Experimental study on the utilization of DIC by Oocystis solitaria Wittr and its influence on the precipitation of calcium carbonate in karst and non-karst waters
The difference in dissolved inorganic carbon (DIC) utilization and calcium carbonate precipitation by Oocystis solitaria Wittr grown in closed systems of karst water and non-karst water was investigated by using a free pH-drift experiment. It was found that the HCO 3 − as carbon resource of Oocystis...
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| Veröffentlicht in: | Carbonates and evaporites 2010-03, Vol.25 (1), p.21-26 |
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| creator | Liu, Yan Liu, Zaihua Zhang, Jinliu He, Yuanyuan Sun, Hailong |
| description | The difference in dissolved inorganic carbon (DIC) utilization and calcium carbonate precipitation by
Oocystis solitaria Wittr
grown in closed systems of karst water and non-karst water was investigated by using a free pH-drift experiment. It was found that the HCO
3
−
as carbon resource of
Oocystis solitaria Wittr
photosynthesis was catalyzed by carbonic anhydrase to CO
2
at low CO
2
concentration. The DIC utilization and induced calcium carbonate precipitation by
Oocystis solitaria Wittr
were much higher (4.6 and 10-fold, respectively) in karst water than in non-karst water. In karst waters, 42.6% of decreased calcium ions were precipitated as calcium carbonate; in non-karst waters, 8.9% were precipitated via physiochemical effect and the remaining were utilized by
Oocystis solitaria Wittr
for its growth. These findings clearly show the greater importance of karst water environment in DIC fertilization effect on the growth of
Oocystis solitaria Wittr
due to its higher concentrations of DIC, which is significant to the karst process-related carbon sink. |
| doi_str_mv | 10.1007/s13146-009-0002-9 |
| format | Article |
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Oocystis solitaria Wittr
grown in closed systems of karst water and non-karst water was investigated by using a free pH-drift experiment. It was found that the HCO
3
−
as carbon resource of
Oocystis solitaria Wittr
photosynthesis was catalyzed by carbonic anhydrase to CO
2
at low CO
2
concentration. The DIC utilization and induced calcium carbonate precipitation by
Oocystis solitaria Wittr
were much higher (4.6 and 10-fold, respectively) in karst water than in non-karst water. In karst waters, 42.6% of decreased calcium ions were precipitated as calcium carbonate; in non-karst waters, 8.9% were precipitated via physiochemical effect and the remaining were utilized by
Oocystis solitaria Wittr
for its growth. These findings clearly show the greater importance of karst water environment in DIC fertilization effect on the growth of
Oocystis solitaria Wittr
due to its higher concentrations of DIC, which is significant to the karst process-related carbon sink.</description><identifier>ISSN: 0891-2556</identifier><identifier>EISSN: 1878-5212</identifier><identifier>DOI: 10.1007/s13146-009-0002-9</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer-Verlag</publisher><subject>Biological fertilization ; Calcium ; Calcium carbonate ; Calcium carbonates ; Calcium ions ; Carbon ; Carbon dioxide ; Carbon sinks ; Carbonates ; Carbonic anhydrase ; Chemical precipitation ; Closed systems ; Dissolved inorganic carbon ; Earth and Environmental Science ; Earth Sciences ; Fertilization ; Geology ; Karst ; Mineral Resources ; Mineralogy ; Oocystis solitaria ; Original Article ; Photosynthesis ; Physiochemistry ; Utilization ; Water</subject><ispartof>Carbonates and evaporites, 2010-03, Vol.25 (1), p.21-26</ispartof><rights>Springer-Verlag 2010</rights><rights>Springer-Verlag 2010.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a339t-bb5c2abb8686fcd2d888734180f6bff5d61a19185657e407233d081cee0da7253</citedby><cites>FETCH-LOGICAL-a339t-bb5c2abb8686fcd2d888734180f6bff5d61a19185657e407233d081cee0da7253</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/s13146-009-0002-9$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s13146-009-0002-9$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Liu, Yan</creatorcontrib><creatorcontrib>Liu, Zaihua</creatorcontrib><creatorcontrib>Zhang, Jinliu</creatorcontrib><creatorcontrib>He, Yuanyuan</creatorcontrib><creatorcontrib>Sun, Hailong</creatorcontrib><title>Experimental study on the utilization of DIC by Oocystis solitaria Wittr and its influence on the precipitation of calcium carbonate in karst and non-karst waters</title><title>Carbonates and evaporites</title><addtitle>Carbonates Evaporites</addtitle><description>The difference in dissolved inorganic carbon (DIC) utilization and calcium carbonate precipitation by
Oocystis solitaria Wittr
grown in closed systems of karst water and non-karst water was investigated by using a free pH-drift experiment. It was found that the HCO
3
−
as carbon resource of
Oocystis solitaria Wittr
photosynthesis was catalyzed by carbonic anhydrase to CO
2
at low CO
2
concentration. The DIC utilization and induced calcium carbonate precipitation by
Oocystis solitaria Wittr
were much higher (4.6 and 10-fold, respectively) in karst water than in non-karst water. In karst waters, 42.6% of decreased calcium ions were precipitated as calcium carbonate; in non-karst waters, 8.9% were precipitated via physiochemical effect and the remaining were utilized by
Oocystis solitaria Wittr
for its growth. These findings clearly show the greater importance of karst water environment in DIC fertilization effect on the growth of
Oocystis solitaria Wittr
due to its higher concentrations of DIC, which is significant to the karst process-related carbon sink.</description><subject>Biological fertilization</subject><subject>Calcium</subject><subject>Calcium carbonate</subject><subject>Calcium carbonates</subject><subject>Calcium ions</subject><subject>Carbon</subject><subject>Carbon dioxide</subject><subject>Carbon sinks</subject><subject>Carbonates</subject><subject>Carbonic anhydrase</subject><subject>Chemical precipitation</subject><subject>Closed systems</subject><subject>Dissolved inorganic carbon</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Fertilization</subject><subject>Geology</subject><subject>Karst</subject><subject>Mineral Resources</subject><subject>Mineralogy</subject><subject>Oocystis solitaria</subject><subject>Original Article</subject><subject>Photosynthesis</subject><subject>Physiochemistry</subject><subject>Utilization</subject><subject>Water</subject><issn>0891-2556</issn><issn>1878-5212</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kc1KxDAUhYMoOI4-gLuA62p-mjZZyvg3MOBGcRnSNNVoJ6lJio6P45MarYMrF5fL5Z7zXbgHgGOMTjFC9VnEFJdVgZDIhUghdsAM85oXjGCyC2aIC1wQxqp9cBDjM0KVKIWYgc_L98EEuzYuqR7GNLYb6B1MTwaOyfb2QyWbZ9_Bi-UCNht46_UmJhth9L1NKlgFH2xKASrXQpsitK7rR-O02XKGYLQdsnZL0qrXdlznHhrvVDLZA19UiOkH4rwrpukt70I8BHud6qM5-u1zcH91ebe4KVa318vF-apQlIpUNA3TRDUNr3jV6Za0nPOalpijrmq6jrUVVlhgzipWmxLVhNIWcayNQa2qCaNzcDJxh-BfRxOTfPZjcPmkJCVimFOagXOAJ5UOPsZgOjnk96mwkRjJ7yjkFIXMUcjvKKTIHjJ5Yta6RxP-yP-bvgAWjI7X</recordid><startdate>20100301</startdate><enddate>20100301</enddate><creator>Liu, Yan</creator><creator>Liu, Zaihua</creator><creator>Zhang, Jinliu</creator><creator>He, Yuanyuan</creator><creator>Sun, Hailong</creator><general>Springer-Verlag</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope></search><sort><creationdate>20100301</creationdate><title>Experimental study on the utilization of DIC by Oocystis solitaria Wittr and its influence on the precipitation of calcium carbonate in karst and non-karst waters</title><author>Liu, Yan ; Liu, Zaihua ; Zhang, Jinliu ; He, Yuanyuan ; Sun, Hailong</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a339t-bb5c2abb8686fcd2d888734180f6bff5d61a19185657e407233d081cee0da7253</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2010</creationdate><topic>Biological fertilization</topic><topic>Calcium</topic><topic>Calcium carbonate</topic><topic>Calcium carbonates</topic><topic>Calcium ions</topic><topic>Carbon</topic><topic>Carbon dioxide</topic><topic>Carbon sinks</topic><topic>Carbonates</topic><topic>Carbonic anhydrase</topic><topic>Chemical precipitation</topic><topic>Closed systems</topic><topic>Dissolved inorganic carbon</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Fertilization</topic><topic>Geology</topic><topic>Karst</topic><topic>Mineral Resources</topic><topic>Mineralogy</topic><topic>Oocystis solitaria</topic><topic>Original Article</topic><topic>Photosynthesis</topic><topic>Physiochemistry</topic><topic>Utilization</topic><topic>Water</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Liu, Yan</creatorcontrib><creatorcontrib>Liu, Zaihua</creatorcontrib><creatorcontrib>Zhang, Jinliu</creatorcontrib><creatorcontrib>He, Yuanyuan</creatorcontrib><creatorcontrib>Sun, Hailong</creatorcontrib><collection>CrossRef</collection><collection>Water Resources Abstracts</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><jtitle>Carbonates and evaporites</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Liu, Yan</au><au>Liu, Zaihua</au><au>Zhang, Jinliu</au><au>He, Yuanyuan</au><au>Sun, Hailong</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Experimental study on the utilization of DIC by Oocystis solitaria Wittr and its influence on the precipitation of calcium carbonate in karst and non-karst waters</atitle><jtitle>Carbonates and evaporites</jtitle><stitle>Carbonates Evaporites</stitle><date>2010-03-01</date><risdate>2010</risdate><volume>25</volume><issue>1</issue><spage>21</spage><epage>26</epage><pages>21-26</pages><issn>0891-2556</issn><eissn>1878-5212</eissn><abstract>The difference in dissolved inorganic carbon (DIC) utilization and calcium carbonate precipitation by
Oocystis solitaria Wittr
grown in closed systems of karst water and non-karst water was investigated by using a free pH-drift experiment. It was found that the HCO
3
−
as carbon resource of
Oocystis solitaria Wittr
photosynthesis was catalyzed by carbonic anhydrase to CO
2
at low CO
2
concentration. The DIC utilization and induced calcium carbonate precipitation by
Oocystis solitaria Wittr
were much higher (4.6 and 10-fold, respectively) in karst water than in non-karst water. In karst waters, 42.6% of decreased calcium ions were precipitated as calcium carbonate; in non-karst waters, 8.9% were precipitated via physiochemical effect and the remaining were utilized by
Oocystis solitaria Wittr
for its growth. These findings clearly show the greater importance of karst water environment in DIC fertilization effect on the growth of
Oocystis solitaria Wittr
due to its higher concentrations of DIC, which is significant to the karst process-related carbon sink.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer-Verlag</pub><doi>10.1007/s13146-009-0002-9</doi><tpages>6</tpages></addata></record> |
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| source | Springer Nature - Complete Springer Journals |
| subjects | Biological fertilization Calcium Calcium carbonate Calcium carbonates Calcium ions Carbon Carbon dioxide Carbon sinks Carbonates Carbonic anhydrase Chemical precipitation Closed systems Dissolved inorganic carbon Earth and Environmental Science Earth Sciences Fertilization Geology Karst Mineral Resources Mineralogy Oocystis solitaria Original Article Photosynthesis Physiochemistry Utilization Water |
| title | Experimental study on the utilization of DIC by Oocystis solitaria Wittr and its influence on the precipitation of calcium carbonate in karst and non-karst waters |
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