om_decomposition
Table of Contents
Select a slide or start at the
beginning
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X. Organic Matter Decomposition
A. Carbon Nutrition
1. Heterotrophic soil organisms
1. Heterotrophic Reactions
b) Anaerobic Respiration -
c) Fermentation -
Other examples -
2. Autotrophic soil organisms
2. Autotrophic Reactions -
B. Assimilation
Add 100 g of sugar (50% C) to medium - 50 gm
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2. Ecological significance of assimilation efficiency
C. Mineralization/Immobilization
D. Decomposition of Soil Organic Matter
1. Steady State System -
What factors limit microbial activity under “steady state” soil conditions?
a. Soil O.M. levels (pools) in a steady state system
2) O.M./ carbon losses -
b) Carbon losses by leaching
c) Carbon/O.M. losses from fire
b. Management activities:
Example - If soil is affected by timber harvesting,
2. Decomposition of Added Organic Matter
a. % Nitrogen
Examples -
Above 1.5 % N
Immobilized N will eventually become available to plants
b. C:N Ratio
e.g. 100g of grass has 50 gm of C
As O.M. is decomposed,
Example:
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When these fungal cells die
At C:N of 10:1
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c. Immobilization of soil N
Practical significance -
d. Effect of C substrate
e. Microbial Populations
The type and composition of O.M. greatly affects the composition of soil microflora:
E. Humus Formation
Once humus formed and incorporated into mineral soil,
F. Methods of Measurement
1. “Steady state” conditions
Problems with this method?
b. CO2 Evolution
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Sources of CO2
Methods of CO2 measurement
d) CO2 absorption -
2. Added Organic Matter
Size of mesh bag
Problems with method?
2) Brian Titus popsicle sticks
b. Substrate Change
c. Changes in OM physical properties
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Take pictures of cloth in lab
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Example from a wetland soil
2) Wood stake strength
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4. Microbial Populations
4. Microbial Biomass
b. Chloroform fumigation
Soluble carbon can measured in several ways: