Chapter 12: Weathering, Erosion, and Soil Resources Flashcards

1
Q

What is soil?

A

all unconsolidated material that overlies bedrock, material capable of supporting plant growth

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2
Q

How is soil produced?

A

produced by weathering: the chemical, physical, and biological processes that break down rocks and minerals

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3
Q

Mechanical Weathering

A

(physical weathering) anything that breaks up a rock without altering its composition; (ice, wind, water). Breaks larger chunks of rock into smaller ones, increasing the exposed surface area.

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4
Q

Chemical Weathering

A

Break down of minerals by chemical reactions with water, other chemicals dissolved in the water, and gases in the air.

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5
Q

What conditions make weathering more rapid?

A

Higher amounts of water (wetter climate), higher temperatures (warmer climate): chemical reactions proceed more rapidly at higher temperatures than at low ones

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6
Q

How does soil form?

A
  1. chemical and physical weathering of rocks produce debris.
  2. mildly acidic rain percolates through the debris and dissolves parts of it, carrying those ions deeper into the ground
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7
Q

Zone of Leaching

A

the layer of soil from which ions have been extracted or removed, this is an upper soil layer

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8
Q

Zone of Accumulation

A

the ions that have been leached out precipitate deeper in the soil column forming new minerals and clays in a region, this is a deeper soil layer

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9
Q

Microbes interaction with soil

A

microbes further weathering and soil breakup, when they die they accumulate in the soil to form an organic-rich soil material (humus) found in the “O” horizon

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10
Q

Soil Profile

A

a cross-section of soil reveals layers consisting of horizons

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11
Q

A Horizon

A
  1. The “O” in O horizon stands for “organic layer” and consists of organic matter, or humus.
  2. The O and A horizons together make up topsoil, the fertile portion of soil that farmers till for planting crops.
  3. Below the A horizon is the E horizon.
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12
Q

What zone do O, A, and E horizons form?

A

form the zone of leaching because rainwater percolates through this initial layer, dissolves soluble minerals, and carries them away

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13
Q

B Horizon

A

Lies in the zone of accumulation, B horizon is called the subsoil, where ions, clay minerals, and iron oxides accumulate. Organic matter from the surface is largely absent from this layer.

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14
Q

C Horizon

A

Consists of material from the underlying bedrock that has undergone some weathering, and consists of mostly broken-up bedrock.

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15
Q

What is soil composition influenced by?

A
  1. Climate: large amounts of rainfall and warm temperatures accelerate chemical
    weathering and lead to heavily leached soils. Cooler temperatures and lower rainfalls may inhibit soil formation by slowing down the weathering process.
  2. Substrate composition (i.e., what is the bedrock that underlies the composed of): soils can form on basalt, granite, volcanic ash, and quartz sand; leading to soils of different compositions.
  3. Time: in temperate regions, it takes approximately 15,000 years to form 1 meter of soil. This estimate is based on glacial evidence.
  4. Vegetation: plant roots help prevent soil from washing away
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16
Q

Color of Soil

A

color reflects the minerals which make it up, the soil’s composition. black soils are rich in organic matter, red soils are rich in iron, and white soils are depleted in organic matter

17
Q

What is soil texture and the three components?

A

The texture is the size of the soil fragments, Components: sand, silt, clay (larger > small)

18
Q

Loam

A

a soil that has a roughly equal mix of sand and silt and 10-30% clay

19
Q

Soil Structures

A

How well soil clumps together forming a structure called ped. Soil that forms peds are typically more resistant to erosion.

20
Q

What are the two broad categories of soil classification?

A

Pedalfer and Pedocal

21
Q

Pedalfer Soils

A
  • reflects soil in more humid regions
  • soils are more leached leaving the B horizon - more enriched in aluminum and iron minerals
    usually acidic
  • in North America, these soils are found in the southwestern US
22
Q

Pedocal Soils

A
  • reflects soils in drier regions
  • soils are less leached, even soluble minerals such as calcium carbonate remain in the B horizon
  • usually more alkaline, due to the presence of calcium carbonate
  • in North America soils found in southwestern US
23
Q

Lateritic Soil

A

Heavily leached, very oxidized, an extreme pedalfer

24
Q

Where are Lateritic Soils commonly found?

A

common in rainforests, laterite soils develop in tropical climates with high temperatures and heavy rainfall

25
Q

Wetland Soil

A
  • contains an abundance of organic matter, the soil is soft
  • acts as settling ponds reducing pollution from sediments carried in from water passing through, and also help serve as retention ponds for floodwaters
  • many are drained for farmland or development, and others are threatened due to the rising global sea level.
26
Q

Weathering

A

breakdown of rock or minerals material in place

27
Q

Erosion

A

physical removal of material from one place to another (can occur through wind, rain, surface runoff, steep slopes, etc.)

28
Q

Dust Bowl

A

a portion of the American Midwest that experienced a farming crisis in the 1930s brought about by poor farming practices, and the destruction of the natural topsoil due to intensive farming

29
Q

Loss of topsoil in farming leads to several consequences

A
  1. loss of organic matter and nutrients, native topsoil is more permeable and has better structure for crops
  2. Lower crop yields (6” of topsoil loss in western TN reduced corn yields by over 40%).
  3. Further reliance on fertilizer and other chemicals.
  4. persistence of toxic residues of herbicides and pesticides in the soil (microorganisms that would normally break
    these substances down are gone).
  5. Increased soil erosion leads to sediment pollution: eroded soil may contain agricultural herbicides and toxic
    chemical residues that ultimately end up in rivers and lakes, decreasing water quality, harming wildlife, and
    ultimately having to be dredged.
30
Q

Soil erosion impact on soil formation

A

soil erosion is stripping away farmland far faster than the soil is being replaced: soil and high-quality farmland is a nonrenewable resources in many populated areas

31
Q

Strategies for Reducing Erosion

A
  1. Reduce erosion rate: contour plowing to reduce surface runoff
  2. protect soil from agents of erosion
  3. disadvantages: high short-term cost to the farmer; reduces crop yield, may lose out to competitive practices in other states