SOIL BIOLOGY

  soil biology

outline 

1.  Soil is alive!

1. In most ecosystems, more life and diversity lives underground than above.
2. Energy flows from the sun, through plants, and through many trophic levels of soil organisms.
3. Soil organisms can be divided into six groups: bacteria, fungi, protozoa, nematodes, arthropods, and earthworms. Each group of organisms plays important roles. Even within each group, there is great diversity in form and function.
4. The rhizosphere is the interface between plant roots and the soil environment. It is the location of much soil biological activity and plant-microbe interactions including symbioses, pathogenic infection, and competition.
5. Soil organisms are part of a living system.  Ecosystem characteristics largely determine the structure of soil communities. Weather determines daily and seasonal variations in biological activity.

1. The types of species present and their level of activity depends on micro-environmental conditions including temperature, moisture, aeration, pH, pore size, and types of food sources.
2. Arid systems have few earthworms, but have termites, ants and other invertebrates that serve similar functions.
3. Grasslands have near equal amounts of fungal and bacterial biomass, or may be dominated by bacteria. Coniferous forests may have 100 to 1000 times more fungal biomass than bacterial biomass.

2. We need soil organisms for the services they provide. They play critical roles in plant health and water dynamics.

1. Soil organisms are an integral part of the cycling of nutrients through the environment. They drive:

1. Decomposition,
2. Mineralization  (E.g., protozoa and nematodes excrete excess nitrogen into the soil when they eat nitrogen-rich bacteria and fungi.)
3. Storage and release of nutrients,
4. Degradation of pollutants before they reached groundwater or surface water,
5. Carbon cycling, carbon sequestration, and soil organic matter transformations,
6. Nitrogen cycling (N fixation, denitrification, nitrification).

2. Soil biological activity substantially affects soil structure including the size of soil pores, the stability of soil aggregates, and the existence of macropores. Soil structure impacts how water flows over, into, and through soil and how much water is held within reach of plant roots.

1. Large, burrowing invertebrates (e.g., earthworms, ants, termites, beetles) create macropores that allow rapid flow of water into or through soil.
2. Even tiny arthropods produce fecal pellets that are mixtures of soil and organic matter. These became stable soil aggregates.
3. Fungi and bacteria produce substances that help bind soil particles together and stabilize soil aggregates.
4. Soil organic matter can be physically protected from degradation within stable soil aggregates.

3. Plant pest dynamics depend on the whole mix of organisms in the soil. Some organisms prey on or compete with disease-causing organisms. Some bacteria release plant growth factors that directly increase plant growth.
4. In arid lands, biological soil crusts seem to be important for all the purposes listed above. They help fix nitrogen, stabilize the soil surface, affect water flow, and prevent the establishment of some exotic plant species.
5. Mycorrhizal fungi help plants acquire nutrients from the soil and they help stabilize soil aggregates.
6. Resilience is the ability of a soil to recover its functions after a disturbance such as fire, compaction, tillage, etc. The mix of organisms in the soil partially determine a soil’s resilience.

3. Management affects soil organisms

1. We know that land management practices change the soil community. The link between specific changes and soil function is less clear.
2. Soil biological crusts are very sensitive to trampling.
3. Reducing tillage tends to result in increased growth of fungi, including mycorrhizal fungi.
4. Soil compaction, lack of vegetation, or lack of plant litter covering the soil surface tends to reduce the number of soil arthropods.

posted by:
crozland 23