1301.0 - Year Book Australia, 2012
ARCHIVED ISSUE Released at 11:30 AM (CANBERRA TIME) 24/05/2012
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Statistics contained in the Year Book are the most recent available at the time of preparation. In many cases, the ABS website and the websites of other organisations provide access to more recent data. Each Year Book table or graph and the bibliography at the end of each chapter provides hyperlinks to the most up to date data release where available.
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AGRICULTURAL ENVIRONMENT
Australia's average elevation is the lowest of any continent, with a mean elevation of only 330 metres. The dominant topographical feature of the continent is the Great Dividing Range, which spans the length of the eastern seaboard and has a profound influence on regional weather patterns and land use.
Australia's agricultural landscapes support a wide range of soils. Most are ancient, strongly weathered and infertile by world standards, with deficiencies in phosphorus and nitrogen. Those on flood plains are younger and more fertile. Very few are considered good quality soils for agriculture. To offset nutrient deficiencies, superphosphate and nitrogenous fertilisers are widely used, particularly on pasture and cereal crops. Fragile soil structure and a susceptibility to waterlogging are other common features of Australian soils, while large areas are naturally affected by salt or acidity. These soil characteristics restrict particular agricultural activities, sometimes ruling out agricultural activity altogether.
With the exception of Antarctica, Australia is the world's driest continent. More than a third of the continent is effectively desert, and over two-thirds of the continent is classified as arid or semi-arid. The wet summer conditions of northern Australia are suited to beef cattle grazing in inland areas and the growing of sugar and tropical fruits in coastal areas. The drier summer conditions of southern Australia favour wheat and other dryland cereal farming, sheep grazing, beef cattle and dairy cattle (in the higher rainfall areas). There is also a high degree of annual rainfall variability within regions and this is most pronounced in arid and semi-arid regions.
Rainfall variability is very high by global standards and often results in lengthy periods without rain. The variability and seasonality of rainfall in Australia requires that water be stored. Under normal seasonal conditions, the ability of primary producers to store water ensures that there are adequate supplies for those agricultural activities requiring a continuous supply. The development of large scale irrigation schemes has opened up areas of inland Australia to agricultural activities that otherwise would not have been possible.
Evaporation is another important element of Australia's environment, affecting agricultural production, with hot dry summers causing high rates of evaporation in many parts of the country.
Since European settlement, the vegetation of Australia has altered significantly. In particular, large areas of Australia's forest and woodland vegetation systems have been cleared, predominantly for agricultural activity. The areas that have been altered most are those that have been opened up to cultivation or intensive grazing. Some semi-arid regions previously cleared of timber and scrub to allow grazing of native grasses, now show signs of returning to their previous condition. In recent years, various state and territory legislation has seen restrictions applied to the area of old growth and regrowth forest and woodland that can be cleared without a permit.
LAND USE
In spite of Australia's generally harsh environment, agriculture is the most extensive form of land use. During 2009–10, the estimated total area of businesses with agricultural activity was 399 million hectares, representing 52% of the total land area – 6.5% of which had been cropped (table 16.7).
(b) Total area of agricultural businesses with an estimated value of agricultural operations (EVAO) of $5,000 or more.
(c) Total area of Australia includes Jervis Bay.
Source: Agricultural Commodities, Australia (7121.0).
Queensland had 130 million hectares devoted to agricultural activity, while Western Australia had 94 million hectares (graph 16.8). Land area not used for agriculture consisted of unoccupied land (mainly desert in western and central Australia), Aboriginal land reserves (mainly located in the Northern Territory and Western Australia), forests, mining leases, national parks and urban areas.
IRRIGATION
High variability in annual rainfall and river flow is a feature of the Australian environment and this means that successful ongoing production of many crops and pastures is dependent on irrigation. In 2009–10, 30% (40,816) of all agricultural businesses reported irrigation activity and in total 6,600 gigalitres of irrigation water was applied – an average application rate of 3.6 megalitres per irrigated hectare.
Rice, cotton, grapes, vegetables and nurseries/cut flowers/cultivated turf are the most intensively irrigated crops, with 100%, 100%, 95%, 86%, and 78% respectively of their total growing areas being irrigated in 2009–10. However, the total area of land irrigated, about 1.8 million hectares in 2009–10, represents less than 1% of the total land used for agriculture (table 16.9).
Most irrigated land is located within the confines of the Murray-Darling Basin, which covers parts of New South Wales, Victoria, Queensland and South Australia, and all of the Australian Capital Territory.
AREA IRRIGATED (ha)
VOLUME APPLIED (ML)
^ estimate has a relative standard error of 10% to less than 25% and should be used with caution
* estimate has a relative standard error of 25% to 50% and should be used with caution
** estimate has a relative standard error greater than 50% and is considered too unreliable for general use
– nil or rounded to zero (including null cells)
(a) Includes Australian Capital Territory.
Source: Water Use on Australian Farms (4618.0).