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Soil microbiology

Study of microorganisms in soil

  • 16 min read
  • 11 chapters

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Through Microorganism, Soil and Photosynthesis

Up to 10 billion culturable bacterial cells inhabit each gram of soil in and around plant roots, a region known as the rhizosphere, which is a hotspot of microbial diversity, and in particular the rhizoplane. In 2011, a team detected more than 33,000 bacterial and archaeal species on sugar beet roots.

The composition of the rhizobiome can change rapidly in response to changes in the biotic and abiotic environment. The diversity of microorganisms in soils is dependant on pH, soil texture, organic matter content, plant community composition, and contaminants such as heavy metals.

Bacteria

Bacteria and archaea (initially classified as bacteria), the smallest organisms in soil apart from viruses, are prokaryotic. They are the most abundant microorganisms in the soil, and serve many important purposes, including nitrogen fixation and organic matter decomposition for bacteria. Soil archaea are still poorly known but they could play a significant role in nitrification and methanogenesis.

Some bacteria can colonize minerals in the soil and help influence weathering and the breaking down of these minerals. The overall composition of the soil can determine the amount and distribution of bacteria growing in it. The more clay minerals that are found in an area can result in a higher abundance of bacteria living as biofilms at their surface. Soil bacteria also contribute to the formation of soil aggregates, which increases the overall health of the soil.

Apart from the rhizosphere, where bacterial activity is stimulated by rhizodeposition and root exudation, most bacteria of the bulk soil are in a quiescent state, in the form of bacterial colonies embedded in a polysaccharidic matrix covered with clay platelets, and resistant to drought. These bacterial microaggregates may remain in this state of quiescence for a long time, until being reached by exudates from growing root tips or the mucus of burrowing earthworms. Accordingly, sugar-rich lixiviates (e.g. after a pollen rain) may also stimulate respiration, reproduction and dissemination of resting soil bacteria, exerting a priming effect on soil microbial activity.

In the mycorhizosphere mycorrhiza helper bacteria form symbiotic associations with mycorrhizal fungi, assisting mycorrhiza formation or enhancing their functions.

Biochemical processes

One of the most distinguished features of bacteria is their biochemical versatility. A bacterial genus called Pseudomonas can metabolize a wide range of chemicals and fertilizers. In contrast, another genus known as Nitrobacter can only derive its energy by oxidizing nitrite to nitrate. The genus Clostridium is an example of bacterial versatility because it, unlike most species, can grow in the absence of oxygen, respiring anaerobically. Several species of Pseudomonas, such as Pseudomonas aeruginosa are able to respire both aerobically and anaerobically, using nitrate as the terminal electron acceptor.

Archaea are particularly adapted to chemically and physically harsh environments, with their unique membrane lipids, and their methanogenic pathways which incorporate a number of coenzymes unique to this microbial group.

Nitrogen fixation

Nitrogen is often the most limiting nutrient in soil and water. Bacteria are responsible for the process of nitrogen fixation, which is the conversion of atmospheric dinitrogen into nitrogen-containing compounds (such as ammonia) that can be used by plants. Some nitrogen-fixing bacteria (e.g. cyanobacteria) are autotroph and derive their carbon from the atmosphere through photosynthesis while others are heterotroph and derive their carbon either from soil organic matter (e.g. Clostridium) of from a symbiotic host (e.g. Rhizobium). Some soil chemotroph bacteria derive their energy through the oxidation of nitrite ions, which they transform in nitrate ions, like Nitrobacter. These bacteria are not nitrogen-fixing microorganisms but contribute to nitrification, an important step in the nitrogen cycle.

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