State of the Environment

2006

Issue: Direct pressure of human activities on the land - Land clearing

This is an issue under the Land theme of the Data Reporting System.

Why we need to know about this issue

Generally, the pressures that affect the condition of the land do so by affecting the condition of the things that live in and on it, and the pressures that affect the condition of terrestrial biodiversity do so by affecting the condition of the land on which life depends for habitat and survival.

As land cover is crucial to land condition, land clearing is a very significant pressure on land condition. Removal of vegetation for various human purposes exerts pressure on the remaining vegetation and everything else that lives in it by removing its habitat.

Removal of vegetation also leaves soil bare (unstable) and vulnerable to erosion. Soil stability is essential to land health and 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 themselves.

Another way in which removal of terrestrial vegetation for various human purposes exerts pressure on other biota is by removing a source of nutrient replenishment. 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. Loss of nutrients from the land can be facilitated by the removal of original vegetation, or of the crops or animals that graze on the vegetation, and can ultimately impact back on vegetation and other life forms through a reduced capacity of the soil to sustain life.

A further way in which land clearing places pressure on the land is by interfering with hydrology, with potential impacts on water availability that may be further reaching than the actual area cleared. One of these far-reaching impacts is dryland salinity. Ground water in Australia can be very saline but deep-rooted vegetation absorbs it so that it does not rise to the surface and mix with surface water. Removal of deep-rooted vegetation reduces this absorption, allowing the saline water to rise, causing salt contamination of the surface soil. Dryland salinity exerts pressure on the land because it inhibits the recovery or re-establishment of vegetation (either natural or crops for human use).

Removing vegetation also damages the microclimate by removing shade and reducing humidity, and contributes to changes to the global climate by diminishing the capacity of the world’s vegetation to absorb carbon dioxide.

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