Factors
in Acid Soils Detrimental to Plant Growth
Acid Soil
Complex -- plant growth problems at low pH are often multi-faceted.
1. ALUMINUM
toxicity.
Affects
plant roots Sparsely branched large diameter roots at low pH.
Tissue
levels of Al relate poorly to toxicity.
2. Manganese
toxicity.
Affects
plant tops. Occurs below pH 5.5. Cotton, soybean, and tobacco are
sensitive.
3. Iron
toxicity minor problem
4. Calcium
deficiency. Peanut, tobacco, and tomato are sensitive.
5. Magnesium
deficiency.
Conditions
that are conducive to Mg deficiency are:
1.
low CEC
2. use of low magnesium liming material
3. high rate of NH4+ fertilizer
4. high rate of K fertilizer
5. excessive leaching of soil profile
6. crops with high requirement for Mg -- tobacco, cotton, and soybean.
6. Molybdenum
deficiency (soybeans and cauliflower).
In most
cases liming to pH 5.5 to 6.0 alleviates Mo deficiency. In
some cases liming > 6.0 needed to eliminate Mo deficiency.
7. Nitrogen,
phosphorous, and sulfur deficiency because of slow organic matter decomposition
minor problem.
8. Reduced
phosphorous availability due to precipitation with aluminum.
9. Poor
nodulation of legumes.
|
|
Chemical
Formula
|
Rel.
Neutr. Value
|
Origin
|
Calcitic
limestone |
CaC03
|
90
- 100
|
Natural
deposits
|
Dolomitic
limestone |
CaC03:MgCO3
|
95
- 108
|
Natural
deposits
|
Hydrated
lime |
Ca(OH)2
|
120
- 135
|
Steam
burned
|
Burned
lime |
Ca0
|
150
- 175
|
Kiln
burned
|
Calcium
silicate |
CaSi03
|
30
- 60
|
Slag
|
Wood
ashes |
variable
|
40
- 85
|
Steam
boilers
|
Factors
Affecting Lime Reaction
Back
Relative
Neutralizing Value
Relative
ability of a liming material to neutralize acidity compared with pure
CaC03
Chemical
measure which:
reflects
chemical composition oxide, hydroxide, carbonates (handout)
level of impurities
Does
not necessarily relate to rate and extent of reaction in soil.
Fineness
The smaller
the particle the faster the reaction. (overhead)
Effective
calcium carbonate or neutralizing index. An attempt to integrate calcium
carbonate equivalence and fineness so that various liming materials
can be compared. (p. 254, note 8-2).
Lime
law (handout/overhead)
Chemical
Composition
Dolomite
particles are less reactive than calcitic.
"When
lime is required and soil test for magnesium is medium plus or above,
any source of lime may be used. When lime is required and soil test
magnesium is medium or less, use dolomitic limestone. The use of dolomitic
limestone every time the soil is limed will not result in magnesium
toxicity or cause a ration imbalance situation in the soils in South
Carolina." (Circular 476, p. 13)
Incorporation and Mixing
Expose
as much lime surface area to as much soil surface area as possible.
Time
and Frequency of Liming
At anytime
in the cropping sequence that soil pH is below the acceptable range.
Frequency
of liming is dependent on several factors.
1.
Neutralization by acid forming nutrient sources; particularly those
containing organic N, ammonium N, and ammonia N.
2.
Organic matter decomposition and carbon dioxide release.
3.
Leaching of basic cations.
4.
Removal of basic cations by crop harvesting.
5.
Erosion of topsoil, releaving acid subsoil behind.
6.
Acid rain.
|