Microorganisms in Soil: Effects and Examples
Soil microbiology is a vital branch of soil science that focuses on microorganisms living in soil, their functions, and their activities within the soil ecosystem. This interdisciplinary subject links closely with soil biochemistry and microbial ecology, involving principles of soil science, microbiology, and the chemistry of biological systems.
Approaches to Soil Microbiology
There are two primary approaches:
Soil as a Habitat
Soil is a heterogeneous habitat with varying environmental conditions, supporting a high number of microorganisms with diverse metabolic activities. These microorganisms play crucial roles in nutrient cycling and pollutant removal. Soil provides a variety of substrates, from simple sugars to complex materials like humus, and numerous microsites with different nutrient, moisture, pH, and redox conditions.
Microorganisms in Soil
Soil microorganisms are classified into seven categories: bacteria, fungi, viruses, blue-green algae (cyanobacteria), actinomycetes, protozoa, and nematodes. They inhabit both surface and subsurface soil, with their numbers generally decreasing with depth. The composition of the microbial community can change with environmental conditions. The rhizosphere, the soil region influenced by plant roots, harbors more microorganisms due to the compounds released by plants.
Bacteria in Soil
What are Bacteria? Bacteria are the smallest and most numerous cellular organisms in soils. They are prokaryotic and come in various shapes, with the most common being short rods. Bacteria are abundant, especially in the rhizosphere.
Examples and Functions Common soil bacteria include genera like Bacillus, Arthrobacter, Pseudomonas, and Mycobacterium. They exhibit vast metabolic diversity, contributing to nutrient cycling and soil structure improvement. Bacteria participate in biogeochemical cycles and help degrade complex organic substances.
Positive Effects
Negative Effects
Fungi in Soil
What are Fungi? Soil fungi are eukaryotic organisms, either unicellular or multicellular with complex life cycles. Most fungi are aerobic, except for yeasts that can ferment sugars anaerobically.
Examples and Functions Soil fungi include groups like Ascomycetes, Basidiomycetes, and Imperfect fungi. They decompose organic matter, form symbiotic relationships with plants (mycorrhizae), and can be pathogens.
Positive Effects
Negative Effects
Establishing the ideal symbiotic relationship between crop roots and soil relies on a diverse population of bacteria and fungi. Each unique microbial functional group is responsible for specific tasks that trigger a chain reaction, resulting in enzymatic exchange, metabolite production, and efficient nutrient uptake. This process culminates in the crop’s ability to achieve its maximum genetic potential.
This is accomplished through principles familiar to many: balancing nutrients within soils through fertilization and amending. The same method applies to biological inputs. Consistent, balanced doses yield the greatest benefits. Excessive doses of any one input, whether a macronutrient or single microbe, can disrupt overall plant health. Utilizing full-spectrum biology is an invaluable tool for managing living soil systems.
This approach underpins the microbial populations found in Buffalo Mountain's Life To Soil Microbial Activator.
These populations are carefully selected to achieve a balanced exchange between plants and soil, with multiple species from each functional group present in agriculturally potent populations. This inoculant is equally effective at initiating biological activity in newly built soil mixes and maintaining ongoing populations in well-established soils.
Consistent follow-up doses are recommended to encourage optimal nutrient cycling.
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