This topic has 16 questions:
Organic matter is anything that contains carbon compounds that were formed by living organisms. It covers a wide range of things like lawn clippings, leaves, stems, branches, moss, algae, lichens any parts of animals, manure, droppings, sewage sludge, sawdust, insects, earthworms and microbes.
There are 3 main components of organic matter in soils:
By far the largest component is the dead matter - it constitutes about 85% of all organic matter in soils. Living roots make up about another 10% and the microbes and soil animals make up the last few percent.
Organic matter in soil
Soil sand - no organic matter
In answering this question, we concentrate mainly on dead plant matter as this constitutes the major part of organic matter in soil (apart from living roots). However, the broad principles also apply to the degradation of animal and microbial matter.
Living organisms are made up of thousands of different compounds, so when they die there are thousands of compounds in the soil to be decomposed. As these compounds are decomposed, the organic matter in soil is transformed and gradually changes so that eventually it is no longer recognisable as part of the original plant. These stages are:
Compounds in the first group are quick and easy for fungi and bacteria to decompose, so the carbon and energy they provide is readily available. Most of the microbes living in the soil have the enzymes needed to decompose these simple compounds. This type of decomposition is the first stage during the degradation of organic matter. Mites and small soil animals often help this stage by breaking up the organic matter into smaller pieces exposing more of the material to colonisation by bacteria and fungi.
The second stage involves the microbes decomposing more complicated compounds - the second group listed above. Many, but not all, fungi and bacteria can decompose these compounds. The compounds take longer to decompose because they are much larger and they are made up of more complicated units than the compounds in the first group. Specific enzymes, not commonly produced by most microorganisms are required to break down these compounds.
Hyphae asociated with organic matter
(photo van Vliet and Gupta).
It's important to realise that decomposition will only take place if conditions are suitable. The rate of breakdown is greatly affected by the conditions in soil. There must be some moisture available, soil temperatures must be suitable (usually between 10 and 35°C) and the soil must not be too acidic or alkaline. Decomposition also occurs at higher temperatures, as in composts, or under waterlogged conditions. The types of organisms involved in breaking down the organic matter will depend on the conditions.
Incorporating organic matter into soil can have several impacts because it disturbs the physical, chemical and biological balances in the soil. It can:
All of these changes are related to the way organic matter is decomposed when it is incorporated into soil and to the particular type of organic matter used.
When organic matter is incorporated into soil, the larger organisms like mites and soil animals break it into smaller pieces. Then the fungi and bacteria start to decompose it (they secrete enzymes to break up the chemical compounds it is made of). When the enzymes break the molecules into smaller sections, the bacteria and fungi can use some of energy or nutrients released for their own growth. For example, when an enzyme stimulates the breakdown of a protein, the microbe may be able to use the carbon, nitrogen and sulphur (if there is some) for its own physiological processes.
If there are nutrients that the microbes do not use, they will be available for other soil organisms or plants to take up and use. When microbes die, their cells are degraded and nutrients contained within them become available to plants and other soil organisms.
Microbes can access nitrogen in the soil more easily than plants can, so the plants sometimes miss out. This means that if there is not enough nitrogen for all the organisms, the plants will probably be nitrogen deficient. This is why incorporating organic matter into soils can change the amount of nitrogen (and other nutrients) that is available to plants. These will be a short-term effect that happens when soils do not have high levels of organic matter and soil microbes.
If the number of fungi and bacteria associated with the breakdown of organic matter increases, there may be some improvements to the soil structure. Adding organic matter can also increase the activity of earthworms, which in turn can also improve soil aggregation. If organic matter is retained in the soil, the number of microbes in the soil increases. This is because the microbes can use the organic matter as a source of energy and so they can grow and multiply.
Humus is composed of organic compounds that are highly complex in structure. Like other organic matter, humus originates from dead organic material. The compounds that make up humus are highly complex organic compounds that have resisted decomposition and have accumulated in the soil. Humus organic matter is so altered that it can no longer be recognised as plant material.
The amount of organic matter in the soil is an important factor controlling the potential sustainability of a system. Soil organic matter plays a key role in supplying plants with the nutrients they require (especially nitrogen, sulphur and phosphorus). Organic matter also helps to improve soil structure, binds pollutants, and influences soil buffering capacity.
To maintain or improve organic matter levels we need inputs of new organic matter (from plant debris and/or animals) to exceed losses of organic matter by decomposition or erosion. Farming systems have traditionally ‘mined’ the soil for nutrients, causing soil organic matter levels to decline. This decline continues until management practices are improved.
When soil is lost by erosion organic matter, microorganisms and nutrients are also lost. Most animal waste and plant material (except deep roots) are returned to the soil at or near its surface. Soil organic matter therefore accumulates at the soil surface. The organic matter is food for microorganisms so they also concentrate in the surface few centimetres of soil. The loss of even a thin layer of soil during wind or water erosion results in a disproportionately large reduction in organic matter and microorganisms. This problem is increased in soils in the south west of Western Australia because they usually have poor soil structure and minimal plant cover during summer. Decreasing soil disturbance, creating wind breaks, maintaining crop cover or increasing clay content are all practices that can help to minimise soil loss.
Large losses of soil organic matter can be attributed to cultivation. Organic matter that is inside aggregates or coated with soil particles is protected by decomposition because microorganisms are unable to come into physical contact with it. Tillage disturbs the soil and brings "protected" organic matter in to physical contact with microorganisms, which then decompose it. No-till systems can overcome this problem. No-till systems also decrease soil erosion. Organic matter and microorganisms are restricted to the top layers of the soil. This increases the potential for losing organic matter if management practices cause soil loss.
Light fraction organic matter is the recently added and partially decomposed organic matter. It is called "light" fraction organic matter because it floats on the surface of water. This distinguishes it from organic matter that has been in soil longer, which is denser and sinks in water.
A simple method to extract light fraction organic matter.
Compost is the semi-stabilised product obtained after organic materials have undergone biological degradation under controlled conditions. Basically, compost is organic matter. Compost can be made from any organic material such as garden waste, food scraps, manure, sewage effluent, sawmill waste, leaves and cardboard. Composts vary greatly depending on their maturity, the organic materials used to make the compost, the type of composting (aerobic/anaerobic) and length of the composting.
The composting process relies on a variety on organisms that feed on the organic matter. Therefore factors that influence these organisms can affect the final compost product. By understanding the biology of composting, it is possible to manipulate processes, maximise the rate of decomposition and meet quality standards for final product.
Many of the organisms involved in composting need aerobic conditions. How aerobic the conditions are is influenced by factors such as such as moisture, temperature, frequency of turning and the size of the pile. Also the quality of the organic matter at the start of the composting process also affects the organisms, especialy the pH and carbon to nitrogen ratio of the organic materials.
During aerobic composting the material undergoes several phases each involving a separate set of organisms. The two main phases are:
A mature compost is one in which the rate of decomposition has decreased. The maturity of a compost is important because applying immature compost to soil can lead to the immobilisation of nitrogen in the soil. This process could make nitrogen less available to plants. Most compost producers should be able to advise you on the maturity and qualities of their products. One way you can test the maturity of a compost yourself is by giving it suitable conditions to continue decomposing and observing whether is heats up. If it does not heat up, it is likely to be mature.
In general, composts can have many benefits for soil fertility including modifying pH, absorbing pollutants and excess nutrients, controlling erosion, buffering temperature, suppressing weeds and providing a source of essential nutrients (major and micronutrients).
Composts can be applied to soil in two main ways and composts for each use have different properties and benefits for soil fertility.
In viticultural regions, the harvest waste (or grape marc) poses a significant management problem for growers. It is because of this that many growers have been informally composting grape marc and applying it under-vine as an organic mulch.
A field trial near Busselton in Western Australia measured changes in soil biological fertility following the application of grape marc on the ground under vines. The grape marc was applied at 60 tonnes/ha and at 120 tonnes/ha. The quantity of microorganisms in the soil (microbial biomass) were assessed at a later time.
The study found that 8 weeks after application of grape marc, the quantity of soil organisms (microbial biomass) had almost doubled and at 16 weeks it was three times greater. Both quantities of grape marc had the same effect. The soil microbial biomass plays a significant role in organic matter turnover and nutrient cycling. Therefore, increases in microbial biomass may lead to improved nutrient cycling and increased soil biological fertility.