Groundwater quality distribution by geostatistical investigation (GIS), Nile Delta, Northern Egypt

Mohamed ElKashouty
{"title":"Groundwater quality distribution by geostatistical investigation (GIS), Nile Delta, Northern Egypt","authors":"Mohamed ElKashouty","doi":"10.5897/JECE2018.0437","DOIUrl":null,"url":null,"abstract":"The Nile Delta represents two-thirds of agricultural output with low precipitation and population growth that depletes the groundwater. The Quaternary aquifer is consisted of Holocene (aquitard) underlain by Pleistocene (aquifer), and groundwater flows from south to north, northwest, and northeast directions. The total dissolved solids (TDS) concentration increases toward the western and northeastern part in 1997 by seawater intrusion and irrigation practices. The TDS concentration anomalies were in the north and east, and are attributed to pumping within 2003, 2010, and 2013 periods. There is a good match between hydrogeochemistry (TDS content) and hydrogeology (groundwater flow) with the TDS concentration change found to decline mainly in the southwestern and northeastern part within 1997, 2003, and 2013 periods. The TDS concentration change declines toward the northern part of the eastern Nile Delta by increase in potentiometric surface from the River Nile in 2010. The geostatistical application (GIS) is used to determine the groundwater quality and hydrogeochemical parameters distribution, which is accomplished by ordinary kriging. The first produced map is the default options, while the next map (2nd) incorporated more of the spatial relationships constructed. When the latter is estimated, the exploratory spatial data investigation (ESDA) techniques check parameters extent. Trends were deleted and spatial autocorrelation was modeled. The ESDA and geostatistical techniques were used and the surfaces of the major ions were found more accurate. The third surface showed critical probability that TDS concentration threshold point increase drinking and irrigation purposes in the northeastern part and decrease in the southwestern parts of the Nile Delta. The default kriging is the best for mapping the hydrogeochemical parameters. \n \n Key words: Total dissolved solids (TDS) change, major ions, geostatistical tools, GIS, Nile Delta.","PeriodicalId":254567,"journal":{"name":"Journal of Environmental Chemistry and Ecotoxicology","volume":"27 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2019-01-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Environmental Chemistry and Ecotoxicology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5897/JECE2018.0437","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 3

Abstract

The Nile Delta represents two-thirds of agricultural output with low precipitation and population growth that depletes the groundwater. The Quaternary aquifer is consisted of Holocene (aquitard) underlain by Pleistocene (aquifer), and groundwater flows from south to north, northwest, and northeast directions. The total dissolved solids (TDS) concentration increases toward the western and northeastern part in 1997 by seawater intrusion and irrigation practices. The TDS concentration anomalies were in the north and east, and are attributed to pumping within 2003, 2010, and 2013 periods. There is a good match between hydrogeochemistry (TDS content) and hydrogeology (groundwater flow) with the TDS concentration change found to decline mainly in the southwestern and northeastern part within 1997, 2003, and 2013 periods. The TDS concentration change declines toward the northern part of the eastern Nile Delta by increase in potentiometric surface from the River Nile in 2010. The geostatistical application (GIS) is used to determine the groundwater quality and hydrogeochemical parameters distribution, which is accomplished by ordinary kriging. The first produced map is the default options, while the next map (2nd) incorporated more of the spatial relationships constructed. When the latter is estimated, the exploratory spatial data investigation (ESDA) techniques check parameters extent. Trends were deleted and spatial autocorrelation was modeled. The ESDA and geostatistical techniques were used and the surfaces of the major ions were found more accurate. The third surface showed critical probability that TDS concentration threshold point increase drinking and irrigation purposes in the northeastern part and decrease in the southwestern parts of the Nile Delta. The default kriging is the best for mapping the hydrogeochemical parameters. Key words: Total dissolved solids (TDS) change, major ions, geostatistical tools, GIS, Nile Delta.
基于地理统计调查(GIS)的埃及北部尼罗河三角洲地下水水质分布
尼罗河三角洲占农业产量的三分之二,降水少,人口增长导致地下水枯竭。第四纪含水层由全新世(含水层)下覆更新世(含水层)组成,地下水从南向北、西北和东北方向流动。1997年由于海水入侵和灌溉,总溶解固形物(TDS)浓度向西部和东北部增加。TDS浓度异常分布在北部和东部,主要是由2003年、2010年和2013年的抽水引起的。水文地球化学(TDS含量)与水文地质(地下水流量)吻合较好,1997年、2003年和2013年期间,TDS浓度变化主要在西南部和东北部下降。TDS浓度变化在东尼罗河三角洲北部呈下降趋势,且呈上升趋势。利用地质统计学应用(GIS)确定地下水水质和水文地球化学参数分布,这是由普通克里格法完成的。第一个生成的地图是默认选项,而下一个地图(第二个)包含了更多构建的空间关系。当后者被估计时,探索性空间数据调查(ESDA)技术检查参数程度。趋势被删除,空间自相关建模。利用ESDA和地质统计技术,发现主要离子的表面更准确。第三面呈现出TDS浓度阈值点在尼罗河三角洲东北部增加饮用和灌溉用途、在西南地区减少的临界概率。默认克里格是绘制水文地球化学参数的最佳方法。关键词:总溶解固形物变化,主要离子,地质统计工具,GIS,尼罗河三角洲
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
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