Ahmed A. S. Alothman, M. Ahmed, S. Radjarejesri, G. Ramkumar, R. Prasad, P. Lakshmi, M. Sillanpaa, Subash Thanappan
{"title":"基于统计方法和地理信息系统技术的干旱区或半干旱区地下水水质评价","authors":"Ahmed A. S. Alothman, M. Ahmed, S. Radjarejesri, G. Ramkumar, R. Prasad, P. Lakshmi, M. Sillanpaa, Subash Thanappan","doi":"10.1155/2022/7902301","DOIUrl":null,"url":null,"abstract":"<jats:p>This study takes place in year of 2021 during the premonsoon and postmonsoon seasons and twenty water samples were collected. Chemical factors like chloride, fluoride, sulphate, nitrate, and phosphate were measured in water samples. There is a significant difference in anion dominance between pre- and postmonsoonal (PRM and POM) water samples. The following anions are <jats:inline-formula>\n <math xmlns=\"http://www.w3.org/1998/Math/MathML\" id=\"M1\">\n <mtext>HC</mtext>\n <msub>\n <mrow>\n <mtext>O</mtext>\n </mrow>\n <mrow>\n <mn>3</mn>\n </mrow>\n </msub>\n <mo>></mo>\n <mtext>TDS</mtext>\n <mo>></mo>\n <mtext>C</mtext>\n <msup>\n <mrow>\n <mtext>l</mtext>\n </mrow>\n <mrow>\n <mo>−</mo>\n </mrow>\n </msup>\n <mo>></mo>\n <mtext>S</mtext>\n <msup>\n <mrow>\n <msub>\n <mrow>\n <mtext>O</mtext>\n </mrow>\n <mrow>\n <mn>4</mn>\n </mrow>\n </msub>\n </mrow>\n <mrow>\n <mn>2</mn>\n <mo>−</mo>\n </mrow>\n </msup>\n <mo>></mo>\n <mtext>TH</mtext>\n <mo>></mo>\n <mtext>N</mtext>\n <msub>\n <mrow>\n <mtext>O</mtext>\n </mrow>\n <mrow>\n <mn>3</mn>\n </mrow>\n </msub>\n <mo>></mo>\n <msup>\n <mrow>\n <mtext>F</mtext>\n </mrow>\n <mrow>\n <mo>−</mo>\n </mrow>\n </msup>\n <mo>></mo>\n <mtext>P</mtext>\n <msub>\n <mrow>\n <mtext>O</mtext>\n </mrow>\n <mrow>\n <mn>4</mn>\n </mrow>\n </msub>\n </math>\n </jats:inline-formula> and <jats:inline-formula>\n <math xmlns=\"http://www.w3.org/1998/Math/MathML\" id=\"M2\">\n <mtext>TDS</mtext>\n <mo>></mo>\n <mtext>HC</mtext>\n <msup>\n <mrow>\n <msub>\n <mrow>\n <mtext>O</mtext>\n </mrow>\n <mrow>\n <mn>3</mn>\n </mrow>\n </msub>\n </mrow>\n <mrow>\n <mo>−</mo>\n </mrow>\n </msup>\n <mo>></mo>\n <mtext>S</mtext>\n <msup>\n <mrow>\n <msub>\n <mrow>\n <mtext>O</mtext>\n </mrow>\n <mrow>\n <mn>4</mn>\n </mrow>\n </msub>\n </mrow>\n <mrow>\n <mn>2</mn>\n <mo>−</mo>\n </mrow>\n </msup>\n <mo>></mo>\n <mtext>C</mtext>\n <msup>\n <mrow>\n <mtext>l</mtext>\n </mrow>\n <mrow>\n <mo>−</mo>\n </mrow>\n </msup>\n <mo>></mo>\n <mtext>TH</mtext>\n <mo>></mo>\n <mtext>N</mtext>\n <msup>\n <mrow>\n <msub>\n <mrow>\n <mtext>O</mtext>\n </mrow>\n <mrow>\n <mn>3</mn>\n </mrow>\n </msub>\n </mrow>\n <mrow>\n <mo>−</mo>\n </mrow>\n </msup>\n <mo>></mo>\n <msup>\n <mrow>\n <mtext>F</mtext>\n </mrow>\n <mrow>\n <mo>−</mo>\n </mrow>\n </msup>\n <mo>></mo>\n <mtext>P</mtext>\n <msup>\n <mrow>\n <msub>\n <mrow>\n <mtext>O</mtext>\n </mrow>\n <mrow>\n <mn>4</mn>\n </mrow>\n </msub>\n </mrow>\n <mrow>\n <mo>−</mo>\n </mrow>\n </msup>\n </math>\n </jats:inline-formula>. In both seasons, particular way of cations is <jats:inline-formula>\n <math xmlns=\"http://www.w3.org/1998/Math/MathML\" id=\"M3\">\n <msup>\n <mrow>\n <mtext>Na</mtext>\n </mrow>\n <mrow>\n <mo>+</mo>\n </mrow>\n </msup>\n <mo>></mo>\n <msup>\n <mrow>\n <mtext>Ca</mtext>\n </mrow>\n <mrow>\n <mn>2</mn>\n <mo>+</mo>\n </mrow>\n </msup>\n <mo>></mo>\n <msup>\n <mrow>\n <mtext>Mg</mtext>\n </mrow>\n <mrow>\n <mn>2</mn>\n <mo>+</mo>\n </mrow>\n </msup>\n <mo>></mo>\n <msup>\n <mrow>\n <mtext>K</mtext>\n </mrow>\n <mrow>\n <mo>+</mo>\n </mrow>\n </msup>\n </math>\n </jats:inline-formula>. SAR, Kelly’s ratio, residual sodium carbonate, potential salinity, permeability index, and sodium percentage were used to evaluate the irrigation water quality. To investigate the geochemical regulation and hydrogeochemistry of groundwater, two approaches were used: according to the findings, groundwater in various parts of the investigation was determined to be unfit for human consumption.</jats:p>","PeriodicalId":14195,"journal":{"name":"International Journal of Photoenergy","volume":null,"pages":null},"PeriodicalIF":2.1000,"publicationDate":"2022-09-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":"{\"title\":\"Estimation of Groundwater Quality in Arid Region or Semiarid Region by Using Statistical Methods and Geographical Information System Technique\",\"authors\":\"Ahmed A. S. Alothman, M. Ahmed, S. Radjarejesri, G. Ramkumar, R. Prasad, P. Lakshmi, M. Sillanpaa, Subash Thanappan\",\"doi\":\"10.1155/2022/7902301\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<jats:p>This study takes place in year of 2021 during the premonsoon and postmonsoon seasons and twenty water samples were collected. Chemical factors like chloride, fluoride, sulphate, nitrate, and phosphate were measured in water samples. There is a significant difference in anion dominance between pre- and postmonsoonal (PRM and POM) water samples. The following anions are <jats:inline-formula>\\n <math xmlns=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M1\\\">\\n <mtext>HC</mtext>\\n <msub>\\n <mrow>\\n <mtext>O</mtext>\\n </mrow>\\n <mrow>\\n <mn>3</mn>\\n </mrow>\\n </msub>\\n <mo>></mo>\\n <mtext>TDS</mtext>\\n <mo>></mo>\\n <mtext>C</mtext>\\n <msup>\\n <mrow>\\n <mtext>l</mtext>\\n </mrow>\\n <mrow>\\n <mo>−</mo>\\n </mrow>\\n </msup>\\n <mo>></mo>\\n <mtext>S</mtext>\\n <msup>\\n <mrow>\\n <msub>\\n <mrow>\\n <mtext>O</mtext>\\n </mrow>\\n <mrow>\\n <mn>4</mn>\\n </mrow>\\n </msub>\\n </mrow>\\n <mrow>\\n <mn>2</mn>\\n <mo>−</mo>\\n </mrow>\\n </msup>\\n <mo>></mo>\\n <mtext>TH</mtext>\\n <mo>></mo>\\n <mtext>N</mtext>\\n <msub>\\n <mrow>\\n <mtext>O</mtext>\\n </mrow>\\n <mrow>\\n <mn>3</mn>\\n </mrow>\\n </msub>\\n <mo>></mo>\\n <msup>\\n <mrow>\\n <mtext>F</mtext>\\n </mrow>\\n <mrow>\\n <mo>−</mo>\\n </mrow>\\n </msup>\\n <mo>></mo>\\n <mtext>P</mtext>\\n <msub>\\n <mrow>\\n <mtext>O</mtext>\\n </mrow>\\n <mrow>\\n <mn>4</mn>\\n </mrow>\\n </msub>\\n </math>\\n </jats:inline-formula> and <jats:inline-formula>\\n <math xmlns=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M2\\\">\\n <mtext>TDS</mtext>\\n <mo>></mo>\\n <mtext>HC</mtext>\\n <msup>\\n <mrow>\\n <msub>\\n <mrow>\\n <mtext>O</mtext>\\n </mrow>\\n <mrow>\\n <mn>3</mn>\\n </mrow>\\n </msub>\\n </mrow>\\n <mrow>\\n <mo>−</mo>\\n </mrow>\\n </msup>\\n <mo>></mo>\\n <mtext>S</mtext>\\n <msup>\\n <mrow>\\n <msub>\\n <mrow>\\n <mtext>O</mtext>\\n </mrow>\\n <mrow>\\n <mn>4</mn>\\n </mrow>\\n </msub>\\n </mrow>\\n <mrow>\\n <mn>2</mn>\\n <mo>−</mo>\\n </mrow>\\n </msup>\\n <mo>></mo>\\n <mtext>C</mtext>\\n <msup>\\n <mrow>\\n <mtext>l</mtext>\\n </mrow>\\n <mrow>\\n <mo>−</mo>\\n </mrow>\\n </msup>\\n <mo>></mo>\\n <mtext>TH</mtext>\\n <mo>></mo>\\n <mtext>N</mtext>\\n <msup>\\n <mrow>\\n <msub>\\n <mrow>\\n <mtext>O</mtext>\\n </mrow>\\n <mrow>\\n <mn>3</mn>\\n </mrow>\\n </msub>\\n </mrow>\\n <mrow>\\n <mo>−</mo>\\n </mrow>\\n </msup>\\n <mo>></mo>\\n <msup>\\n <mrow>\\n <mtext>F</mtext>\\n </mrow>\\n <mrow>\\n <mo>−</mo>\\n </mrow>\\n </msup>\\n <mo>></mo>\\n <mtext>P</mtext>\\n <msup>\\n <mrow>\\n <msub>\\n <mrow>\\n <mtext>O</mtext>\\n </mrow>\\n <mrow>\\n <mn>4</mn>\\n </mrow>\\n </msub>\\n </mrow>\\n <mrow>\\n <mo>−</mo>\\n </mrow>\\n </msup>\\n </math>\\n </jats:inline-formula>. In both seasons, particular way of cations is <jats:inline-formula>\\n <math xmlns=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M3\\\">\\n <msup>\\n <mrow>\\n <mtext>Na</mtext>\\n </mrow>\\n <mrow>\\n <mo>+</mo>\\n </mrow>\\n </msup>\\n <mo>></mo>\\n <msup>\\n <mrow>\\n <mtext>Ca</mtext>\\n </mrow>\\n <mrow>\\n <mn>2</mn>\\n <mo>+</mo>\\n </mrow>\\n </msup>\\n <mo>></mo>\\n <msup>\\n <mrow>\\n <mtext>Mg</mtext>\\n </mrow>\\n <mrow>\\n <mn>2</mn>\\n <mo>+</mo>\\n </mrow>\\n </msup>\\n <mo>></mo>\\n <msup>\\n <mrow>\\n <mtext>K</mtext>\\n </mrow>\\n <mrow>\\n <mo>+</mo>\\n </mrow>\\n </msup>\\n </math>\\n </jats:inline-formula>. SAR, Kelly’s ratio, residual sodium carbonate, potential salinity, permeability index, and sodium percentage were used to evaluate the irrigation water quality. 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引用次数: 2
摘要
本研究于2021年季风前和季风后季节进行,收集了20个水样。在水样中测量了氯化物、氟化物、硫酸盐、硝酸盐和磷酸盐等化学因素。阴离子优势在季风前和季风后(PRM和POM)水样中有显著差异。 下面的阴离子是HC O 3 > TDS >c1−> 0 0 42 - >0 - > n - 3 >F−> p o 4TDS b> h3c3−> 0 0 42−> C 1−> TH > NO 3−>F−> p o 4− . 在这两个季节里,阳离子的特殊方式是Na + > + ca2 +Mg 2 + K+ .利用SAR、凯利比、剩余碳酸钠、潜在盐度、渗透指数和钠含量对灌溉水水质进行评价。为了调查地下水的地球化学规律和水文地球化学,采用了两种方法:根据调查结果,确定了各调查地区的地下水不适合人类使用。
Estimation of Groundwater Quality in Arid Region or Semiarid Region by Using Statistical Methods and Geographical Information System Technique
This study takes place in year of 2021 during the premonsoon and postmonsoon seasons and twenty water samples were collected. Chemical factors like chloride, fluoride, sulphate, nitrate, and phosphate were measured in water samples. There is a significant difference in anion dominance between pre- and postmonsoonal (PRM and POM) water samples. The following anions are and . In both seasons, particular way of cations is . SAR, Kelly’s ratio, residual sodium carbonate, potential salinity, permeability index, and sodium percentage were used to evaluate the irrigation water quality. To investigate the geochemical regulation and hydrogeochemistry of groundwater, two approaches were used: according to the findings, groundwater in various parts of the investigation was determined to be unfit for human consumption.
期刊介绍:
International Journal of Photoenergy is a peer-reviewed, open access journal that publishes original research articles as well as review articles in all areas of photoenergy. The journal consolidates research activities in photochemistry and solar energy utilization into a single and unique forum for discussing and sharing knowledge.
The journal covers the following topics and applications:
- Photocatalysis
- Photostability and Toxicity of Drugs and UV-Photoprotection
- Solar Energy
- Artificial Light Harvesting Systems
- Photomedicine
- Photo Nanosystems
- Nano Tools for Solar Energy and Photochemistry
- Solar Chemistry
- Photochromism
- Organic Light-Emitting Diodes
- PV Systems
- Nano Structured Solar Cells