Hydrochemistry of the Tumen River Estuary, Sea of Japan
The hydrological and hydrochemical parameters of the Tumen River estuary were collected at 13 stations in May and October 2015. Vertical temperature, conductivity, dissolved oxygen, chlorophyll fluorescence, and turbidity profiles were obtained. Water was sampled from the surface and bottom layer. T...
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Veröffentlicht in: | Oceanology (Washington. 1965) 2018-03, Vol.58 (2), p.175-186 |
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creator | Tishchenko, P. Ya Semkin, P. Yu Pavlova, G. Yu Tishchenko, P. P. Lobanov, V. B. Marjash, A. A. Mikhailik, T. A. Sagalaev, S. G. Sergeev, A. F. Tibenko, E. Yu Khodorenko, N. D. Chichkin, R. V. Shvetsova, M. G. Shkirnikova, E. M. |
description | The hydrological and hydrochemical parameters of the Tumen River estuary were collected at 13 stations in May and October 2015. Vertical temperature, conductivity, dissolved oxygen, chlorophyll fluorescence, and turbidity profiles were obtained. Water was sampled from the surface and bottom layer. The water samples were analyzed for major ions, pH, salinity, concentrations of dissolved oxygen, major nutrients, dissolved organic carbon, humic matter, and δ
18
О and δD isotopes. This estuary is attributed to microtidal type with a flushing time of about 10 h. A phytoplakton bloom occurred in the top layer of the estuary. For surface horizons, the hydrochemical parameters show a linear correlation with salinity. In the bottom horizons, all these parameters, except for major ions and δ
18
О and δD isotopes, reveal substantial nonconservative behavior. The nonconservative behavior of the hydrochemical parameters in the bottom waters was mainly caused by degradation of the phytoplankton biomass at the water/sediment interface. Hypoxic conditions were established in the bottom waters of the estuary in May. |
doi_str_mv | 10.1134/S0001437018010149 |
format | Article |
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18
О and δD isotopes. This estuary is attributed to microtidal type with a flushing time of about 10 h. A phytoplakton bloom occurred in the top layer of the estuary. For surface horizons, the hydrochemical parameters show a linear correlation with salinity. In the bottom horizons, all these parameters, except for major ions and δ
18
О and δD isotopes, reveal substantial nonconservative behavior. The nonconservative behavior of the hydrochemical parameters in the bottom waters was mainly caused by degradation of the phytoplankton biomass at the water/sediment interface. Hypoxic conditions were established in the bottom waters of the estuary in May.</description><identifier>ISSN: 0001-4370</identifier><identifier>EISSN: 1531-8508</identifier><identifier>DOI: 10.1134/S0001437018010149</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Biodegradation ; Blooms ; Chlorophyll ; Chlorophylls ; Dissolved organic carbon ; Dissolved oxygen ; Earth and Environmental Science ; Earth Sciences ; Estuaries ; Estuarine dynamics ; Fluorescence ; Flushing time ; Hydrochemistry ; Hydrology ; Hypoxia ; Ions ; Isotopes ; Marine Chemistry ; Mineral nutrients ; Nutrients ; Oceanography ; Parameters ; Phytoplankton ; Profiles ; Rivers ; Salinity ; Salinity effects ; Turbidity ; Water analysis ; Water sampling</subject><ispartof>Oceanology (Washington. 1965), 2018-03, Vol.58 (2), p.175-186</ispartof><rights>Pleiades Publishing, Inc. 2018</rights><rights>Oceanology is a copyright of Springer, (2018). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c382t-7e08185e2195f1f7b577afb3d1b31710895f8f18cfe215e01e03b2594ac8ef433</citedby><cites>FETCH-LOGICAL-c382t-7e08185e2195f1f7b577afb3d1b31710895f8f18cfe215e01e03b2594ac8ef433</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S0001437018010149$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S0001437018010149$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Tishchenko, P. Ya</creatorcontrib><creatorcontrib>Semkin, P. Yu</creatorcontrib><creatorcontrib>Pavlova, G. Yu</creatorcontrib><creatorcontrib>Tishchenko, P. P.</creatorcontrib><creatorcontrib>Lobanov, V. B.</creatorcontrib><creatorcontrib>Marjash, A. A.</creatorcontrib><creatorcontrib>Mikhailik, T. A.</creatorcontrib><creatorcontrib>Sagalaev, S. G.</creatorcontrib><creatorcontrib>Sergeev, A. F.</creatorcontrib><creatorcontrib>Tibenko, E. Yu</creatorcontrib><creatorcontrib>Khodorenko, N. D.</creatorcontrib><creatorcontrib>Chichkin, R. V.</creatorcontrib><creatorcontrib>Shvetsova, M. G.</creatorcontrib><creatorcontrib>Shkirnikova, E. M.</creatorcontrib><title>Hydrochemistry of the Tumen River Estuary, Sea of Japan</title><title>Oceanology (Washington. 1965)</title><addtitle>Oceanology</addtitle><description>The hydrological and hydrochemical parameters of the Tumen River estuary were collected at 13 stations in May and October 2015. Vertical temperature, conductivity, dissolved oxygen, chlorophyll fluorescence, and turbidity profiles were obtained. Water was sampled from the surface and bottom layer. The water samples were analyzed for major ions, pH, salinity, concentrations of dissolved oxygen, major nutrients, dissolved organic carbon, humic matter, and δ
18
О and δD isotopes. This estuary is attributed to microtidal type with a flushing time of about 10 h. A phytoplakton bloom occurred in the top layer of the estuary. For surface horizons, the hydrochemical parameters show a linear correlation with salinity. In the bottom horizons, all these parameters, except for major ions and δ
18
О and δD isotopes, reveal substantial nonconservative behavior. The nonconservative behavior of the hydrochemical parameters in the bottom waters was mainly caused by degradation of the phytoplankton biomass at the water/sediment interface. Hypoxic conditions were established in the bottom waters of the estuary in May.</description><subject>Biodegradation</subject><subject>Blooms</subject><subject>Chlorophyll</subject><subject>Chlorophylls</subject><subject>Dissolved organic carbon</subject><subject>Dissolved oxygen</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Estuaries</subject><subject>Estuarine dynamics</subject><subject>Fluorescence</subject><subject>Flushing time</subject><subject>Hydrochemistry</subject><subject>Hydrology</subject><subject>Hypoxia</subject><subject>Ions</subject><subject>Isotopes</subject><subject>Marine Chemistry</subject><subject>Mineral nutrients</subject><subject>Nutrients</subject><subject>Oceanography</subject><subject>Parameters</subject><subject>Phytoplankton</subject><subject>Profiles</subject><subject>Rivers</subject><subject>Salinity</subject><subject>Salinity effects</subject><subject>Turbidity</subject><subject>Water analysis</subject><subject>Water sampling</subject><issn>0001-4370</issn><issn>1531-8508</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kE1Lw0AQhhdRMFZ_gLcFr0Znsll2c5RSrVIQbD2HTTprU8yHu4nQf98NETyIpxnmfd75Yuwa4Q5RpPdrAMBUKEANGLLshEUoBcZagj5l0SjHo37OLrzfA4jA6Iip5WHr2nJHdeV7d-Ct5f2O-GaoqeFv1Tc5vvD9YNzhlq_JjPqL6Uxzyc6s-fR09RNn7P1xsZkv49Xr0_P8YRWXQid9rAg0akkJZtKiVYVUythCbLEQqBB0KGuLurQBkQRIIIpEZqkpNdlUiBm7mfp2rv0ayPf5vh1cE0bmCYg0CzfrkcKJKl3rvSObd66qw9I5Qj7-J__zn-BJJo8PbPNB7rfz_6YjxBJkTw</recordid><startdate>20180301</startdate><enddate>20180301</enddate><creator>Tishchenko, P. 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Water was sampled from the surface and bottom layer. The water samples were analyzed for major ions, pH, salinity, concentrations of dissolved oxygen, major nutrients, dissolved organic carbon, humic matter, and δ
18
О and δD isotopes. This estuary is attributed to microtidal type with a flushing time of about 10 h. A phytoplakton bloom occurred in the top layer of the estuary. For surface horizons, the hydrochemical parameters show a linear correlation with salinity. In the bottom horizons, all these parameters, except for major ions and δ
18
О and δD isotopes, reveal substantial nonconservative behavior. The nonconservative behavior of the hydrochemical parameters in the bottom waters was mainly caused by degradation of the phytoplankton biomass at the water/sediment interface. Hypoxic conditions were established in the bottom waters of the estuary in May.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S0001437018010149</doi><tpages>12</tpages></addata></record> |
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subjects | Biodegradation Blooms Chlorophyll Chlorophylls Dissolved organic carbon Dissolved oxygen Earth and Environmental Science Earth Sciences Estuaries Estuarine dynamics Fluorescence Flushing time Hydrochemistry Hydrology Hypoxia Ions Isotopes Marine Chemistry Mineral nutrients Nutrients Oceanography Parameters Phytoplankton Profiles Rivers Salinity Salinity effects Turbidity Water analysis Water sampling |
title | Hydrochemistry of the Tumen River Estuary, Sea of Japan |
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