Chapter 21 - Decompositions and Nutrient Cycling Flashcards
Detritus
dead organic matter
Where is detritus found in soil profile
on surface of soil
Macroscopic decomposers
earthworms, nematodes, insect larvae
Microscopic decomposers
bacteria, fungi, actinomycetes (thread-like bacteria)
Abiotic factors that influence decomposition
- Soil temperature
- Soil moisture
- Soil pH
- Litter quality
Mineralization
release of inorganic compounds from decomposing matter (Nitrogen and phosphorus)
Immobilization
is the reverse process of mineralization, wherein nutrients are converted from the inorganic to organic forms
Low molecular weight carbon compounds
easy to degrade
Nutrients – Inputs and Recycling: Wetfall
input via precipitation
Nutrients – Inputs and Recycling: Dryfall
input from aerosols
affects of nutrient poor sites
- Nutrient-poor sites encourage below ground productivity
- Nutrient-poor sites produce plants with low quality tissue for herbivory (quantitative inhibitors)
- Nutrient-poor sites produce low quality litter
Nutrient spiraling in streams
- Measured as the distance needed to complete one cycle — the longer the distance required, the more open the spiral
- Nutrients are carried downstream via the organic matter
Why are Estuaries very productive
- Shallow water with ample sunlight – a lot of primary producers
- Nutrients are available
- Ocean tides bring in oxygenated water
- Comparison (East vs. West Coast