Topic 8) Soil Organic Matter Flashcards

1
Q

Influance of Carbon

A

CEC
Water capacity
Soil Aggregates
Nutrients storehouse
Soil quality and fertility
Global carbon balance

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2
Q

Soil Carbon Storage

A

Most Carbon is stored within the soil

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3
Q

Decomposition in Organic Soils

A

1) Oxidation
Enymes oxidize carbon compounds.
2) Release
Essential elements are realsed
3) Synthesis
New Compounds created by mircobes
4) Protection

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4
Q

r-stragtegists

A

Quick popultion increase with increase of organic compounds then decrease after it has all been consmued

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5
Q

k-strategists

A

Longterm organism thats populations do not explode when increaecd amount of organic matter is added to the envirement

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6
Q

Rates of Decompostions and Mineralization

A

Enviromental Conditions in the soil and Quailiy of added residues

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7
Q

Compostion Rates of Plant residues

A

the more simple the compound the faster. The more complex the longer it will take.

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8
Q

Carbon to Nitrogen Ratio

A

1) compettion for available soil nitrogen
2) Determines rate of decay and nitrogen availability

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9
Q

SOM vs SOC

A

Labile C is accessble to plants and organism. Humus is super stable and is not acessable by plants.

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10
Q

Formation of Char.

A

Produced by smouldering and charring under low oxygen condtions. Contains alot of Carbon

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11
Q

Influcances of OM on plant growth.

A

Direct influcance (availability of nutrients)
Allelochemical effects
(plants can impact the growth of others)
Soil physical properites
(water retention, CEC capacity, food).

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12
Q

Levels of OM and SOC in natural ecosystems

A

Forests:
Increased biomass
OM oxidation is much slower
Increased Leaching
Deacreased erosion

Grasslands
Large role of plant root biomass
Decays More slowy. SOC distruted more uniformly the in forsts
Frequent fire

Wetlands
Very high productivity
Lack of Oxygen

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13
Q

Impacts of climate change on soil

A

Changing Balence between gains and losses
Active vs stable fractions of SOM

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14
Q

Solutions to Climate Change

A

Reforstatsion
Converson of cultivated land to pereniial vegation
Reducing tillage

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15
Q

Artic Carbon Stores

A

Soil in the artic contain alot of stored carbon

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16
Q

Cryoturbation

A

refers to soil movement as a result of of freez-thaw proceses

17
Q

SOM Pools

A

1) Active (1-2 years)
2) Slow (5-50 years)
3)Very slow (500-5000)

18
Q

Presravation of SOM

A

Regulation of mircobal activity by temperate and moisture