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Published online by Cambridge University Press: 05 November 2011
Introduction
Rainfall is the dominant factor controlling the growth of plants in arid lands throughout the world (Beatley, 1969; Ross, 1969, 1976; Noy-Meir, 1973; Ross & Lendon, 1973; Gutterman, 1981; Orr, 1981). Much of the variability of pasture biomass can be explained by rainfall (Noy-Meir, 1973; Chapter 4). Temperature also plays a role in the initiation and success of germination and the survival of seedlings (Beatley, 1967; Gates & Muirhead, 1967; Lendon & Ross, 1978). Hence, rain falling at different seasons in the arid zone stimulates the germination of different suites of plant species.
This chapter reports the effect of rainfall and temperature on changes in soil moisture, pasture biomass, pasture growth and species composition on the two major soil types of Kinchega National Park.
The study posed the following questions:
(1) What is the relationship between rainfall and soil moisture and how does it differ between the two major soil types within the Park?
(2) Can trends in soil moisture or a knowledge of rainfall and temperature be used to predict changes in pasture growth and biomass?
The study was conducted within two exclosures, one on each of the two major soil types within Kinchega National Park. A fence excluded mammalian herbivores. Hence, growth, dieback and trends in biomass are measured in the absence of grazing. There is considerable evidence that grazing affects the growth rate of plants, sometimes stimulating growth and sometimes depressing growth or killing the plant (Harper, 1977; McNaughton, 1979).
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