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102 Terms
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What are the major controls of cation selectivity?
Concentration, charge and hydration, exchange site composition, and clay mineralogy.
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How does concentration affect exchange?
More of a replacing ion drives exchange through mass action.
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How do charge and hydration affect retention?
Higher-charge and less strongly hydrated ions are retained more strongly (Lyotropic series).
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How does exchange site composition affect replaceability?
Replaceability changes with the ions and saturation levels already present.
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How does clay mineralogy affect selectivity?
Different minerals show different selectivity patterns.
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Is exchange reversible?
Yes, but cations are not retained equally.
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What does the Lyotropic series represent?
The strength of cation adsorption.
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What is the Lyotropic series based on?
Charge density.
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How does charge density change?
Increases with charge, decreases with increasing size.
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What is the consequence of stronger adsorption of H+ and Al3+ than other cations?
Leaches out sodium, potassium, etc., leaving behind Al3+ and H+.
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What does heavy leaching leave in the soil?
Al and H (non-essential nutrients that can be toxic in high concentrations).
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What type of soil environment does this create?
A very acidic environment.
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Which ions form inner sphere complexes?
Phosphates, arsenates, molybdates, sulfates.
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How do they react(ions)?
They react with the particle surface.
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What is the effect on net positive charge?
Reduces net + charge in soil.
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How tightly are inner sphere complexes held?
Very tightly, not readily available.
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Which anions are retained more strongly?
Phosphate, arsenate, fluoride.
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Which anions are retained more weakly?
Nitrate and chloride.
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What is the management implication of AEC?
AEC influences phosphorus availability and the mobility of nitrate and contaminants.
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Where is AEC important?
Highly weathered acidic soils, Fe and Al oxide-rich surfaces, variable-charge minerals at low pH.
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What are the three ways to determine CEC?
1. Sum exchangeable cations, 2. Displace and measure, 3. Estimate from soil properties.
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What must be reported with a CEC value?
The extraction method and soil pH conditions.
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How do you calculate CEC using the summation method?
Add Ca2+, Mg2+, K+, Na+, exchangeable acidity (H+), and Al3+ from soil test reports.
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Example: If K+=0.2, Mg2+=2.0, Ca2+=8.0, Na+=0.3, H+=1.0, Al3+=1.0, what is the CEC?
12.5 cmolc kg^-1.
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What is important before adding components in the summation method?
Keep units consistent.
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How does the displacement method measure CEC?
Leach soil with NH4 acetate (pH 7) to saturate sites, remove excess with alcohol, then displace NH4 with Na or K and titrate to find CEC.
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How is CEC estimated?
Use clay amount, clay mineralogy, organic matter, and a calibrated equation.
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Does texture alone determine CEC?
No. Clay type, organic matter, and measurement pH can shift the value.
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Does high CEC always mean high fertility?
No. Exchange sites may be occupied with H, Al, or other non-nutrient cations.
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How are soil cations separated?
Into basic and acidic cations.
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What is Base Saturation?
The percentage of CEC occupied by basic cations.
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What does % acidity represent?
The percentage of CEC occupied by acidic cations.
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How does high BS affect soil pH?
Higher soil pH results from higher BS.
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Why are soils with high BS generally more fertile?
They contain greater amounts of essential plant nutrient cations (K+, Ca2+, Mg2+).
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What toxic cation is absent in high BS soils?
Al3+ (aluminum).
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How does high BS buffer the soil?
More buffered against acid cations from plant roots and soil processes (nitrification, acid rain, etc.).
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What happens to Al3+ at lower soil pH?
Greater amounts of toxic Al3+ are present.
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At what pH is Al3+ present in significantly high concentrations?
When soil pH < 5.4.
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How does Al3+ affect plants?
Hinders growth of most plant species.
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How is % Base Saturation calculated?
%BS = [(Total of basic cations) / CEC] x 100.
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What is the formula for pH?
pH = -log[H+].
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What does [H+] represent?
mol/liter, or M.
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How much does one pH unit represent?
A tenfold change.
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What is the pH of a solution with 0.01 g of H per 1000 liters?
pH 5. (0.01 mol / 1000 L = 0.00001 M; -log(0.00001) = 5).
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What is the pH of a 0.1 M HCl solution?
1.
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What fraction of global soils are acidic?
About 1/3.
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Where are acid soils found in the US?
SE and NW regions.
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Where are acid soils found globally?
A northern and southern belt.
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In what climate do acid soils form?
Where precipitation is greater than 24 inches (60 cm) per year.
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What is the pH of H2O in equilibrium with atmospheric CO2?
~5.7.
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What is the chemical reaction for CO2 in water?
H2O + CO2 ⇄ H2CO3 ⇄ H+ + HCO3-.
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Why do areas with greater precipitation result in more acidic soils?
More precipitation leads to more leaching and acidification via this reaction.
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What is Source 1 of soil acidity?
Formation of carbonic acid from CO2 (atmospheric CO2 dissolved in rainwater results in greater acidity in soil than in the atmosphere).
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What is Source 2 of soil acidity?
Natural occurrence of many organic acids in soil (low molecular weight organic acids produced by roots and soil microbes, such as citric and malic acids).
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What is Source 3 of soil acidity?
Oxidation of N, S, and Fe compounds.
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Besides N oxidation, where else do you get NH4+ from regarding oxidation?
Sulfur and Iron oxidation.
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What is Source 4 of soil acidity?
Acid Precipitation.
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What produces sulfur and nitrogen gases for acid precipitation?
Lightning, volcanic eruptions, forest fires, and combustion of fossil fuels.
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Where are the impacts of acid precipitation stronger?
Downwind from industrial areas.
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How do plants uptake cations and anions regarding pH?
By altering pH to maintain electrical neutrality.
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What happens when plants absorb cations?
They extrude H+ (or uptake anion) to maintain electrical neutrality.
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What happens when plants absorb anions?
They extrude OH- or HCO3- (or uptake cation) to maintain electrical neutrality.
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What happens when cation uptake exceeds anion uptake?
Excess H+ is released (acidifying the soil).
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Do most plants uptake more cations or anions?
More cations.
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What is the result of most plants uptaking more cations?
The soil is acidified.
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Why do legumes add H+ to the soil?
Most N comes from N-fixation (little NO3- uptake), so H+ is added to balance charge.
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Where does deprotonation of pH-dependent charges occur?
From edges of clay minerals, Fe and Al oxides, and OM.
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What is the result of deprotonation?
A reduction in pH.
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What happens to Al3+ concentration as pH decreases?
It increases due to the dissolution of Al(OH)3 (gibbsite).
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What does Al hydrolysis generate?
H+ and lowers pH.
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Why is Al considered an acid cation?
Its dissolution generates H+ and lowers pH.
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How does Al buffer pH?
pH won’t increase until enough base is added to decrease soluble Al3+.
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At what pH does Al(OH)3 precipitate?
pH 6.5 (decreasing Al3+ and increasing pH).
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How does Al3+ on exchange sites buffer pH?
When neutralized with a base, Al3+ precipitates as Al(OH)3. Exchangeable Al3+ is released to replace Al3+ in solution, resulting in a gradual pH increase.
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What is the reverse reaction of Al buffering?
Addition of acid neutralizes OH-, Al(OH)3 dissolves to release Al3+ into solution, resupplying exchangeable sites.
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How do pH-dependent CEC sites buffer pH?
When a base is added, deprotonation occurs from pH-dependent sites.
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What determines buffering capacity?
Clay mineral and OM content.
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How does CEC relate to buffering capacity?
Higher CEC = greater buffering capacity.
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If a sandy loam and a clay loam both have pH 5.0 and receive the same lime, which shows the larger pH increase?
The sandy soil (lower buffering capacity).
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What is Active Acidity?
H+ activity in the soil solution; measured as soil pH; small pool; immediate root environment.
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What is Exchangeable Acidity?
Readily displaced H+ and Al species held on clay and OM surfaces; often extracted with an unbuffered salt.
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What is Residual Acidity?
Less readily neutralized solid-phase acidity associated with OM mineral edges and hydroxy-Al forms.
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What is Total Acidity?
Active acidity + Potential acidity (Exchangeable + Residual).
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How do carbonate/bicarbonate inputs consume H+?
Weathering of calcium carbonate (CaCO3) and bicarbonates consumes free protons.
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How does anion protonation consume H+?
Functional groups on organic matter consume H+ during reverse association (RCOO- + H+ → RCOOH).
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How do reduction reactions consume H+?
Biological reduction of N, S, and Fe compounds consumes H+.
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How does mineral weathering consume H+?
Dissolution and weathering of primary silicate and non-silicate minerals consume protons and release base cations.
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How does anion uptake by plants consume H+?
It removes acidity from the soil system.
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What are two human causes of soil acidification?
Acid rain and nitrogen fertilization.
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Are CaCO3 equivalents of N fertilizers usually accurate?
No, they usually overestimate acidity.
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Why do CaCO3 equivalents overestimate acidity?
Root absorption of anion fertilizers (NO3-, SO42-, H2PO4-) neutralizes some acidity.
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By how much is the acidity from N fertilizers usually reduced?
By 50%.
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How does nitrate leaching accelerate soil acidification?
NO3- is a product of nitrification of NH4+ (from fertilizer, OM, manure). If all NO3- is absorbed, no H+ is produced. But crop recovery is incomplete, so leaching occurs.
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Where is nitrate leaching greater?
Under legumes than unfertilized grass pastures.
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What factors determine the net effect of crop growth on soil acidity?
Plant species, proportion of NO3- and NH4+ uptake, quantity of NO3- leached, total yield, and quantity of plant material harvested.
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How does increasing biomass left in the field affect acidity?
It increases acidity produced by microbial degradation of crop residues.
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How does soil type affect pH decline from fertilizer?
Shorter period of decline on sandy soil; longer period on clayey soil.
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How does duration of fertilizer application affect pH?
Longer period of application = greater pH decrease.
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What happens during liming regarding exchange sites?
Ca2+ replaces acids on exchange sites.
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What happens to Al3+ and H+ during liming?
They leave exchange sites to replace acid neutralized in solution.