Estimation of Nutrient Fluxes on the Interface Bottom Water–Sediments in Shallow Bights of the Peter the Great Bay, Sea of Japan

Abstract— Fluxes of nutrients (ammonium, total nitrogen, dissolved inorganic phosphorus, total phosphorus, silica, and dissolved organic carbon) across the interface between bottom water and sediments were studied in three shallow bights (Voevoda, Novgorodskaya, and Uglovoj) of the Peter the Great B...
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Autor*in:	Tishchenko, P. Ya. [verfasserIn] Borisenko, G. V. Barabanshchikov, Yu. A. Pavlova, G. Yu. Riumina, A. A. Sagalaev, S. G. Semkin, P. Yu. Tishchenko, P. P. Ulanova, O. A. Shvetsova, M. G. Shkirnikova, E. M.

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2022

Anmerkung:	© Pleiades Publishing, Ltd. 2022. ISSN 0016-7029, Geochemistry International, 2022, Vol. 60, No. 9, pp. 891–904. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Geokhimiya, 2022, Vol. 67, No. 9, pp. 881–895.

Übergeordnetes Werk:	Enthalten in: Geochemistry international - Berlin : Springer Science + Business Media, 1996, 60(2022), 9 vom: Sept., Seite 891-904
Übergeordnetes Werk:	volume:60 ; year:2022 ; number:9 ; month:09 ; pages:891-904

Links:	Volltext

DOI / URN:	10.1134/S0016702922090087

Katalog-ID:	SPR050985213

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100	1		\|a Tishchenko, P. Ya. \|e verfasserin \|4 aut
245	1	0	\|a Estimation of Nutrient Fluxes on the Interface Bottom Water–Sediments in Shallow Bights of the Peter the Great Bay, Sea of Japan
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520			\|a Abstract— Fluxes of nutrients (ammonium, total nitrogen, dissolved inorganic phosphorus, total phosphorus, silica, and dissolved organic carbon) across the interface between bottom water and sediments were studied in three shallow bights (Voevoda, Novgorodskaya, and Uglovoj) of the Peter the Great Bay in the course of survey in September–October, 2019. At two stations in each of the bights, nutrient concentrations were measured in seawater sampled at 10 cm above the seafloor and in the pore waters of the sediment cores; and organic carbon, fulvic acids, humic acids, and chlorophyll a were analyzed in the solid phase of the sediments. Bioturbation coefficients were estimated from variations in chlorophyll a concentration with depth in the sediment cores. The fluxes of nutrients (ammonium, total nitrogen, phosphorus, total phosphorus, and silicon) and dissolved organic carbon (DOC) were evaluated by model calculations. The estimated nutrients fluxes were, with regard to the bioturbation, about one order of magnitude higher than those estimated by the Fick law. The highest concentrations of organic carbon, 6.5 and 5.5% per dry weight of sediments, were found in the top layer of sediments retrieved at sites covered by Zostera marina L. in the Voevoda and Novgorodskaya bights, respectively. However, the highest fluxes across the water–sediment interface were obtained for a site devoid of seagrass in the Novgorodskaya bight, where the top sediment layer contained 2.8% organic carbon. The annual specific fluxes of nutrients estimated for the water–sediment interface were comparable to or even higher than the annual specific fluxes of nutrients brought per surface area unit of the Amur bay by the Razdolnaya River and domestic waste waters from the city of Vladivostok.
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700	1		\|a Barabanshchikov, Yu. A. \|4 aut
700	1		\|a Pavlova, G. Yu. \|4 aut
700	1		\|a Riumina, A. A. \|4 aut
700	1		\|a Sagalaev, S. G. \|4 aut
700	1		\|a Semkin, P. Yu. \|4 aut
700	1		\|a Tishchenko, P. P. \|4 aut
700	1		\|a Ulanova, O. A. \|4 aut
700	1		\|a Shvetsova, M. G. \|4 aut
700	1		\|a Shkirnikova, E. M. \|4 aut
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912			\|a GBV_ILN_4333
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allfields	10.1134/S0016702922090087 doi (DE-627)SPR050985213 (SPR)S0016702922090087-e DE-627 ger DE-627 rakwb eng Tishchenko, P. Ya. verfasserin aut Estimation of Nutrient Fluxes on the Interface Bottom Water–Sediments in Shallow Bights of the Peter the Great Bay, Sea of Japan 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 0016-7029, Geochemistry International, 2022, Vol. 60, No. 9, pp. 891–904. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Geokhimiya, 2022, Vol. 67, No. 9, pp. 881–895. Abstract— Fluxes of nutrients (ammonium, total nitrogen, dissolved inorganic phosphorus, total phosphorus, silica, and dissolved organic carbon) across the interface between bottom water and sediments were studied in three shallow bights (Voevoda, Novgorodskaya, and Uglovoj) of the Peter the Great Bay in the course of survey in September–October, 2019. At two stations in each of the bights, nutrient concentrations were measured in seawater sampled at 10 cm above the seafloor and in the pore waters of the sediment cores; and organic carbon, fulvic acids, humic acids, and chlorophyll a were analyzed in the solid phase of the sediments. Bioturbation coefficients were estimated from variations in chlorophyll a concentration with depth in the sediment cores. The fluxes of nutrients (ammonium, total nitrogen, phosphorus, total phosphorus, and silicon) and dissolved organic carbon (DOC) were evaluated by model calculations. The estimated nutrients fluxes were, with regard to the bioturbation, about one order of magnitude higher than those estimated by the Fick law. The highest concentrations of organic carbon, 6.5 and 5.5% per dry weight of sediments, were found in the top layer of sediments retrieved at sites covered by Zostera marina L. in the Voevoda and Novgorodskaya bights, respectively. However, the highest fluxes across the water–sediment interface were obtained for a site devoid of seagrass in the Novgorodskaya bight, where the top sediment layer contained 2.8% organic carbon. The annual specific fluxes of nutrients estimated for the water–sediment interface were comparable to or even higher than the annual specific fluxes of nutrients brought per surface area unit of the Amur bay by the Razdolnaya River and domestic waste waters from the city of Vladivostok. Borisenko, G. V. aut Barabanshchikov, Yu. A. aut Pavlova, G. Yu. aut Riumina, A. A. aut Sagalaev, S. G. aut Semkin, P. Yu. aut Tishchenko, P. P. aut Ulanova, O. A. aut Shvetsova, M. G. aut Shkirnikova, E. M. aut Enthalten in Geochemistry international Berlin : Springer Science + Business Media, 1996 60(2022), 9 vom: Sept., Seite 891-904 (DE-627)341913286 (DE-600)2071136-0 1556-1968 nnns volume:60 year:2022 number:9 month:09 pages:891-904 https://dx.doi.org/10.1134/S0016702922090087 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_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_4126 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 AR 60 2022 9 09 891-904
spelling	10.1134/S0016702922090087 doi (DE-627)SPR050985213 (SPR)S0016702922090087-e DE-627 ger DE-627 rakwb eng Tishchenko, P. Ya. verfasserin aut Estimation of Nutrient Fluxes on the Interface Bottom Water–Sediments in Shallow Bights of the Peter the Great Bay, Sea of Japan 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 0016-7029, Geochemistry International, 2022, Vol. 60, No. 9, pp. 891–904. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Geokhimiya, 2022, Vol. 67, No. 9, pp. 881–895. Abstract— Fluxes of nutrients (ammonium, total nitrogen, dissolved inorganic phosphorus, total phosphorus, silica, and dissolved organic carbon) across the interface between bottom water and sediments were studied in three shallow bights (Voevoda, Novgorodskaya, and Uglovoj) of the Peter the Great Bay in the course of survey in September–October, 2019. At two stations in each of the bights, nutrient concentrations were measured in seawater sampled at 10 cm above the seafloor and in the pore waters of the sediment cores; and organic carbon, fulvic acids, humic acids, and chlorophyll a were analyzed in the solid phase of the sediments. Bioturbation coefficients were estimated from variations in chlorophyll a concentration with depth in the sediment cores. The fluxes of nutrients (ammonium, total nitrogen, phosphorus, total phosphorus, and silicon) and dissolved organic carbon (DOC) were evaluated by model calculations. The estimated nutrients fluxes were, with regard to the bioturbation, about one order of magnitude higher than those estimated by the Fick law. The highest concentrations of organic carbon, 6.5 and 5.5% per dry weight of sediments, were found in the top layer of sediments retrieved at sites covered by Zostera marina L. in the Voevoda and Novgorodskaya bights, respectively. However, the highest fluxes across the water–sediment interface were obtained for a site devoid of seagrass in the Novgorodskaya bight, where the top sediment layer contained 2.8% organic carbon. The annual specific fluxes of nutrients estimated for the water–sediment interface were comparable to or even higher than the annual specific fluxes of nutrients brought per surface area unit of the Amur bay by the Razdolnaya River and domestic waste waters from the city of Vladivostok. Borisenko, G. V. aut Barabanshchikov, Yu. A. aut Pavlova, G. Yu. aut Riumina, A. A. aut Sagalaev, S. G. aut Semkin, P. Yu. aut Tishchenko, P. P. aut Ulanova, O. A. aut Shvetsova, M. G. aut Shkirnikova, E. M. aut Enthalten in Geochemistry international Berlin : Springer Science + Business Media, 1996 60(2022), 9 vom: Sept., Seite 891-904 (DE-627)341913286 (DE-600)2071136-0 1556-1968 nnns volume:60 year:2022 number:9 month:09 pages:891-904 https://dx.doi.org/10.1134/S0016702922090087 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_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_4126 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 AR 60 2022 9 09 891-904
allfields_unstemmed	10.1134/S0016702922090087 doi (DE-627)SPR050985213 (SPR)S0016702922090087-e DE-627 ger DE-627 rakwb eng Tishchenko, P. Ya. verfasserin aut Estimation of Nutrient Fluxes on the Interface Bottom Water–Sediments in Shallow Bights of the Peter the Great Bay, Sea of Japan 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 0016-7029, Geochemistry International, 2022, Vol. 60, No. 9, pp. 891–904. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Geokhimiya, 2022, Vol. 67, No. 9, pp. 881–895. Abstract— Fluxes of nutrients (ammonium, total nitrogen, dissolved inorganic phosphorus, total phosphorus, silica, and dissolved organic carbon) across the interface between bottom water and sediments were studied in three shallow bights (Voevoda, Novgorodskaya, and Uglovoj) of the Peter the Great Bay in the course of survey in September–October, 2019. At two stations in each of the bights, nutrient concentrations were measured in seawater sampled at 10 cm above the seafloor and in the pore waters of the sediment cores; and organic carbon, fulvic acids, humic acids, and chlorophyll a were analyzed in the solid phase of the sediments. Bioturbation coefficients were estimated from variations in chlorophyll a concentration with depth in the sediment cores. The fluxes of nutrients (ammonium, total nitrogen, phosphorus, total phosphorus, and silicon) and dissolved organic carbon (DOC) were evaluated by model calculations. The estimated nutrients fluxes were, with regard to the bioturbation, about one order of magnitude higher than those estimated by the Fick law. The highest concentrations of organic carbon, 6.5 and 5.5% per dry weight of sediments, were found in the top layer of sediments retrieved at sites covered by Zostera marina L. in the Voevoda and Novgorodskaya bights, respectively. However, the highest fluxes across the water–sediment interface were obtained for a site devoid of seagrass in the Novgorodskaya bight, where the top sediment layer contained 2.8% organic carbon. The annual specific fluxes of nutrients estimated for the water–sediment interface were comparable to or even higher than the annual specific fluxes of nutrients brought per surface area unit of the Amur bay by the Razdolnaya River and domestic waste waters from the city of Vladivostok. Borisenko, G. V. aut Barabanshchikov, Yu. A. aut Pavlova, G. Yu. aut Riumina, A. A. aut Sagalaev, S. G. aut Semkin, P. Yu. aut Tishchenko, P. P. aut Ulanova, O. A. aut Shvetsova, M. G. aut Shkirnikova, E. M. aut Enthalten in Geochemistry international Berlin : Springer Science + Business Media, 1996 60(2022), 9 vom: Sept., Seite 891-904 (DE-627)341913286 (DE-600)2071136-0 1556-1968 nnns volume:60 year:2022 number:9 month:09 pages:891-904 https://dx.doi.org/10.1134/S0016702922090087 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_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_4126 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 AR 60 2022 9 09 891-904
allfieldsGer	10.1134/S0016702922090087 doi (DE-627)SPR050985213 (SPR)S0016702922090087-e DE-627 ger DE-627 rakwb eng Tishchenko, P. Ya. verfasserin aut Estimation of Nutrient Fluxes on the Interface Bottom Water–Sediments in Shallow Bights of the Peter the Great Bay, Sea of Japan 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 0016-7029, Geochemistry International, 2022, Vol. 60, No. 9, pp. 891–904. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Geokhimiya, 2022, Vol. 67, No. 9, pp. 881–895. Abstract— Fluxes of nutrients (ammonium, total nitrogen, dissolved inorganic phosphorus, total phosphorus, silica, and dissolved organic carbon) across the interface between bottom water and sediments were studied in three shallow bights (Voevoda, Novgorodskaya, and Uglovoj) of the Peter the Great Bay in the course of survey in September–October, 2019. At two stations in each of the bights, nutrient concentrations were measured in seawater sampled at 10 cm above the seafloor and in the pore waters of the sediment cores; and organic carbon, fulvic acids, humic acids, and chlorophyll a were analyzed in the solid phase of the sediments. Bioturbation coefficients were estimated from variations in chlorophyll a concentration with depth in the sediment cores. The fluxes of nutrients (ammonium, total nitrogen, phosphorus, total phosphorus, and silicon) and dissolved organic carbon (DOC) were evaluated by model calculations. The estimated nutrients fluxes were, with regard to the bioturbation, about one order of magnitude higher than those estimated by the Fick law. The highest concentrations of organic carbon, 6.5 and 5.5% per dry weight of sediments, were found in the top layer of sediments retrieved at sites covered by Zostera marina L. in the Voevoda and Novgorodskaya bights, respectively. However, the highest fluxes across the water–sediment interface were obtained for a site devoid of seagrass in the Novgorodskaya bight, where the top sediment layer contained 2.8% organic carbon. The annual specific fluxes of nutrients estimated for the water–sediment interface were comparable to or even higher than the annual specific fluxes of nutrients brought per surface area unit of the Amur bay by the Razdolnaya River and domestic waste waters from the city of Vladivostok. Borisenko, G. V. aut Barabanshchikov, Yu. A. aut Pavlova, G. Yu. aut Riumina, A. A. aut Sagalaev, S. G. aut Semkin, P. Yu. aut Tishchenko, P. P. aut Ulanova, O. A. aut Shvetsova, M. G. aut Shkirnikova, E. M. aut Enthalten in Geochemistry international Berlin : Springer Science + Business Media, 1996 60(2022), 9 vom: Sept., Seite 891-904 (DE-627)341913286 (DE-600)2071136-0 1556-1968 nnns volume:60 year:2022 number:9 month:09 pages:891-904 https://dx.doi.org/10.1134/S0016702922090087 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_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_4126 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 AR 60 2022 9 09 891-904
allfieldsSound	10.1134/S0016702922090087 doi (DE-627)SPR050985213 (SPR)S0016702922090087-e DE-627 ger DE-627 rakwb eng Tishchenko, P. Ya. verfasserin aut Estimation of Nutrient Fluxes on the Interface Bottom Water–Sediments in Shallow Bights of the Peter the Great Bay, Sea of Japan 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 0016-7029, Geochemistry International, 2022, Vol. 60, No. 9, pp. 891–904. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Geokhimiya, 2022, Vol. 67, No. 9, pp. 881–895. Abstract— Fluxes of nutrients (ammonium, total nitrogen, dissolved inorganic phosphorus, total phosphorus, silica, and dissolved organic carbon) across the interface between bottom water and sediments were studied in three shallow bights (Voevoda, Novgorodskaya, and Uglovoj) of the Peter the Great Bay in the course of survey in September–October, 2019. At two stations in each of the bights, nutrient concentrations were measured in seawater sampled at 10 cm above the seafloor and in the pore waters of the sediment cores; and organic carbon, fulvic acids, humic acids, and chlorophyll a were analyzed in the solid phase of the sediments. Bioturbation coefficients were estimated from variations in chlorophyll a concentration with depth in the sediment cores. The fluxes of nutrients (ammonium, total nitrogen, phosphorus, total phosphorus, and silicon) and dissolved organic carbon (DOC) were evaluated by model calculations. The estimated nutrients fluxes were, with regard to the bioturbation, about one order of magnitude higher than those estimated by the Fick law. The highest concentrations of organic carbon, 6.5 and 5.5% per dry weight of sediments, were found in the top layer of sediments retrieved at sites covered by Zostera marina L. in the Voevoda and Novgorodskaya bights, respectively. However, the highest fluxes across the water–sediment interface were obtained for a site devoid of seagrass in the Novgorodskaya bight, where the top sediment layer contained 2.8% organic carbon. The annual specific fluxes of nutrients estimated for the water–sediment interface were comparable to or even higher than the annual specific fluxes of nutrients brought per surface area unit of the Amur bay by the Razdolnaya River and domestic waste waters from the city of Vladivostok. Borisenko, G. V. aut Barabanshchikov, Yu. A. aut Pavlova, G. Yu. aut Riumina, A. A. aut Sagalaev, S. G. aut Semkin, P. Yu. aut Tishchenko, P. P. aut Ulanova, O. A. aut Shvetsova, M. G. aut Shkirnikova, E. M. aut Enthalten in Geochemistry international Berlin : Springer Science + Business Media, 1996 60(2022), 9 vom: Sept., Seite 891-904 (DE-627)341913286 (DE-600)2071136-0 1556-1968 nnns volume:60 year:2022 number:9 month:09 pages:891-904 https://dx.doi.org/10.1134/S0016702922090087 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_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_4126 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 AR 60 2022 9 09 891-904
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source	Enthalten in Geochemistry international 60(2022), 9 vom: Sept., Seite 891-904 volume:60 year:2022 number:9 month:09 pages:891-904
sourceStr	Enthalten in Geochemistry international 60(2022), 9 vom: Sept., Seite 891-904 volume:60 year:2022 number:9 month:09 pages:891-904
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authorswithroles_txt_mv	Tishchenko, P. Ya. @@aut@@ Borisenko, G. V. @@aut@@ Barabanshchikov, Yu. A. @@aut@@ Pavlova, G. Yu. @@aut@@ Riumina, A. A. @@aut@@ Sagalaev, S. G. @@aut@@ Semkin, P. Yu. @@aut@@ Tishchenko, P. P. @@aut@@ Ulanova, O. A. @@aut@@ Shvetsova, M. G. @@aut@@ Shkirnikova, E. M. @@aut@@
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author	Tishchenko, P. Ya.
spellingShingle	Tishchenko, P. Ya. Estimation of Nutrient Fluxes on the Interface Bottom Water–Sediments in Shallow Bights of the Peter the Great Bay, Sea of Japan
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topic_title	Estimation of Nutrient Fluxes on the Interface Bottom Water–Sediments in Shallow Bights of the Peter the Great Bay, Sea of Japan
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title	Estimation of Nutrient Fluxes on the Interface Bottom Water–Sediments in Shallow Bights of the Peter the Great Bay, Sea of Japan
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title_full	Estimation of Nutrient Fluxes on the Interface Bottom Water–Sediments in Shallow Bights of the Peter the Great Bay, Sea of Japan
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author_browse	Tishchenko, P. Ya. Borisenko, G. V. Barabanshchikov, Yu. A. Pavlova, G. Yu. Riumina, A. A. Sagalaev, S. G. Semkin, P. Yu. Tishchenko, P. P. Ulanova, O. A. Shvetsova, M. G. Shkirnikova, E. M.
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doi_str_mv	10.1134/S0016702922090087
title_sort	estimation of nutrient fluxes on the interface bottom water–sediments in shallow bights of the peter the great bay, sea of japan
title_auth	Estimation of Nutrient Fluxes on the Interface Bottom Water–Sediments in Shallow Bights of the Peter the Great Bay, Sea of Japan
abstract	Abstract— Fluxes of nutrients (ammonium, total nitrogen, dissolved inorganic phosphorus, total phosphorus, silica, and dissolved organic carbon) across the interface between bottom water and sediments were studied in three shallow bights (Voevoda, Novgorodskaya, and Uglovoj) of the Peter the Great Bay in the course of survey in September–October, 2019. At two stations in each of the bights, nutrient concentrations were measured in seawater sampled at 10 cm above the seafloor and in the pore waters of the sediment cores; and organic carbon, fulvic acids, humic acids, and chlorophyll a were analyzed in the solid phase of the sediments. Bioturbation coefficients were estimated from variations in chlorophyll a concentration with depth in the sediment cores. The fluxes of nutrients (ammonium, total nitrogen, phosphorus, total phosphorus, and silicon) and dissolved organic carbon (DOC) were evaluated by model calculations. The estimated nutrients fluxes were, with regard to the bioturbation, about one order of magnitude higher than those estimated by the Fick law. The highest concentrations of organic carbon, 6.5 and 5.5% per dry weight of sediments, were found in the top layer of sediments retrieved at sites covered by Zostera marina L. in the Voevoda and Novgorodskaya bights, respectively. However, the highest fluxes across the water–sediment interface were obtained for a site devoid of seagrass in the Novgorodskaya bight, where the top sediment layer contained 2.8% organic carbon. The annual specific fluxes of nutrients estimated for the water–sediment interface were comparable to or even higher than the annual specific fluxes of nutrients brought per surface area unit of the Amur bay by the Razdolnaya River and domestic waste waters from the city of Vladivostok. © Pleiades Publishing, Ltd. 2022. ISSN 0016-7029, Geochemistry International, 2022, Vol. 60, No. 9, pp. 891–904. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Geokhimiya, 2022, Vol. 67, No. 9, pp. 881–895.
abstractGer	Abstract— Fluxes of nutrients (ammonium, total nitrogen, dissolved inorganic phosphorus, total phosphorus, silica, and dissolved organic carbon) across the interface between bottom water and sediments were studied in three shallow bights (Voevoda, Novgorodskaya, and Uglovoj) of the Peter the Great Bay in the course of survey in September–October, 2019. At two stations in each of the bights, nutrient concentrations were measured in seawater sampled at 10 cm above the seafloor and in the pore waters of the sediment cores; and organic carbon, fulvic acids, humic acids, and chlorophyll a were analyzed in the solid phase of the sediments. Bioturbation coefficients were estimated from variations in chlorophyll a concentration with depth in the sediment cores. The fluxes of nutrients (ammonium, total nitrogen, phosphorus, total phosphorus, and silicon) and dissolved organic carbon (DOC) were evaluated by model calculations. The estimated nutrients fluxes were, with regard to the bioturbation, about one order of magnitude higher than those estimated by the Fick law. The highest concentrations of organic carbon, 6.5 and 5.5% per dry weight of sediments, were found in the top layer of sediments retrieved at sites covered by Zostera marina L. in the Voevoda and Novgorodskaya bights, respectively. However, the highest fluxes across the water–sediment interface were obtained for a site devoid of seagrass in the Novgorodskaya bight, where the top sediment layer contained 2.8% organic carbon. The annual specific fluxes of nutrients estimated for the water–sediment interface were comparable to or even higher than the annual specific fluxes of nutrients brought per surface area unit of the Amur bay by the Razdolnaya River and domestic waste waters from the city of Vladivostok. © Pleiades Publishing, Ltd. 2022. ISSN 0016-7029, Geochemistry International, 2022, Vol. 60, No. 9, pp. 891–904. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Geokhimiya, 2022, Vol. 67, No. 9, pp. 881–895.
abstract_unstemmed	Abstract— Fluxes of nutrients (ammonium, total nitrogen, dissolved inorganic phosphorus, total phosphorus, silica, and dissolved organic carbon) across the interface between bottom water and sediments were studied in three shallow bights (Voevoda, Novgorodskaya, and Uglovoj) of the Peter the Great Bay in the course of survey in September–October, 2019. At two stations in each of the bights, nutrient concentrations were measured in seawater sampled at 10 cm above the seafloor and in the pore waters of the sediment cores; and organic carbon, fulvic acids, humic acids, and chlorophyll a were analyzed in the solid phase of the sediments. Bioturbation coefficients were estimated from variations in chlorophyll a concentration with depth in the sediment cores. The fluxes of nutrients (ammonium, total nitrogen, phosphorus, total phosphorus, and silicon) and dissolved organic carbon (DOC) were evaluated by model calculations. The estimated nutrients fluxes were, with regard to the bioturbation, about one order of magnitude higher than those estimated by the Fick law. The highest concentrations of organic carbon, 6.5 and 5.5% per dry weight of sediments, were found in the top layer of sediments retrieved at sites covered by Zostera marina L. in the Voevoda and Novgorodskaya bights, respectively. However, the highest fluxes across the water–sediment interface were obtained for a site devoid of seagrass in the Novgorodskaya bight, where the top sediment layer contained 2.8% organic carbon. The annual specific fluxes of nutrients estimated for the water–sediment interface were comparable to or even higher than the annual specific fluxes of nutrients brought per surface area unit of the Amur bay by the Razdolnaya River and domestic waste waters from the city of Vladivostok. © Pleiades Publishing, Ltd. 2022. ISSN 0016-7029, Geochemistry International, 2022, Vol. 60, No. 9, pp. 891–904. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Geokhimiya, 2022, Vol. 67, No. 9, pp. 881–895.
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container_issue	9
title_short	Estimation of Nutrient Fluxes on the Interface Bottom Water–Sediments in Shallow Bights of the Peter the Great Bay, Sea of Japan
url	https://dx.doi.org/10.1134/S0016702922090087
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author2	Borisenko, G. V. Barabanshchikov, Yu. A. Pavlova, G. Yu Riumina, A. A. Sagalaev, S. G. Semkin, P. Yu Tishchenko, P. P. Ulanova, O. A. Shvetsova, M. G. Shkirnikova, E. M.
author2Str	Borisenko, G. V. Barabanshchikov, Yu. A. Pavlova, G. Yu Riumina, A. A. Sagalaev, S. G. Semkin, P. Yu Tishchenko, P. P. Ulanova, O. A. Shvetsova, M. G. Shkirnikova, E. M.
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doi_str	10.1134/S0016702922090087
up_date	2024-07-03T19:03:17.164Z
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Estimation of Nutrient Fluxes on the Interface Bottom Water–Sediments in Shallow Bights of the Peter the Great Bay, Sea of Japan

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