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Australia Yearbook - 2001

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602 Year Book <strong>Australia</strong> <strong>2001</strong><br />

The <strong>Australia</strong>n landscape has undergone<br />

significant change since European settlement. For<br />

example, in 1788 forests covered around 252<br />

million hectares, but by 1997 this had diminished<br />

to around 156 million hectares, a 38% reduction<br />

in 209 years. The growth of agriculture, which has<br />

been a feature of the growth and prosperity of<br />

the <strong>Australia</strong>n nation, has been a key reason for<br />

tree clearing. By 1980 Victoria, New South Wales<br />

and South <strong>Australia</strong> had cleared half of their<br />

native forests (table 14.33). Clearing has occurred<br />

in all State and Territories since 1980, with<br />

Queensland clearing the greatest area between<br />

1980 and 1997 (Glanzig 1995; Barson 1999).<br />

However, the percentage of forests cleared in<br />

Queensland (39%) is lower than in all other States<br />

and Territories except the Northern Territory<br />

(effectively zero) and Western <strong>Australia</strong> (25%).<br />

The clearing of native vegetation, whether for<br />

agriculture or forestry, has been a significant<br />

environmental issue for more than a decade,<br />

because the loss of trees can lead to declines in<br />

the abundance of wildlife and increased levels of<br />

land degradation.<br />

14.33 ESTIMATED CHANGE IN FOREST<br />

COVER(a)—1788 to 1980<br />

1788 1980 1997<br />

Difference<br />

1788–1997<br />

State/<br />

Territory mill. ha. mill. ha. mill. ha.<br />

%<br />

ACT 236 124 120 –0.49<br />

NSW 54 710 22 910 20 787 –0.62<br />

NT 27 565 27 474 35 385 +0.28<br />

Qld 80 609 55 963 49 056 –0.39<br />

SA 18 417 9 058 5 499 –0.70<br />

Tas. 5 604 3 871 2 904 0.48<br />

Vic. 18 513 7 538 7 285 –0.61<br />

WA 46 346 32 934 34 800 –0.25<br />

Aust. 252 000 159 872 155 835 –0.38<br />

(a) The total area of native forest differs from other<br />

estimates given in Year Book <strong>Australia</strong> <strong>2001</strong> due to<br />

differences in the definition of forest and improved data<br />

sources.<br />

Source: <strong>Australia</strong>’s State of the Forest Report, 1998.<br />

Land degradation<br />

Salinity<br />

Land degradation is a significant concern of<br />

<strong>Australia</strong>n farmers, governments and the general<br />

public. In 1999 around 20% of farms experienced<br />

some form of land degradation, 16% reported<br />

productivity declines and 10% removed land from<br />

agricultural production (Kemp and Alexander<br />

2000). Estimates of the cost of land degradation<br />

vary. One estimate put the cost at 6% of the value<br />

of agricultural production or $1.5b per annum<br />

(Gretton and Salma 1996). Another study<br />

estimated the cost of three types of land<br />

degradation—salinity, acidity and sodicity—to be<br />

$2.4b per annum (CRCSLM 1999). The variation<br />

in the estimates reflects the difficulties and<br />

different approaches used in valuing the damage,<br />

which includes the cost of lost production as well<br />

as the damage to public and private<br />

infrastructure. For example, saline (salty) water<br />

can cause damage to water pipes, hot water<br />

systems, rainwater tanks, roads, municipal water<br />

treatment plants, dams, and sewers (Wilson<br />

2000). Estimates of the cost of salinity to <strong>Australia</strong><br />

are in the range $250–330m per annum (MDMC<br />

1999; CRCSLM 1999).<br />

Salinity is related to the loss of trees as well as the<br />

increasing use of irrigation for crops and<br />

pastures. This gives rise to two types of salinity:<br />

irrigation salinity and dryland salinity. Both types<br />

occur when water tables rise, bringing salts<br />

normally stored well below ground to near the<br />

soil surface. In the case of irrigation salinity, water<br />

is applied in greater amounts than is used by<br />

crops. The excess water feeds into the water table<br />

and may cause it to rise. Dryland salinity occurs<br />

outside of irrigated areas. It can occur naturally,<br />

but is also caused when trees and other deep<br />

rooted native vegetation are removed and<br />

replaced with annual shallow rooted agricultural<br />

crops. The shallow rooted crops do not use as<br />

much rainwater as native vegetation and hence<br />

more water reaches the water table, causing it to<br />

creep nearer to the soil surface.<br />

Around 2.5 million hectares of land are currently<br />

affected by salinity, which could in time rise to<br />

over 15 million hectares (PMSEIC 1999). At<br />

present around three-quarters of the salt affected<br />

land is in Western <strong>Australia</strong>, but the State with the<br />

greatest potential problem is New South Wales<br />

with 7.5 million hectares at risk (table 14.34). The<br />

National Land and Water Resources Audit has<br />

produced a map of ground water flows which can<br />

be used to assess the risk of areas becoming<br />

saline (see http://www.nlwr.gov.au).<br />

Salinity can be prevented and reversed in many<br />

cases. Appropriate measures depend on local<br />

circumstances, but could include reducing the<br />

amount of water used in irrigation, growing<br />

alternative, more deeply rooted crops, planting<br />

salt tolerant trees (Bell 1999), pumping water and<br />

building drains or other engineered works.

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