Making Sense of Biological Indicators – Queensland
Biological indicators give information on living organisms in soil. Biological indicators of soil quality therefore measure dynamic soil properties, i.e. properties that change over time and/or with management. It is important to monitor biological indicators as they respond more quickly to changes in management or environment than physical and chemical indicators.
For most biological indicators, there is little evidence currently available which directly links the value of the indicators to productivity or, in some cases, the risk of adverse environmental impact. However, there is good evidence from field trials carried out on a range of soils in Australia of links between biological indicators and soil processes. These have been used to create guideline ranges for the biological indicators, similar to those used for the dynamic physical and chemical indicators.
- Indicators falling in the RED zone are high risk and need to be investigated urgently.
- Indicators falling in the AMBER zone are moderate risk and should be investigated further.
- Indicators falling in the GREEN zone are low risk, regular monitoring should be continued.
Diseases and Nematodes
Indicators of soil inoculum status for soil borne disease and/or nematode abundance are used to guide practical paddock by paddock decisions about using control measures. The pathogen–host cycles are complex and affected by a range of environmental, crop and management factors (see Take-all Disease, Cereal Cyst Nematode, Root Lesion Nematode fact sheets).
Because the pathogens are highly variable across a paddock, it is very important to use an appropriate sampling strategy to gain results that are representative of the paddock. A medium or high value obtained as part of routine soil monitoring may not lead to a high risk of the disease or significant yield loss. Approaches to managing pathogens need to be specific to each paddock and farmers should seek the advice of an appropriately qualified agronomist.
Figure 1: Symptoms of RLN infection of an intolerant wheat variety include lower leaf yellowing, decreased tillers and wilting. (Photo: Kirsty Owen)
Total organic carbon
Organic matter in soil refers to all the materials that are or were associated with living organisms. Organic matter is difficult to measure directly and total organic carbon (usually expressed as % C —the percentage of carbon in the soil), which makes up over
50 % of organic matter, is measured instead. The value for total organic carbon can be converted to give tonnes of carbon per hectare using information about bulk density (see Total Organic Carbon fact sheet).
Low levels of total organic carbon can indicate that there might be problems such as unstable soil structure, low cation exchange capacity and poor nutrient turnover. Where total organic carbon in a paddock is lower than the soil’s capacity to store organic matter, it may be increased by increasing ground cover, reducing fallow, retaining stubble, increasing the proportion of pasture in the rotation or other management strategies that increase inputs of organic materials into the soil.
Total organic carbon can be separated into its components (termed fractions or pools), which differ in their chemical structure. The labile pool, which turns over relatively rapidly (weeks to years), results from the addition of fresh residues such as plant roots and living organisms. In contrast, resistant fractions, such as humus, are slower to turn over (decades to centuries) because they are physically or chemically protected. Soils in Australia also contain charcoal, which is almost inert, as a result of burning. The proportion of total organic carbon in the labile fraction can be used to identify soils with low amounts of regular residue input.
The size of the soil microbial biomass (measured as mg C per kg) is affected by climate and many soil properties (see Microbial Biomass fact sheet). Microbial biomass is the powerhouse of almost all biological processes in soil (figure 2). Generally up to 5 % of the total organic carbon can be found in the living tissues of the microbial biomass. It is generally considered that the higher the microbial biomass, the better.
Figure 2: The main soil properties affecting the microbial biomass and factors influenced by it.
The National Soil Quality Monitoring Program is being funded by the Grains Research and Development Corporation, as part of the second Soil Biology Initiative.
The participating organisations accept no liability whatsoever by reason of negligence or otherwise arising from the use or release of this information or any part of it.