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The continuity equation explains the change in storage to be the difference between mass flowing in and out across the boundaries for a given increment of time (Δt).
Using a load cell and capillary, we measured the change of mass flowing through capillary tube with respect to the time, m(t), from which viscosity and shear rate were mathematically calculated.
During this time, the amount of vapor flowing out of the condenser is computed to be around 96% of the H2O mass flowing into the condenser, yielding very low (negative) condensate pH values at elevated temperatures, in qualitative agreement with the preliminary analyses discussed earlier.
For the inner binary, we assume a fraction (beta_{1rightarrow2}) of the wind mass lost from (m_{1}) at a rate (dot{m}_{1}) can be accreted by (m_{2}), and (beta_{2rightarrow1}) for the mass flowing in the other direction.
Structure-induced hyporheic zone denitrification did not exceed 3.1% of mass flowing in from the upstream channel, was achieved only during favorable background groundwater hydraulic conditions (i.e. summer baseflow), and was transport-limited such that non-trivial removal rates were achieved only when the streambed hydraulic conductivity (K) was at least 10−4 m/s.
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"Mass flow correction factor," from Jones (1997).
Therefore, layers only exchange signal flows and not mass flows across layer boundaries.
Mass flows occur within layers and do not cross layer boundaries.
The grinding is done when the mass flows easily.
Amazingly, temperature and salinity are enough to track individual water masses flowing around the world's oceans.
Mass, mass flow rate.
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