week 6- weathering and soils Flashcards

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1
Q

what are the differences between solid rock and the critical zone

A
  • colour due to different minerals
  • disaggregated
  • less dense
  • plants on top of the CZ as there is pore space for roots and nutrients can be provided
  • more water due to pore space, leading to more hydrated minerals
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2
Q

how is the critical zone formed

A
  • through chemical physical and biological weathering
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3
Q

how does physical weathering occur

A
  • rocks and minerals go to smaller fragments
  • through temperature, abrasion and plants and animals
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4
Q

how does temperature cause physical weathering

A
  • driven by the diurnal cycle
  • contraction and expansion causing differential stress which can form cracks
  • exfoliation temp influenced peeling away of rock layers due to stress induced by outer layers being warmer/colder than inner
  • frost wedging, breaking rock when water expands as ice inside pore space
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5
Q

how does abrasion by water ice and wind cause physical weathering

A

WATER
- freeze thaw where flow can dislodge loose bits of rock
- debris in water abrade which can cause rounding of rocks in rivers

WIND
debri in wind abrades rocks

ICE
- freeze/thaw
- debris in ice
- ice also transports lots of ground up rock material

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6
Q

how do plants and animals cause physical weathering

A
  • plant roots pry cracks apart
  • burrowing organisms very minor
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7
Q

why is a larger surface area significant

A
  • increases exposure to chemical weathering
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8
Q

why does chemical weathering occur

A
  • as most rock forming minerals are not thermodynamically stable at earths surface temp/pressure
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9
Q

what factors effect chemical weathering

A
  • temperature
  • water and its flow (reactants = acids and/or oxygen and products= if conc of dissolved products is too high then reaction will stop)
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10
Q

what are the net results of chemical weathering

A
  • primary to secondary minerals
  • deliver nutrients from rocks to biosphere in soluble forms
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11
Q

types of chem weathering reactions

A
  • dissolution
  • direct transformation of minerals
  • precipitation of secondary minerals
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12
Q

how does dissolution occur

A
  • acid attack
  • h+ from water and other acids
  • these ions dissolve minerals thru hydrolysis
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13
Q

what compound is on of the main influencers of chem weathering

A
  • carbonic acid which occurs in rainwater and from microbial respiration
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14
Q

what is congruent

A
  • dissolution where the whole mineral dissolves
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15
Q

reactions for direct mineral transformation

A
  • hydration
  • redox
  • cation exchange
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16
Q

what minerals are secondary precipitated

A
  • soluble
  • oxides and hydroxides
  • clays
17
Q

how do lichens enhance chem and phys weathering

A
  • penetrate cracks
  • secrete organic acids
18
Q

name of soil formation

A

pedogenesis

19
Q

what is a soil profile

A
  • vertical cross section of soil horizons revealed by digging a pit
20
Q

what factors affect soil formation

A

CLORPTS

21
Q

what is residual material

A
  • inorganic parent material, developed in place from weathering of underlying rock

warm climate- oxidation
cool climate- closely resembles original rock

such as: saprolite derived from granite in a dry, cold region

22
Q

organic deposit name and explanation

A
  • peat
    -moss,woody, herbaceous, sedimentary
23
Q

what does a water deficiency do

A
  • promotes formation of salts
  • promotes accumulation of carbonates
  • limited chem weathering
24
Q

high effective rain leads too…..

A
  • increasing clay and organic matter contents
  • higher soil acidity
  • lower si/Al ratio
25
Q

how does nutrient upcycling by tress operate

A
  • conifers take up and store very small amounts of ca,mg, and K
  • conifers retain needles and debris released are very acidic and resinous
  • conifer debris accumulate as thick O horizon
  • soils have low PH and highly leached
26
Q

what helps to identify time-dependancies

A
  • chronosequences
27
Q

stages of soil profile development

A
  • no layering/OM just accumulating/ weathering start/ OM allows nutrient accum so faster plant growth

a activity of organism and plant decay- cm of OM rich soil/ soluble ions move down to form clays

  • deeper OM- distinctive A
  • b is deeper and differentiation into sub horizons