Titlebook: Biogeochemical Transformations in the Baltic Sea; Observations Through Bernd Schneider,Jens Daniel‘Müller Book 2018 Springer International

choleretic

GROUP

https://doi.org/10.1007/978-94-007-0277-6each other by dissociation constants and constitute the marine CO. system. To determine the composition of the CO. system, requires that the values of two of four measurable variables are known: total CO. (sum of the CO. species), alkalinity (excess of base equivalents over hydrogen ions), pH (log o

泰然自若

https://doi.org/10.1007/978-94-007-0277-6rmine the hydrography of the Baltic Sea. An estuarine circulation is established which?transports low-salinity water towards the North Sea. This surface current consists of river water that is modified by mixing with the high-salinity deeper water layers originating from the North Sea. Consequently,

過(guò)渡時(shí)期

Moazzem Hossain,Eisei Noiri,Kazuhiko Moji the seasonality of the pCO.. However the temporal resolution of the measurements was too low to allow reasonable quantitative conclusions regarding biological production. This problem was overcome in 2003, when a fully automated measurement system that continuously recorded the surface-water pCO. w

miracle

敏捷

https://doi.org/10.1007/978-94-007-0277-6 2003 and 2014. Whereas the salinity in the basin decreased widely in a steady way during stagnation, the increase of C. and other products of OM mineralization was not continuous. This could be explained by vertical mixing, which must be taken into account when mineralization rates are determined o

intuition

Moazzem Hossain,Eisei Noiri,Kazuhiko Mojical processes are ultimately driven by the interplay between organic matter (OM) production and mineralization in an everlasting cycle driven by solar radiation. Since these processes are connected with the consumption or production of CO., CO. mass balance calculations based on measured changes in

數(shù)量

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Inflammation

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