Investigating Soil MARCH 2014 Riverina Environmental Education Centre Table of Contents 1. 2. 3. 4. 5. 6. 7. Important Stuff What is soil? Describing soil Soil Erosion Soils and Farming Soil Bugs Investigating: soil erosion Riverina Environmental Education Centre 1. Important Information Soil contains broken down rock, dead animals and plants, live animals and plants, air and water. They are all important for healthy soil. Plants obtain most of their nutrients from soil. We depend on many plants for food such as wheat for bread so we depend on the soil for our food. Soil can lose its ability to help grow healthy plants (soil degradation) if we do not care for it. Rocks break down very slowly to help form soil. Soil is lost through erosion. Many Australian soils are very shallow so we can't afford to lose it through erosion. 2. What is soil? Layers Soil is made of: Topsoil has many nutrients and plant roots Broken down rock (minerals) Dead animals and plants Living animals and plants Water Subsoil has clay and holds more moisture Air Weathered rock Rock Rock Riverina Environmental Education Centre 3. Describing soil Horizons Soil usually changes from the surface down to the bottom. Different layers, called horizons, can be seen in the diagram (top soil and sub-soil). Each horizon can be described using the following features. Colour Topsoil: darker colours (browns/blacks) indicate more humus is present (broken down plant matter). Sub-soil: red, orange and grey indicate whether the soil is in a dry or moist area. Iron in the clay changes colour depending on whether it is dry (red) or moist (yellow to grey). Slaking Indicates the stability of soil in water and whether it is an erosion hazard. To test take a dry, pea size sample of soil, place it in a dish of water and observe it for one minute. If the aggregate falls apart it slakes, if it stays together it does not slake and is stable in water. The sample must be dry or the test will not work. Texture This is the size of mineral particles in the soil, sand, silt and clay. Take a hand full of soil, crush it, remove any rocks and slowly add water while needing it in your hand until it is just sticky. Form a ball and then squeeze the soil between your thumb and finger to produce a ribbon of soil. Keep pushing the soil out with the thumb until the ribbon breaks. The length of ribbon indicates the soil texture. Riverina Environmental Education Centre 4. Soil Erosion Erosion is the removal of soil by water and wind. Moving water can pick up soil particles and wash them away. Rain drops landing on bare soil are like small bombs and blast the soil apart. Water flowing over bare soil can pick up soil particles and wash them away causing gullies to form. Photo: erosion gully near Lake Albert, Wagga Wagga. Wind can pick up soil and blow it away. In really bad dust storms, some of our soil has landed in New Zealand. Photo: dust storm near Wagga Wagga- John Rodham Riverina Environmental Education Centre 5. Soil Degradation Soil degradation occurs when soils get "sick" because of poor management by people. The result can be soil erosion, low fertility or very acid soils. This can occur because: ploughing the land breaks up the natural soil clumps; soil animals such as earth worms are killed by chemical sprays; too much fertiliser and some plants make the soil acid; and hard hoofed animals compact the soil reducing the number of holes for air and water to circulate. pH Indicates weather the soil is acid or alkaline. If the soil is too acid, some nutrients cannot be taken up by the plants and they will not be healthy. Soil acidity test, called a pH test. Take half a teaspoon of crushed soil. Add 3 drops of universal indicator which changes colour depending on soil acidity. Sprinkle with barium sulphate, a white, neutral powder which absorbs the indicator and shows the colour better. Wait 2 minutes for the colour to develop and compare with the colour card. Numbers below 7 are acidic. If the acidity is in the yellow range or lower the soil may be too acidic for healthy plants. Riverina Environmental Education Centre 6. Soils and farming Breaking up the natural chunks of soil (structure) by ploughing destroys the natural cracks and holes through which air and water pass. It also destroys the habitat of many important soil organisms such as earth worms. Compare the two photos showing old and new farming methods. In the top photo the soil is being prepared for sowing the crop. In the bottom photo the seeds are being sown directly into the stubble of the previous crop. What is happening to the soil and soil organisms in each photo? Left photo courtesy Dept. Infrastructure, Planning & Natural Resources. Photo at right courtesy John Deere. Riverina Environmental Education Centre 7. Soil bugs (Soil fauna) Animals living in the soil have very important jobs: they burrow through the soil creating holes for air and water to enter; they eat leaf litter and dead animals returning the nutrients back into the soil. Larger soil animals Flat cockroaches live in leaf litter in colonies with a few friends and communicate using scent. An important farm worker helping to keep the soil healthy. Numbers are declining with the use of poison sprays and chemical fertilisers. Millipedes hate light and hide under leaf litter or burrow into the soil. They are almost blind. They eat plant material. Smaller soil animals seen under the microscope These little soil animals can be seen under the microscope, especially in compost. They are less than one millimetre long. Photos: CSIRO Riverina Environmental Education Centre