Production-destruction processes in estuaries of the rivers of Artemovka and Shkotovka (Usuri Bay) in summer
Abstract Production and hydrochemical characteristics of the estuaries of the rivers of Artemovka and Shkotovka, flowing into the apex of the Ussuri Bay (the Sea of Japan), were studied in the summer of 2011. Because of the high rate of destruction processes, the partial pressure in river waters of...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Semkin, P. Yu. [verfasserIn] Tishchenko, P. Ya. [verfasserIn] Khodorenko, N. D. [verfasserIn] Zvalinskii, V. I. [verfasserIn] Mikhailik, T. A. [verfasserIn] Sagalaev, S. G. [verfasserIn] Stepanova, V. I. [verfasserIn] Tishchenko, P. P. [verfasserIn] Shvetsova, M. G. [verfasserIn] Shkirnikova, E. M. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Water resources - Moscow : MAIK Nauka/Interperiodica Publ., 1974, 42(2015), 3 vom: Mai, Seite 352-361 |
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| Übergeordnetes Werk: |
volume:42 ; year:2015 ; number:3 ; month:05 ; pages:352-361 |
| Links: |
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| DOI / URN: |
10.1134/S0097807815030161 |
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| Katalog-ID: |
SPR018358535 |
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| 520 | |a Abstract Production and hydrochemical characteristics of the estuaries of the rivers of Artemovka and Shkotovka, flowing into the apex of the Ussuri Bay (the Sea of Japan), were studied in the summer of 2011. Because of the high rate of destruction processes, the partial pressure in river waters of the Shkotovka, Artemovka, and Knevichanka (the Artemovka’s major tributary) was 800, 1800, and 3700 μatm, respectively. Unlike the Shkotovka R. estuary, the high trophic level of the Artemovka R. and a favorable combination of hydrological and hydrochemical conditions in the study period determined the high rate of production processes (chlorophyll a concentration reached 200 μg/L, oxygen oversaturation was more than twofold, the partial pressure of carbon dioxide dropped to 25 μatm). A conservative and nonconservative dependence of alkalinity on salinity was also found to exist in the water of the Shkotovka and Artemovka rivers, respectively. | ||
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| 650 | 4 | |a carbonate system |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a estuary |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Tishchenko, P. Ya. |e verfasserin |4 aut | |
| 700 | 1 | |a Khodorenko, N. D. |e verfasserin |4 aut | |
| 700 | 1 | |a Zvalinskii, V. I. |e verfasserin |4 aut | |
| 700 | 1 | |a Mikhailik, T. A. |e verfasserin |4 aut | |
| 700 | 1 | |a Sagalaev, S. G. |e verfasserin |4 aut | |
| 700 | 1 | |a Stepanova, V. I. |e verfasserin |4 aut | |
| 700 | 1 | |a Tishchenko, P. P. |e verfasserin |4 aut | |
| 700 | 1 | |a Shvetsova, M. G. |e verfasserin |4 aut | |
| 700 | 1 | |a Shkirnikova, E. M. |e verfasserin |4 aut | |
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10.1134/S0097807815030161 doi (DE-627)SPR018358535 (SPR)S0097807815030161-e DE-627 ger DE-627 rakwb eng 690 ASE 58.51 bkl Semkin, P. Yu. verfasserin aut Production-destruction processes in estuaries of the rivers of Artemovka and Shkotovka (Usuri Bay) in summer 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Production and hydrochemical characteristics of the estuaries of the rivers of Artemovka and Shkotovka, flowing into the apex of the Ussuri Bay (the Sea of Japan), were studied in the summer of 2011. Because of the high rate of destruction processes, the partial pressure in river waters of the Shkotovka, Artemovka, and Knevichanka (the Artemovka’s major tributary) was 800, 1800, and 3700 μatm, respectively. Unlike the Shkotovka R. estuary, the high trophic level of the Artemovka R. and a favorable combination of hydrological and hydrochemical conditions in the study period determined the high rate of production processes (chlorophyll a concentration reached 200 μg/L, oxygen oversaturation was more than twofold, the partial pressure of carbon dioxide dropped to 25 μatm). A conservative and nonconservative dependence of alkalinity on salinity was also found to exist in the water of the Shkotovka and Artemovka rivers, respectively. dissolved carbon (dpeaa)DE-He213 production-destruction processes of organic matter (dpeaa)DE-He213 eutrophication (dpeaa)DE-He213 carbonate system (dpeaa)DE-He213 estuary (dpeaa)DE-He213 Tishchenko, P. Ya. verfasserin aut Khodorenko, N. D. verfasserin aut Zvalinskii, V. I. verfasserin aut Mikhailik, T. A. verfasserin aut Sagalaev, S. G. verfasserin aut Stepanova, V. I. verfasserin aut Tishchenko, P. P. verfasserin aut Shvetsova, M. G. verfasserin aut Shkirnikova, E. M. verfasserin aut Enthalten in Water resources Moscow : MAIK Nauka/Interperiodica Publ., 1974 42(2015), 3 vom: Mai, Seite 352-361 (DE-627)334716829 (DE-600)2058341-2 1608-344X nnns volume:42 year:2015 number:3 month:05 pages:352-361 https://dx.doi.org/10.1134/S0097807815030161 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 58.51 ASE AR 42 2015 3 05 352-361 |
| spelling |
10.1134/S0097807815030161 doi (DE-627)SPR018358535 (SPR)S0097807815030161-e DE-627 ger DE-627 rakwb eng 690 ASE 58.51 bkl Semkin, P. Yu. verfasserin aut Production-destruction processes in estuaries of the rivers of Artemovka and Shkotovka (Usuri Bay) in summer 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Production and hydrochemical characteristics of the estuaries of the rivers of Artemovka and Shkotovka, flowing into the apex of the Ussuri Bay (the Sea of Japan), were studied in the summer of 2011. Because of the high rate of destruction processes, the partial pressure in river waters of the Shkotovka, Artemovka, and Knevichanka (the Artemovka’s major tributary) was 800, 1800, and 3700 μatm, respectively. Unlike the Shkotovka R. estuary, the high trophic level of the Artemovka R. and a favorable combination of hydrological and hydrochemical conditions in the study period determined the high rate of production processes (chlorophyll a concentration reached 200 μg/L, oxygen oversaturation was more than twofold, the partial pressure of carbon dioxide dropped to 25 μatm). A conservative and nonconservative dependence of alkalinity on salinity was also found to exist in the water of the Shkotovka and Artemovka rivers, respectively. dissolved carbon (dpeaa)DE-He213 production-destruction processes of organic matter (dpeaa)DE-He213 eutrophication (dpeaa)DE-He213 carbonate system (dpeaa)DE-He213 estuary (dpeaa)DE-He213 Tishchenko, P. Ya. verfasserin aut Khodorenko, N. D. verfasserin aut Zvalinskii, V. I. verfasserin aut Mikhailik, T. A. verfasserin aut Sagalaev, S. G. verfasserin aut Stepanova, V. I. verfasserin aut Tishchenko, P. P. verfasserin aut Shvetsova, M. G. verfasserin aut Shkirnikova, E. M. verfasserin aut Enthalten in Water resources Moscow : MAIK Nauka/Interperiodica Publ., 1974 42(2015), 3 vom: Mai, Seite 352-361 (DE-627)334716829 (DE-600)2058341-2 1608-344X nnns volume:42 year:2015 number:3 month:05 pages:352-361 https://dx.doi.org/10.1134/S0097807815030161 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 58.51 ASE AR 42 2015 3 05 352-361 |
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10.1134/S0097807815030161 doi (DE-627)SPR018358535 (SPR)S0097807815030161-e DE-627 ger DE-627 rakwb eng 690 ASE 58.51 bkl Semkin, P. Yu. verfasserin aut Production-destruction processes in estuaries of the rivers of Artemovka and Shkotovka (Usuri Bay) in summer 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Production and hydrochemical characteristics of the estuaries of the rivers of Artemovka and Shkotovka, flowing into the apex of the Ussuri Bay (the Sea of Japan), were studied in the summer of 2011. Because of the high rate of destruction processes, the partial pressure in river waters of the Shkotovka, Artemovka, and Knevichanka (the Artemovka’s major tributary) was 800, 1800, and 3700 μatm, respectively. Unlike the Shkotovka R. estuary, the high trophic level of the Artemovka R. and a favorable combination of hydrological and hydrochemical conditions in the study period determined the high rate of production processes (chlorophyll a concentration reached 200 μg/L, oxygen oversaturation was more than twofold, the partial pressure of carbon dioxide dropped to 25 μatm). A conservative and nonconservative dependence of alkalinity on salinity was also found to exist in the water of the Shkotovka and Artemovka rivers, respectively. dissolved carbon (dpeaa)DE-He213 production-destruction processes of organic matter (dpeaa)DE-He213 eutrophication (dpeaa)DE-He213 carbonate system (dpeaa)DE-He213 estuary (dpeaa)DE-He213 Tishchenko, P. Ya. verfasserin aut Khodorenko, N. D. verfasserin aut Zvalinskii, V. I. verfasserin aut Mikhailik, T. A. verfasserin aut Sagalaev, S. G. verfasserin aut Stepanova, V. I. verfasserin aut Tishchenko, P. P. verfasserin aut Shvetsova, M. G. verfasserin aut Shkirnikova, E. M. verfasserin aut Enthalten in Water resources Moscow : MAIK Nauka/Interperiodica Publ., 1974 42(2015), 3 vom: Mai, Seite 352-361 (DE-627)334716829 (DE-600)2058341-2 1608-344X nnns volume:42 year:2015 number:3 month:05 pages:352-361 https://dx.doi.org/10.1134/S0097807815030161 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 58.51 ASE AR 42 2015 3 05 352-361 |
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10.1134/S0097807815030161 doi (DE-627)SPR018358535 (SPR)S0097807815030161-e DE-627 ger DE-627 rakwb eng 690 ASE 58.51 bkl Semkin, P. Yu. verfasserin aut Production-destruction processes in estuaries of the rivers of Artemovka and Shkotovka (Usuri Bay) in summer 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Production and hydrochemical characteristics of the estuaries of the rivers of Artemovka and Shkotovka, flowing into the apex of the Ussuri Bay (the Sea of Japan), were studied in the summer of 2011. Because of the high rate of destruction processes, the partial pressure in river waters of the Shkotovka, Artemovka, and Knevichanka (the Artemovka’s major tributary) was 800, 1800, and 3700 μatm, respectively. Unlike the Shkotovka R. estuary, the high trophic level of the Artemovka R. and a favorable combination of hydrological and hydrochemical conditions in the study period determined the high rate of production processes (chlorophyll a concentration reached 200 μg/L, oxygen oversaturation was more than twofold, the partial pressure of carbon dioxide dropped to 25 μatm). A conservative and nonconservative dependence of alkalinity on salinity was also found to exist in the water of the Shkotovka and Artemovka rivers, respectively. dissolved carbon (dpeaa)DE-He213 production-destruction processes of organic matter (dpeaa)DE-He213 eutrophication (dpeaa)DE-He213 carbonate system (dpeaa)DE-He213 estuary (dpeaa)DE-He213 Tishchenko, P. Ya. verfasserin aut Khodorenko, N. D. verfasserin aut Zvalinskii, V. I. verfasserin aut Mikhailik, T. A. verfasserin aut Sagalaev, S. G. verfasserin aut Stepanova, V. I. verfasserin aut Tishchenko, P. P. verfasserin aut Shvetsova, M. G. verfasserin aut Shkirnikova, E. M. verfasserin aut Enthalten in Water resources Moscow : MAIK Nauka/Interperiodica Publ., 1974 42(2015), 3 vom: Mai, Seite 352-361 (DE-627)334716829 (DE-600)2058341-2 1608-344X nnns volume:42 year:2015 number:3 month:05 pages:352-361 https://dx.doi.org/10.1134/S0097807815030161 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 58.51 ASE AR 42 2015 3 05 352-361 |
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10.1134/S0097807815030161 doi (DE-627)SPR018358535 (SPR)S0097807815030161-e DE-627 ger DE-627 rakwb eng 690 ASE 58.51 bkl Semkin, P. Yu. verfasserin aut Production-destruction processes in estuaries of the rivers of Artemovka and Shkotovka (Usuri Bay) in summer 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Production and hydrochemical characteristics of the estuaries of the rivers of Artemovka and Shkotovka, flowing into the apex of the Ussuri Bay (the Sea of Japan), were studied in the summer of 2011. Because of the high rate of destruction processes, the partial pressure in river waters of the Shkotovka, Artemovka, and Knevichanka (the Artemovka’s major tributary) was 800, 1800, and 3700 μatm, respectively. Unlike the Shkotovka R. estuary, the high trophic level of the Artemovka R. and a favorable combination of hydrological and hydrochemical conditions in the study period determined the high rate of production processes (chlorophyll a concentration reached 200 μg/L, oxygen oversaturation was more than twofold, the partial pressure of carbon dioxide dropped to 25 μatm). A conservative and nonconservative dependence of alkalinity on salinity was also found to exist in the water of the Shkotovka and Artemovka rivers, respectively. dissolved carbon (dpeaa)DE-He213 production-destruction processes of organic matter (dpeaa)DE-He213 eutrophication (dpeaa)DE-He213 carbonate system (dpeaa)DE-He213 estuary (dpeaa)DE-He213 Tishchenko, P. Ya. verfasserin aut Khodorenko, N. D. verfasserin aut Zvalinskii, V. I. verfasserin aut Mikhailik, T. A. verfasserin aut Sagalaev, S. G. verfasserin aut Stepanova, V. I. verfasserin aut Tishchenko, P. P. verfasserin aut Shvetsova, M. G. verfasserin aut Shkirnikova, E. M. verfasserin aut Enthalten in Water resources Moscow : MAIK Nauka/Interperiodica Publ., 1974 42(2015), 3 vom: Mai, Seite 352-361 (DE-627)334716829 (DE-600)2058341-2 1608-344X nnns volume:42 year:2015 number:3 month:05 pages:352-361 https://dx.doi.org/10.1134/S0097807815030161 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 58.51 ASE AR 42 2015 3 05 352-361 |
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Semkin, P. Yu. @@aut@@ Tishchenko, P. Ya. @@aut@@ Khodorenko, N. D. @@aut@@ Zvalinskii, V. I. @@aut@@ Mikhailik, T. A. @@aut@@ Sagalaev, S. G. @@aut@@ Stepanova, V. I. @@aut@@ Tishchenko, P. P. @@aut@@ Shvetsova, M. G. @@aut@@ Shkirnikova, E. M. @@aut@@ |
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Because of the high rate of destruction processes, the partial pressure in river waters of the Shkotovka, Artemovka, and Knevichanka (the Artemovka’s major tributary) was 800, 1800, and 3700 μatm, respectively. Unlike the Shkotovka R. estuary, the high trophic level of the Artemovka R. and a favorable combination of hydrological and hydrochemical conditions in the study period determined the high rate of production processes (chlorophyll a concentration reached 200 μg/L, oxygen oversaturation was more than twofold, the partial pressure of carbon dioxide dropped to 25 μatm). 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Semkin, P. Yu. |
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Semkin, P. Yu. ddc 690 bkl 58.51 misc dissolved carbon misc production-destruction processes of organic matter misc eutrophication misc carbonate system misc estuary Production-destruction processes in estuaries of the rivers of Artemovka and Shkotovka (Usuri Bay) in summer |
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690 ASE 58.51 bkl Production-destruction processes in estuaries of the rivers of Artemovka and Shkotovka (Usuri Bay) in summer dissolved carbon (dpeaa)DE-He213 production-destruction processes of organic matter (dpeaa)DE-He213 eutrophication (dpeaa)DE-He213 carbonate system (dpeaa)DE-He213 estuary (dpeaa)DE-He213 |
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Production-destruction processes in estuaries of the rivers of Artemovka and Shkotovka (Usuri Bay) in summer |
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Semkin, P. Yu. Tishchenko, P. Ya. Khodorenko, N. D. Zvalinskii, V. I. Mikhailik, T. A. Sagalaev, S. G. Stepanova, V. I. Tishchenko, P. P. Shvetsova, M. G. Shkirnikova, E. M. |
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Semkin, P. Yu. |
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production-destruction processes in estuaries of the rivers of artemovka and shkotovka (usuri bay) in summer |
| title_auth |
Production-destruction processes in estuaries of the rivers of Artemovka and Shkotovka (Usuri Bay) in summer |
| abstract |
Abstract Production and hydrochemical characteristics of the estuaries of the rivers of Artemovka and Shkotovka, flowing into the apex of the Ussuri Bay (the Sea of Japan), were studied in the summer of 2011. Because of the high rate of destruction processes, the partial pressure in river waters of the Shkotovka, Artemovka, and Knevichanka (the Artemovka’s major tributary) was 800, 1800, and 3700 μatm, respectively. Unlike the Shkotovka R. estuary, the high trophic level of the Artemovka R. and a favorable combination of hydrological and hydrochemical conditions in the study period determined the high rate of production processes (chlorophyll a concentration reached 200 μg/L, oxygen oversaturation was more than twofold, the partial pressure of carbon dioxide dropped to 25 μatm). A conservative and nonconservative dependence of alkalinity on salinity was also found to exist in the water of the Shkotovka and Artemovka rivers, respectively. |
| abstractGer |
Abstract Production and hydrochemical characteristics of the estuaries of the rivers of Artemovka and Shkotovka, flowing into the apex of the Ussuri Bay (the Sea of Japan), were studied in the summer of 2011. Because of the high rate of destruction processes, the partial pressure in river waters of the Shkotovka, Artemovka, and Knevichanka (the Artemovka’s major tributary) was 800, 1800, and 3700 μatm, respectively. Unlike the Shkotovka R. estuary, the high trophic level of the Artemovka R. and a favorable combination of hydrological and hydrochemical conditions in the study period determined the high rate of production processes (chlorophyll a concentration reached 200 μg/L, oxygen oversaturation was more than twofold, the partial pressure of carbon dioxide dropped to 25 μatm). A conservative and nonconservative dependence of alkalinity on salinity was also found to exist in the water of the Shkotovka and Artemovka rivers, respectively. |
| abstract_unstemmed |
Abstract Production and hydrochemical characteristics of the estuaries of the rivers of Artemovka and Shkotovka, flowing into the apex of the Ussuri Bay (the Sea of Japan), were studied in the summer of 2011. Because of the high rate of destruction processes, the partial pressure in river waters of the Shkotovka, Artemovka, and Knevichanka (the Artemovka’s major tributary) was 800, 1800, and 3700 μatm, respectively. Unlike the Shkotovka R. estuary, the high trophic level of the Artemovka R. and a favorable combination of hydrological and hydrochemical conditions in the study period determined the high rate of production processes (chlorophyll a concentration reached 200 μg/L, oxygen oversaturation was more than twofold, the partial pressure of carbon dioxide dropped to 25 μatm). A conservative and nonconservative dependence of alkalinity on salinity was also found to exist in the water of the Shkotovka and Artemovka rivers, respectively. |
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Production-destruction processes in estuaries of the rivers of Artemovka and Shkotovka (Usuri Bay) in summer |
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| score |
7.4007063 |