Weathering & Soil Notes Flashcards

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1
Q

What is weathering?

A

The breaking down of rock due to physical and/or chemical changes in the rock as it is exposed to the atmosphere

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2
Q

Where does weathering occur?

A

It occurs at the interface between the atmosphere and the lithosphere

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3
Q

What does weathering result in?

A

Smaller pieces of rock called sediments

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4
Q

Physical Weathering Types:

A
  • Frost action
  • Plant action
  • Pressure unloading
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5
Q

Frost action:

A

Occurs in a cold and moist climate, alternating freezing and melting of water in the rock cracks the rock

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6
Q

Plant action:

A

Plant roots grow into small cracks in the rock and widen them

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7
Q

Pressure unloading:

A

Rock cracks when pressure over the rock is removed

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8
Q

What results of physical weathering?

A

A change in appearance of rock (size, shape, state of matter)

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9
Q

What results from chemical weathering?

A

A change in chemical composition of the rock

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10
Q

Types of Chemical Weathering:

A
  • Oxidation
  • Acid Reactions
  • Hydrolysis
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11
Q

Oxidation:

A

Addition of oxygen to metal, results in rust (iron oxide)

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12
Q

Hydrolysis:

A

Chemical weathering by reaction of water with other substances, when certain minerals are exposed to water they dissolve into ions, water will help any chemical reaction

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13
Q

Hydrolysis Example:

A

Feldspar will chemically weather into clay (kaolinite)

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14
Q

Acids:

A

Gases such as sulfur dioxide, nitrogen dioxide and carbon dioxide will dissolve in rainwater forming acid rain

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15
Q

Acid Rain Example:

A

Calcite will dissolve completely in carbonic acid-thus chemically weather any rock containing this mineral easily

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16
Q

Destructive Forces:

A
  • Plate tectonics builds up the earth’s surface, but what goes up must come down
  • Once exposed to the air, water or wind, rock will begin its destructive cycle and will weather down
17
Q

How does acid rain form and harm?

A
  • Acid rain forms naturally by volcanic activity or by pollutants
  • Acid rain harms any exposed rock, buildings and monuments
18
Q

End result of weathering:

A

Sediments, including clay, silt, sand, pebbles and cobbles

19
Q

What can affect the rate of weathering?

A
  • Size of sediment
  • Type of mineral (hardness, Moh’s scale)
  • Temperature
  • Humidity (amount of moisture present)
20
Q

How does weathering connect to the rock cycle?

A

Without weathering, no sedimentary rocks will form

21
Q

What is soil?

A

A mixture of weathered rock and organic remains (humus)

22
Q

Where does soil form?

A

Forms at the interface between the atmosphere and the lithosphere

23
Q

How does soil form?

A

1) Rocks weather
2) Leaching of minerals adds nutrients to lower layers from top layer
3) Biological activity such as decomposition add organic matter (humus) to soil, soil is mixed by earthworms

24
Q

How long does soil take to form?

A

Takes 500-1,000 years to form

25
Q

Soil horizons:

A

Horizon A: Topsoil (fertile layer)
Horizon B: Subsoil
Horizon C: Parent rock

26
Q

Types of soil:

A

1) Residual: stays

2) Transported: moved

27
Q

What measure can be done to conserve soil?

A
  • Soil is a natural resource and must be protected-
  • Several methods exist to protect soil such as contour farming, no-till farming, terracing and crop rotation
  • These all prevent erosion of the topsoil by wind or water
28
Q

Why is it important to protect soil?

A
  • We need it to sustain ecosystems
  • Producers take nutrients from the soil and convert it to food with the help of sunlight
  • Basis of the food chain