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Main Cycle
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Cl- cycling in soils
Plant and Animal
residues
Atmospheric
ClPlant
Primary
and
Secondary
Cl
minerals
Dissolution
Precipitation
Uptake
Soil Solution
ClMineralization
Immobilization
Adsorption
Adsorbed
or labile
Cl-
Desorption
Leaching
Soil
Organic
matter
Main Cycle
More Info
Cl- cycling in soils
Plant and Animal
residues
Atmospheric
ClPlant
Primary
and
Secondary
Cl
minerals
Dissolution
Precipitation
Uptake
Soil Solution
ClMineralization
Immobilization
Adsorption
Adsorbed
or labile
Cl-
Desorption
Leaching
Soil
Organic
matter
Main Cycle
More Info
Cl- cycling in soils
Plant and Animal
residues
Atmospheric
ClPlant
Primary
and
Secondary
Cl
minerals
Dissolution
Precipitation
Uptake
Soil Solution
ClMineralization
Immobilization
Adsorption
Adsorbed
or labile
Cl-
Desorption
Leaching
Soil
Organic
matter
Main Cycle
More Info
Cl- cycling in soils
Plant and Animal
residues
Atmospheric
ClPlant
Primary
and
Secondary
Cl
minerals
Dissolution
Precipitation
Uptake
Soil Solution
ClMineralization
Immobilization
Adsorption
Adsorbed
or labile
Cl-
Desorption
Leaching
Soil
Organic
matter
Main Cycle
More Info
Cl- cycling in soils
Plant and Animal
residues
Atmospheric
ClPlant
Primary
and
Secondary
Cl
minerals
Dissolution
Precipitation
Uptake
Soil Solution
ClMineralization
Immobilization
Adsorption
Adsorbed
or labile
Cl-
Desorption
Leaching
Soil
Organic
matter
More Information on Chloride
Form taken up by plants:
Deficiency symptoms:
Mobility in soil:
Effect of pH on availability:
Mobility in plant:
Origins of Cl in soil and plants:
Role of nutrient in plant growth:
Fertilizer Sources:
Role in microbial growth:
Behavior in soil:
Interactions of Cl:
Accumulations of Cl in soil:
Effects:
Concentration in plants:
Forms in soil:
Main Cycle
References:
Other:
Toxicity Symptoms:
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Main Cycle
Form taken up by plants
ClMobility in Soil
Mobile
Mobility in plant
Mobile
Effect of pH on availability:
Non adsorbed at pH >7
Non specific adsorption pH <7
No effect on availability
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Main Cycle
Role of nutrient in plant growth:
Stimulates splitting of water in photosynthesis, essential for roots, cell
division in leaves and as an osmotically active solute.
Winter Wheat: Suppresses take-all, stripe rust, tan spot.
Wheat: Suppresses leaf rust and tan spot.
Oats: Suppresses leaf rust
Corn: Suppresses stalk rot
Role in microbial growth:
Unknown
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Main Cycle
Interactions with other nutrients:
Uptake of NO3 and SO4 can be reduced by the competitive effects of
Cl. Lower protein concentrations in winter wheat are attributed to strong
competitive relationships between Cl and NO3 when Cl levels are high.
Negative interaction between Cl and NO3 has been attributed to
competition for carrier sites at root surfaces.
Fertilizer Sources:
Source
%Cl
Ammonium Chloride
66
Calcium Chloride
65
Potassium Chloride
47
Magnesium Chloride
74
Sodium Chloride
60
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Main Cycle
Concentration in plants:
Normal concentration is 0.2 - 2.0 % of dry matter. Cereal grain
concentrations are 10-20 ppm, sugarbeet leaves 100-200 ppm.
Tobacco plants require concentrations in soil of 10-15 ppm. <70-700
ug/g in tissue is deficient.
Deficiency symptoms:
pH unknown. Reduced growth, wilting, development of necrotic and
chlorotic spots on leaves, with leaves eventually attaining a bronze
color. Roots become stunted in length but thickened or club shaped
near the tips. Acts as a counter ion during rapid K+ fluxes, contributes
to turgor of leaves. Deficiency occurs in soils, <2ppm.
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Main Cycle
Behavior in Soil
Cl anion is very soluble in most soils. It is rapidly cycled through soil systems
due to mobility (except in extremely acid soils). Exchangeable Cl can occur in
acid, kaolinitic soils which have pH dependent positive charges. In humid climate
zones Cl is leached through the soil system and in Arid to Semi-arid zones it is
concentrated in the soil horizon.
Origins of Cl in Soil and Plants:
Most Cl in soil comes from salt trapped in parent material, marine aerosols, and
volcanic emissions. Most often found in apatite, hornblende, and some
feldspars. Nearly all soil Cl has been in the oceans at least once and returned
to land by uplift and subsequent leaching of marine sediments or by oceanic salt
spray carried in rain or snow. Sea spray near coastal regions provides about
100 kg/ha/yr and for inland regions accumulations are 1-2 kg/ha/yr. For inland
regions these amounts are adequate since no deficiencies have been reported.
Salt droplets and dust particles can be absorbed by plant leaves in adequate
amounts for plant requirements.
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Accumulations of Cl in soils:
Accumulates where internal drainage of soils is restricted and in
shallow groundwater where Cl can move by capillary action into the
root zone and be deposited at or near the soil surface.
Effects: Primary effect is an increase of osmotic pressure of soil water
and thereby lowers the availability of water to plants.
Forms in Soil:
Most Cl exists as soluble salts of NaCl, CaCl2, or MgCl2.
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Toxicity Symptoms:
pH unknown. Can reduce yield and quality of crops. High levels will
increase total leaf water potential and cell sap osmotic potential in wheat.
Improves moisture relations in some crops. Leaves of tobacco and
potatoes become thickened and tend to roll when excessive Cl
concentrations occur. Storage quality of potato tubers are adversely
affected by surplus uptake of Cl.
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Other:
In recent years water softening, industrial brines, and road deicing have
contributed significant amounts of Cl to local areas. Irrigation water that
is highly mineralized, salt water spills associated with extraction of oil,
natural gas, some coal deposits and improper disposal of feedlot wastes
can supply Cl to soil. Wind erosion of salt evaporates can also affect
enrichment of soils.
Main Cycle
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References
Bohn, H.L., B.L. McNeal and G.A. O’Connor. 1979. Soil Chemistry, WileyInterscience, New York, 219, 232, 286 pp.
Pendias-Kabata, Alina and Henryk Pendias. 1992. Trace Elements in Soils and
Plants. 2nd ed. CRC Press, Florida, 251-252pp.
Salisbury, Frank B. and Cleon W. Ross. 1992. Plant Physiology, 4th ed. Wadsworth
Inc., California, 120, 129, 133, 135, 148, 215, 217 pp.
Tisdale, S.L., W.L. Nelson, J.D. Beaton and J.L. Havlin. 1993. Soil Fertility and
Fertilizers. 5th ed. Macmillan, New York, 73-75, 342-344 pp.
Authors: David Gay, Justin Carpenter, Mark Wood, Curt Woolfolk and J. Clemn
Turner
Main Cycle
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Chloride Crop Nutrition
Nutrient Cycles
Main Cycle
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**A Great Resource**
Chlorine Cycle
Air pollution
Atmosphere
Ocean
CH3 Cl
Dry fallout
Cl2
CFC’s
(Sea Spray)
Cl- cycling in soils
Atmospheric
Biomass Burning
Volcanic emissions
HClO
Precipitation
Plants
Road salts, Feedlots,
Irrigation water
Industrial wastewater
ClWind erosion of
salt evaporates
Soil
Municipal water
NaCl
(Drinking + Swimming)
Parent material
MgCl2 CaCl2
Negligible addition
Fertilizers
Plastics
(PVC-polyvinyl chloride)
Runoff
8 kg/ha/hr
Leaching
AEC
only in
acid soils
KCl
0-0-62
47% Cl-
Air Pollution
CFC’s
Ocean
(sea spray)
Chlorine Cycle
Soils
Atmosphere
Biomass Burning
Precipitation
Plants
Cl-
Road Salts, Feedlots,
Irrigation Water,
Industrial Wastewater
Wind Erosion of
Salt Evaporates
Soil
Municipal Water
NaCl MgCl2 CaCl2
Runoff
Plastics
Volcanic Emissions
Parent Material
Leaching
Fertilizers