HYDROCHEMICAL STUDIES OF THE PARTIZANSKAYA RIVER ESTUARY (NAKHODKA BAY, JAPAN SEA) IN SUMMER SEASON OF LOW WATER DISCHARGE

Chemical water parameters in the Partizanskaya River estuary were measured on July 18–19, 2012 in conditions of low water discharge (20.1 m3 /s). In these conditions, the cline of salt water at the bottom penetrated up to 11 km upstream from the river mouth and the fresh river water passed the estua...

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Main Authors: P. Yu. Semkin, P. A. Tishchenko, T. A. Mikhailik, Yu. A. Barabanshchikov, G. Yu. Pavlova, S. G. Sagalaev, P. P. Tishchenko, M. G. Shvetsova, E. M. Shkirnikova
Format: Article
Language:Russian
Published: Transactions of the Pacific Research Institute of Fisheries and Oceanography 2018-06-01
Series:Известия ТИНРО
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Online Access:https://izvestiya.tinro-center.ru/jour/article/view/386
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author P. Yu. Semkin
P. A. Tishchenko
T. A. Mikhailik
Yu. A. Barabanshchikov
G. Yu. Pavlova
S. G. Sagalaev
P. P. Tishchenko
M. G. Shvetsova
E. M. Shkirnikova
author_facet P. Yu. Semkin
P. A. Tishchenko
T. A. Mikhailik
Yu. A. Barabanshchikov
G. Yu. Pavlova
S. G. Sagalaev
P. P. Tishchenko
M. G. Shvetsova
E. M. Shkirnikova
author_sort P. Yu. Semkin
collection DOAJ
description Chemical water parameters in the Partizanskaya River estuary were measured on July 18–19, 2012 in conditions of low water discharge (20.1 m3 /s). In these conditions, the cline of salt water at the bottom penetrated up to 11 km upstream from the river mouth and the fresh river water passed the estuarine zone of mixing in approximately 2 days. Salt composition of the mixed water in the estuary had conservative dependence on salinity. By dynamical signs, the estuary could be divided into two zones: i) zone of active exchange between the surface freshwater layer and the bottom salted layer on the distance 5.5 km from the river mouth to the first sandy riverbank that the fresh river water passed in 12 hours, and ii) the upper part of the estuary with limited water exchange. The complex of water environments in the estuary, as good water transparency, strong stratification, and high concentrations of terrestrial nutrients, was favorable for phytoplankton blooming, so the chlorophyll concentration in the estuarine waters exceeded 40 μg/L. Destruction of autochthonous organic matter caused anomalies in distribution of carbonate and nutrient parameters and was accompanied by hypoxia in the bottom layer with the dissolved oxygen content lowering to 61 μM/kg.
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institution Kabale University
issn 1606-9919
2658-5510
language Russian
publishDate 2018-06-01
publisher Transactions of the Pacific Research Institute of Fisheries and Oceanography
record_format Article
series Известия ТИНРО
spelling doaj-art-242321885d71434bb364fc5f3c7293ca2025-08-20T03:39:45ZrusTransactions of the Pacific Research Institute of Fisheries and OceanographyИзвестия ТИНРО1606-99192658-55102018-06-01193214315210.26428/1606-9919-2018-193-143-152377HYDROCHEMICAL STUDIES OF THE PARTIZANSKAYA RIVER ESTUARY (NAKHODKA BAY, JAPAN SEA) IN SUMMER SEASON OF LOW WATER DISCHARGEP. Yu. Semkin0P. A. Tishchenko1T. A. Mikhailik2Yu. A. Barabanshchikov3G. Yu. Pavlova4S. G. Sagalaev5P. P. Tishchenko6M. G. Shvetsova7E. M. Shkirnikova8Тихоокеанский океанологический институт им. В.И. Ильичева ДВО РАНТихоокеанский океанологический институт им. В.И. Ильичева ДВО РАНТихоокеанский океанологический институт им. В.И. Ильичева ДВО РАНТихоокеанский океанологический институт им. В.И. Ильичева ДВО РАНТихоокеанский океанологический институт им. В.И. Ильичева ДВО РАНТихоокеанский океанологический институт им. В.И. Ильичева ДВО РАНТихоокеанский океанологический институт им. В.И. Ильичева ДВО РАНТихоокеанский океанологический институт им. В.И. Ильичева ДВО РАНТихоокеанский океанологический институт им. В.И. Ильичева ДВО РАНChemical water parameters in the Partizanskaya River estuary were measured on July 18–19, 2012 in conditions of low water discharge (20.1 m3 /s). In these conditions, the cline of salt water at the bottom penetrated up to 11 km upstream from the river mouth and the fresh river water passed the estuarine zone of mixing in approximately 2 days. Salt composition of the mixed water in the estuary had conservative dependence on salinity. By dynamical signs, the estuary could be divided into two zones: i) zone of active exchange between the surface freshwater layer and the bottom salted layer on the distance 5.5 km from the river mouth to the first sandy riverbank that the fresh river water passed in 12 hours, and ii) the upper part of the estuary with limited water exchange. The complex of water environments in the estuary, as good water transparency, strong stratification, and high concentrations of terrestrial nutrients, was favorable for phytoplankton blooming, so the chlorophyll concentration in the estuarine waters exceeded 40 μg/L. Destruction of autochthonous organic matter caused anomalies in distribution of carbonate and nutrient parameters and was accompanied by hypoxia in the bottom layer with the dissolved oxygen content lowering to 61 μM/kg.https://izvestiya.tinro-center.ru/jour/article/view/386partizanskaya rivernakhodka bayestuaryhypoxianutrientprimary productiondestruction of organic matterwater dynamicswater mixingriverbed profile
spellingShingle P. Yu. Semkin
P. A. Tishchenko
T. A. Mikhailik
Yu. A. Barabanshchikov
G. Yu. Pavlova
S. G. Sagalaev
P. P. Tishchenko
M. G. Shvetsova
E. M. Shkirnikova
HYDROCHEMICAL STUDIES OF THE PARTIZANSKAYA RIVER ESTUARY (NAKHODKA BAY, JAPAN SEA) IN SUMMER SEASON OF LOW WATER DISCHARGE
Известия ТИНРО
partizanskaya river
nakhodka bay
estuary
hypoxia
nutrient
primary production
destruction of organic matter
water dynamics
water mixing
riverbed profile
title HYDROCHEMICAL STUDIES OF THE PARTIZANSKAYA RIVER ESTUARY (NAKHODKA BAY, JAPAN SEA) IN SUMMER SEASON OF LOW WATER DISCHARGE
title_full HYDROCHEMICAL STUDIES OF THE PARTIZANSKAYA RIVER ESTUARY (NAKHODKA BAY, JAPAN SEA) IN SUMMER SEASON OF LOW WATER DISCHARGE
title_fullStr HYDROCHEMICAL STUDIES OF THE PARTIZANSKAYA RIVER ESTUARY (NAKHODKA BAY, JAPAN SEA) IN SUMMER SEASON OF LOW WATER DISCHARGE
title_full_unstemmed HYDROCHEMICAL STUDIES OF THE PARTIZANSKAYA RIVER ESTUARY (NAKHODKA BAY, JAPAN SEA) IN SUMMER SEASON OF LOW WATER DISCHARGE
title_short HYDROCHEMICAL STUDIES OF THE PARTIZANSKAYA RIVER ESTUARY (NAKHODKA BAY, JAPAN SEA) IN SUMMER SEASON OF LOW WATER DISCHARGE
title_sort hydrochemical studies of the partizanskaya river estuary nakhodka bay japan sea in summer season of low water discharge
topic partizanskaya river
nakhodka bay
estuary
hypoxia
nutrient
primary production
destruction of organic matter
water dynamics
water mixing
riverbed profile
url https://izvestiya.tinro-center.ru/jour/article/view/386
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