dt=dw+dn. If nitrification exceeds the total denitrification rate, nitrate is released
into the water column at rate wNO: equation(8) wNO={nx−dt,nx≥dt0,nx
bd (mg l−1)−1 2.61 Oxygen slope for potential denitrification Cd mg l−1 0.44 Oxygen Parvulin offset for potential denitrification ax dimensionless 5.15 Oxygen slope for nitrification bx mg l− 1 1.10 Oxygen offset for nitrification k mol m−3 8.62 Nitrate diffusion resistance PS mmol m− 2 285 Organic phosphorus concentration in bottom sediments rCP mol mol− 1 106 Carbon – phosphorus ratio in sediment organic matter amP mmol m−2 day−1 0.00036 Organic phosphorus mineralisation rate constant bmP °C−1 0.0102 Temperature constant for organic phosphorus mineralisation qbP dimensionless 0.459 Maximum fraction of generated PO4 adsorbed abP dimensionless
7.031 Oxygen slope for PO4 adsorption bbP mg l− 1 1.87 Oxygen offset for PO4 adsorption Full-size table Table options View in workspace Download as CSV “
“The aim of our studies is to derive regional algorithms for calculating chlorophyll and suspended matter concentrations in surface waters of the Gulf of Finland from satellite ocean colour scanner data. The Gulf of Finland is strongly influenced by river runoff, primarily from the Neva (2/3 of the total runoff), and this influence is evident not only in the low salinity (< 10 PSU) but also in their optical properties of these waters. The standard algorithms for calculating bio-optical characteristics from satellite ocean colour scanners, designed mainly on the basis of data measured in ocean waters (http://oceancolor.gsfc.nasa.