Chapter 3 Flashcards

(49 cards)

1
Q

The most reactive component of the soil.

A

soil colloid

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2
Q

What are the two types of the soil colloids?

A

organic colloids
inorganic colloids

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3
Q

The highly decomposed organic matter?

A

Humus

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4
Q

The type of colloid that is composed of highly decomposed organic matter?

A

Organic colloid

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5
Q

More reactive type of colloid?

A

organic colloid

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6
Q

_____ are more reactive chemically and generally have a greater influence on soil properties per unit weight than the inorganic colloids.

A

Organic colloids

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7
Q

Inorganic colloids include what?

A

silicate clays
oxides
hydrous oxides
amorphous clays

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8
Q

The size of soil colloid

A

0.001 mm

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9
Q

The charge of colloids in very acid soils

A

net positive charge

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10
Q

Exhibit positive as well as negative charge.

A

amphoteric

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11
Q

The pH at which the surface charge is neutral.

A

Zero point of Charge

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12
Q

The dissociation of H from hydroxyl group also decreases CEC.

A

increases CEC

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13
Q

Fe/Al oxide minerals are stable at what pH?

A

pH 5

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14
Q

Variable charge soils can be limed up to what pH.

A

pH 5.5

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15
Q

Is it viable to increase the pH of variable charge soils up to pH 6?

A

no, it is costly because variable charge soils are buffered below or above pH0

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16
Q

What are the effects of lime?

A

increase pH
precipitate Al to Al(OH)3
replace precipitated Al with Ca

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17
Q

The reaction involved in reacting H+ with OH- with the release of H2O.

A

neutralization

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18
Q

What is the main value of lime?

A

provide hydroxyl ions

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19
Q

What is the surface charge if pH0-pH is (-)?

A

net negative charge

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20
Q

What is the net surface charge if pH0-pH is (+)?

A

net positive charge

21
Q

Which has lower pH0:
surface soil vs subsoil

A

surface soil due to higher OM

22
Q

soils that have low pH0?

23
Q

This is the point at which net surface charge is independent of salt concentration so the titration curves should intersect at this point.

A

Zero Net Charge

24
Q

The pH0 value of Fe/Al oxides

A

7-9 ( high AEC)

25
Parameters that affect the sign and magnitude of charge on variable charge colloids
pH0 soil pH electrolyte concentration valence counterion Dielectric constant
26
Enumerate the theories of Electrical Double Layer
Helmholtz Double Layer Theory Gouy-Chapman Diffuse DL Theory Stern DL Theory
27
consist of an inner layer of strongly adsorbed counterions and an outer layer of ion swarm.
Stern DL
28
2 fundamental equations to describe ionic concentration near the surface and potential distribution with distance from the surface:
Poisson equation Boltzman distribution
29
Describes the coulombic interaction between charges.
Poisson equation
30
Describes the change in concentration of counterions near a charged surface.
Boltzman distribution
31
What happens to DDL at increasing concentration?
decrease thickness
32
What happens to DDL in monovalent cations?
thicker
33
What happens to DDL in divalent cations?
thinner
34
It accounts for the thermal motion of counterions at the charged surface.
Gouy-Chapman Diffuse Double Layer Theory
35
Gouy-Chapman Diffuse DL theory was developed by Gouy in what year?
1910
36
What are the sources of Negative Charge in Colloidal Surfaces
Isomorphous substitution Ionization of exposed hydroxyl group broken bonds at edges of silica-alumina units
37
What are the sources of Positive Charge in Colloidal surface
Isomorphous substitution Protonation of exposed hydroxyl group
38
if Al3+ is being replaced with Mg2+, what will happen to the charge?
leads to increase in negative
39
Source of the positive charge of organic colloid at low pH?
protonation of hydroxyl group and NH group
40
What will happen to the charge if there is IS of Al3+ to Mg2+
gain positive charge
41
Examples of minerals with permanent charge
2:1 clay minerals 2:2 intergrades
42
Enumerate minerals with pH-dependent or variable charge
1:1 clay minerals Fe and Al oxides or sesquioxides Amorphous aluminosilicate Amorphous Fe/Al hydrous oxides Organic colloids
43
They balance or neutralize the net negative charge generated by clay particles
Adsorbing cations
44
It refers to the amount of charge associated per unit area of the clay colloid.
surface charge density
45
if the change in pH is positive, what is the charge of the colloid
negative
46
If the change in pH is negative, what is the charge of the colloid?
positive
47
Implications of charge colloids to soil management
increasing cation retention liming acid soil
48
What will happen to phosphate applied to an oxisol decreased pH0?
increase CEC
49
Mg-dominated octahedral sheets minerals
vermiculite chlorite