| Soil Organic Matter | |
|---|---|
| SOM | |
| Organic soil component | |
| Profile | Surface horizon, humus layer |
| Key minerals | Carbon-rich compounds, lignin, cellulose |
| Key process | Decomposition, humification |
| Parent material | Plant and animal detritus, microbial biomass |
| Climate | Variable, higher in cooler and wetter regions |
| pH | Typically 5.5 – 7.0 |
| O (organic), A (topsoil) | |
| Primary | Carbon (C), Nitrogen (N), Phosphorus (P), micronutrients |
| Secondary | Minerals, microbial by-products |
Soil organic matter (SOM) is the organic matter component of soil, consisting of plant and animal detritus at various stages of decomposition, cells and tissues of soil microbes, and substances that soil microbes synthesize. SOM provides numerous benefits to soil's physical and chemical properties and its capacity to provide regulatory ecosystem services.[1] SOM is especially critical for soil functions and quality.[2]
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. SOM increases soil fertility by providing cation exchange sites and being a reserve of plant nutrients, especially nitrogen (N), phosphorus (P), and sulfur (S), along with micronutrients, which the mineralization of SOM slowly releases. As such, the amount of SOM and soil fertility are significantly correlated.[3]
SOM also acts as a major sink and source of soil carbon (C). Although the C content of SOM varies considerably,[4][5] SOM is ordinarily estimated to contain 58% C, and "soil organic carbon" (SOC) is often used as a synonym for SOM, with measured SOC content often serving as a proxy for SOM. Soil represents one of the largest C sinks on Earth and is significant in the global carbon cycle and, therefore, for climate change mitigation.[6] Therefore, SOM/SOC dynamics and the capacity of soils to provide the ecosystem service of carbon sequestration through SOM management have received considerable attention.[7]
The concentration of SOM in soils generally ranges from 1% to 6% of the total mass of topsoil for most upland soils. Soils whose upper horizons consist of less than 1% of organic matter are mainly limited to deserts, while the SOM content of soils in low-lying, wet areas can be as great as 90%. Soils containing 12% to 18% SOC are generally classified as organic soils.[8]
SOM can be divided into three genera: the living biomass of microbes, fresh and partially decomposed detritus, and humus. Surface plant litter, i.e., fresh vegetal residue, is generally excluded from SOM.[9]