The distribution of iodine and effects of phosphatization on it in the ferromanganese crusts from the Mid-Pacific Ocean
In the present paper, iodine （I）, iron （Fe）, manganese （Mn）, cobalt （Co）, phosphorus （P） and calcium （Ca） contents in three ferromanganese crusts from the Pacific Ocean are measured by spectrophotometric method and inductively coupled plasma atomic emission spectrometers （ICP-AES） to investigate the...
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| Veröffentlicht in: | Acta oceanologica Sinica 2015-08, Vol.34 (8), p.13-19 |
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| creator | Ji, Lihong Liu, Guangshan Huang, Yipu Xing, Na Chen, Zhigang |
| description | In the present paper, iodine （I）, iron （Fe）, manganese （Mn）, cobalt （Co）, phosphorus （P） and calcium （Ca） contents in three ferromanganese crusts from the Pacific Ocean are measured by spectrophotometric method and inductively coupled plasma atomic emission spectrometers （ICP-AES） to investigate the contents and distribution of iodine in ferromanganese crusts. The results show that iodine contents in three crusts vary between 27.1 and 836 mg/kg, with an average of 172 mg/kg, and the profile of iodine in the three crusts all exhibits a two-stage distribution zone： a young non-phosphatized zone and an old phosphatized zone that is rich in I, P and Ca. The iodine content ratios of old to young zone in MP5D44, CXD62-1 and CXD08-1 are 2.3, 3.4 and 13.7, respectively. The boundary depths of two-stage zone in MP5D44, CXD62-1 and CXD08-1 locate at 4.0 cm, 2.5 cm and 3.75 cm, respectively, and the time of iodine mutation in three crusts ranges from 17-37 Ma derived from 129I dating and Co empirical formula, which is consistent with the times of Cenozoic phosphatization events. The present study shows that the intensity of phosphatization is the main responsible for the distribution pattern of iodine in the crusts on the basis of the correlation analysis. Consequently, iodine is a sensitive indicator for phosphatization. |
| doi_str_mv | 10.1007/s13131-015-0704-x |
| format | Article |
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The results show that iodine contents in three crusts vary between 27.1 and 836 mg/kg, with an average of 172 mg/kg, and the profile of iodine in the three crusts all exhibits a two-stage distribution zone： a young non-phosphatized zone and an old phosphatized zone that is rich in I, P and Ca. The iodine content ratios of old to young zone in MP5D44, CXD62-1 and CXD08-1 are 2.3, 3.4 and 13.7, respectively. The boundary depths of two-stage zone in MP5D44, CXD62-1 and CXD08-1 locate at 4.0 cm, 2.5 cm and 3.75 cm, respectively, and the time of iodine mutation in three crusts ranges from 17-37 Ma derived from 129I dating and Co empirical formula, which is consistent with the times of Cenozoic phosphatization events. The present study shows that the intensity of phosphatization is the main responsible for the distribution pattern of iodine in the crusts on the basis of the correlation analysis. Consequently, iodine is a sensitive indicator for phosphatization.</description><identifier>ISSN: 0253-505X</identifier><identifier>EISSN: 1869-1099</identifier><identifier>DOI: 10.1007/s13131-015-0704-x</identifier><language>eng</language><publisher>Beijing: The Chinese Society of Oceanography</publisher><subject>Calcium ; Cenozoic ; Climatology ; Cobalt ; Concretions ; Correlation analysis ; Crusts ; Distribution ; Earth and Environmental Science ; Earth Sciences ; Ecology ; Emission analysis ; Empirical analysis ; Engineering Fluid Dynamics ; Environmental Chemistry ; Ferromanganese ; Ferromanganese nodules ; ICP-AES ; Inductively coupled plasma ; Iodine ; Iron ; Manganese ; Marine & Freshwater Sciences ; Metal oxides ; Mountains ; Oceanography ; Phosphating (coating) ; Phosphatization ; Phosphorus ; Sediments ; Spectrometers ; Spectrophotometry ; 中太平洋 ; 分光光度法测定 ; 富钴结壳 ; 电感耦合等离子体原子发射光谱仪 ; 碘 ; 磷化 ; 经验公式</subject><ispartof>Acta oceanologica Sinica, 2015-08, Vol.34 (8), p.13-19</ispartof><rights>The Chinese Society of Oceanography and Springer-Verlag Berlin Heidelberg 2015</rights><rights>The Chinese Society of Oceanography and Springer-Verlag Berlin Heidelberg 2015.</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c436t-bbf17adffeaeeb17a5b55f45aa02f37c6371ed53a9a3086f827add9d0686c7363</citedby><cites>FETCH-LOGICAL-c436t-bbf17adffeaeeb17a5b55f45aa02f37c6371ed53a9a3086f827add9d0686c7363</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/86790X/86790X.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s13131-015-0704-x$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2920268426?pq-origsite=primo$$EHTML$$P50$$Gproquest$$H</linktohtml><link.rule.ids>314,776,780,21367,27901,27902,33721,33722,41464,42533,43781,51294</link.rule.ids></links><search><creatorcontrib>Ji, Lihong</creatorcontrib><creatorcontrib>Liu, Guangshan</creatorcontrib><creatorcontrib>Huang, Yipu</creatorcontrib><creatorcontrib>Xing, Na</creatorcontrib><creatorcontrib>Chen, Zhigang</creatorcontrib><title>The distribution of iodine and effects of phosphatization on it in the ferromanganese crusts from the Mid-Pacific Ocean</title><title>Acta oceanologica Sinica</title><addtitle>Acta Oceanol. Sin</addtitle><addtitle>Acta Oceanologica Sinica</addtitle><description>In the present paper, iodine （I）, iron （Fe）, manganese （Mn）, cobalt （Co）, phosphorus （P） and calcium （Ca） contents in three ferromanganese crusts from the Pacific Ocean are measured by spectrophotometric method and inductively coupled plasma atomic emission spectrometers （ICP-AES） to investigate the contents and distribution of iodine in ferromanganese crusts. The results show that iodine contents in three crusts vary between 27.1 and 836 mg/kg, with an average of 172 mg/kg, and the profile of iodine in the three crusts all exhibits a two-stage distribution zone： a young non-phosphatized zone and an old phosphatized zone that is rich in I, P and Ca. The iodine content ratios of old to young zone in MP5D44, CXD62-1 and CXD08-1 are 2.3, 3.4 and 13.7, respectively. The boundary depths of two-stage zone in MP5D44, CXD62-1 and CXD08-1 locate at 4.0 cm, 2.5 cm and 3.75 cm, respectively, and the time of iodine mutation in three crusts ranges from 17-37 Ma derived from 129I dating and Co empirical formula, which is consistent with the times of Cenozoic phosphatization events. The present study shows that the intensity of phosphatization is the main responsible for the distribution pattern of iodine in the crusts on the basis of the correlation analysis. Consequently, iodine is a sensitive indicator for phosphatization.</description><subject>Calcium</subject><subject>Cenozoic</subject><subject>Climatology</subject><subject>Cobalt</subject><subject>Concretions</subject><subject>Correlation analysis</subject><subject>Crusts</subject><subject>Distribution</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Ecology</subject><subject>Emission analysis</subject><subject>Empirical analysis</subject><subject>Engineering Fluid Dynamics</subject><subject>Environmental Chemistry</subject><subject>Ferromanganese</subject><subject>Ferromanganese nodules</subject><subject>ICP-AES</subject><subject>Inductively coupled plasma</subject><subject>Iodine</subject><subject>Iron</subject><subject>Manganese</subject><subject>Marine & Freshwater Sciences</subject><subject>Metal oxides</subject><subject>Mountains</subject><subject>Oceanography</subject><subject>Phosphating (coating)</subject><subject>Phosphatization</subject><subject>Phosphorus</subject><subject>Sediments</subject><subject>Spectrometers</subject><subject>Spectrophotometry</subject><subject>中太平洋</subject><subject>分光光度法测定</subject><subject>富钴结壳</subject><subject>电感耦合等离子体原子发射光谱仪</subject><subject>碘</subject><subject>磷化</subject><subject>经验公式</subject><issn>0253-505X</issn><issn>1869-1099</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2015</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kU1v3CAQhq2qkbpN-gN6Q-2hvbgdwIB9rKL0Q0qVHBKpN4QxrIl2YQO2ssmvz2wdRVUPERKMhud9Z2Cq6j2FLxRAfS2U46qBihoUNPX-VbWirexqCl33uloBE7wWIP68qd6WcgMgqOBqVd1djY4MoUw59PMUUiTJk5CGEB0xcSDOe2encsjuxlR2o5nCg1nASMJEQiQTWniXc9qauDbRFUdsnguqPOb-Xv8OQ31pbPDBkgvrTDypjrzZFPfu6Tyurr-fXZ3-rM8vfvw6_XZe24bLqe57T5UZsAnjXI-h6IXwjTAGmOfKSq6oGwQ3neHQSt8ypIduANlKq7jkx9WnxffORI_t6Zs054gV9Xi_77Vj-GPQAjAkPy_kLqfb2ZVJb0OxbrPBF6W5aKooU4o1AIh-_A99dmUdAybbhsmXKKqAMiFwR4oulM2plOy83uWwNfleU9CH0epltBob1YfR6j1q2KIpyMa1y_84vyD68FRoTHF9i7rnSlJKKhjvBH8El7-yPg</recordid><startdate>20150801</startdate><enddate>20150801</enddate><creator>Ji, 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distribution of iodine and effects of phosphatization on it in the ferromanganese crusts from the Mid-Pacific Ocean</title><author>Ji, Lihong ; Liu, Guangshan ; Huang, Yipu ; Xing, Na ; Chen, Zhigang</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c436t-bbf17adffeaeeb17a5b55f45aa02f37c6371ed53a9a3086f827add9d0686c7363</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2015</creationdate><topic>Calcium</topic><topic>Cenozoic</topic><topic>Climatology</topic><topic>Cobalt</topic><topic>Concretions</topic><topic>Correlation analysis</topic><topic>Crusts</topic><topic>Distribution</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Ecology</topic><topic>Emission analysis</topic><topic>Empirical analysis</topic><topic>Engineering Fluid Dynamics</topic><topic>Environmental Chemistry</topic><topic>Ferromanganese</topic><topic>Ferromanganese 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(COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Acta oceanologica Sinica</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ji, Lihong</au><au>Liu, Guangshan</au><au>Huang, Yipu</au><au>Xing, Na</au><au>Chen, Zhigang</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The distribution of iodine and effects of phosphatization on it in the ferromanganese crusts from the Mid-Pacific Ocean</atitle><jtitle>Acta oceanologica Sinica</jtitle><stitle>Acta Oceanol. Sin</stitle><addtitle>Acta Oceanologica Sinica</addtitle><date>2015-08-01</date><risdate>2015</risdate><volume>34</volume><issue>8</issue><spage>13</spage><epage>19</epage><pages>13-19</pages><issn>0253-505X</issn><eissn>1869-1099</eissn><abstract>In the present paper, iodine （I）, iron （Fe）, manganese （Mn）, cobalt （Co）, phosphorus （P） and calcium （Ca） contents in three ferromanganese crusts from the Pacific Ocean are measured by spectrophotometric method and inductively coupled plasma atomic emission spectrometers （ICP-AES） to investigate the contents and distribution of iodine in ferromanganese crusts. The results show that iodine contents in three crusts vary between 27.1 and 836 mg/kg, with an average of 172 mg/kg, and the profile of iodine in the three crusts all exhibits a two-stage distribution zone： a young non-phosphatized zone and an old phosphatized zone that is rich in I, P and Ca. The iodine content ratios of old to young zone in MP5D44, CXD62-1 and CXD08-1 are 2.3, 3.4 and 13.7, respectively. The boundary depths of two-stage zone in MP5D44, CXD62-1 and CXD08-1 locate at 4.0 cm, 2.5 cm and 3.75 cm, respectively, and the time of iodine mutation in three crusts ranges from 17-37 Ma derived from 129I dating and Co empirical formula, which is consistent with the times of Cenozoic phosphatization events. The present study shows that the intensity of phosphatization is the main responsible for the distribution pattern of iodine in the crusts on the basis of the correlation analysis. Consequently, iodine is a sensitive indicator for phosphatization.</abstract><cop>Beijing</cop><pub>The Chinese Society of Oceanography</pub><doi>10.1007/s13131-015-0704-x</doi><tpages>7</tpages></addata></record> |
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| subjects | Calcium Cenozoic Climatology Cobalt Concretions Correlation analysis Crusts Distribution Earth and Environmental Science Earth Sciences Ecology Emission analysis Empirical analysis Engineering Fluid Dynamics Environmental Chemistry Ferromanganese Ferromanganese nodules ICP-AES Inductively coupled plasma Iodine Iron Manganese Marine & Freshwater Sciences Metal oxides Mountains Oceanography Phosphating (coating) Phosphatization Phosphorus Sediments Spectrometers Spectrophotometry 中太平洋 分光光度法测定 富钴结壳 电感耦合等离子体原子发射光谱仪 碘 磷化 经验公式 |
| title | The distribution of iodine and effects of phosphatization on it in the ferromanganese crusts from the Mid-Pacific Ocean |
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