Lecture 6: Aeration and nutrient cycling Flashcards

1
Q

Healthy soil aeration

A

solids with bound water with large pores

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2
Q

poor draining clays

A

decreasing aeration with soil depth and season

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3
Q

aggregate size

A

large causes anaerobic soil centre

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4
Q

nitrogen cycle

A

sedimentary OM provides organic N
mineral weathering provides NH4 and NO3
organic N neutralised to NH4
nitrification NH4 to NO2
denitrification NO3 to N2O or N2
fixation

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5
Q

nitrification (NH4+ to NO2-)

A

NH4+ to NO2-
aerobic
archaea
nitrosomes
nitrosococcus

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6
Q

nitrification (NO2- to NO3-)

A

nitrobacter and nitrospira
release CO2 for C for growth

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7
Q

denitrification (NO3- to N2O and N2)

A

pracoccus denitrificans and pseudomonas
need anaerobic and root exudates
anoxic needed

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8
Q

podzolisation

A

soil forming processes where dissolved OM moved with water deeper into soil

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9
Q

podzol

A

under-ashed soil

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10
Q

podzol horizons

A

organic surface layer (O)
topsoil (A)
eluviated horizon (E) - no OM
illuviated horizon (B) - redposition of OM
parent material (R)

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11
Q

surface soil layer pod

A

acidic as decomposers inhibited

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12
Q

iron pans

A

low pH at top and higher at bottom
rust forms

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13
Q

nutrient cycling

A

biomass store
inorganic store
organic store
nutrient entering
nutrient escaping

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14
Q

absorption

A

inorganic to biomass nutrients

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15
Q

mineralisation

A

organic to inorganic

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16
Q

immmobilisation

A

organic to biomass

17
Q

nitrogen cycle fixation

A

legumes, lightning, bacteria (rhizobia)

18
Q

rhizobia

A

fix N in return for C

19
Q

legumes

A

signal to rhizobia via alkaloids
positive chemotaxis
Nod-factors induced to form nodules

20
Q

root nodule formation

A

nod factor detected
flaccid to curled
open up tip
infection thread
colonise
differentiation of cells
vascular system produced
gas tight so no oxygen

21
Q

leghaemoglobin

A

anaerobic conditions around rhizobia
buffers oxygen for optimal N fixation

22
Q

phosphorous cycle

A

weathering of bedrock
unavailble organic converted to inorganic via mineralisation

23
Q

phosphate forms

A

dissolved most available
labile phosphomonomers require hydrolysis but low energy needed
phosphodiesters harder to break
inositol phosphate hard to break down

24
Q

what is undisputed about P crisis

A

high grade rock depleted
harder to access
lower P conc.
impurities
waste
extraction
prices
environmental cost

25
Q

disputed P crisis

A

size of reserves
longeivity of supply
future demand

26
Q

dealing with P crisis

A

engineer sustainable organic phytate fertilisers