Primary and secondary minerals Flashcards

1
Q

what is the definition of a mineral?

A
  • naturally occuring
  • inorganic
  • solid at room temperature
  • regular crystal structure
  • defined chemical composition
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2
Q

what are three things that are influenced by soil mineralogy?

A
  1. chemical weathering
  2. nutrient supply
  3. buffering capacity
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3
Q

where do primary minerals come from? and where are they found?

A
  • derived from igneous or metamorphic rocks
  • mostly found in sand and silt fraction
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4
Q

where do secondary minerals come from and where are they found?

A
  • they are inhereted from parent material or formed in situ at surface of Earth or in soil solution
  • mostly found in clay fraction
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5
Q

what is the basic structural unit of primary minerals?

A

silicon tetrahedon [SiO4]^4-

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6
Q

what capacity grows when more oxygen atoms are shared by Si?

A

resistance to chemical weathering

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7
Q

from smallest to largest, what are the most resistant to weathering structures of silicate tetrahedron polymers?

A

isolated > rings > chains > sheets > 3-dimensional network

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8
Q

what is isomorphous substitution?

A

the replacement of central Si atom by Al to make aluminosilicate minerals
–> similar size but different valency because Si is 4+ and Al is 3+

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9
Q

what happens after isomorphous substitution?

A

because the valency is different, a cation must be incorporated into the mineral lattice to provide an extra + charge

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10
Q

what is the weakest bonding cation in minerals?

A

K+ (potassium)

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11
Q

what are the 5 most common primary minerals in soils?

A
  1. quartz
  2. Feldspar
  3. Mica
  4. Olivine
  5. Haematite
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12
Q

what are some characteristics of quartz?

A

SiO2 –> 3D sharing of Si tetrahedra
- very resistant to weathering

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13
Q

what are feldspars?

A

substitution of ~25% of Si by Al and incorporation of cation into mineral lattice

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14
Q

what is mica?

A

complicated isomorphous substitution

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15
Q

where do primary phosphate-containing minerals come from?

A
  • sedimentary and igneous rock
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16
Q

how do secondary minerals form?

A

under conditions close to surface temperature and pressure, they are the result of weathering of primary minerals or formed right away in soil

17
Q

what secondary minerals are most common in soils of temperate regions?

A

alumino-silicates

18
Q

what secondary minerals are most common in soils of tropical regions?

A

hydroxides of iron and aluminum

19
Q

how are clay minerals formed?

A

formed by varying combination of Si and Al sheets and by isomorphous substitution

20
Q

what are 5 characteristics of clay minerals?

A
  1. large surface area
  2. expansion and contraction upon wetting and drying
  3. control cation and anion exchange capacity
  4. have both permanent and pH variable charge capable of attracting and retaining plant nutrients with impacts on soil fertility
  5. most chemically active inorganic phases in soil
21
Q

what is the additional building block (other than SiO4) in secondary minerals?

A

aluminum octahedron

22
Q

what would be left if all minerals were weathered away?

A

would be left with just quartz

23
Q

where does soil chemistry occur (associated with clay minerals)?

A

in between clay mineral sheets

24
Q

describe the kaolinite mineral

A
  • ratio of 1:1 of sheets of silicon tetrahedron and aluminum octahedron with shared oxygen atom
  • hydrogen bonds between sheets
25
Q

describe smecite

A

2:1 clay mineral (meaning two tetrahedron and one octahedron) and sheets bonded together with hydrated cation

26
Q

which bond is weaker: cation or hydrogen?

A

cation exchange bonds are weaker than hydrogen bonds

27
Q

describe mica clay mineral

A
  • 2:1 clay mineral
  • a lot of isomorphic substitution
  • often balanced with potassium cation that is not hydrated
  • has been developed from the mica primary mineral
28
Q

describe the chlorite clay mineral

A
  • 2:1:1
  • between the 2:1 sheets, there is an octahedron sheet
29
Q

what happens when water molecules are in clay minerals?

A

allows for expansion and contraction. –When water becomes gaseous, water evaporates and sheets collapse and minerals shrink -> cracking soils because minerals need much less space