Soils Lecture 3- Marc Flashcards

1
Q

in soil types, which stores the most Carbon?

A

permafrost
Soils contain estimated 1500-2400 PgC (P = peta = 1015)
Permafrost contains an additional ~1700 PgC
All vegetation 450-650 PgC
Oil reserves 173-264 PgC
Atmosphere contains ~730 PgC

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2
Q

What services are provided by our soil?

A

Soils are nature’s recycling system, returning biomass and nutrients to forms that can be used by the next “generation” of life.
diversity, biomass, microorganisms. indirectly supports all life

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3
Q

name some of the organisms which live in soil

A

nematodes
microbes
fungal hyphae
fungi
mites
springtails

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4
Q

what is humus?

A

Humus is carbon that has resisted degradation

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5
Q

characteristics of humus?

A

VERY slowly decomposed
Plant and microbial origin
Provides soil with its dark colour, especially in the A horizon

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6
Q

what is the A horizon, when considering humus and soil

A

A horizon is the most biologically active layer, with higher organic matter and nutrients

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7
Q

What is the exchange mechanism responsible for nutrient retention

A

Cation exchange

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8
Q

what are Colloids?

A

Colloids are the smallest particles: of clay (mineral) or humus (organic) chemically active
Mainly negatively charged

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9
Q

what would make a good soil?

A

one with High CEC = high nutrient
retention and good soil
fertility
Caiton Exchange Capacity

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10
Q

which element is a Cation which can affect soil pH?

A

H+

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11
Q

list things that will affect soil fertility

A

Nutrient abundance and balance (macro and micronutrients)
Bioavailable phosphorus often limiting
Type of clay; proportion of various sized particles (sand, silt)
pH (acidity, alkalinity)
Toxic elements
Salinity
Microbes

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12
Q

how is soil fertility defined?

A

the ability to sustain plants

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13
Q

define the following:
GEP:

ER:

NEP:

A

Gross ecosystem productivity (photosynthesis)
R: Ecosystem respiration
NEP: Net ecosystem productivity

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14
Q

define GEP

A

Gross ecosystem productivity (photosynthesis)

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15
Q

Define ER

A

ER: Ecosystem respiration

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16
Q

define NEP

A

NEP: Net ecosystem productivity

17
Q

how are some of the ways forest soils fix carbon?

A

uptake and storage through photosynthesis and primary production minus decomposition/respiration
CO2 efflux through autotrophic respiration (leaf, shoot, and roots)
CO2 efflux through heterotrophic respiration (primarily from litter and SOM decomposition)

18
Q

how do forest soils lock in Methane and N2O

A

CH4 uptake by methane-oxidizing soil bacteria

N2O efflux through microbial nitrification and denitrification processes

19
Q

how do forest soils lock in Methane and N2O

A

CH4 uptake by methane-oxidizing soil bacteria

N2O efflux through microbial nitrification and denitrification processes

20
Q

how much carbon do peatlands hold globally

A

1/3

21
Q

how much carbon do peatlands hold globally

A

1/3

22
Q

what can a High water-table cause?

A

(when precipitation is ample) leads to anoxia, slow decomposition, but greater CH4 emissions

23
Q

why does Sphagnum peat decomposes slowly in bogs?

A

It is flooded, which makes it anoxic/anaerobic
It is acidic
It is nutrient poor

24
Q

what is peat subsidence?

A

irreversible lowering of the surface (subsidence) as a consequence of peat shrinkage and biological oxidation, with the latter resulting in a loss of carbon stock

25
Q

what is peat subsidence?

A

irreversible lowering of the surface (subsidence) as a consequence of peat shrinkage and biological oxidation, with the latter resulting in a loss of carbon stock

26
Q

how does pasture grazers affect soil degredation and erosion?

A

compaction due to hoof traffic often associated with over-grazing

27
Q

how does tillage and heavy equipment affect soil degredation and erosion?

A

Tillage and very heavy equipment (sugarcane production): soil structure is further degraded

28
Q

how does tillage and heavy equipment affect soil degredation and erosion?

A

Tillage and very heavy equipment (sugarcane production): soil structure is further degraded

29
Q

when native grasses are removed, what can happen to the soil? i.e. America 1930s

A

Ploughing and also livestock disturb the soil structure
Soils became highly susceptible to wind erosion

30
Q

how much does 1mm of soil from 1 hectare weigh?

A

4.5tons

31
Q

What are the 4 characteristics of chemical degradation

A

Depletion of organic matter and nutrients (from vegetation loss)
Contamination with chemical pollutants
Salinization – in dry areas (particularly with irrigation)
Desertification – only occurs in arid, semi-arid and dry sub-humid areas

32
Q

what causes salinzation?

A

Poor water management
Too much water evaporates from surface
Salts left behind
Toxic to plants

33
Q

what a consequence of soil acidification?

A

acid rain

34
Q

how does acid rain cause damage?

A
  1. displaces nutrients from cation exchange sites –> leached away –> no longer available for plant growth
  2. toxic aluminium is soluble in water at low pH (non-mobile and safe at neutral and high/ basic pH) injures plants and soil microorganisms
35
Q

other than acidifaction from acid rain, how else may this be caused?

A

excessive ammonium fertilisation via nitrification by soil microbes:
(NH4+ –>–> NO3- + H+)

36
Q

what does acid rain cause?

A

causes flooding of cation exchange sites on soil colloids with protons (H+)

37
Q

what is the Yield Plateaus

A

where production is maximised, but cannot grow. this is a threat to growing population.

38
Q

T/F Soil degradation is an additional threat to food security

A

True