Chapter 4 Flashcards

(41 cards)

1
Q

Adsorbed cations are also known as ____.

A

exchangeable cations

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2
Q

What is the charge of agriculturally important soils?

A

negative charge

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3
Q

The process whereby cations adsorbed on the surface of soil colloids is exchanged for those in the soil solution or in any medium that comes in contact with the soil colloids.

A

Cation exchange

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4
Q

If nutrients are not absorbed by soil colloids, they are subject to what.

A

Loss through leaching

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5
Q

Na-rich soils are in what state?

A

dispersed

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6
Q

The element that is responsible in dispersing soil.

A

Na

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7
Q

Ca-rich soils make the soil to be?

A

flocculated

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8
Q

Element responsible in making flocculated soil

A

Ca

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9
Q

Is dispersion a desirable characteristic of productive soil?

A

NOT desirable

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10
Q

The CEC of permanent charge clays.

A

low CEC

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11
Q

The buffering capacity of permanent charge clays?

A

low buffering capacity

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12
Q

Accompanying ions

A

complementary ions

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13
Q

What will happen to the ion of interest if the complementary ion is strongly adsorbed?

A

easily released

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14
Q

The quantitative measure of the ability of soil to adsorb and exchange cations with those in the surrounding solution and with plant roots.

A

cation exchange capacity

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15
Q

The sum of the negative charges of the soil.

A

cation exchange capacity

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16
Q

The sum total of the exchangeable cations that a soil can adsorb.

A

cation exchange capacity

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17
Q

The easily exchangeable cations.

A

electrostatically retained cations

18
Q

The cations that are readily available for plant uptake.

A

electrostatically retained cations

19
Q

The dissociation of H from OH- groups

A

deprotonation

20
Q

What will happen to the charge if there is deprotonation?

A

additional negative charge

21
Q

What is the CEC of OM?

A

100-300 cmolc/kg soil

22
Q

Tells us the degree to which the exchange sites are occupied by basic cations.

A

percentage base saturation

23
Q

Give examples of basic cations.

24
Q

Give examples of acidic cations.

25
The atomic weight of Ca.
40 g/mol
26
The atomic weight of Na.
23g/mol
27
The atomic weight of K?
39g/mol
28
The atomic weight of Mg.
24g/mol
29
What will happen to the cations if there is high percentage cation saturation?
easily and rapidly released
30
Enumerate the practical applications of CEC.
plant nutrition liming amelioration of Na affected soil environmental quality
31
Enumerate the soil properties that determine CEC.
soil texture organic matter content nature of clay colloid pH percentage base saturation
32
Enumerate the methods of determining CEC.
CEC determination at pH7 ammonium acetate:1N calculation of effective CEC CC determination using BaCl2
33
Enumerate the soil processes that affect cation exchange.
weathering nutrient retention dispersion and flocculation buffering pH change
34
The characteristics of cation exchange reactions
ER are stoichiometric and take place in equivalent amounts CE are instantaneous ER are reversible
35
Factors affecting the extent of cation exchange.
1. Relative adsorbability of the cation on soil colloid or the relative replacing the power of the cation 2. Concentration of the solution 3. Nature of exchange materials 4. Geometric fit of ions into the mineral structure 5. Influence of complementary ions
36
Between Kaolinite and Illite which has a rapid cation exchange?
Kaolinite
37
Between kaolinite and illite which takes longer time?
illite
38
High level of Ca is antagonistic to?
inhibit K
39
High K would lead to
interfere Mg
40
ESP stands for
Exchangeable Sodium Percentage
41
Soils with high amounts of soluble sodium
Sodic soils