Soils Flashcards

1
Q

organic soils

A

decomposition of organic matter from bogs and marshes

higher (60%) of organic matter

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2
Q

soil formation

A

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

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3
Q

O horizon

A

in the open air

in soils, its often not there as we often change it

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4
Q

A horizon

A

organic matter, some nutrients, microbes, root zone, minerals

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5
Q

B horizon

A

less organic matter

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6
Q

C

A

mostly bed rock
not a lot of organic matter
can have microbes / living in the bed rock

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7
Q

D

A

can have microbes living in the bedrock

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8
Q

rhizosphere

A

richer than normal soil, absorbs acids, etc.

-surround plant roots

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9
Q

determinants of microbial activity in soil

A
  • water availibility, affecting O2 availibility
  • nutrient status, can limit microbes with C,N,P
  • adding fungals metabolize and release material helping bacterials for food
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10
Q

Cold water and microbes

A

cold water is more soluble and hence is used up by aerobes and becomes anoxic

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11
Q

Congregation

A

cells congregate near edges of pores as theres more nutrients there

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12
Q

rhizoplane

A

root surface, source of root exudates (sugar, aa, hormones, vitamins)

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13
Q

phyllosphere

A

surface of plant leaf

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14
Q

Deep terrestrial surface is a microbial habitat

A
  • primarily prokaryotes
  • low nutrient habitat, v.low metabolic activity
  • 10km below ground surface
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15
Q

Aquatic environments: Freshwater - lakes

A

O2 produced near surface, depleted further down due to low solubility and consumption
anaerobic inhabitants are in deeper regions

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16
Q

Epilimnion

A

oxygenic area of lake

17
Q

hypolomnion

A

anoxic region of lake

18
Q

Aquatic environments: Freshwater - Rivers

A

re-oxygenation is affected, organic matter, nutrient inputs affect productivity, leading to O2 depletion
-Biochemical Oxygen Demand (BOD) is the change in dissolved oxygen after 5 days at 20deg C (the measure of organic matter that can be oxidized by microorganisms)

19
Q

Aquatic environments: Marine - Open ocean

A

low primaryproductivity, often limiting N, P, Fe resulting in low heterotrophic activity

20
Q

Aquatic environments: Marine - Inshore area

A

nutrient rich, resulting in greater productivity

21
Q

Aquatic environments: Deep Sea

A
  • cold, high hydrostatic pressure, low nutrient input
  • low microbial activity; inhabitants are psychrotolerant or psychrophilic, piezotolerant (barotolerant) or piezophilic (barophilic)
22
Q

Hydrothermal vent communities

A

driven by geothermal energies

  • free living organisms
  • include S-oxidizing chemolithotrophs (Thiothrix, Beggiatoa, Thiobacillus)
  • may also be H2-, Fe2+-, Mn2+-oxidizers, methanotrophs, nitrifiers
  • may also be methanogens, S0-reducers, sulfate-reducers, Fe(III)-reducers
  • microbe-animal symbioses
  • S-oxidizers & tube worms, clams, mussels

-animals that graze directly on the microbiota

23
Q

tube worms

A
  • possess a trophosome - spongy tissue packed with S granules and S-oxidizing bacteria
  • tube worm traps O2, H2S in blood and delivers to bacteria
  • bacteria grow on H2S, thiosulfate and CO2
  • products of bacterial metabolism support tube worm growth