Author:
Bolger T. P.,Turner N. C.
Abstract
There is a perception in the farming and research communities that annual
pastures have low produc- tivity and water use, and contribute
disproportionately to problems of rising watertables and dryland salinity. Our
aim was to determine potential pasture production in relation to water use and
the influence of management factors on this relationship. Experiments were
initiated at 4 locations along a gradient of 300–1100 mm annual rainfall
across the Western Australian agricultural zone. At each site a high input
treatment was compared with a low input control. There was a strong linear
relationship between water use and pasture production up to 440 mm of growing-
season water use. After 30 mm of water use the potential pasture production
was 30 kg/ha.mm. An upper limit to pasture production may be reached at
about 12 000 kg/ha in this environment due to rainfall distribution
patterns and soil water holding capacity in the root-zone. Although pasture
production was increased by as much as 3500 kg/ha, water use was generally
similar or only slightly more for high input compared with control plots. The
marginally higher water use by the high input pastures resulted in an extra 18
mm of water extracted from the subsoil at one location by the end of the third
season. A drier subsoil may provide a buffer for storing excess rainfall and
reduce deep drainage. Estimated drainage was small at low rainfall sites so
even marginal increases in water use by highly productive annual pastures
could play a significant role in reducing water loss to deep drainage and
mitigating water-table rise and secondary salinisation in low rainfall
regions. Management practices aimed at promoting early growth and adequate
leaf area should maximise water use, water use efficiency, and yield. The
linear relationship defining potential pasture production provides a useful
benchmark to farmers.
Subject
General Agricultural and Biological Sciences
Cited by
37 articles.
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