Hydrochemical conditions of the “Chistaya Banka” polygon in the Volga’s avant delta
Characteristics of different types of river drainage were obtained during studies of a polygon in the near-mouth part of the Volga River in 2000–2003: “fast” (flowing through deep channels) and “slow” (that which passes through the littoral parts of the delta (1–2 m)). The low current velocities (lo...
Gespeichert in:
| Veröffentlicht in: | Oceanology (Washington. 1965) 2009-10, Vol.49 (5), p.630-642 |
|---|---|
| Hauptverfasser: | , , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 642 |
|---|---|
| container_issue | 5 |
| container_start_page | 630 |
| container_title | Oceanology (Washington. 1965) |
| container_volume | 49 |
| creator | Ambrosimov, A. K. Ambrosimov, D. A. Makkaveev, P. N. Nalbandov, Yu. R. Skibinskii, L. E. Hlebopashev, P. V. |
| description | Characteristics of different types of river drainage were obtained during studies of a polygon in the near-mouth part of the Volga River in 2000–2003: “fast” (flowing through deep channels) and “slow” (that which passes through the littoral parts of the delta (1–2 m)). The low current velocities (lower than in the channel waters by a factor of ten), the abundance of water vegetation, and the strong heating of the waters lead to the high intensity of the biochemical processes. Therefore, the chemical composition of the waters is subjected to significant transformation with intensity so high that it allows comparing these regions with some sort of “bioreactor.” These changes influence the dissolved oxygen and various forms of carbon content. |
| doi_str_mv | 10.1134/S000143700905004X |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_21263563</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>21263563</sourcerecordid><originalsourceid>FETCH-LOGICAL-c346t-380c5cdeb965076593d1953417bad846f1072233fbc422856b566c4f5f109f6c3</originalsourceid><addsrcrecordid>eNp1kM1Kw0AUhQdRsFYfwN3gwl30zm-SpRa1QsGFP-gqTCaTNjWdqTOpkF1fQ9CX65OYWkFQXF245zvnXg5ChwROCGH89BYACGcxQAoCgD9uoR4RjESJgGQb9dZytNZ30V4IUwBGeJr00NOwLbzTEzOrtKqxdraomsrZgF2Jm4nBq-X7YFKFRrUKnyv7rFbLDzx3dTt2Flf2i3lw9bjbvwWsXpVtcGHqRu2jnVLVwRx8zz66v7y4Gwyj0c3V9eBsFGnGZROxBLTQhclTKSCWImUFSQXjJM5VkXBZEogpZazMNac0ETIXUmpeik5IS6lZHx1vcufevSxMaLJZFbSpa2WNW4SMEiqZkKwDj36BU7fwtvstoyBoknbXOohsIO1dCN6U2dxXM-XbjEC2bjr703TnoRtP6Fg7Nv4n-H_TJ37UgR8</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>205289846</pqid></control><display><type>article</type><title>Hydrochemical conditions of the “Chistaya Banka” polygon in the Volga’s avant delta</title><source>SpringerLink Journals - AutoHoldings</source><creator>Ambrosimov, A. K. ; Ambrosimov, D. A. ; Makkaveev, P. N. ; Nalbandov, Yu. R. ; Skibinskii, L. E. ; Hlebopashev, P. V.</creator><creatorcontrib>Ambrosimov, A. K. ; Ambrosimov, D. A. ; Makkaveev, P. N. ; Nalbandov, Yu. R. ; Skibinskii, L. E. ; Hlebopashev, P. V.</creatorcontrib><description>Characteristics of different types of river drainage were obtained during studies of a polygon in the near-mouth part of the Volga River in 2000–2003: “fast” (flowing through deep channels) and “slow” (that which passes through the littoral parts of the delta (1–2 m)). The low current velocities (lower than in the channel waters by a factor of ten), the abundance of water vegetation, and the strong heating of the waters lead to the high intensity of the biochemical processes. Therefore, the chemical composition of the waters is subjected to significant transformation with intensity so high that it allows comparing these regions with some sort of “bioreactor.” These changes influence the dissolved oxygen and various forms of carbon content.</description><identifier>ISSN: 0001-4370</identifier><identifier>EISSN: 1531-8508</identifier><identifier>DOI: 10.1134/S000143700905004X</identifier><language>eng</language><publisher>Dordrecht: SP MAIK Nauka/Interperiodica</publisher><subject>Bioreactors ; Brackish ; Chemical elements ; Chemical oceanography ; Dissolved oxygen ; Earth and Environmental Science ; Earth Sciences ; Freshwater ; Hydrology ; Marine Chemistry ; Oceanography ; Rivers ; Sea level</subject><ispartof>Oceanology (Washington. 1965), 2009-10, Vol.49 (5), p.630-642</ispartof><rights>Pleiades Publishing, Ltd. 2009</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c346t-380c5cdeb965076593d1953417bad846f1072233fbc422856b566c4f5f109f6c3</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S000143700905004X$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S000143700905004X$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27923,27924,41487,42556,51318</link.rule.ids></links><search><creatorcontrib>Ambrosimov, A. K.</creatorcontrib><creatorcontrib>Ambrosimov, D. A.</creatorcontrib><creatorcontrib>Makkaveev, P. N.</creatorcontrib><creatorcontrib>Nalbandov, Yu. R.</creatorcontrib><creatorcontrib>Skibinskii, L. E.</creatorcontrib><creatorcontrib>Hlebopashev, P. V.</creatorcontrib><title>Hydrochemical conditions of the “Chistaya Banka” polygon in the Volga’s avant delta</title><title>Oceanology (Washington. 1965)</title><addtitle>Oceanology</addtitle><description>Characteristics of different types of river drainage were obtained during studies of a polygon in the near-mouth part of the Volga River in 2000–2003: “fast” (flowing through deep channels) and “slow” (that which passes through the littoral parts of the delta (1–2 m)). The low current velocities (lower than in the channel waters by a factor of ten), the abundance of water vegetation, and the strong heating of the waters lead to the high intensity of the biochemical processes. Therefore, the chemical composition of the waters is subjected to significant transformation with intensity so high that it allows comparing these regions with some sort of “bioreactor.” These changes influence the dissolved oxygen and various forms of carbon content.</description><subject>Bioreactors</subject><subject>Brackish</subject><subject>Chemical elements</subject><subject>Chemical oceanography</subject><subject>Dissolved oxygen</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Freshwater</subject><subject>Hydrology</subject><subject>Marine Chemistry</subject><subject>Oceanography</subject><subject>Rivers</subject><subject>Sea level</subject><issn>0001-4370</issn><issn>1531-8508</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</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>eNp1kM1Kw0AUhQdRsFYfwN3gwl30zm-SpRa1QsGFP-gqTCaTNjWdqTOpkF1fQ9CX65OYWkFQXF245zvnXg5ChwROCGH89BYACGcxQAoCgD9uoR4RjESJgGQb9dZytNZ30V4IUwBGeJr00NOwLbzTEzOrtKqxdraomsrZgF2Jm4nBq-X7YFKFRrUKnyv7rFbLDzx3dTt2Flf2i3lw9bjbvwWsXpVtcGHqRu2jnVLVwRx8zz66v7y4Gwyj0c3V9eBsFGnGZROxBLTQhclTKSCWImUFSQXjJM5VkXBZEogpZazMNac0ETIXUmpeik5IS6lZHx1vcufevSxMaLJZFbSpa2WNW4SMEiqZkKwDj36BU7fwtvstoyBoknbXOohsIO1dCN6U2dxXM-XbjEC2bjr703TnoRtP6Fg7Nv4n-H_TJ37UgR8</recordid><startdate>20091001</startdate><enddate>20091001</enddate><creator>Ambrosimov, A. K.</creator><creator>Ambrosimov, D. A.</creator><creator>Makkaveev, P. N.</creator><creator>Nalbandov, Yu. R.</creator><creator>Skibinskii, L. E.</creator><creator>Hlebopashev, P. V.</creator><general>SP MAIK Nauka/Interperiodica</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope><scope>H97</scope></search><sort><creationdate>20091001</creationdate><title>Hydrochemical conditions of the “Chistaya Banka” polygon in the Volga’s avant delta</title><author>Ambrosimov, A. K. ; Ambrosimov, D. A. ; Makkaveev, P. N. ; Nalbandov, Yu. R. ; Skibinskii, L. E. ; Hlebopashev, P. V.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c346t-380c5cdeb965076593d1953417bad846f1072233fbc422856b566c4f5f109f6c3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>Bioreactors</topic><topic>Brackish</topic><topic>Chemical elements</topic><topic>Chemical oceanography</topic><topic>Dissolved oxygen</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Freshwater</topic><topic>Hydrology</topic><topic>Marine Chemistry</topic><topic>Oceanography</topic><topic>Rivers</topic><topic>Sea level</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ambrosimov, A. K.</creatorcontrib><creatorcontrib>Ambrosimov, D. A.</creatorcontrib><creatorcontrib>Makkaveev, P. N.</creatorcontrib><creatorcontrib>Nalbandov, Yu. R.</creatorcontrib><creatorcontrib>Skibinskii, L. E.</creatorcontrib><creatorcontrib>Hlebopashev, P. V.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</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>ProQuest Central Student</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>Science Database</collection><collection>Environmental Science Database</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><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 3: Aquatic Pollution & Environmental Quality</collection><jtitle>Oceanology (Washington. 1965)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ambrosimov, A. K.</au><au>Ambrosimov, D. A.</au><au>Makkaveev, P. N.</au><au>Nalbandov, Yu. R.</au><au>Skibinskii, L. E.</au><au>Hlebopashev, P. V.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Hydrochemical conditions of the “Chistaya Banka” polygon in the Volga’s avant delta</atitle><jtitle>Oceanology (Washington. 1965)</jtitle><stitle>Oceanology</stitle><date>2009-10-01</date><risdate>2009</risdate><volume>49</volume><issue>5</issue><spage>630</spage><epage>642</epage><pages>630-642</pages><issn>0001-4370</issn><eissn>1531-8508</eissn><abstract>Characteristics of different types of river drainage were obtained during studies of a polygon in the near-mouth part of the Volga River in 2000–2003: “fast” (flowing through deep channels) and “slow” (that which passes through the littoral parts of the delta (1–2 m)). The low current velocities (lower than in the channel waters by a factor of ten), the abundance of water vegetation, and the strong heating of the waters lead to the high intensity of the biochemical processes. Therefore, the chemical composition of the waters is subjected to significant transformation with intensity so high that it allows comparing these regions with some sort of “bioreactor.” These changes influence the dissolved oxygen and various forms of carbon content.</abstract><cop>Dordrecht</cop><pub>SP MAIK Nauka/Interperiodica</pub><doi>10.1134/S000143700905004X</doi><tpages>13</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0001-4370 |
| ispartof | Oceanology (Washington. 1965), 2009-10, Vol.49 (5), p.630-642 |
| issn | 0001-4370 1531-8508 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_21263563 |
| source | SpringerLink Journals - AutoHoldings |
| subjects | Bioreactors Brackish Chemical elements Chemical oceanography Dissolved oxygen Earth and Environmental Science Earth Sciences Freshwater Hydrology Marine Chemistry Oceanography Rivers Sea level |
| title | Hydrochemical conditions of the “Chistaya Banka” polygon in the Volga’s avant delta |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-13T01%3A28%3A04IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Hydrochemical%20conditions%20of%20the%20%E2%80%9CChistaya%20Banka%E2%80%9D%20polygon%20in%20the%20Volga%E2%80%99s%20avant%20delta&rft.jtitle=Oceanology%20(Washington.%201965)&rft.au=Ambrosimov,%20A.%20K.&rft.date=2009-10-01&rft.volume=49&rft.issue=5&rft.spage=630&rft.epage=642&rft.pages=630-642&rft.issn=0001-4370&rft.eissn=1531-8508&rft_id=info:doi/10.1134/S000143700905004X&rft_dat=%3Cproquest_cross%3E21263563%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=205289846&rft_id=info:pmid/&rfr_iscdi=true |