Lecture 6: Aeration and nutrient cycling Flashcards
Healthy soil aeration
solids with bound water with large pores
poor draining clays
decreasing aeration with soil depth and season
aggregate size
large causes anaerobic soil centre
nitrogen cycle
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
nitrification (NH4+ to NO2-)
NH4+ to NO2-
aerobic
archaea
nitrosomes
nitrosococcus
nitrification (NO2- to NO3-)
nitrobacter and nitrospira
release CO2 for C for growth
denitrification (NO3- to N2O and N2)
pracoccus denitrificans and pseudomonas
need anaerobic and root exudates
anoxic needed
podzolisation
soil forming processes where dissolved OM moved with water deeper into soil
podzol
under-ashed soil
podzol horizons
organic surface layer (O)
topsoil (A)
eluviated horizon (E) - no OM
illuviated horizon (B) - redposition of OM
parent material (R)
surface soil layer pod
acidic as decomposers inhibited
iron pans
low pH at top and higher at bottom
rust forms
nutrient cycling
biomass store
inorganic store
organic store
nutrient entering
nutrient escaping
absorption
inorganic to biomass nutrients
mineralisation
organic to inorganic