Apes SOIL Flashcards

1
Q

What is physical weathering?

A

The mechanical breakdown of rock through wind, water, temperature, or biological components. Increases surface area for more weathering.

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2
Q

Examples of physical weathering

A

Water freezing in cracks of rocks
Expanding and contracting minerals from temperature
Burrowing animals
Plant roots

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3
Q

Chemical weathering

A

The breakdown of rocks and minerals by chemical reactions, dissolving of chemical elements from rocks, or both. Occurs on newly exposed (primary) minerals.

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4
Q

What primary minerals is found in granite rock

A

feldspar

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5
Q

What does chemical weathering do?

A

Alters the primary minerals to form a secondary mineral and ionic forms of their constituent chemical element

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6
Q

What happens when feldspar is exposed to natural acids in rain?

A

Forms clay particles as a secondary mineral, and releases ions such as potassium.

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7
Q

Examples of chemical weathering

A

Natural acids in rains reacting with minerals
Lichens producing weak acids (soft gravestones, masonry)
Acid precipitation, or acid rain

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8
Q

Which rocks weather quickly?

A

Rocks with compounds that dissolve easily , such as calcium carbonate (found in limestone). EX: carbonic acid in water from vaporized carbon dioxide dissolves limestone when it’s cracks.

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9
Q

What is acid precipitation or acid rain from

A

Humans release sulfer from fossil fuel combustion + 02= sulfer dioxide = sulfuric acid. Similar emissions of nitrous oxide and water vapor form nitric acid. Leads to high concentrations of these acid, and are responsible for rapid degradation of many old statues, gravestones, limestone an dmarble structures.

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10
Q

What is erosion

A

physical removal of rock fragments from landscape/ecosystem, which accumulates in are of deposition.

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11
Q

Examples of soil erosion

A

winter, water and ice move soil down the slope with gravity
animals burrow under soil
Deforestation, overgrazing, unmanaged construction activity and road building.

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12
Q

Cations are

A

positively charged mineral ions. Can be used as nutrients by the plants.

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13
Q

Parent Material

A

original rocks that were broken down to form the basis of the soil

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14
Q

Soil is formed when….

A

Parent Material is weathered, transported and deposited, with the accumulation of organic matter.

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15
Q

Factor in soil formation (PARENT MATERIAL)

A

Soil tends to retain basic properties of these rock

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16
Q

Factor is soil formation (CLIMATE)

A

Average temperature and moisture change rate of weathering and leaching (nutrients in water), wind redistribution as well.

17
Q

Factor in soil formation (TOPOGRAPHY)

A

Slope of land may affect erosion

18
Q

Factor in soil formation (ORGANISMS - Bioloigical)

A

Plants, animals, microrganisms

19
Q

Time

A

Soil formation is continuous, there is no end.

20
Q

What is a soil profile?

A

The soil horizons built over time (common layers)

21
Q

O Horizon

A

Organic Matter

22
Q

A Horizon

A

(Surface Horizon) - lots of humus and organic material.

23
Q

B Horizon

A

(Subsoil) mix of rock and organic material.

24
Q

C Horizon

A

Substrata - mostly parent material

25
Q

Order of particle size in soil, largest to smallest

A

Sand (2 to 0.05mm) , Silt ( 0.05mm to 0.002mm), caly (less than 0.002mm)

26
Q

Large particle size permeability?

A

(sand) allow water to pass through quickly

27
Q

Smaller particle size permeability?

A

(clay) doesn’t allow water pass through easily

28
Q

What determines soil type?

A

The percentage of sand, silt, and clay using a soil triangle.

29
Q

Loam is

A

A combination of sand, silt, and clay.

30
Q

Percolation and infiltration can be determined by

A

Percentage of sand, silt, and clay

31
Q

Percolation

A

Movement of water into ground

32
Q

Define percolation

A

movement of water into ground

33
Q

Define infiltration

A

movement of ions or chemicals through percolation

34
Q

What is soil composition?

A

The percentage of sand, silt, and clay.