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Soil Acidity and Review of Colloid Charge. Mineral Charge. “Perfect” Mineral. Si. Al. =. Positive charge. Negative charge. Al 3+ Si 4+. OH - O 2-. Tetrahedral Substitution. Al. Al 3+ for Si 4+. Aluminum contributes less (+) charge than silicon. =. Positive charge. - PowerPoint PPT Presentation
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Soil Acidity and Review of Colloid Charge
Mineral Charge
Positive charge
Al3+ Si4+
Negative charge
OH- O2-
“Perfect” Mineral
=
Si
Al
Tetrahedral Substitution
Al3+ for Si4+
Positive charge
Al3+ Si4+
Negative charge
OH- O2-
=
Al
Aluminum contributes less (+) charge than silicon
Octahedral Substitution
Mg2+ for Al3+
Positive charge
Al3+ Si4+
Negative charge
OH- O2-
=
Magnesium contributes less (+) charge than Aluminum
Na+
Na+
Na+Na+
Na+Na+
Na+
Charge
K
HH
O
HH
O
HH
O
H H
O
+
Hydrated Cations
SmectitesSignificant substitution in the octahedra
(Mg2+ for Al3+)
Ca2+ Mg2+ Na+
Cations satisfying charge
CEC = 80-120 cmolc kg
•Layers weakly held together by cations•Highly expansible
Mg2+Mg2+
Source of negative charge Is very close to the adsorbedcations
Layers tightly boundModerately expansible
Vermiculite
Significant substitution in tetrahedra
CEC = 100-180 cmolc kg
Soil Organic Matter and Reactivity
The functional groups on organic colloids are weak acids.
Acids give up hydrogen ions (H+) to water.
HCl H+ + Cl-
Strong acids give up all their H+ ions
Weak acids give up some of their H+ ions
COOH COO- + H+
OH O- + H+
Soil Solution
COOH COO- + H+
Dissociation of weak acid functional groupsresults in the development of negative charge
The amount of negative charge dependson how much dissociation takes place
Low pH = lots of H+ = less dissociation = low chargeHigh pH = little H+ = more dissociation = high charge
The dissociation is inhibited by H+ in soil solution
COOH COO- + H+
COOH
O-
K+ K+COO-
COO-
COO-
COO-
OHO-
O-
O-
COO-
K+K+
Ca2+
Na+K+
Na+
Na+Na+
Mg2+
Mg2+Mg2+
Mg2+
Na+
Na+
Na+
Soil Solution
H+
H+
H+
H+
Mineral Colloids derive charge from substitution of lower-charged cations for higher charged cationsin the crystal matrix during mineral formation. The result is permanent negative charge.
Organic colloids derive their charge from dissociationof hydrogen ions from acidic functional groups on organic matter/humus. The result is pH-dependentcharge
Mineral Colloids – 0 – 180 cmol/kgOrganic Colloids – 100 – 500 cmol/kg
SiAlSi
Total CEC =
Mineral Organic
+
Soil Cation Exchange Capacity
pH-Dependent
You have 2 identical soils (same clay content, mineralogy, and O.M. content).
Soil A has a pH of 6.5Soil B has a pH of 4.0
Which soil has the higher CEC?
Reactivity of Soil Horizons
Contribution to fertility.
Silicate Clay
Organic Matter Organic Matter Organic Matter
Silicate Clay
Silicate Clay
Soil Acidity and pHSoil Acidity and pH
AcidAcid
Any substance which increases the Hydrogenion concentration in solution.
H+
Hydrogen Ions and Organic MatterHydrogen Ions and Organic Matter
0 7 14
Acidic basic
High H+concentration
Low H+concentration
Inhibits dissociationof acidic functional groups
Increases dissociationof acidic functional groups
Low charge onOrganic Colloids
High charge onOrganic Colloids
COOH COO- + H+
Sources of Hydrogen Ions
CO2 from microbial respiration/atmosphere
CO2 dissolved in water produces carbonic acid H2CO3
Acid functional groups on organic matter
COOH COO- + H+
Plant root exudation (release) of H+
Anthropogenic acids in rainfall
Gaseous nitrogen and sulfur oxides make acid rain
Hydrolysis of aluminum can produce acids
CO2 + H2O H2CO3
What are the acids in soils?
Two Ions considered Acidic in Soils
H+ Aluminum
Remember that aluminum is a common constituent of silicate clays
Aluminum participates in “hydrolysis”reactions with water.
Both are cationic
Hydrolysis of Water
(ionization of water)
H2O OH- + H+
H+ is the acid OH- is the base
In pure water, the amounts of H+ and OH- are equal
Bases are the opposite of acids
Aluminum has the ability to breakwater apart and react with the resulting OH-
Aluminum
H2O OH- + H+
Hydrogen and AluminumHydrogen and Aluminum
The only soil ions considered to be acidic
Hydolysis by Aluminum
Al3+ + H20 = Al(OH)2+ + H+
Al(OH)2+ + H20 = Al(OH)2+ + H+
Al(OH)2+ + H20 = Al(OH)o
3 + H+
H2O OH- + H+
Strongly Acid Soils (pH < 5)
Aluminum is soluble => Al3+ or Al(OH)2+
Both are exchangeable and strongly adsorbedThey are also in equilibrium with aluminum in solutionThe aluminum cations in solution can hydrolyze => H+
Moderately Acid Soils (pH 5 – 6.5)
Aluminum exists as Al(OH)2+ and Al(OH)2+
Both are exchangeable and can be strongly adsorbedThey are also in equilibrium with aluminum in solution.The solution aluminum cations hydrolyze => H+
Types of Soil Acidity
Active Acidity
Acidity associated with soil solution
H+ ions
Active Acidity
Acidity associated with the soil solution
Typically a 1:1 or 2:1 extract
10 g soil and 10 mL water
10 g soil and 20 mL water
0 7 14
Acidic basic
5.6
pH meter
0 7 14
Acidic basic
PlantAlfalfaSweet CloverBeetsCauliflowerSpinachPeasCarrotsCotton Wheat TomatoesPotatoesBlueberriesAzaleas
pH Range
6.0 – 8.0
5.5 - 8.0
5.3 - 7.5
5.0 – 7.2
4.5 – 5.5< 5
Sometimes soil pH must be adjusted to accommodate plants
Active Acidity
Exchangeable Acidity
Exchangeable Acidity
Acidity associated with cation exchange sites on mineral or organic colloids.
H+ Al+3
Types of AcidityTypes of Acidity
Active Acidity
H+ H+
H+ H+H+
H+
H+
H+
H+ H+
H+
H+
H+
H+
Soil Solution
Al+3 Na+ H+
H+ H+ K+
H+ Al+3
Na+
Ca2+ Ca2+
Ca2+
H+
H+
Clay minerals/Organic matter
Exchangeable
Measurement of Exchangeable Acidity
Initial EquilibriumInitial Equilibrium
Ca+2 Ba+2
Na+
Na+
Mg+2
K+
Ca+2
Ca+2Ca+2
Cu+2
Ca+2
Mg+2
Soil Solution
Al+3 Na+ H+
H+ H+ K+
H+ Al+3
Na+
Ca2+ Ca2+
Ca2+
H+
H+
Clay minerals/Organic matter
ExchangeableActive
H+
H+H+
H+
H+
H+
H+
Flood System with BaFlood System with Ba2+2+
Ba+2 Ba+2
Ba+2
Ba+2
Ba+2
Ba+2
Ba+2
Ba+2Ba+2
Ba+2
Ba+2
Ba+2
Soil Solution
Al+3 Na+ H+
H+ H+ K+
H+ Al+3
Na+
Ca2+ Ca2+
Ca2+
H+
H+
Clay minerals/Organic matter
Exchangeable
Total AcidityTotal Acidity
Ba+2
Soil Solution
Ba+2 Ba+2 Ba+2
Ba+2 Ba+2 B+2
Ba+2 Ba+2
Ba+2
Ba2+ Ba2+
Ba2+
Ba+
H+
Clay minerals/Organic matter
Active and Exchangeable
H+ H+
H+ H+H+
H+
H+
H+
H+ H+
H+
H+
H+
H+
Na+
Ca2+
K+
K+
K+
Ca2+
Exchangeable acidity can be many times greater than
active acidity.
Managing soil acidity must accountfor exchangeable acidity as well as
active acidity.
Next: Acidity and Fertility