Arid Zone Surface Runoff - a Neglected but Significant Resource
Ian Cordery
Abstract
Ian Cordery
Abstract
The Australian arid zone has quite large resources of surface water. For example in western New South Wales an average of 7 runoff events are observed each year and in these the median depth of runoff is about 0.4mm, or 400m3/km2, providing at least 2.8 ML/km2/yr of surface water. The key to utilisation of this water is to catch it where it is, when it occurs. Simple earthworks, constructed with a blade mounted on a tractor, can be used to direct water from natural small channels to a point of concentration where it can be protected from evaporation and seepage losses, say in an excavated hole or 'tank'. Even with 90% loss of the stored water a constant supply of at least 700 litres/km2/day would be available, enough to provide an adequate supply for the average Australian household.
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The Australian arid zone has quite large resources of surface water. For example in western New South Wales an average of 7 runoff events are observed each year and in these the median depth of runoff is about 0.4mm, or 400m3/km2, providing at least 2.8 ML/km2/yr of surface water. The key to utilisation of this water is to catch it where it is, when it occurs. Simple earthworks, constructed with a blade mounted on a tractor, can be used to direct water from natural small channels to a point of concentration where it can be protected from evaporation and seepage losses, say in an excavated hole or 'tank'. Even with 90% loss of the stored water a constant supply of at least 700 litres/km2/day would be available, enough to provide an adequate supply for the average Australian household.
Key concepts: Surface runoff, Arid, Hydrology (agriculture), Environmental science, Surface water, Earthworks, Water resources, Water resource management