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  2. Soil organic matter - Wikipedia

    en.wikipedia.org/wiki/Soil_organic_matter

    The benefits of SOM result from several complex, interactive, edaphic factors; a non-exhaustive list of these benefits to soil function includes improvement of soil structure, aggregation, water retention, soil biodiversity, absorption and retention of pollutants, buffering capacity, and the cycling and storage of plant nutrients.

  3. Agricultural microbiology - Wikipedia

    en.wikipedia.org/wiki/Agricultural_microbiology

    By dominating the soil's microbial environment, effective microorganisms encourage other beneficial microbes to thrive and outcompete smaller groups of pathogenic or opportunistic microbes. This natural balancing act leads to stronger, more resilient plants and higher crop yields, positioning effective microorganisms as a key player in the ...

  4. Soil - Wikipedia

    en.wikipedia.org/wiki/Soil

    Soil, also commonly referred to as earth, is a mixture of organic matter, minerals, gases, liquids, and organisms that together support the life of plants and soil organisms. Some scientific definitions distinguish dirt from soil by restricting the former term specifically to displaced soil. Soil measuring and surveying device

  5. Carbon-to-nitrogen ratio - Wikipedia

    en.wikipedia.org/wiki/Carbon-to-nitrogen_ratio

    In microbial communities like soil, the C:N ratio is a key indicator as it describes a balance between energetic foods (represented by carbon) and material to build protein with (represented by nitrogen). An optimal C:N ratio of around 24:1 provides for higher microbial activity. [16] [17]

  6. Soil biology - Wikipedia

    en.wikipedia.org/wiki/Soil_biology

    Soil biology is the study of microbial and faunal activity and ecology in soil. Soil life , soil biota , soil fauna , or edaphon is a collective term that encompasses all organisms that spend a significant portion of their life cycle within a soil profile, or at the soil- litter interface.

  7. Chemostat - Wikipedia

    en.wikipedia.org/wiki/Chemostat

    One of the most important features of chemostats is that microorganisms can be grown in a physiological steady state under constant environmental conditions. In this steady state, growth occurs at a constant specific growth rate and all culture parameters remain constant (culture volume, dissolved oxygen concentration, nutrient and product concentrations, pH, cell density, etc.).

  8. Fungal extracellular enzyme activity - Wikipedia

    en.wikipedia.org/wiki/Fungal_extracellular...

    Soil fertility and plant production: Use of enzyme activity as indicator of soil quality [71] [72] Composting. Impacts of composting municipal solid waste on soil microbial activity [10] Soil organic matter stability: Impact of temperature and soil respiration on enzymatic activity and its effect on soil fertility [73] Climate change indicators

  9. Dissolved organic carbon - Wikipedia

    en.wikipedia.org/wiki/Dissolved_organic_carbon

    In the soil, DOM availability depends on its interactions with mineral components (e.g., clays, Fe and Al oxides) modulated by adsorption and desorption processes. [43] It also depends on SOM fractions (e.g., stabilized organic molecules and microbial biomass) by mineralization and immobilization processes.