Titlebook: Biogeochemistry of the Atmosphere, Ice and Water of the White Sea; The White Sea Enviro Alexander P. Lisitsyn,Viacheslav V. Gordeev Book 20

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Conclusions,new approaches and methods and to create the system of the investigations of the seas and the oceans of the new generation on the example of this sea. In Vol. 1 of the book, the processes in the water column of the sea are presented and discussed. Special attention was paid to dispersed form of subs

Genteel

1867-979X ons. Together with the companion volume?.Sedimentation Processes in the White Sea: The White Sea Environment Part II.,?it offers an essential source of information for postgraduate students, researchers 978-3-030-05150-1Series ISSN 1867-979X Series E-ISSN 1616-864X

發(fā)微光

Introduction,phere, anthroposphere, and vulcanosphere) in a four-dimensional regime (three coordinates in space, plus time)..We attempted to apply these approaches during our 15-year studies of the White Sea (2001–2016). In volume 1 of the present book we present the most significant results of these investigati

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The Geochemical Features of the River Discharge to the White Sea,nd in the whole sea in the frameworks of the program “The White Sea System.” Results of these expeditions allowed to obtain absolutely new materials for investigations of biogeochemical processes in the rivers and in the sea..These unique data, in particular about the concentrations of organic carbo

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虛弱

BADGE

Organic Matter of the White Sea,depend on both the penetration of the transformed Barents Sea waters and the intensity of biological processes. The oxidation processes are intensive in Kandalaksha Bay, while the minimum rates of oxidation characterize the waters of Dvina and Onega Bays. The maximum rates of the organophosphorus mi

Flavouring

Trace Elements in Water and Suspended Matter in the Open Part of the White Sea,ypical for the open ocean are absent in the shallow White Sea with active hydrological regime..The concentration of SPM in sea water is in average near 1?mg/L. Among the major elements, especially organic carbon (14.1%) and P (0.28%) are very high. The important interannual variations in river disch

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