lecture 8 Flashcards

1
Q

5 reasons soils are important

A
  • Foundation of terrestrial ecosystems, influence ecosystem function
    • Provides nutrients, water, anchoring medium for plants
    • Influences plant sp. Composition and productivity
    • Habitat for diverse below ground community, esp. decomposers
      Ecosystem services: C storage, water filtration and storage, decomp, etc
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2
Q

soil comp (rough %)

A

25% air, 25% water, 45% mineral, rest om

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3
Q

5 soil horizons?

A

O (LFH)
A
B
C

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4
Q

what is soil development a balance btwn

A

balance between formation and loss

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5
Q

what 5 state factors influence soil development

A

○ CLIMATE
○ Topography
○ Biological activity
○ Time
Parent material

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6
Q

is soil always there

A
  • Soil we see isnt always there -result of dynamic processes that span geological time and short daily cycles
    BALANCE between forces that produce soils and forces that erode it
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7
Q

parent material origins? what factors impact it?

A
  • Parent material - origins
    ○ Granular soils - air from geological processes + production with climate
    • Topography is important - where it is, how it is made
      biological activity = source of organic matter in the soil = important for life
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8
Q

briefly describe A- C horizons

A
  • At the topLFH - organic matter, a result of things growing and falling into the soil - dark coloration due to decomp - *
    Lfh - organic horizon, active process of decomp
    • Organic matter and middle components interact more at A horizon, shallow roots
    • At B horizon - anything going down has to leech down from the top - lighter coloration, deeper roots,
      C - less organic material (30-40% organic material at most)
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9
Q

are soil horizons the same at every biome

A
  • Layers may differ in proportion in different biomes
    Rainforest - more rain = clearing of substantial amount of lower horizon
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10
Q

what are soil properties strongly influenced by

A

The physical and chemical properties of rocks strongly influence soil properties

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11
Q

chemical properties of soil?

A

properties
* Chemical properties:
Ph, elements, nutrient status, toxins, cations, anions

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12
Q

physical properties of soil

A
  • Physical properties:
    Particle size/surface area: movement and retention of water and nutrients
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13
Q

how does parent material turn into soil

A

Parent material comes from earth - magma comes to the surface, forms igneous rocks then cools, weathered and broken down into sediments, weight + temp = sedimentary rocks, heat and pressure = metamorphic rocks which melt back into magma

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14
Q

what two ways can parent material form soil

A

Sedentary - formed in place (consolidated)
Transported - moved from elsewhere (unconsolidated)

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15
Q

describe sedentary PM

A
  1. Sedentary - formed in place (consolidated)
    • Cumulous - organic (preserved plant residues)
      Residual (bedrock)
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16
Q

describe transported P,

A
  1. Transported - moved from elsewhere (unconsolidated)
    • Loess /eolian - wind (clay/slit/sand)
    • Till- receding glaciers
    • Alluvial/lacustrine - rivers/lakes
      Colluvial - gravity
17
Q

how do temp and moisture impact soil development?

A

○ Influence rates of physical and chemical weathering, plant growth, decomposition
○ Water and temp go up = chemical and biological processes increase
Extreme or variable temps = physical weathering goes up

18
Q

how does precip + wind and rain impact soil development

A
  • Precipitation
    ○ Input of materials into systems (e.g. minerals and water)
    • Wind and rain- erosion and parent material formation
      Driver of soil develoment
19
Q

what impact does topography have on soil development

A

Major impact

20
Q

how does topography impact soil development?

A
  • Effects via microclimate (temp and moisture); rate of biological and chemical processes (slope, aspect, exposure)
    • Effects via erosion and deposition; PM formation
    • Determines distribution of water on landscape (e.g. convex -> sheds water)
    • Where rocks are exposed is where weathering will take place
      Graph - lots of movement and transport of parent material depending on amount of water and slope of a particular area - steeper + water moves faster = transport material faster