Deepperc Hist
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Runoff History
Runoff consists of stormflow plus baseflow from a specific catchment, where stormflow is generated from rain falling on the soil/vegetation surface. The stormflow amount depends on the amount of rain on a given day, how much is intercepted by the…
Soil Water Content at Saturation
Marked spatial differences in agricultural productivity occur within a region because of different soil properties. The vertical sequence of soil properties regulates water entry into, storage and retention in, and redistribution within and out of the soil profile. The following…
Moth Life Cycle
Lower and upper temperature (°C) thresholds and accumulated heat units (degree days) for one life cycle of codling moth are, respectively, 11.1°C, 34.4°C and 603°days. Life cycles per annum of codling moth were determined by computing degree days with a…
Soil Thickness
Marked spatial differences in agricultural productivity occur within a region because of different soil properties. The vertical sequence of soil properties regulates water entry into, storage and retention in, and redistribution within and out of the soil profile. The following…
Plant Available Water
Marked spatial differences in agricultural productivity occur within a region because of different soil properties. The vertical sequence of soil properties regulates water entry into, storage and retention in, and redistribution within and out of the soil profile. The following…
Mean Annual Precipitation
The mean annual precipitation (MAP, in mm) characterises the long-term quantity of water available to a region for hydrological and agricultural purposes, and is one of the most used statistics in crop production. Note that while simple to calculate and…
Irrig Hist
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Streamflow History
The term ‘accumulated streamflow’ is defined as the runoff (i.e. stormflow plus baseflow) from a specific catchment plus the runoff from all catchment areas upstream of the specific Quinary catchment in question. From these, the accumulated streamflows were derived and…