Pavel Semkin

Dr. Pavel Semkin

orcid

Research Focus & Metrics

Academic Career Length

13Years (2014-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 October 2018 in Estuarine, Coastal and Shelf Science
Verified
Journal Article
Closed access
VSVladimir Shulkin
Vladimir Shulkin
PTPavel Tishchenko
Pavel Tishchenko
PSPavel Semkin
Pavel Semkin
MSMaria Shvetsova
Maria Shvetsova

1 March 2018 in Oceanology
Verified
Journal Article
Closed access
PDF file
PTPavel Tishchenko
Pavel Tishchenko
PSPavel Semkin
Pavel Semkin
GPG. Yu. Pavlova
G. Yu. Pavlova
PTP. P. Tishchenko
P. P. Tishchenko
VLV. B. Lobanov
V. B. Lobanov
ESE. M. Shkirnikova
E. M. Shkirnikova
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...

1 April 2016 in Continental Shelf Research
Verified
Journal Article
Closed access
PTPavel Tishchenko
Pavel Tishchenko
PTPavel Tishchenko
Pavel Tishchenko
VLVyacheslav Lobanov
Vyacheslav Lobanov
ASAlexander Sergeev
Alexander Sergeev
PSPavel Semkin
Pavel Semkin
VZVladimir Zvalinsky
Vladimir Zvalinsky

1 July 2020 in Estuarine, Coastal and Shelf Science
Verified
Journal Article
Closed access
PTPavel Ya. Tishchenko
Pavel Ya. Tishchenko
PTPetr P. Tishchenko
Petr P. Tishchenko
VLVyacheslav B. Lobanov
Vyacheslav B. Lobanov
TMTatyana A. Mikhaylik
Tatyana A. Mikhaylik
ASAleksander F. Sergeev
Aleksander F. Sergeev
MSMaria G. Shvetsova
Maria G. Shvetsova

1 March 2016 in Doklady Earth Sciences
Verified
Journal Article
Closed access
PSP. A. Stunzhas
P. A. Stunzhas
PTP. Ya. Tishchenko
P. Ya. Tishchenko
VIV. V. Ivin
V. V. Ivin
YBYu. A. Barabanshchikov
Yu. A. Barabanshchikov
TVT. I. Volkova
T. I. Volkova
FGF. M. Golovchenko
F. M. Golovchenko

1 October 2017 in Doklady Earth Sciences
Verified
Journal Article
Open access
PDF file
PTP. Ya. Tishchenko
P. Ya. Tishchenko
PSPavel Semkin
Pavel Semkin
PTPavel Tishchenko
Pavel Tishchenko
VZV. I. Zvalinsky
V. I. Zvalinsky
YBYu. A. Barabanshchikov
Yu. A. Barabanshchikov
VSV. M. Shulkin
V. M. Shulkin
The hypoxia of the bottom waters in the Razdolnaya River estuary was observed for the first time in September 2014 during the survey. It is formed as in the seaward part: oxygen is absorbed as a result of destruction of excessive phytoplankton biomass that settles to the bottom and is synthesized on the upper horizon. The high value of primary production in the riverine part of the estuary was caused by the pycnocline formed. Thus, phytoplankton “blooms” above and undergoes destruction beneath the pycnocline. Oxygen is distributed symmetrically in both parts of the estuary with respect to a bar: similar oxygen concentrations, which are maximum on the surface and minimum at the bottom, 300 and <60 μm/L, respectively, are recorded. The anomalies of hydrochemical parameters that have been formed during this process are sharply different in the two parts of the estuary, which most vividly manifests itself in the N/P value and the partial pressure of carbon dioxide pCO2. The causes of this unique situation are discussed.