Hydrochemistry of the Tumen River Estuary, Sea of Japan
Abstract 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...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Tishchenko, P. Ya. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2018 |
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| Anmerkung: |
© Pleiades Publishing, Inc. 2018 |
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| Übergeordnetes Werk: |
Enthalten in: Oceanology - Pleiades Publishing, 1966, 58(2018), 2 vom: März, Seite 175-186 |
|---|---|
| Übergeordnetes Werk: |
volume:58 ; year:2018 ; number:2 ; month:03 ; pages:175-186 |
| Links: |
|---|
| DOI / URN: |
10.1134/S0001437018010149 |
|---|
| Katalog-ID: |
OLC2071621522 |
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| 520 | |a Abstract 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. | ||
| 700 | 1 | |a Semkin, P. Yu. |4 aut | |
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| 700 | 1 | |a Tishchenko, P. P. |4 aut | |
| 700 | 1 | |a Lobanov, V. B. |4 aut | |
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| 700 | 1 | |a Mikhailik, T. A. |4 aut | |
| 700 | 1 | |a Sagalaev, S. G. |4 aut | |
| 700 | 1 | |a Sergeev, A. F. |4 aut | |
| 700 | 1 | |a Tibenko, E. Yu. |4 aut | |
| 700 | 1 | |a Khodorenko, N. D. |4 aut | |
| 700 | 1 | |a Chichkin, R. V. |4 aut | |
| 700 | 1 | |a Shvetsova, M. G. |4 aut | |
| 700 | 1 | |a Shkirnikova, E. M. |4 aut | |
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10.1134/S0001437018010149 doi (DE-627)OLC2071621522 (DE-He213)S0001437018010149-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Tishchenko, P. Ya. verfasserin aut Hydrochemistry of the Tumen River Estuary, Sea of Japan 2018 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2018 Abstract 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. Semkin, P. Yu. aut Pavlova, G. Yu. aut Tishchenko, P. P. aut Lobanov, V. B. aut Marjash, A. A. aut Mikhailik, T. A. aut Sagalaev, S. G. aut Sergeev, A. F. aut Tibenko, E. Yu. aut Khodorenko, N. D. aut Chichkin, R. V. aut Shvetsova, M. G. aut Shkirnikova, E. M. aut Enthalten in Oceanology Pleiades Publishing, 1966 58(2018), 2 vom: März, Seite 175-186 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:58 year:2018 number:2 month:03 pages:175-186 https://doi.org/10.1134/S0001437018010149 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_201 AR 58 2018 2 03 175-186 |
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10.1134/S0001437018010149 doi (DE-627)OLC2071621522 (DE-He213)S0001437018010149-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Tishchenko, P. Ya. verfasserin aut Hydrochemistry of the Tumen River Estuary, Sea of Japan 2018 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2018 Abstract 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. Semkin, P. Yu. aut Pavlova, G. Yu. aut Tishchenko, P. P. aut Lobanov, V. B. aut Marjash, A. A. aut Mikhailik, T. A. aut Sagalaev, S. G. aut Sergeev, A. F. aut Tibenko, E. Yu. aut Khodorenko, N. D. aut Chichkin, R. V. aut Shvetsova, M. G. aut Shkirnikova, E. M. aut Enthalten in Oceanology Pleiades Publishing, 1966 58(2018), 2 vom: März, Seite 175-186 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:58 year:2018 number:2 month:03 pages:175-186 https://doi.org/10.1134/S0001437018010149 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_201 AR 58 2018 2 03 175-186 |
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10.1134/S0001437018010149 doi (DE-627)OLC2071621522 (DE-He213)S0001437018010149-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Tishchenko, P. Ya. verfasserin aut Hydrochemistry of the Tumen River Estuary, Sea of Japan 2018 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2018 Abstract 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. Semkin, P. Yu. aut Pavlova, G. Yu. aut Tishchenko, P. P. aut Lobanov, V. B. aut Marjash, A. A. aut Mikhailik, T. A. aut Sagalaev, S. G. aut Sergeev, A. F. aut Tibenko, E. Yu. aut Khodorenko, N. D. aut Chichkin, R. V. aut Shvetsova, M. G. aut Shkirnikova, E. M. aut Enthalten in Oceanology Pleiades Publishing, 1966 58(2018), 2 vom: März, Seite 175-186 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:58 year:2018 number:2 month:03 pages:175-186 https://doi.org/10.1134/S0001437018010149 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_201 AR 58 2018 2 03 175-186 |
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10.1134/S0001437018010149 doi (DE-627)OLC2071621522 (DE-He213)S0001437018010149-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Tishchenko, P. Ya. verfasserin aut Hydrochemistry of the Tumen River Estuary, Sea of Japan 2018 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2018 Abstract 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. Semkin, P. Yu. aut Pavlova, G. Yu. aut Tishchenko, P. P. aut Lobanov, V. B. aut Marjash, A. A. aut Mikhailik, T. A. aut Sagalaev, S. G. aut Sergeev, A. F. aut Tibenko, E. Yu. aut Khodorenko, N. D. aut Chichkin, R. V. aut Shvetsova, M. G. aut Shkirnikova, E. M. aut Enthalten in Oceanology Pleiades Publishing, 1966 58(2018), 2 vom: März, Seite 175-186 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:58 year:2018 number:2 month:03 pages:175-186 https://doi.org/10.1134/S0001437018010149 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_201 AR 58 2018 2 03 175-186 |
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10.1134/S0001437018010149 doi (DE-627)OLC2071621522 (DE-He213)S0001437018010149-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Tishchenko, P. Ya. verfasserin aut Hydrochemistry of the Tumen River Estuary, Sea of Japan 2018 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2018 Abstract 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. Semkin, P. Yu. aut Pavlova, G. Yu. aut Tishchenko, P. P. aut Lobanov, V. B. aut Marjash, A. A. aut Mikhailik, T. A. aut Sagalaev, S. G. aut Sergeev, A. F. aut Tibenko, E. Yu. aut Khodorenko, N. D. aut Chichkin, R. V. aut Shvetsova, M. G. aut Shkirnikova, E. M. aut Enthalten in Oceanology Pleiades Publishing, 1966 58(2018), 2 vom: März, Seite 175-186 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:58 year:2018 number:2 month:03 pages:175-186 https://doi.org/10.1134/S0001437018010149 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_201 AR 58 2018 2 03 175-186 |
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Hydrochemistry of the Tumen River Estuary, Sea of Japan |
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Tishchenko, P. Ya. |
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Oceanology |
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Oceanology |
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500 - Science |
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2018 |
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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. |
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Tishchenko, P. Ya. |
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10.1134/S0001437018010149 |
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550 |
| title_sort |
hydrochemistry of the tumen river estuary, sea of japan |
| title_auth |
Hydrochemistry of the Tumen River Estuary, Sea of Japan |
| abstract |
Abstract 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. © Pleiades Publishing, Inc. 2018 |
| abstractGer |
Abstract 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. © Pleiades Publishing, Inc. 2018 |
| abstract_unstemmed |
Abstract 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. © Pleiades Publishing, Inc. 2018 |
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Hydrochemistry of the Tumen River Estuary, Sea of Japan |
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https://doi.org/10.1134/S0001437018010149 |
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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. |
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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. |
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