Geochronology of a surface core in the northern basin of Lake Qinghai: Evidence from ^210pb and ^137Cs radionuclides

The radioactivities of ^210Pb and ^137Cs have been measured to estimate the dates of the sediments of a surface core (QH0407-C-2) in the northern basin of Lake Qinghai. The sedimentation rate derived from ^210Pb radioactivity correlates well with that inferred from ^137Cs radioactivity. The dates ca...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Acta geochimica 2006-11, Vol.25 (4), p.301-306
1. Verfasser: 徐海 艾莉 谭亮成 安芷生
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 306
container_issue 4
container_start_page 301
container_title Acta geochimica
container_volume 25
creator 徐海 艾莉 谭亮成 安芷生
description The radioactivities of ^210Pb and ^137Cs have been measured to estimate the dates of the sediments of a surface core (QH0407-C-2) in the northern basin of Lake Qinghai. The sedimentation rate derived from ^210Pb radioactivity correlates well with that inferred from ^137Cs radioactivity. The dates calculated from depth sedimentation rate (cm/a) are similar to those derived from mass accumulation rate (g ·cm^-2 ·a^-1) between 0 5 cm, but are significantly different below 5 cm, which has been ascribed to the compaction of surface sediments during early diagenesis. The dates derived from mass accumulation rate are consistent with those calculated from the AMS ^14C dating model. The precipitation-controlled indices based on the chronology data derived from mass accumulation rate are similar in trends to the precipitation reconstructed from tree rings in adjacent region, which further verifies the reliability of the geochronology data.
doi_str_mv 10.1007/s11631-006-0301-y
format Article
fullrecord <record><control><sourceid>wanfang_jour_proqu</sourceid><recordid>TN_cdi_proquest_journals_204737073</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><cqvip_id>23318313</cqvip_id><wanfj_id>zgdqhx_e200604001</wanfj_id><sourcerecordid>zgdqhx_e200604001</sourcerecordid><originalsourceid>FETCH-LOGICAL-c1781-d4f9e0ae4ee381649b1c6c3f899bfa7e2c44c4a96213c0a9c47a84d509c597f83</originalsourceid><addsrcrecordid>eNpFkU1OIzEQhVsIJCDMAWZnsWPRM1Vt024vUQQMUiSEBNtY1W67u5NgJzZhJhxlzsKduMIYZSRW9aOvXknvFcV3hB8IIH8mxJpjCVCXwAHL3UFxgkrxPNXiMPcAUCpR1cfFaUoLgIpzKU-K11sbzBCDD6vQ71hwjFjaRkfGMhOiZaNnL4NlPsRcomctpbzK3IyWlj2Mvh9o_Hj_y65fx876fOZieGbzCmHdMvIdmyOX08QidWPwW7PKWDorjhytkv32v06Kp5vrx-mvcnZ_eze9mpUGZYNlJ5yyQFZYyxushWrR1Ia7RqnWkbSVEcIIUnWF3AApIyQ1orsEZS6VdA2fFBd73d_kHfleL8I2-vxRv_XdZvijbZUtAwGAmT3fs-sYNlubXr7gCoTkEiTPEO4hE0NK0Tq9juMzxZ1G0J9J6H0SOsvqzyT07kvYDMH3m2yZbsks3biyOseADUfO_wGTVId4</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>204737073</pqid></control><display><type>article</type><title>Geochronology of a surface core in the northern basin of Lake Qinghai: Evidence from ^210pb and ^137Cs radionuclides</title><source>Alma/SFX Local Collection</source><source>SpringerLink Journals - AutoHoldings</source><creator>徐海 艾莉 谭亮成 安芷生</creator><creatorcontrib>徐海 艾莉 谭亮成 安芷生</creatorcontrib><description>The radioactivities of ^210Pb and ^137Cs have been measured to estimate the dates of the sediments of a surface core (QH0407-C-2) in the northern basin of Lake Qinghai. The sedimentation rate derived from ^210Pb radioactivity correlates well with that inferred from ^137Cs radioactivity. The dates calculated from depth sedimentation rate (cm/a) are similar to those derived from mass accumulation rate (g ·cm^-2 ·a^-1) between 0 5 cm, but are significantly different below 5 cm, which has been ascribed to the compaction of surface sediments during early diagenesis. The dates derived from mass accumulation rate are consistent with those calculated from the AMS ^14C dating model. The precipitation-controlled indices based on the chronology data derived from mass accumulation rate are similar in trends to the precipitation reconstructed from tree rings in adjacent region, which further verifies the reliability of the geochronology data.</description><identifier>ISSN: 1000-9426</identifier><identifier>ISSN: 2096-0956</identifier><identifier>EISSN: 1993-0364</identifier><identifier>EISSN: 2365-7499</identifier><identifier>DOI: 10.1007/s11631-006-0301-y</identifier><language>eng</language><publisher>Dordrecht: Springer Nature B.V</publisher><subject>Accumulation ; Cesium radioisotopes ; Diagenesis ; Geochemistry ; Lakes ; Radioactivity ; Sedimentation ; Sedimentation &amp; deposition ; Studies ; 深度沉降率 ; 表面核 ; 质量积累率 ; 青海湖</subject><ispartof>Acta geochimica, 2006-11, Vol.25 (4), p.301-306</ispartof><rights>Science Press 2006</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c1781-d4f9e0ae4ee381649b1c6c3f899bfa7e2c44c4a96213c0a9c47a84d509c597f83</citedby><cites>FETCH-LOGICAL-c1781-d4f9e0ae4ee381649b1c6c3f899bfa7e2c44c4a96213c0a9c47a84d509c597f83</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/85079X/85079X.jpg</thumbnail><link.rule.ids>314,780,784,27923,27924</link.rule.ids></links><search><creatorcontrib>徐海 艾莉 谭亮成 安芷生</creatorcontrib><title>Geochronology of a surface core in the northern basin of Lake Qinghai: Evidence from ^210pb and ^137Cs radionuclides</title><title>Acta geochimica</title><addtitle>Chinese Journal of Geochemistry</addtitle><description>The radioactivities of ^210Pb and ^137Cs have been measured to estimate the dates of the sediments of a surface core (QH0407-C-2) in the northern basin of Lake Qinghai. The sedimentation rate derived from ^210Pb radioactivity correlates well with that inferred from ^137Cs radioactivity. The dates calculated from depth sedimentation rate (cm/a) are similar to those derived from mass accumulation rate (g ·cm^-2 ·a^-1) between 0 5 cm, but are significantly different below 5 cm, which has been ascribed to the compaction of surface sediments during early diagenesis. The dates derived from mass accumulation rate are consistent with those calculated from the AMS ^14C dating model. The precipitation-controlled indices based on the chronology data derived from mass accumulation rate are similar in trends to the precipitation reconstructed from tree rings in adjacent region, which further verifies the reliability of the geochronology data.</description><subject>Accumulation</subject><subject>Cesium radioisotopes</subject><subject>Diagenesis</subject><subject>Geochemistry</subject><subject>Lakes</subject><subject>Radioactivity</subject><subject>Sedimentation</subject><subject>Sedimentation &amp; deposition</subject><subject>Studies</subject><subject>深度沉降率</subject><subject>表面核</subject><subject>质量积累率</subject><subject>青海湖</subject><issn>1000-9426</issn><issn>2096-0956</issn><issn>1993-0364</issn><issn>2365-7499</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNpFkU1OIzEQhVsIJCDMAWZnsWPRM1Vt024vUQQMUiSEBNtY1W67u5NgJzZhJhxlzsKduMIYZSRW9aOvXknvFcV3hB8IIH8mxJpjCVCXwAHL3UFxgkrxPNXiMPcAUCpR1cfFaUoLgIpzKU-K11sbzBCDD6vQ71hwjFjaRkfGMhOiZaNnL4NlPsRcomctpbzK3IyWlj2Mvh9o_Hj_y65fx876fOZieGbzCmHdMvIdmyOX08QidWPwW7PKWDorjhytkv32v06Kp5vrx-mvcnZ_eze9mpUGZYNlJ5yyQFZYyxushWrR1Ia7RqnWkbSVEcIIUnWF3AApIyQ1orsEZS6VdA2fFBd73d_kHfleL8I2-vxRv_XdZvijbZUtAwGAmT3fs-sYNlubXr7gCoTkEiTPEO4hE0NK0Tq9juMzxZ1G0J9J6H0SOsvqzyT07kvYDMH3m2yZbsks3biyOseADUfO_wGTVId4</recordid><startdate>20061101</startdate><enddate>20061101</enddate><creator>徐海 艾莉 谭亮成 安芷生</creator><general>Springer Nature B.V</general><general>State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8BQ</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>D1I</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>JG9</scope><scope>KB.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M2P</scope><scope>M7S</scope><scope>PCBAR</scope><scope>PDBOC</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>Q9U</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20061101</creationdate><title>Geochronology of a surface core in the northern basin of Lake Qinghai: Evidence from ^210pb and ^137Cs radionuclides</title><author>徐海 艾莉 谭亮成 安芷生</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c1781-d4f9e0ae4ee381649b1c6c3f899bfa7e2c44c4a96213c0a9c47a84d509c597f83</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Accumulation</topic><topic>Cesium radioisotopes</topic><topic>Diagenesis</topic><topic>Geochemistry</topic><topic>Lakes</topic><topic>Radioactivity</topic><topic>Sedimentation</topic><topic>Sedimentation &amp; deposition</topic><topic>Studies</topic><topic>深度沉降率</topic><topic>表面核</topic><topic>质量积累率</topic><topic>青海湖</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>徐海 艾莉 谭亮成 安芷生</creatorcontrib><collection>中文科技期刊数据库</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>中文科技期刊数据库-7.0平台</collection><collection>中文科技期刊数据库-自然科学</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>METADEX</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Materials Science &amp; Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection (ProQuest)</collection><collection>Natural Science Collection (ProQuest)</collection><collection>Earth, Atmospheric &amp; Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Materials Science Collection</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Materials Research Database</collection><collection>Materials Science Database</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Science Database (ProQuest)</collection><collection>Engineering Database</collection><collection>Earth, Atmospheric &amp; Aquatic Science Database</collection><collection>Materials Science Collection</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>ProQuest Central Basic</collection><collection>Wanfang Data Journals - Hong Kong</collection><collection>WANFANG Data Centre</collection><collection>Wanfang Data Journals</collection><collection>万方数据期刊 - 香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Acta geochimica</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>徐海 艾莉 谭亮成 安芷生</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Geochronology of a surface core in the northern basin of Lake Qinghai: Evidence from ^210pb and ^137Cs radionuclides</atitle><jtitle>Acta geochimica</jtitle><addtitle>Chinese Journal of Geochemistry</addtitle><date>2006-11-01</date><risdate>2006</risdate><volume>25</volume><issue>4</issue><spage>301</spage><epage>306</epage><pages>301-306</pages><issn>1000-9426</issn><issn>2096-0956</issn><eissn>1993-0364</eissn><eissn>2365-7499</eissn><abstract>The radioactivities of ^210Pb and ^137Cs have been measured to estimate the dates of the sediments of a surface core (QH0407-C-2) in the northern basin of Lake Qinghai. The sedimentation rate derived from ^210Pb radioactivity correlates well with that inferred from ^137Cs radioactivity. The dates calculated from depth sedimentation rate (cm/a) are similar to those derived from mass accumulation rate (g ·cm^-2 ·a^-1) between 0 5 cm, but are significantly different below 5 cm, which has been ascribed to the compaction of surface sediments during early diagenesis. The dates derived from mass accumulation rate are consistent with those calculated from the AMS ^14C dating model. The precipitation-controlled indices based on the chronology data derived from mass accumulation rate are similar in trends to the precipitation reconstructed from tree rings in adjacent region, which further verifies the reliability of the geochronology data.</abstract><cop>Dordrecht</cop><pub>Springer Nature B.V</pub><doi>10.1007/s11631-006-0301-y</doi><tpages>6</tpages></addata></record>
fulltext fulltext
identifier ISSN: 1000-9426
ispartof Acta geochimica, 2006-11, Vol.25 (4), p.301-306
issn 1000-9426
2096-0956
1993-0364
2365-7499
language eng
recordid cdi_proquest_journals_204737073
source Alma/SFX Local Collection; SpringerLink Journals - AutoHoldings
subjects Accumulation
Cesium radioisotopes
Diagenesis
Geochemistry
Lakes
Radioactivity
Sedimentation
Sedimentation & deposition
Studies
深度沉降率
表面核
质量积累率
青海湖
title Geochronology of a surface core in the northern basin of Lake Qinghai: Evidence from ^210pb and ^137Cs radionuclides
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-09T07%3A09%3A28IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-wanfang_jour_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Geochronology%20of%20a%20surface%20core%20in%20the%20northern%20basin%20of%20Lake%20Qinghai%EF%BC%9A%20Evidence%20from%20%5E210pb%20and%20%5E137Cs%20radionuclides&rft.jtitle=Acta%20geochimica&rft.au=%E5%BE%90%E6%B5%B7%20%E8%89%BE%E8%8E%89%20%E8%B0%AD%E4%BA%AE%E6%88%90%20%E5%AE%89%E8%8A%B7%E7%94%9F&rft.date=2006-11-01&rft.volume=25&rft.issue=4&rft.spage=301&rft.epage=306&rft.pages=301-306&rft.issn=1000-9426&rft.eissn=1993-0364&rft_id=info:doi/10.1007/s11631-006-0301-y&rft_dat=%3Cwanfang_jour_proqu%3Ezgdqhx_e200604001%3C/wanfang_jour_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=204737073&rft_id=info:pmid/&rft_cqvip_id=23318313&rft_wanfj_id=zgdqhx_e200604001&rfr_iscdi=true