Study of uranium toxicity using low-background gamma-ray spectrometry
The natural activity of 238 U, 232 Th and 40 K present in soil, fertilizer and palaeosols besides animal fossils was determined using low background gamma ray spectrometry. The highest uranium activity level were found in animal fossils of geogenic origin compared to palaeosols, soils and fertilizer...
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Veröffentlicht in: | Journal of radioanalytical and nuclear chemistry 2017-11, Vol.314 (2), p.1367-1373 |
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container_title | Journal of radioanalytical and nuclear chemistry |
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creator | Srivastava, A. Chahar, V. Sharma, V. Sun, Y. Bol, R. Knolle, F. Schnug, E. Hoyler, F. Naskar, N. Lahiri, S. Patnaik, R. |
description | The natural activity of
238
U,
232
Th and
40
K present in soil, fertilizer and palaeosols besides animal fossils was determined using low background gamma ray spectrometry. The highest uranium activity level were found in animal fossils of geogenic origin compared to palaeosols, soils and fertilizers, a result of post-mortem uranium assimilation in these fossils via diagenetic processes. Hence, geogenic mobilization is likely a major cause of elevated uranium levels in Malwa region of Punjab, also known for higher than normal cancer incidence. |
doi_str_mv | 10.1007/s10967-017-5466-9 |
format | Article |
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238
U,
232
Th and
40
K present in soil, fertilizer and palaeosols besides animal fossils was determined using low background gamma ray spectrometry. The highest uranium activity level were found in animal fossils of geogenic origin compared to palaeosols, soils and fertilizers, a result of post-mortem uranium assimilation in these fossils via diagenetic processes. Hence, geogenic mobilization is likely a major cause of elevated uranium levels in Malwa region of Punjab, also known for higher than normal cancer incidence.</description><identifier>ISSN: 0236-5731</identifier><identifier>EISSN: 1588-2780</identifier><identifier>DOI: 10.1007/s10967-017-5466-9</identifier><language>eng</language><publisher>Dordrecht: Springer Netherlands</publisher><subject>Background radiation ; Chemistry ; Chemistry and Materials Science ; Diagnostic Radiology ; Fertilizers ; Fossils ; Gamma rays ; Hadrons ; Heavy Ions ; Inorganic Chemistry ; Nuclear Chemistry ; Nuclear energy ; Nuclear Physics ; Physical Chemistry ; Radiation measurement ; Scientific imaging ; Spectrometry ; Spectroscopy ; Toxicity ; Uranium</subject><ispartof>Journal of radioanalytical and nuclear chemistry, 2017-11, Vol.314 (2), p.1367-1373</ispartof><rights>Akadémiai Kiadó, Budapest, Hungary 2017</rights><rights>COPYRIGHT 2017 Springer</rights><rights>Copyright Springer Science & Business Media 2017</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c355t-99bda3bc7398a72a02f0b694a28d17896bd6c2f2c6b7e38ff0f7d7c377e165c23</citedby><cites>FETCH-LOGICAL-c355t-99bda3bc7398a72a02f0b694a28d17896bd6c2f2c6b7e38ff0f7d7c377e165c23</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10967-017-5466-9$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10967-017-5466-9$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27923,27924,41487,42556,51318</link.rule.ids></links><search><creatorcontrib>Srivastava, A.</creatorcontrib><creatorcontrib>Chahar, V.</creatorcontrib><creatorcontrib>Sharma, V.</creatorcontrib><creatorcontrib>Sun, Y.</creatorcontrib><creatorcontrib>Bol, R.</creatorcontrib><creatorcontrib>Knolle, F.</creatorcontrib><creatorcontrib>Schnug, E.</creatorcontrib><creatorcontrib>Hoyler, F.</creatorcontrib><creatorcontrib>Naskar, N.</creatorcontrib><creatorcontrib>Lahiri, S.</creatorcontrib><creatorcontrib>Patnaik, R.</creatorcontrib><title>Study of uranium toxicity using low-background gamma-ray spectrometry</title><title>Journal of radioanalytical and nuclear chemistry</title><addtitle>J Radioanal Nucl Chem</addtitle><description>The natural activity of
238
U,
232
Th and
40
K present in soil, fertilizer and palaeosols besides animal fossils was determined using low background gamma ray spectrometry. The highest uranium activity level were found in animal fossils of geogenic origin compared to palaeosols, soils and fertilizers, a result of post-mortem uranium assimilation in these fossils via diagenetic processes. Hence, geogenic mobilization is likely a major cause of elevated uranium levels in Malwa region of Punjab, also known for higher than normal cancer incidence.</description><subject>Background radiation</subject><subject>Chemistry</subject><subject>Chemistry and Materials Science</subject><subject>Diagnostic Radiology</subject><subject>Fertilizers</subject><subject>Fossils</subject><subject>Gamma rays</subject><subject>Hadrons</subject><subject>Heavy Ions</subject><subject>Inorganic Chemistry</subject><subject>Nuclear Chemistry</subject><subject>Nuclear energy</subject><subject>Nuclear Physics</subject><subject>Physical Chemistry</subject><subject>Radiation measurement</subject><subject>Scientific imaging</subject><subject>Spectrometry</subject><subject>Spectroscopy</subject><subject>Toxicity</subject><subject>Uranium</subject><issn>0236-5731</issn><issn>1588-2780</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNp1kE1LxDAQhoMouK7-AG8Fz1nzsfk6iqwfsOBBPYc0TUrXbbMmKdp_b5Z68CJzGBjeZ2Z4ALjGaIURErcJI8UFRFhAtuYcqhOwwExKSIREp2CBCOWQCYrPwUVKO4SQkpIuwOY1j81UBV-N0Qzd2Fc5fHe2y1M1pm5oq334grWxH20M49BUrel7A6OZqnRwNsfQuxynS3DmzT65q9--BO8Pm7f7J7h9eXy-v9tCSxnLUKm6MbS2gippBDGIeFRztTZENlhIxeuGW-KJ5bVwVHqPvGiEpUI4zJkldAlu5r2HGD5Hl7LehTEO5aTGinGkFFW0pFZzqjV7p7vBhxyNLdW4vrNhcL4r8zuGy8215KoAeAZsDClF5_Uhdr2Jk8ZIH_XqWa8uevVRrz4yZGZSyQ6ti39e-Rf6AY9TfXg</recordid><startdate>20171101</startdate><enddate>20171101</enddate><creator>Srivastava, A.</creator><creator>Chahar, V.</creator><creator>Sharma, V.</creator><creator>Sun, Y.</creator><creator>Bol, R.</creator><creator>Knolle, F.</creator><creator>Schnug, E.</creator><creator>Hoyler, F.</creator><creator>Naskar, N.</creator><creator>Lahiri, S.</creator><creator>Patnaik, R.</creator><general>Springer Netherlands</general><general>Springer</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20171101</creationdate><title>Study of uranium toxicity using low-background gamma-ray spectrometry</title><author>Srivastava, A. ; Chahar, V. ; Sharma, V. ; Sun, Y. ; Bol, R. ; Knolle, F. ; Schnug, E. ; Hoyler, F. ; Naskar, N. ; Lahiri, S. ; Patnaik, R.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c355t-99bda3bc7398a72a02f0b694a28d17896bd6c2f2c6b7e38ff0f7d7c377e165c23</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Background radiation</topic><topic>Chemistry</topic><topic>Chemistry and Materials Science</topic><topic>Diagnostic Radiology</topic><topic>Fertilizers</topic><topic>Fossils</topic><topic>Gamma rays</topic><topic>Hadrons</topic><topic>Heavy Ions</topic><topic>Inorganic Chemistry</topic><topic>Nuclear Chemistry</topic><topic>Nuclear energy</topic><topic>Nuclear Physics</topic><topic>Physical Chemistry</topic><topic>Radiation measurement</topic><topic>Scientific imaging</topic><topic>Spectrometry</topic><topic>Spectroscopy</topic><topic>Toxicity</topic><topic>Uranium</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Srivastava, A.</creatorcontrib><creatorcontrib>Chahar, V.</creatorcontrib><creatorcontrib>Sharma, V.</creatorcontrib><creatorcontrib>Sun, Y.</creatorcontrib><creatorcontrib>Bol, R.</creatorcontrib><creatorcontrib>Knolle, F.</creatorcontrib><creatorcontrib>Schnug, E.</creatorcontrib><creatorcontrib>Hoyler, F.</creatorcontrib><creatorcontrib>Naskar, N.</creatorcontrib><creatorcontrib>Lahiri, S.</creatorcontrib><creatorcontrib>Patnaik, R.</creatorcontrib><collection>CrossRef</collection><jtitle>Journal of radioanalytical and nuclear chemistry</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Srivastava, A.</au><au>Chahar, V.</au><au>Sharma, V.</au><au>Sun, Y.</au><au>Bol, R.</au><au>Knolle, F.</au><au>Schnug, E.</au><au>Hoyler, F.</au><au>Naskar, N.</au><au>Lahiri, S.</au><au>Patnaik, R.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Study of uranium toxicity using low-background gamma-ray spectrometry</atitle><jtitle>Journal of radioanalytical and nuclear chemistry</jtitle><stitle>J Radioanal Nucl Chem</stitle><date>2017-11-01</date><risdate>2017</risdate><volume>314</volume><issue>2</issue><spage>1367</spage><epage>1373</epage><pages>1367-1373</pages><issn>0236-5731</issn><eissn>1588-2780</eissn><abstract>The natural activity of
238
U,
232
Th and
40
K present in soil, fertilizer and palaeosols besides animal fossils was determined using low background gamma ray spectrometry. The highest uranium activity level were found in animal fossils of geogenic origin compared to palaeosols, soils and fertilizers, a result of post-mortem uranium assimilation in these fossils via diagenetic processes. Hence, geogenic mobilization is likely a major cause of elevated uranium levels in Malwa region of Punjab, also known for higher than normal cancer incidence.</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><doi>10.1007/s10967-017-5466-9</doi><tpages>7</tpages></addata></record> |
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subjects | Background radiation Chemistry Chemistry and Materials Science Diagnostic Radiology Fertilizers Fossils Gamma rays Hadrons Heavy Ions Inorganic Chemistry Nuclear Chemistry Nuclear energy Nuclear Physics Physical Chemistry Radiation measurement Scientific imaging Spectrometry Spectroscopy Toxicity Uranium |
title | Study of uranium toxicity using low-background gamma-ray spectrometry |
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