Sedimentation rates and sediment age of the high-altitude cold desert Ramsar Wetland, the Chandratal, inferred from radionuclide (210Pb and 137Cs) technique
In the current scenario, the pristine Himalayan Wetlands are under endangerment due to higher sedimentation rate, including siltation, reduction of ecological value, pollution, and significant anthropogenic encroachment along with advanced civilization. The more increased sedimentation reduces the d...
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| Veröffentlicht in: | Environmental monitoring and assessment 2022-04, Vol.194 (4), p.305-305, Article 305 |
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| description | In the current scenario, the pristine Himalayan Wetlands are under endangerment due to higher sedimentation rate, including siltation, reduction of ecological value, pollution, and significant anthropogenic encroachment along with advanced civilization. The more increased sedimentation reduces the depth and existing expansion of the Wetland. This study articulates the record of sedimentation in the Chandratal present in Western Himalaya, Himachal Pradesh, India, at the altitude of 4300 m. The sedimentation rate of the Chandratal was calculated based on a 1-m core sample considering isotopes of
137
Cs and
210
Pb dating techniques. The present study based on the Constant Rate of Supply (CRS) model of
210
Pb reveals that the Wetland experienced an average sedimentation rate of 1.75 ± 0.04 cm/year during the last 63 years observed from 1953 to 2016. The
137
Cs peak method–based calculated sedimentation rate of the Chandratal is 1.6 ± 0.02 cm/year representing the years for about 62 years from 1954 to 2016. The Wetland’s functional survival prevalence was estimated to be 420 and 459 years based on
210
Pb and
137
Cs dating techniques, respectively. The study communicates that the magnified human interference in the catchment area of the Chandratal is accountable for the faster sedimentation in recent years. |
| doi_str_mv | 10.1007/s10661-022-09984-9 |
| format | Article |
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137
Cs and
210
Pb dating techniques. The present study based on the Constant Rate of Supply (CRS) model of
210
Pb reveals that the Wetland experienced an average sedimentation rate of 1.75 ± 0.04 cm/year during the last 63 years observed from 1953 to 2016. The
137
Cs peak method–based calculated sedimentation rate of the Chandratal is 1.6 ± 0.02 cm/year representing the years for about 62 years from 1954 to 2016. The Wetland’s functional survival prevalence was estimated to be 420 and 459 years based on
210
Pb and
137
Cs dating techniques, respectively. The study communicates that the magnified human interference in the catchment area of the Chandratal is accountable for the faster sedimentation in recent years.</description><identifier>ISSN: 0167-6369</identifier><identifier>EISSN: 1573-2959</identifier><identifier>DOI: 10.1007/s10661-022-09984-9</identifier><identifier>PMID: 35352196</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Altitude ; Anthropogenic factors ; Atmospheric Protection/Air Quality Control/Air Pollution ; Caesium 137 ; Catchment area ; Catchment areas ; Cesium 137 ; Cesium isotopes ; Cesium Radioisotopes ; Dating ; Dating techniques ; Earth and Environmental Science ; Ecology ; Ecotoxicology ; Encroachment ; Environment ; Environmental Management ; Environmental monitoring ; Environmental Monitoring - methods ; Environmental science ; Geologic Sediments ; High altitude ; Humans ; Isotopes ; Lead ; Lead isotopes ; Lead Radioisotopes - analysis ; Monitoring/Environmental Analysis ; Pollution ; Radioisotopes ; Sedimentation ; Sedimentation & deposition ; Sedimentation rates ; Siltation ; Survival ; Wetlands</subject><ispartof>Environmental monitoring and assessment, 2022-04, Vol.194 (4), p.305-305, Article 305</ispartof><rights>The Author(s), under exclusive licence to Springer Nature Switzerland AG 2022</rights><rights>2022. The Author(s), under exclusive licence to Springer Nature Switzerland AG.</rights><rights>The Author(s), under exclusive licence to Springer Nature Switzerland AG 2022.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c305t-c2583eb3bbaea015af29486ad60262af0bb6fde337ab7dbc40aeeb1c3e50569f3</citedby><cites>FETCH-LOGICAL-c305t-c2583eb3bbaea015af29486ad60262af0bb6fde337ab7dbc40aeeb1c3e50569f3</cites><orcidid>0000-0002-2434-9130</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/s10661-022-09984-9$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10661-022-09984-9$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,777,781,27906,27907,41470,42539,51301</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/35352196$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Rout, Sonam Priyadarshini</creatorcontrib><creatorcontrib>Vasudevan, Sivaprakasam</creatorcontrib><title>Sedimentation rates and sediment age of the high-altitude cold desert Ramsar Wetland, the Chandratal, inferred from radionuclide (210Pb and 137Cs) technique</title><title>Environmental monitoring and assessment</title><addtitle>Environ Monit Assess</addtitle><addtitle>Environ Monit Assess</addtitle><description>In the current scenario, the pristine Himalayan Wetlands are under endangerment due to higher sedimentation rate, including siltation, reduction of ecological value, pollution, and significant anthropogenic encroachment along with advanced civilization. The more increased sedimentation reduces the depth and existing expansion of the Wetland. This study articulates the record of sedimentation in the Chandratal present in Western Himalaya, Himachal Pradesh, India, at the altitude of 4300 m. The sedimentation rate of the Chandratal was calculated based on a 1-m core sample considering isotopes of
137
Cs and
210
Pb dating techniques. The present study based on the Constant Rate of Supply (CRS) model of
210
Pb reveals that the Wetland experienced an average sedimentation rate of 1.75 ± 0.04 cm/year during the last 63 years observed from 1953 to 2016. The
137
Cs peak method–based calculated sedimentation rate of the Chandratal is 1.6 ± 0.02 cm/year representing the years for about 62 years from 1954 to 2016. The Wetland’s functional survival prevalence was estimated to be 420 and 459 years based on
210
Pb and
137
Cs dating techniques, respectively. The study communicates that the magnified human interference in the catchment area of the Chandratal is accountable for the faster sedimentation in recent years.</description><subject>Altitude</subject><subject>Anthropogenic factors</subject><subject>Atmospheric Protection/Air Quality Control/Air Pollution</subject><subject>Caesium 137</subject><subject>Catchment area</subject><subject>Catchment areas</subject><subject>Cesium 137</subject><subject>Cesium isotopes</subject><subject>Cesium Radioisotopes</subject><subject>Dating</subject><subject>Dating techniques</subject><subject>Earth and Environmental Science</subject><subject>Ecology</subject><subject>Ecotoxicology</subject><subject>Encroachment</subject><subject>Environment</subject><subject>Environmental Management</subject><subject>Environmental monitoring</subject><subject>Environmental Monitoring - methods</subject><subject>Environmental science</subject><subject>Geologic Sediments</subject><subject>High altitude</subject><subject>Humans</subject><subject>Isotopes</subject><subject>Lead</subject><subject>Lead isotopes</subject><subject>Lead Radioisotopes - analysis</subject><subject>Monitoring/Environmental Analysis</subject><subject>Pollution</subject><subject>Radioisotopes</subject><subject>Sedimentation</subject><subject>Sedimentation & deposition</subject><subject>Sedimentation rates</subject><subject>Siltation</subject><subject>Survival</subject><subject>Wetlands</subject><issn>0167-6369</issn><issn>1573-2959</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kUuLFDEUhYMoTjv6B1xIwM0IE71JKqnOcmh8wYDiA5chqdx01VCPMUkt_C_-WDPdrYILVwm53znnhkPIUw4vOUD7KnPQmjMQgoEx24aZe2TDVSuZMMrcJxvgumVaanNGHuV8AwCmbcxDciaVVIIbvSE_P2MYJpyLK8My0-QKZurmQPPpnbo90iXS0iPth33P3FiGsgak3TIGGjBjKvSTm7JL9BuWsYovD_Sur9dq6MZLOswRU8JAY1qmmhJq2NqNQ7W5EBw--kMml-0uv6AFu34evq_4mDyIbsz45HSek69vXn_ZvWPXH96-311ds06CKqwTaivRS-8dOuDKRWGarXZBg9DCRfBex4BSts63wXcNOETPO4kKlDZRnpOLo-9tWmpsLnYacodj_Qsua7ZCN6pp63a6os__QW-WNc11uzuq0QBc8EqJI9WlJeeE0d6mYXLph-Vg77qzx-5s7c4eurOmip6drFc_Yfgj-V1WBeQRyHU07zH9zf6P7S-A_KWC</recordid><startdate>20220401</startdate><enddate>20220401</enddate><creator>Rout, Sonam Priyadarshini</creator><creator>Vasudevan, Sivaprakasam</creator><general>Springer International Publishing</general><general>Springer Nature B.V</general><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7QH</scope><scope>7QL</scope><scope>7SN</scope><scope>7ST</scope><scope>7T7</scope><scope>7TG</scope><scope>7TN</scope><scope>7U7</scope><scope>7UA</scope><scope>7WY</scope><scope>7WZ</scope><scope>7X7</scope><scope>7XB</scope><scope>87Z</scope><scope>88E</scope><scope>88I</scope><scope>8AO</scope><scope>8C1</scope><scope>8FD</scope><scope>8FI</scope><scope>8FJ</scope><scope>8FK</scope><scope>8FL</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BEZIV</scope><scope>BHPHI</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>FRNLG</scope><scope>FYUFA</scope><scope>F~G</scope><scope>GHDGH</scope><scope>GNUQQ</scope><scope>H97</scope><scope>HCIFZ</scope><scope>K60</scope><scope>K6~</scope><scope>K9.</scope><scope>KL.</scope><scope>L.-</scope><scope>L.G</scope><scope>M0C</scope><scope>M0S</scope><scope>M1P</scope><scope>M2P</scope><scope>M7N</scope><scope>P64</scope><scope>PATMY</scope><scope>PQBIZ</scope><scope>PQBZA</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope><scope>7X8</scope><orcidid>https://orcid.org/0000-0002-2434-9130</orcidid></search><sort><creationdate>20220401</creationdate><title>Sedimentation rates and sediment age of the high-altitude cold desert Ramsar Wetland, the Chandratal, inferred from radionuclide (210Pb and 137Cs) technique</title><author>Rout, Sonam Priyadarshini ; Vasudevan, Sivaprakasam</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c305t-c2583eb3bbaea015af29486ad60262af0bb6fde337ab7dbc40aeeb1c3e50569f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Altitude</topic><topic>Anthropogenic factors</topic><topic>Atmospheric Protection/Air Quality Control/Air Pollution</topic><topic>Caesium 137</topic><topic>Catchment area</topic><topic>Catchment areas</topic><topic>Cesium 137</topic><topic>Cesium isotopes</topic><topic>Cesium Radioisotopes</topic><topic>Dating</topic><topic>Dating techniques</topic><topic>Earth and Environmental Science</topic><topic>Ecology</topic><topic>Ecotoxicology</topic><topic>Encroachment</topic><topic>Environment</topic><topic>Environmental Management</topic><topic>Environmental monitoring</topic><topic>Environmental Monitoring - 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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>Rout, Sonam Priyadarshini</au><au>Vasudevan, Sivaprakasam</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Sedimentation rates and sediment age of the high-altitude cold desert Ramsar Wetland, the Chandratal, inferred from radionuclide (210Pb and 137Cs) technique</atitle><jtitle>Environmental monitoring and assessment</jtitle><stitle>Environ Monit Assess</stitle><addtitle>Environ Monit Assess</addtitle><date>2022-04-01</date><risdate>2022</risdate><volume>194</volume><issue>4</issue><spage>305</spage><epage>305</epage><pages>305-305</pages><artnum>305</artnum><issn>0167-6369</issn><eissn>1573-2959</eissn><abstract>In the current scenario, the pristine Himalayan Wetlands are under endangerment due to higher sedimentation rate, including siltation, reduction of ecological value, pollution, and significant anthropogenic encroachment along with advanced civilization. The more increased sedimentation reduces the depth and existing expansion of the Wetland. This study articulates the record of sedimentation in the Chandratal present in Western Himalaya, Himachal Pradesh, India, at the altitude of 4300 m. The sedimentation rate of the Chandratal was calculated based on a 1-m core sample considering isotopes of
137
Cs and
210
Pb dating techniques. The present study based on the Constant Rate of Supply (CRS) model of
210
Pb reveals that the Wetland experienced an average sedimentation rate of 1.75 ± 0.04 cm/year during the last 63 years observed from 1953 to 2016. The
137
Cs peak method–based calculated sedimentation rate of the Chandratal is 1.6 ± 0.02 cm/year representing the years for about 62 years from 1954 to 2016. The Wetland’s functional survival prevalence was estimated to be 420 and 459 years based on
210
Pb and
137
Cs dating techniques, respectively. The study communicates that the magnified human interference in the catchment area of the Chandratal is accountable for the faster sedimentation in recent years.</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><pmid>35352196</pmid><doi>10.1007/s10661-022-09984-9</doi><tpages>1</tpages><orcidid>https://orcid.org/0000-0002-2434-9130</orcidid></addata></record> |
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| ispartof | Environmental monitoring and assessment, 2022-04, Vol.194 (4), p.305-305, Article 305 |
| issn | 0167-6369 1573-2959 |
| language | eng |
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| source | MEDLINE; SpringerLink Journals |
| subjects | Altitude Anthropogenic factors Atmospheric Protection/Air Quality Control/Air Pollution Caesium 137 Catchment area Catchment areas Cesium 137 Cesium isotopes Cesium Radioisotopes Dating Dating techniques Earth and Environmental Science Ecology Ecotoxicology Encroachment Environment Environmental Management Environmental monitoring Environmental Monitoring - methods Environmental science Geologic Sediments High altitude Humans Isotopes Lead Lead isotopes Lead Radioisotopes - analysis Monitoring/Environmental Analysis Pollution Radioisotopes Sedimentation Sedimentation & deposition Sedimentation rates Siltation Survival Wetlands |
| title | Sedimentation rates and sediment age of the high-altitude cold desert Ramsar Wetland, the Chandratal, inferred from radionuclide (210Pb and 137Cs) technique |
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