2002Water Challenge: Balancing the Risks: Hydrology and Water Resources Symposium 2002Requires access

Arid Zone Surface Runoff - a Neglected but Significant Resource

Ian Cordery

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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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What this paper is about

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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Available 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.

Key concepts: Surface runoff, Arid, Hydrology (agriculture), Environmental science, Surface water, Earthworks, Water resources, Water resource management

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