Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/6081
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dc.contributor.authorPurandara, B. K.-
dc.contributor.authorVaradarajan, N.-
dc.contributor.authorKumar, C. P.-
dc.date.accessioned2021-07-02T20:53:28Z-
dc.date.available2021-07-02T20:53:28Z-
dc.date.issued2004-
dc.identifier.citationJournal of Spatial Hydrology Vol.4, No.2 Fall 2004en_US
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/6081-
dc.description.abstractMass balance calculations carried out for Na, K, Ca, Mg, Cl, SO4 and HCO3 for the study area showed that the major source of contamination is through non-point sources. It is also observed that the river water quality during the non-monsoon season (February, 2000) almost resembles with the groundwater quality of the adjoining aquifer. However, during post-monsoon period (October, 1999) a wide variation was found between groundwater and surface water quality which can be attributed to the movement of fertilizers and agricultural ashes with monsoon flows reaching the stream along with overland flow. The major source of contamination in the Malaprabha river was found to be due to the non-point sources (more than 90%). An immediate attention from the concerned authorities is required in order to protect the land from further salinization.en_US
dc.language.isoenen_US
dc.publisherBrigham Young Universityen_US
dc.subjectMass balanceen_US
dc.subjectSalinityen_US
dc.subjectAdvectionen_US
dc.subjectBase flowen_US
dc.titleApplication of Chemical Mass Balance to Water Quality Data of Malaprabha Riveren_US
dc.typeArticleen_US
Appears in Collections:Research papers in International Journals

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