reason, it is really challenging to determine the present groundwater scenario and predicting groundwater potentials (GWPs) in coastal areas of Purba Medinipur. Here groundwater level is declining day-by-day. But the natural replenishment of groundwater is very low. Nearest rivers Haldi and Rupnarayanpur are less contaminated with seawater intrusion as these rivers are located at eastern coastal parts. Gross drafts from these rivers are becoming very low. Contemporary gross draft from groundwater is enhanced. So it is necessary to determine GWP of study area. Various equations and numerical modelling techniques are available to determine groundwater flux. In this study an attempt has been made to assess the present scenario of groundwater tables in saline prone areas alongwith identification of best method to estimate GWP.","PeriodicalId":303843,"journal":{"name":"CONTEMPORARY ISSUES IN COMPUTING","volume":"434 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2020-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"PRESENT SCENARIO OF GROUNDWATER TABLE IN SALINE PRONE AREAS OF PURBA MEDINIPUR IN WEST BENGAL, INDIA\",\"authors\":\"S. Chakraborty, Subhasish Das\",\"doi\":\"10.26480/cic.01.2020.09.13\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Received 26 October 2020 Accepted 27 November 2020 Available online 03 December 2020 Accurate estimate of groundwater budgeting requires accurate identification of the locations containing freshwater especially if the concerned area is saline prone. Current trends everywhere show that surface water available is low due to low amount of rainfall and other reasons. People are more inclined to use groundwater for irrigation use, domestic use and industrial purpose. According to Ghyben-Herzberg principle, if the groundwater level declines one unit then the seawater intrusion will intrude around forty units towards the inland areas. Therefore the depth interface between the freshwater and saline water will also be shifted towards the inland. For this reason, it is really challenging to determine the present groundwater scenario and predicting groundwater potentials (GWPs) in coastal areas of Purba Medinipur. Here groundwater level is declining day-by-day. But the natural replenishment of groundwater is very low. Nearest rivers Haldi and Rupnarayanpur are less contaminated with seawater intrusion as these rivers are located at eastern coastal parts. Gross drafts from these rivers are becoming very low. Contemporary gross draft from groundwater is enhanced. So it is necessary to determine GWP of study area. Various equations and numerical modelling techniques are available to determine groundwater flux. In this study an attempt has been made to assess the present scenario of groundwater tables in saline prone areas alongwith identification of best method to estimate GWP.\",\"PeriodicalId\":303843,\"journal\":{\"name\":\"CONTEMPORARY ISSUES IN COMPUTING\",\"volume\":\"434 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2020-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"CONTEMPORARY ISSUES IN COMPUTING\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.26480/cic.01.2020.09.13\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"CONTEMPORARY ISSUES IN COMPUTING","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.26480/cic.01.2020.09.13","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

准确的地下水预算估算需要准确识别含有淡水的位置,特别是在相关地区容易含盐的情况下。目前的趋势表明,由于降雨量少和其他原因,可利用的地表水很低。人们更倾向于将地下水用于灌溉、生活和工业用途。根据盖本-赫茨伯格原理,地下水位每下降1个单位,海水就会向内陆地区侵入约40个单位。因此,淡水和咸水之间的深度界面也将向内陆转移。因此,确定Purba Medinipur沿海地区目前的地下水情景和预测地下水潜势(gwp)是非常具有挑战性的。这里的地下水位每天都在下降。但是地下水的自然补给非常少。最近的河流Haldi和Rupnarayanpur受到海水入侵的污染较少,因为这些河流位于东部沿海地区。这些河流的总吃水正变得非常低。当代地下水总抽水量得到了提高。因此,有必要确定研究区全球变暖潜能值。各种方程和数值模拟技术可用于确定地下水通量。在这项研究中,我们试图评估盐渍易发地区地下水位的现状,同时确定估算全球变暖潜能值的最佳方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
PRESENT SCENARIO OF GROUNDWATER TABLE IN SALINE PRONE AREAS OF PURBA MEDINIPUR IN WEST BENGAL, INDIA
Received 26 October 2020 Accepted 27 November 2020 Available online 03 December 2020 Accurate estimate of groundwater budgeting requires accurate identification of the locations containing freshwater especially if the concerned area is saline prone. Current trends everywhere show that surface water available is low due to low amount of rainfall and other reasons. People are more inclined to use groundwater for irrigation use, domestic use and industrial purpose. According to Ghyben-Herzberg principle, if the groundwater level declines one unit then the seawater intrusion will intrude around forty units towards the inland areas. Therefore the depth interface between the freshwater and saline water will also be shifted towards the inland. For this reason, it is really challenging to determine the present groundwater scenario and predicting groundwater potentials (GWPs) in coastal areas of Purba Medinipur. Here groundwater level is declining day-by-day. But the natural replenishment of groundwater is very low. Nearest rivers Haldi and Rupnarayanpur are less contaminated with seawater intrusion as these rivers are located at eastern coastal parts. Gross drafts from these rivers are becoming very low. Contemporary gross draft from groundwater is enhanced. So it is necessary to determine GWP of study area. Various equations and numerical modelling techniques are available to determine groundwater flux. In this study an attempt has been made to assess the present scenario of groundwater tables in saline prone areas alongwith identification of best method to estimate GWP.
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信