Distribution of Microorganisms in Soil
The number of microbes in soil reaches incredible values—up to 10 billion cells per gram. However, their vertical profile distribution is extremely uneven. At the very surface of the soil, the number of microorganisms is relatively small. This is due to the damaging impact of aggressive environmental factors, primarily direct ultraviolet rays and constant drying.
The maximum concentration of microbial biomass is observed in the surface layer down to a depth of 10 centimeters. With further depth, the population of bacteria and fungi begins to drop sharply. The lower boundary of habitation is located at a depth of 3–4 meters, where microorganisms are almost completely absent.
The qualitative and quantitative composition of the flora depends on many factors: the type and current condition of the soil, the nature of the vegetation cover, and key abiotic indicators. Optimal conditions for the vast majority of soil inhabitants are a neutral pH level, high relative humidity, and a temperature range from 25 to 45 °C.
Physiological Groups of Soil Bacteria
Depending on their biochemical functions, bacteria are divided into several main groups that ensure the cycling of substances in nature.
- Nitrogen-fixing bacteria. Their main task is to assimilate molecular nitrogen directly from the atmosphere. Typical representatives include microorganisms of the genera Azotobacter, Azomonas, and Mycobacterium. Cyanobacteria (blue-green algae) also belong here and are actively used in modern agricultural technology to increase land fertility, for example, in flooded rice paddies.
- Ammonifying (putrefactive) bacteria. This group of microorganisms is responsible for the mineralization of complex organic substances. Among them are spore-forming forms, such as non-pathogenic soil bacilli (Bacillus megaterium, Bacillus subtilis), and non-spore-forming species, various representatives of pseudomonads and microbes of the genus Proteus.
Pathogenic Bacteria and Sanitary-Epidemiological Significance
From the standpoint of medicine and epidemiology, soil is considered a potential source of infectious diseases. All pathogenic flora can be divided into two large categories.
- Resident flora (spore-forming pathogens). This group includes true soil inhabitants, such as the causative agents of anthrax (Bacillus anthracis) and bacteria of the genus Clostridium (causative agents of botulism, tetanus, and gas gangrene). Due to their ability to form highly resistant spores, they can maintain viability in adverse conditions for decades. Moreover, some of them, particularly Clostridium botulinum, can actively multiply directly in the soil.
- Transitory flora (enteric bacteria). Representatives of the family Enterobacteriaceae (such as Escherichia coli, Shigella, Salmonella) enter the soil transiently along with human or animal feces. In the soil, they generally do not multiply due to the lack of a suitable nutrient medium and gradually die off.
Normally, enteric bacteria are extremely rare in clean soil. This is why the detection of coliform bacteria (the Escherichia coli group) serves as a reliable indicator of fecal contamination. This fact is a critical sanitary indicator criterion that directly points to the sanitary distress of an area and the high risk of transmitting intestinal infections.
Soil Fungi and Protozoa
In addition to bacterial flora, the microbiocenosis includes numerous eukaryotic organisms that play an equally important role.
- Soil fungi. They perform a key ecological role in soil formation and the complex transformation of nitrogen compounds. Fungi possess high biochemical activity: they can synthesize various antibiotics and toxins. The medical significance of these microorganisms is that toxin-producing species can get onto agricultural food products, causing severe diseases in humans—mycotoxicoses.
- Protozoa. These microorganisms are also an integral part of the ecosystem. Their numbers vary widely and can range from 500 to 500,000 individuals per 1 gram of soil. Protozoa feed on organic residues and bacteria, thereby actively influencing changes in the composition of organic matter in the soil.
Lichens, which represent a unique symbiotic association of fungi and cyanobacteria, also frequently inhabit the soil.