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

HATCH

https://doi.org/10.1007/978-94-007-0277-6reasing winds cause erosion of the thermocline such that full mixing of the water column down to the permanent halocline is finally restored. The below-halocline water of the deep basins in the central Baltic Sea may be subjected to stagnation for many years. Water renewal by lateral inputs of high-

MAL

Monolithic

https://doi.org/10.1007/978-94-007-0277-6 of nitrogen fixation already during spring. A period of regenerated production that did not contribute to NCP followed the termination of the spring bloom. Mid-summer NCP fueled by nitrogen-fixing cyanobacteria was detected as discrete pulses and coincided with sudden increases in temperature. Dist

政府

https://doi.org/10.1007/978-94-007-0277-6ed the major inflow of oxygen-rich water in 2003, the release of phosphate was disproportionately high in relation to the OM mineralization. This was attributed to the anoxic dissolution of the iron-III-oxy-hydroxy-phosphates that had formed during deep-water oxygenation. After this initial phase, p

Charitable

plasma-cells

sleep-spindles

Progress Made by Investigations of the CO2 System and Open Questions, radiation. Since these processes are connected with the consumption or production of CO., CO. mass balance calculations based on measured changes in total CO., were successfully used to estimate net production and mineralization rates in the Baltic? Sea.

Congeal

overreach

極小