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Chemometric approach to evaluate the chemical behavior of rainwater at high altitude in Shaune Garang catchment, Western Himalaya

The present research has been performed to analyze the chemical behavior of rainwater of the Shaune Garang catchment (32.19° N, 78.20° E) in the Baspa basin, located at a high elevation (4221 m above mean sea level) in the Himachal Himalaya, India. During the study period, sixteen rainwater samples...

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Autores principales: Kumar, Ramesh, Kumar, Rajesh, Singh, Atar, Arif, Mohammad, Kumar, Pankaj, Kumari, Anupma
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9329433/
https://www.ncbi.nlm.nih.gov/pubmed/35896609
http://dx.doi.org/10.1038/s41598-022-15422-0
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author Kumar, Ramesh
Kumar, Rajesh
Singh, Atar
Arif, Mohammad
Kumar, Pankaj
Kumari, Anupma
author_facet Kumar, Ramesh
Kumar, Rajesh
Singh, Atar
Arif, Mohammad
Kumar, Pankaj
Kumari, Anupma
author_sort Kumar, Ramesh
collection PubMed
description The present research has been performed to analyze the chemical behavior of rainwater of the Shaune Garang catchment (32.19° N, 78.20° E) in the Baspa basin, located at a high elevation (4221 m above mean sea level) in the Himachal Himalaya, India. During the study period, sixteen rainwater samples were collected from the Shaune Garang catchment at five different sites. The volume-weighted mean (VWM) pH value of rainwater ranged between 4.59 and 6.73, with an average value of 5.47 ± 0.69, indicating the alkaline nature of rainfall. The total ionic strength in the rainwater ranged from 113.4 to 263.3 µeq/l with an average value of 169.1 ± 40.4 µeq/l. The major dominant cations were Ca(2+) (43.10%) and Na(+) (31.97%) and anions were Cl(−) (37.68%), SO(4)(2−) (28.71%) and NO(3)(−) (23.85%) in rainwater. The ionic ratios were calculated among all the ions. The fraction of (NO(3)(−)  +Cl(−)) with SO(4)(2−) was measured as 2.3, which specifies sour faces of rainwater due to HNO(3), H(2)SO(4), and HCl. A multivariate statistical assessment of rainwater chemistry through Principal Component Analysis (PCA) shows the significance of four factors controlling 78.37% of the total variance, including four-component (PC1 explained 27.89%, PC2 explained 24.98%, PC3 explained 14.64%, PC4 explained 10.85%). However, the individual contribution of Factor 1(PC1) explains 27.89% of the total variance (78.37%) and displays a strong optimistic loading for Ca(2+) and Cl(−). Further, high loading of Ca(2+) and NO(3)(−) and moderate loading of SO(4)(2−) signify the contribution of burning fossil fuel and soil dust. Anthropogenic and natural pollutants influence the composition of rainwater in the pristine Himalayas due to local and long-distance transportation. The study area receives precipitation from the West and North-West, transporting dust and fossil fuel emissions from the Thar Desert and Northwestern countries.
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spelling pubmed-93294332022-07-29 Chemometric approach to evaluate the chemical behavior of rainwater at high altitude in Shaune Garang catchment, Western Himalaya Kumar, Ramesh Kumar, Rajesh Singh, Atar Arif, Mohammad Kumar, Pankaj Kumari, Anupma Sci Rep Article The present research has been performed to analyze the chemical behavior of rainwater of the Shaune Garang catchment (32.19° N, 78.20° E) in the Baspa basin, located at a high elevation (4221 m above mean sea level) in the Himachal Himalaya, India. During the study period, sixteen rainwater samples were collected from the Shaune Garang catchment at five different sites. The volume-weighted mean (VWM) pH value of rainwater ranged between 4.59 and 6.73, with an average value of 5.47 ± 0.69, indicating the alkaline nature of rainfall. The total ionic strength in the rainwater ranged from 113.4 to 263.3 µeq/l with an average value of 169.1 ± 40.4 µeq/l. The major dominant cations were Ca(2+) (43.10%) and Na(+) (31.97%) and anions were Cl(−) (37.68%), SO(4)(2−) (28.71%) and NO(3)(−) (23.85%) in rainwater. The ionic ratios were calculated among all the ions. The fraction of (NO(3)(−)  +Cl(−)) with SO(4)(2−) was measured as 2.3, which specifies sour faces of rainwater due to HNO(3), H(2)SO(4), and HCl. A multivariate statistical assessment of rainwater chemistry through Principal Component Analysis (PCA) shows the significance of four factors controlling 78.37% of the total variance, including four-component (PC1 explained 27.89%, PC2 explained 24.98%, PC3 explained 14.64%, PC4 explained 10.85%). However, the individual contribution of Factor 1(PC1) explains 27.89% of the total variance (78.37%) and displays a strong optimistic loading for Ca(2+) and Cl(−). Further, high loading of Ca(2+) and NO(3)(−) and moderate loading of SO(4)(2−) signify the contribution of burning fossil fuel and soil dust. Anthropogenic and natural pollutants influence the composition of rainwater in the pristine Himalayas due to local and long-distance transportation. The study area receives precipitation from the West and North-West, transporting dust and fossil fuel emissions from the Thar Desert and Northwestern countries. Nature Publishing Group UK 2022-07-27 /pmc/articles/PMC9329433/ /pubmed/35896609 http://dx.doi.org/10.1038/s41598-022-15422-0 Text en © The Author(s) 2022 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) .
spellingShingle Article
Kumar, Ramesh
Kumar, Rajesh
Singh, Atar
Arif, Mohammad
Kumar, Pankaj
Kumari, Anupma
Chemometric approach to evaluate the chemical behavior of rainwater at high altitude in Shaune Garang catchment, Western Himalaya
title Chemometric approach to evaluate the chemical behavior of rainwater at high altitude in Shaune Garang catchment, Western Himalaya
title_full Chemometric approach to evaluate the chemical behavior of rainwater at high altitude in Shaune Garang catchment, Western Himalaya
title_fullStr Chemometric approach to evaluate the chemical behavior of rainwater at high altitude in Shaune Garang catchment, Western Himalaya
title_full_unstemmed Chemometric approach to evaluate the chemical behavior of rainwater at high altitude in Shaune Garang catchment, Western Himalaya
title_short Chemometric approach to evaluate the chemical behavior of rainwater at high altitude in Shaune Garang catchment, Western Himalaya
title_sort chemometric approach to evaluate the chemical behavior of rainwater at high altitude in shaune garang catchment, western himalaya
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9329433/
https://www.ncbi.nlm.nih.gov/pubmed/35896609
http://dx.doi.org/10.1038/s41598-022-15422-0
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