Soils Flashcards
organic soils
decomposition of organic matter from bogs and marshes
higher (60%) of organic matter
soil formation
needs 1000s of years to reach a mature soil profile
microbial activity, and other physical processes contribute
-Acids dissolve out rock material
-Water wind etc, erode
-Biological processes
-Microbes can live, using sun, are autotrophic, use rock minerals, produce organic matter and allow for more microbial activity
O horizon
in the open air
in soils, its often not there as we often change it
A horizon
organic matter, some nutrients, microbes, root zone, minerals
B horizon
less organic matter
C
mostly bed rock
not a lot of organic matter
can have microbes / living in the bed rock
D
can have microbes living in the bedrock
rhizosphere
richer than normal soil, absorbs acids, etc.
-surround plant roots
determinants of microbial activity in soil
- water availibility, affecting O2 availibility
- nutrient status, can limit microbes with C,N,P
- adding fungals metabolize and release material helping bacterials for food
Cold water and microbes
cold water is more soluble and hence is used up by aerobes and becomes anoxic
Congregation
cells congregate near edges of pores as theres more nutrients there
rhizoplane
root surface, source of root exudates (sugar, aa, hormones, vitamins)
phyllosphere
surface of plant leaf
Deep terrestrial surface is a microbial habitat
- primarily prokaryotes
- low nutrient habitat, v.low metabolic activity
- 10km below ground surface
Aquatic environments: Freshwater - lakes
O2 produced near surface, depleted further down due to low solubility and consumption
anaerobic inhabitants are in deeper regions