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MRF was calculated by cMRI using either (1) (LV stroke volume − systolic aortic outflow volume by phase contrast)/LV stroke volume (cMRI MRF [volumetric]) or (2) (mitral inflow volume − systolic aortic outflow volume)/mitral inflow volume (cMRI MRF [phase contrast]).
In 2005, the annual inflow volume in the catchment was 6783 m3 and the water retention rate was 80.1%.
We vary the inflow volume, inflow location, discharge rate, water-loss rate (water-rich models only), and simulation time and examine the resulting maximum flow depths and velocities.
Additional analyses then investigated the sensitivity of the results to methodological choices, focussing on annual inflow volume for eight indicator basins and system power.
We studied long-term monotonic trend in inflow volume to 20 reservoirs, plus a measure of system-wide hydroelectric power potentially available for generation, in British Columbia, Canada.
All fluid was collected from the passive outflow tubing of the hysteroscope as well as from the vacuum tubing connected to the inner blade, and both measured volumes were subtracted from the measured inflow volume resulting in the fluid deficit.
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Arterial diameters, peak systolic inflow volumes (PSIVs), mean inflow volumes (MIVs), and a velocity index (VI), representing the peripheral resistance, were obtained at rest.
The data included variable and challenging biofilter operational conditions; e.g. variable inflow volumes, dry and wet period dynamics, and inflow pollutant concentrations.
Performance assessment of a lined biofilter demonstrated that retention of inflow volumes by the filter media, for subsequent loss via evapotranspiration, reduced runoff volumes by 33% on average.
The results show that high NDVI response occurs following flooding in the floodplain and wetlands and was significantly correlated to 40 day inflow volumes.
Retention of water was found to be most influenced by inflow volumes, although only small to medium storms could be assessed.
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