c aring f or o ur c ountry outcomes: by the end of this topic you should be able to: describe how...
TRANSCRIPT
CARING FOR OUR COUNTRYOutcomes:
By the end of this topic you should be able to:
•Describe how Australia’s land surfaces have undergone continuous weathering and erosion at rates that are very slow in comparison to worldwide averages
•Explain why soil is a resource that requires careful management
•Explain the relationship between salinity or soils and water
•Explain the effect of ecessive use of fertilisers and the long term consequences
•Describe the importance of the maintenance of environmental flows and natural processes
•Describe the results of the industrial Revolution on the atmosphere and hydrosphere
•Describe the depletion of the ozone layer
•Describe the rehabilitation and safe use odf previously contaminated sites
TOPIC OVERVIEW
There are 7 parts to this topic1. Australia’s land surfaces exhibit the effects of long
periods of weathering and erosion2. Soil as a resource that requires careful
management3. Salinity of soils and water4. The effect of excessive use and long term
consequences of using some pesticides5. Maintenance of environmental flows and natural
processes in water6. The results of the Industrial Revolution on the
atmosphere and hydrosphere7. Rehabilitation and safe use of previously
contaminated sites
INTRODUCTION The Australian
continent is very old and because of that soils are highly leached and often mineral deficient. Farmers going back as early as the first settlers have had to alter the natural environment in order to grow crops. This has caused significant damage to the environment
INTRODUCTION
Today attempts are being made to reverse some of these negative results and to prevent further damage.
INTRODUCTION
Farmers are not the only ones who have created problems for our environment. Our cities and industry also have negative effects on the environment.
INTRODUCTION
For example mining can damage and destroy environments. Towns produce huge amounts of waste that needs to be disposed of. And the burning of fossil fuels in automobiles and industry is changing the worlds climate.
INTRODUCTION
Such environmental issues are often segmented in today's news headlines. These problems are being addressed however are/should we take them seriously and are we moving fast enough?
THE DEVELOPMENT OF AUSTRALIAN SOILS
Australia has some of the oldest exposed rocks in the world. This is because the Australian continent has been tectonically stable for a long time.
Why has Australia been stable for so long?
POOR SOILS
Australia is located in the centre of the Indo-Australian plate. Because of this, it prevents most of the continent from coming into other continents which we know causes surface changing processes such as: uplift, mountain building, volcanism and earthquakes.
POOR SOILS
As a result of this stability, Australian rocks have had a very long time to weather and erode into soils leaving a very low relief terrain.
POOR SOILS
Lack of weathering and erosion results in a reduction of new sediments being transported to replenish old soils.
POOR SOILS
Leeching is another contributor. This is the process where soluble nutrients are transported from top layers to lower layers often into ground water where plants are unable to access them.
POOR SOILS
The ancient Australian soils have experienced weathering and leeching for up to 300 million years removing nutrients and producing fragile soils with low fertility.
Does Australia have areas of good soil?
GOOD SOILS
What causes good soils? In the Northern Hemisphere recent periods of glaciations has dumped large amounts of freshly ground up rocks which weather to create fertile soil.
GOOD SOILS
Most of Australia’s better soils are a result of recent volcanism. About 40 million years ago Australia passed over a hot spot which created small volcanoes along the East coast.
GOOD SOILS
These volcanoes are now extinct however as they erode, basalt and other volcanic rocks produce very fertile soils. Extinct volcanoes and their basaltic lavas can be found from Cairns to Melbourne.
COMPARISON OF AUSTRALIAN SOILS
Soil Characteristic Basalt derived soil (Eastern Australia)
Deeply Weathered Lateritic Soil (Western Australia)
Colour Black Red
Nutrients Present Nitrates, Phosphates None
Minerals Magnesiuum, zircon, iron
Iron and Aluminium
Structure Blocky Thin, sandy under hardened crust
Water Retention Good Poor
Organic Content High Little or none
Age Less than 10 million years
Up to 300 million years
REFLECTION
Long periods of leeching nutrients from the soil, low relief of the country and continental stability for hundreds of millions of years have all contributed toward the low fertility of Western Australian soils.
Recent volcanic activity (10-20mya) along the East Coast of Australia has resulted in black fertile soils.