Land clearing in Australia describes the removal of native vegetation and deforestation in Australia. Land clearing involves the removal of native vegetation and habitats, including the bulldozing of native bushlands, forests, savannah, woodlands and native grasslands and the draining of natural wetlands for replacement with agriculture, urban and other land uses.
Of the vegetation which existed in Australia at the time of European settlement, approximately 87% remains.[2]
The primary motivator for land clearing in Australia is agricultural production. Where soil fertility and rainfall allow, the clearing of land allows for increased agricultural production and increase in land values. Land clearing was seen as progressive, and there was the general view that land was wasted unless it was developed.
Historically[when?], land clearing has been supported by the Commonwealth and State Governments as an essential part of improved productivity essential for national economic prosperity. A range of institutional incentives for agriculture increased the economic gain from land clearing, with offerings of cheap land along with venture capital in the form of loans or tax concessions. Other incentives included the War Service Land Settlement Scheme, low interest bank loans and financial support programs such as drought relief assistance.
The majority of cleared land in Australia has been developed for cattle, sheep and wheat production. 46.3% of Australia is used for cattle grazing on marginal semi-deserts with natural vegetation. This land is too dry and infertile for any other agricultural use (apart from some kangaroo culling). Some of this grazing land has been cleared of "woody scrub". 15% of Australia is currently in use for all other agriculture and forestry purposes on mostly cleared land. In New South Wales, much of the remaining forests and woodlands have been cleared, due to the high productivity of the land. Urban development is also the cause of some land clearing, though not a major driver. In The Australian Capital Territory for example, much urban development has occurred on previously cleared agricultural land.
Bushfires in Australia are frequently occurring events during the hotter months of the year.
Land clearing destroys plants and local ecosystems and removes the food and habitat on which other native species rely. Clearing allows weeds and invasive animals to spread, affects greenhouse gas emissions and can lead to soil degradation, such as erosion and salinity, which in turn can affect water quality.
The following table shows the native vegetation inventory assessment[2] of native vegetation by type prior to European settlement and as at 2001-2004.
As land cover is crucial to land condition, land clearing exerts significant pressure on land condition. Removal of vegetation also leaves soil bare and vulnerable to erosion. Soil stability is essential to avoid land degradation.
Soil erosion is a very significant pressure on land condition because it undermines existing vegetation and habitats and inhibits vegetation and other biota that inhabit the vegetation from re-establishing. Terrestrial vegetation is a source of nutrient replenishment for soils. If vegetation is removed, there is less biological matter available to break down and replenish the nutrients in the soil. Exposing soil to erosion leads to further nutrient depletion.
Another consequence of land clearing is dryland salinity. Dryland salinity is the movement of salt to the land surface via groundwater. In Australia there are vast amounts of salt stored beneath the land surface. Much of Australian native vegetation has adapted to low rainfall conditions, and use deep root systems to take advantage of any available water beneath the surface. These help to store salt in the earth, by keeping ground water levels low enough so that salt is not pushed to the surface. However, with land clearing, the reduced amount of water that previously got pumped up by the roots of the trees means that the water table rises towards the surface, dissolving salt in the process. Salinity reduces plant productivity and affects the health of rivers and streams.
The extinction of 108 different species (2 mammal, 9 bird and 97 plant species) has been partially attributed to land clearing.[citation needed] While land condition is one indicator of the pressure of vegetation removal, the health and resilience of the vegetation that remains is also largely dependent on the size of the fragments and their distance from each other. This is also true for species living within these habitat fragments. The smaller and more isolated the remnants, the greater the threat from external pressures as their boundaries (or edges) are more exposed to disturbances. Pressure also increases with the distance between fragments.
Land clearing is a major source of Australias greenhouse gas emissions, contributing approximately 12 percent to Australias total emissions in 1998. It has also been found that past clearing of native vegetation contributed to higher temperatures, decreased rainfall and more intense droughts.[citation needed] The removal of vegetation damages the microclimate by removing shade and reducing humidity. It also contributes to global climate change by diminishing the capacity of the vegetation to absorb carbon dioxide. Land clearing could also be responsible for reduced rainfall levels & possible desertification of land as well as soil erosion.[citation needed]
An organisation checked the impacts on climate extremes and droughts by analysing daily rainfall and surface temperature output from the Mark 3 GCM. This work, the first of its kind, demonstrated an increase in the number of dry days (<1mm rainfall) and hot days (maximum temperature >35C), a decrease in daily rainfall intensity and cumulative rainfall on rain days, and an increase in duration of droughts under modified land-cover conditions. These changes were statistically significant for all years across eastern Australia, and especially pronounced during strong El Nio events. Clearly, these studies have demonstrated that LCC has exacerbated the mean climate anomaly and climate extremes in southwest and eastern Australia, thus resulting in longer-lasting and more severe droughts.
Since the 1980s, the rate of land clearing has declined due to changing attitudes and greater awareness of the damaging effects of clearing.
Clearing is now controlled by legislation in Western Australia, South Australia, Victoria, New South Wales, and to a lesser degree in Queensland. Land clearing controls differ substantially between jurisdictions, and despite growing awareness of the effect of land degradation, controls on clearing have been generally opposed by farmers.
Land clearing is controlled indirectly by federal law in the form of the Environment Protection and Biodiversity Conservation Act 1999 (Cth), which may also apply if there are federally protected threatened species (plant or animal) or endangered ecological communities present on the land in question.
Clearing of native vegetation in NSW is regulated by the Native Vegetation Act 2003(NSW), by the protections on the habitat of threatened species contained in the Threatened Species Conservation Act 1995 (NSW) and the National Parks and Wildlife Act 1974 (NSW). It is also regulated by development control and Environmental Planning Instruments (EPIs) under land use planning law, namely the Environmental Planning and Assessment Act 1979 (NSW). Federal law in the form of the Environment Protection and Biodiversity Conservation Act 1999 (Cth) may also apply if there are federally protected threatened species (plant or animal) or endangered ecological communities present on the land in question.
Clearing of native vegetation in Queensland is principally regulated by the Vegetation Management Act 1999 and the Vegetation Management (Regrowth Clearing Moratorium) Act 2009. The Federal EPBC Act may also apply (see above).
Clearing of native vegetation in SA is principally regulated by the Native Vegetation Act 1991 (SA). The Federal EPBC Act may also apply (see above).
More:
Land clearing in Australia - Wikipedia
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