Title: Decomposition
1Decomposition
2Decomposition
- Many organisms are very beneficial in ecosystems
as decomposers. - Breakdown of organic matter recycles nutrients
- Decomposition important for recycling of C and
energy, as well as all nutrient elements (N, P,
K, etc.).
3Types of Decomposition
- Abiotic processes - fire, etc.
- OM O2 ? CO2, etc.
- Biotic processes
- Aerobic respiration
- OM O2 ? CO2, etc.
- Anaerobic respiration
- OM ? CH4, etc.
- Organisms most directly responsible for
decomposition are bacteria and fungi.
4Decomposition Rates
- Decomposition rates vary (measured in litter
bags), depending on - Climate and temperature
- Soil organisms present
- Aeration of the soil
- Composition of the material (CN ratio)
- Etc. season, tillage
5Litter Bag removed from Soil
6Decomposition Rates
- Decomposition rates vary (measured in litter
bags), depending on - Climate and temperature
- Soil organisms present
- Aeration of the soil
- Composition of the material (CN ratio)
- Etc. season, tillage
Temperature affects decomposition rates (heat
units) Less Organic Matter in warm climates
7Decomposition Rates
- Decomposition rates vary (measured in litter
bags), depending on - Climate and temperature
- Soil organisms present
- Aeration of the soil
- Composition of the material (CN ratio)
- Etc. season, tillage
- Season spring fresh green material fall
tough residues - Tillage aerates soil
8CN ratio
- Slower decomposition if CN ratio is high.
- Examples of CN ratios..
9CN Ratios of Selected Materials
10Importance of CN ratio
- With residues of high CN, there is much
competition for the limited N available. - If CN ratio is high
- only some organisms can decompose (some types of
bacteria and fungi, protozoan symbionts of
termites). - they use up N quickly, so N becomes tied up and
unavailable (immobilized).
11Importance of CN Ratio
Bacteria free up N
Organic N
Inorganic N
Mineralization
Immobilization
Bacteria take scarce N for themselves !
12Adding organic N to soil
Organic N materials decompose, release nitrate
13Adding organic N to soil
Organic N materials decompose, release nitrate
Nitrate used in decomposition process by
bacteria, etc.
14Adding organic N to soilLow CN ratio material
Decomposition and release of nitrate is fast,
levels recover quickly
15Adding organic N to soilHigh CN ratio material
Nitrate release difficult, tied up for a long time
16N rob immobility of N in presence of residues
with high CN ratios
Nitrate release difficult, tied up for a long time
17Risky Mix of High and Low CN
- High CN residue
- Inorganic N fertilizer
- N from fertilizer immobilized by bacteria
18Importance of CN ratio
- As CN ratio goes lower (as it does during
decomposition), more organisms (especially fungi,
different bacteria types, even some insects) can
join in, so decomposition proceeds much faster. - Most insects and other animals join later in the
process, as the CN ratio of their food is low - e.g., fungi 101, decomposed animals 61,
nematodes 101.
19Composting
- Accelerates decomposition process
- Reduces CN ratio
- High temperatures 60-80oC (140-175oF)
- Thermophilic bacteria
- Many recipes available
20Sequence of Events in Decomposition
soil animals bacteria, fungi soil
chemistry Organic ? ? ? detritus ? ?
? humus ? ? ? mineralization material
(small particles) (litter)
- Applies to OM of plant origin
- OM of animal origin has low CN, easily
decomposed by animals, etc.
21Sequence of Events in Decomposition
- Animals speed decomposition
- break litter into small pieces.
- add products (excretion) to stimulate microbial
growth. - feeding on fungi and bacteria often increases
growth rate of these decomposers, since new
surface area is exposed to decomposition. - Predators regulate densities of animals that
consume bacteria and fungi. - Move decomposers (bacteria, fungi) to new
locations
22References
- Text, pp. 68-73.
- Brady and Weil, 1996. The Nature and Properties
of Soils. Prentice Hall, Upper Saddle River, NJ. - Odum, 1983.