Assessment of landuse change impact on runoff and sediment yield of Patiala-Ki-Rao watershed in Shivalik foot-hills of northwest India
Landuse change significantly alters the hydrologic characteristics of the land surface within a watershed. In the present study, the impact of landuse change (2006–2016) on runoff and sediment yield has been assessed in Patiala-Ki-Rao watershed (5140 ha) located in Shivalik foot-hills, using remote...
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description | Landuse change significantly alters the hydrologic characteristics of the land surface within a watershed. In the present study, the impact of landuse change (2006–2016) on runoff and sediment yield has been assessed in Patiala-Ki-Rao watershed (5140 ha) located in
Shivalik
foot-hills, using remote sensing, geographical information system (GIS), and Water Erosion Prediction Project (WEPP) watershed model. The watershed has seven major landuse classes, namely agriculture, built-up, fallow land, forest, grass land, streams, and water bodies. The landuse change analysis indicated that the area under all the landuses decreased except built-up that increased by 372.27 ha (112.04%). Forest is the most affected landuse among all watershed landuses that shrinked by 194.90 ha followed by agriculture (64.57 ha), grass land (50.81 ha), streams (30.42 ha), fallow land (21.86 ha), and water bodies (9.72 ha). Runoff and sediment yield for the landuse of the years 2006 and 2016 were simulated by the WEPP model using two climate scenarios (2006 and 2016). The simulated runoff, sediment yield, and sediment delivery ratio increased by 18.62%, 48.04%, and 32.23% under Climate-2006 and 26.78%, 30.23%, and 16.09% under Climate-2016 due to change in landuse during a period of 10 years. This clearly indicates that landuse change in 10 years has greatly influenced the hydrology of the watershed and requires urgent land allocation policy in place for sustainable development in the area. |
doi_str_mv | 10.1007/s10661-019-7932-z |
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Shivalik
foot-hills, using remote sensing, geographical information system (GIS), and Water Erosion Prediction Project (WEPP) watershed model. The watershed has seven major landuse classes, namely agriculture, built-up, fallow land, forest, grass land, streams, and water bodies. The landuse change analysis indicated that the area under all the landuses decreased except built-up that increased by 372.27 ha (112.04%). Forest is the most affected landuse among all watershed landuses that shrinked by 194.90 ha followed by agriculture (64.57 ha), grass land (50.81 ha), streams (30.42 ha), fallow land (21.86 ha), and water bodies (9.72 ha). Runoff and sediment yield for the landuse of the years 2006 and 2016 were simulated by the WEPP model using two climate scenarios (2006 and 2016). The simulated runoff, sediment yield, and sediment delivery ratio increased by 18.62%, 48.04%, and 32.23% under Climate-2006 and 26.78%, 30.23%, and 16.09% under Climate-2016 due to change in landuse during a period of 10 years. This clearly indicates that landuse change in 10 years has greatly influenced the hydrology of the watershed and requires urgent land allocation policy in place for sustainable development in the area.</description><identifier>ISSN: 0167-6369</identifier><identifier>EISSN: 1573-2959</identifier><identifier>DOI: 10.1007/s10661-019-7932-z</identifier><identifier>PMID: 31741091</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Agricultural production ; Agriculture ; Atmospheric Protection/Air Quality Control/Air Pollution ; Climate ; Climate change ; Climate models ; Computer simulation ; Earth and Environmental Science ; Ecology ; Ecotoxicology ; Environment ; Environmental Management ; Environmental Monitoring ; Environmental science ; Erosion ; Fallow land ; Feet ; Foothills ; Forests ; Geographic information systems ; Geographical information systems ; Geologic Sediments - analysis ; Grasses ; Hills ; Hydrology ; India ; Information systems ; Models, Theoretical ; Monitoring/Environmental Analysis ; Poaceae ; Remote sensing ; Rivers ; Rivers - chemistry ; Runoff ; Satellite navigation systems ; Sediment ; Sediment yield ; Sediments ; Streams ; Sustainable development ; Water ; Water erosion ; Water Movements ; Watersheds</subject><ispartof>Environmental monitoring and assessment, 2019-12, Vol.191 (12), p.757-14, Article 757</ispartof><rights>Springer Nature Switzerland AG 2019</rights><rights>Environmental Monitoring and Assessment is a copyright of Springer, (2019). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c372t-eac2fc6c8a83bf7d06af80fba62a016a03a6414078aab30fd5860a5df656cd283</citedby><cites>FETCH-LOGICAL-c372t-eac2fc6c8a83bf7d06af80fba62a016a03a6414078aab30fd5860a5df656cd283</cites><orcidid>0000-0002-2565-7880</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10661-019-7932-z$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10661-019-7932-z$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/31741091$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Sushanth, Kallem</creatorcontrib><creatorcontrib>Bhardwaj, Anil</creatorcontrib><title>Assessment of landuse change impact on runoff and sediment yield of Patiala-Ki-Rao watershed in Shivalik foot-hills of northwest India</title><title>Environmental monitoring and assessment</title><addtitle>Environ Monit Assess</addtitle><addtitle>Environ Monit Assess</addtitle><description>Landuse change significantly alters the hydrologic characteristics of the land surface within a watershed. In the present study, the impact of landuse change (2006–2016) on runoff and sediment yield has been assessed in Patiala-Ki-Rao watershed (5140 ha) located in
Shivalik
foot-hills, using remote sensing, geographical information system (GIS), and Water Erosion Prediction Project (WEPP) watershed model. The watershed has seven major landuse classes, namely agriculture, built-up, fallow land, forest, grass land, streams, and water bodies. The landuse change analysis indicated that the area under all the landuses decreased except built-up that increased by 372.27 ha (112.04%). Forest is the most affected landuse among all watershed landuses that shrinked by 194.90 ha followed by agriculture (64.57 ha), grass land (50.81 ha), streams (30.42 ha), fallow land (21.86 ha), and water bodies (9.72 ha). Runoff and sediment yield for the landuse of the years 2006 and 2016 were simulated by the WEPP model using two climate scenarios (2006 and 2016). The simulated runoff, sediment yield, and sediment delivery ratio increased by 18.62%, 48.04%, and 32.23% under Climate-2006 and 26.78%, 30.23%, and 16.09% under Climate-2016 due to change in landuse during a period of 10 years. This clearly indicates that landuse change in 10 years has greatly influenced the hydrology of the watershed and requires urgent land allocation policy in place for sustainable development in the area.</description><subject>Agricultural production</subject><subject>Agriculture</subject><subject>Atmospheric Protection/Air Quality Control/Air Pollution</subject><subject>Climate</subject><subject>Climate change</subject><subject>Climate models</subject><subject>Computer simulation</subject><subject>Earth and Environmental Science</subject><subject>Ecology</subject><subject>Ecotoxicology</subject><subject>Environment</subject><subject>Environmental Management</subject><subject>Environmental Monitoring</subject><subject>Environmental science</subject><subject>Erosion</subject><subject>Fallow land</subject><subject>Feet</subject><subject>Foothills</subject><subject>Forests</subject><subject>Geographic information systems</subject><subject>Geographical information systems</subject><subject>Geologic Sediments - 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Academic</collection><jtitle>Environmental monitoring and assessment</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Sushanth, Kallem</au><au>Bhardwaj, Anil</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Assessment of landuse change impact on runoff and sediment yield of Patiala-Ki-Rao watershed in Shivalik foot-hills of northwest India</atitle><jtitle>Environmental monitoring and assessment</jtitle><stitle>Environ Monit Assess</stitle><addtitle>Environ Monit Assess</addtitle><date>2019-12-01</date><risdate>2019</risdate><volume>191</volume><issue>12</issue><spage>757</spage><epage>14</epage><pages>757-14</pages><artnum>757</artnum><issn>0167-6369</issn><eissn>1573-2959</eissn><abstract>Landuse change significantly alters the hydrologic characteristics of the land surface within a watershed. In the present study, the impact of landuse change (2006–2016) on runoff and sediment yield has been assessed in Patiala-Ki-Rao watershed (5140 ha) located in
Shivalik
foot-hills, using remote sensing, geographical information system (GIS), and Water Erosion Prediction Project (WEPP) watershed model. The watershed has seven major landuse classes, namely agriculture, built-up, fallow land, forest, grass land, streams, and water bodies. The landuse change analysis indicated that the area under all the landuses decreased except built-up that increased by 372.27 ha (112.04%). Forest is the most affected landuse among all watershed landuses that shrinked by 194.90 ha followed by agriculture (64.57 ha), grass land (50.81 ha), streams (30.42 ha), fallow land (21.86 ha), and water bodies (9.72 ha). Runoff and sediment yield for the landuse of the years 2006 and 2016 were simulated by the WEPP model using two climate scenarios (2006 and 2016). The simulated runoff, sediment yield, and sediment delivery ratio increased by 18.62%, 48.04%, and 32.23% under Climate-2006 and 26.78%, 30.23%, and 16.09% under Climate-2016 due to change in landuse during a period of 10 years. This clearly indicates that landuse change in 10 years has greatly influenced the hydrology of the watershed and requires urgent land allocation policy in place for sustainable development in the area.</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><pmid>31741091</pmid><doi>10.1007/s10661-019-7932-z</doi><tpages>14</tpages><orcidid>https://orcid.org/0000-0002-2565-7880</orcidid></addata></record> |
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subjects | Agricultural production Agriculture Atmospheric Protection/Air Quality Control/Air Pollution Climate Climate change Climate models Computer simulation Earth and Environmental Science Ecology Ecotoxicology Environment Environmental Management Environmental Monitoring Environmental science Erosion Fallow land Feet Foothills Forests Geographic information systems Geographical information systems Geologic Sediments - analysis Grasses Hills Hydrology India Information systems Models, Theoretical Monitoring/Environmental Analysis Poaceae Remote sensing Rivers Rivers - chemistry Runoff Satellite navigation systems Sediment Sediment yield Sediments Streams Sustainable development Water Water erosion Water Movements Watersheds |
title | Assessment of landuse change impact on runoff and sediment yield of Patiala-Ki-Rao watershed in Shivalik foot-hills of northwest India |
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