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Determining contribution of sand dune potential sources using radionuclides, trace and major elements in central Iran
The present research describes a first attempt to use quantitative fingerprinting to quantify source contributions of sand dunes. Forty-nine surface samples from the main potential sources within Yazd-Ardekan Plain in the central Iran were collected and compared with eight samples of sand dunes, col...
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Published in: | Arabian journal of geosciences 2017-04, Vol.10 (7), p.1-9, Article 163 |
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description | The present research describes a first attempt to use quantitative fingerprinting to quantify source contributions of sand dunes. Forty-nine surface samples from the main potential sources within Yazd-Ardekan Plain in the central Iran were collected and compared with eight samples of sand dunes, collected on various sites of Ashkzar erg. Three major categories of sand dune source were identified: young terraces and gravel fans (Qt
2
), clay flat (Qc), and gypsiferous marl (Egm). After sample preparation, concentrations of geochemical elements such as rare earth element (REE), major and trace elements, and isotopes of strontium (
87
Sr and
86
Sr) and neodymium (
143
Nd and
144
Nd) were measured. The results indicated, based on discriminant function analysis, 81.6% of the samples to be correctly assigned to their source areas. The mean contributions from Qt
2
, Qc, and Egm sources in the study area were estimated as 59, 30, and 11%, respectively. The efficiency coefficient for mixing model was calculated to be 0.99, which represents that the fingerprinting technique has a great potential for apportionment of sand dune sources. |
doi_str_mv | 10.1007/s12517-017-2917-0 |
format | article |
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2
), clay flat (Qc), and gypsiferous marl (Egm). After sample preparation, concentrations of geochemical elements such as rare earth element (REE), major and trace elements, and isotopes of strontium (
87
Sr and
86
Sr) and neodymium (
143
Nd and
144
Nd) were measured. The results indicated, based on discriminant function analysis, 81.6% of the samples to be correctly assigned to their source areas. The mean contributions from Qt
2
, Qc, and Egm sources in the study area were estimated as 59, 30, and 11%, respectively. The efficiency coefficient for mixing model was calculated to be 0.99, which represents that the fingerprinting technique has a great potential for apportionment of sand dune sources.</description><identifier>ISSN: 1866-7511</identifier><identifier>EISSN: 1866-7538</identifier><identifier>DOI: 10.1007/s12517-017-2917-0</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Clay ; Dunes ; Earth ; Earth and Environmental Science ; Earth science ; Earth Sciences ; Fingerprinting ; Function analysis ; Gravel ; Isotopes ; Major elements ; Marl ; Neodymium ; Neodymium isotopes ; Original Paper ; Radioisotopes ; Radionuclide kinetics ; Rare earth elements ; Sample preparation ; Sand ; Strontium ; Strontium 87 ; Strontium isotopes ; Terraces ; Trace elements</subject><ispartof>Arabian journal of geosciences, 2017-04, Vol.10 (7), p.1-9, Article 163</ispartof><rights>Saudi Society for Geosciences 2017</rights><rights>Copyright Springer Science & Business Media 2017</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a339t-a7de642a0b04099ecb499bbefa7d7d89ef25c582f70d0fd7126f01a5fea337723</citedby><cites>FETCH-LOGICAL-a339t-a7de642a0b04099ecb499bbefa7d7d89ef25c582f70d0fd7126f01a5fea337723</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Gholami, Hamid</creatorcontrib><creatorcontrib>Middleton, Nick</creatorcontrib><creatorcontrib>Nazari Samani, Ali Akbar</creatorcontrib><creatorcontrib>Wasson, Robert</creatorcontrib><title>Determining contribution of sand dune potential sources using radionuclides, trace and major elements in central Iran</title><title>Arabian journal of geosciences</title><addtitle>Arab J Geosci</addtitle><description>The present research describes a first attempt to use quantitative fingerprinting to quantify source contributions of sand dunes. Forty-nine surface samples from the main potential sources within Yazd-Ardekan Plain in the central Iran were collected and compared with eight samples of sand dunes, collected on various sites of Ashkzar erg. Three major categories of sand dune source were identified: young terraces and gravel fans (Qt
2
), clay flat (Qc), and gypsiferous marl (Egm). After sample preparation, concentrations of geochemical elements such as rare earth element (REE), major and trace elements, and isotopes of strontium (
87
Sr and
86
Sr) and neodymium (
143
Nd and
144
Nd) were measured. The results indicated, based on discriminant function analysis, 81.6% of the samples to be correctly assigned to their source areas. The mean contributions from Qt
2
, Qc, and Egm sources in the study area were estimated as 59, 30, and 11%, respectively. The efficiency coefficient for mixing model was calculated to be 0.99, which represents that the fingerprinting technique has a great potential for apportionment of sand dune sources.</description><subject>Clay</subject><subject>Dunes</subject><subject>Earth</subject><subject>Earth and Environmental Science</subject><subject>Earth science</subject><subject>Earth Sciences</subject><subject>Fingerprinting</subject><subject>Function analysis</subject><subject>Gravel</subject><subject>Isotopes</subject><subject>Major elements</subject><subject>Marl</subject><subject>Neodymium</subject><subject>Neodymium isotopes</subject><subject>Original Paper</subject><subject>Radioisotopes</subject><subject>Radionuclide kinetics</subject><subject>Rare earth elements</subject><subject>Sample preparation</subject><subject>Sand</subject><subject>Strontium</subject><subject>Strontium 87</subject><subject>Strontium isotopes</subject><subject>Terraces</subject><subject>Trace elements</subject><issn>1866-7511</issn><issn>1866-7538</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNp1kM1OxCAUhYnRxHH0AdyRuLUKdFro0ox_k0ziRteEwmXCZAoj0IVvL02NcePi5p6E851LDkLXlNxRQvh9oqyhvCJlWDeJE7Sgom0r3tTi9FdTeo4uUtoT0grCxQKNj5AhDs47v8M6-BxdP2YXPA4WJ-UNNqMHfAwZfHbqgFMYo4aExzQRUZniHfXBGUi3OEelAU_UoPYhYjjAULiEnce6iFgCNlH5S3Rm1SHB1c9eoo_np_f1a7V9e9msH7aVqusuV4obaFdMkZ6sSNeB7ldd1_dgywM3ogPLGt0IZjkxxBpOWWsJVY2FwnPO6iW6mXOPMXyOkLLcl-_7clJSIRgtLTRNcdHZpWNIKYKVx-gGFb8kJXJqV87tytKunNqVpDBsZlLx-h3EP8n_Qt-zTn9Y</recordid><startdate>20170401</startdate><enddate>20170401</enddate><creator>Gholami, Hamid</creator><creator>Middleton, Nick</creator><creator>Nazari Samani, Ali Akbar</creator><creator>Wasson, Robert</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20170401</creationdate><title>Determining contribution of sand dune potential sources using radionuclides, trace and major elements in central Iran</title><author>Gholami, Hamid ; Middleton, Nick ; Nazari Samani, Ali Akbar ; Wasson, Robert</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a339t-a7de642a0b04099ecb499bbefa7d7d89ef25c582f70d0fd7126f01a5fea337723</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Clay</topic><topic>Dunes</topic><topic>Earth</topic><topic>Earth and Environmental Science</topic><topic>Earth science</topic><topic>Earth Sciences</topic><topic>Fingerprinting</topic><topic>Function analysis</topic><topic>Gravel</topic><topic>Isotopes</topic><topic>Major elements</topic><topic>Marl</topic><topic>Neodymium</topic><topic>Neodymium isotopes</topic><topic>Original Paper</topic><topic>Radioisotopes</topic><topic>Radionuclide kinetics</topic><topic>Rare earth elements</topic><topic>Sample preparation</topic><topic>Sand</topic><topic>Strontium</topic><topic>Strontium 87</topic><topic>Strontium isotopes</topic><topic>Terraces</topic><topic>Trace elements</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Gholami, Hamid</creatorcontrib><creatorcontrib>Middleton, Nick</creatorcontrib><creatorcontrib>Nazari Samani, Ali Akbar</creatorcontrib><creatorcontrib>Wasson, Robert</creatorcontrib><collection>CrossRef</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Arabian journal of geosciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Gholami, Hamid</au><au>Middleton, Nick</au><au>Nazari Samani, Ali Akbar</au><au>Wasson, Robert</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Determining contribution of sand dune potential sources using radionuclides, trace and major elements in central Iran</atitle><jtitle>Arabian journal of geosciences</jtitle><stitle>Arab J Geosci</stitle><date>2017-04-01</date><risdate>2017</risdate><volume>10</volume><issue>7</issue><spage>1</spage><epage>9</epage><pages>1-9</pages><artnum>163</artnum><issn>1866-7511</issn><eissn>1866-7538</eissn><abstract>The present research describes a first attempt to use quantitative fingerprinting to quantify source contributions of sand dunes. Forty-nine surface samples from the main potential sources within Yazd-Ardekan Plain in the central Iran were collected and compared with eight samples of sand dunes, collected on various sites of Ashkzar erg. Three major categories of sand dune source were identified: young terraces and gravel fans (Qt
2
), clay flat (Qc), and gypsiferous marl (Egm). After sample preparation, concentrations of geochemical elements such as rare earth element (REE), major and trace elements, and isotopes of strontium (
87
Sr and
86
Sr) and neodymium (
143
Nd and
144
Nd) were measured. The results indicated, based on discriminant function analysis, 81.6% of the samples to be correctly assigned to their source areas. The mean contributions from Qt
2
, Qc, and Egm sources in the study area were estimated as 59, 30, and 11%, respectively. The efficiency coefficient for mixing model was calculated to be 0.99, which represents that the fingerprinting technique has a great potential for apportionment of sand dune sources.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s12517-017-2917-0</doi><tpages>9</tpages></addata></record> |
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subjects | Clay Dunes Earth Earth and Environmental Science Earth science Earth Sciences Fingerprinting Function analysis Gravel Isotopes Major elements Marl Neodymium Neodymium isotopes Original Paper Radioisotopes Radionuclide kinetics Rare earth elements Sample preparation Sand Strontium Strontium 87 Strontium isotopes Terraces Trace elements |
title | Determining contribution of sand dune potential sources using radionuclides, trace and major elements in central Iran |
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