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Appendix

Appendix 1. Water Quality Tests, Units of Measure, and Conversions
Test Units of Measurement Symbol Multiply To Convert to Symbol
Water Salinity
a. electrical conductivity (ECw)
millimhos per centimeter mmhos/cm 1 deciSiemens per meter dS/m
millimhos per centimeter mmhos/cm 1000 µmhos/cm Moderate to Severe
Siemens per meter S/m 10 deciSiemens per meter dS/m
microSiemens per centimeter µS/cm 1 micromhos per centimeter µmhos/cm
Water Salinity
b. total dissolved salts (TDS)(1)(2)
milligrams per liter mg/l 1 parts per million ppm
percent % 10000 parts per million ppm
percent % 10000 milligrams per liter mg/l
Water Sodium Hazard
a. sodium adsorption ratio (SAR) (3)
NA NA      
Water Sodium Hazard
b. percentage
NA NA      
Specific Ion Toxicity milliequivalents per liter meq/l(4) See A.    

(1)To approximate TDS, multiply ECw X 640 if the EC value <5 dS/m
(2)To approximate TDS, multiply ECw X 800 if the EC value >5 dS/m
(3)The SAR value for water with significant amounts of bicarbonate needs to be adjusted.
(4)meq/l equals mg/l divided by the equivalent weight were equivalent weight equals atomic weight divided by atomic charge.

Appendix 2. Specific Ion Charges, Atomic Weights, and Equivalent Weights
Ion

Symbol

Charge (Valence) Atomic Weight Equivalent Weight
calcium CA ++ +2 40.1 20.05
magnesium Mg ++ +2 24.3 12.15
sodium Na + +1 23.0 23.00
chloride Cl - -1 35.3 35.30
sulfate SO 4 -- -2 96.1 48.00
carbonate CO 3- - -1 60.0 30.00
bicarbonate HCO 3 - -1 61.0 61.00


Appendix 3. Multiplication Factors for Converting between ppm and meq/l
Salt Ion Symbol ppm to meq/l
Multiply ppm value by:
meq/l to ppm
Multiply meq/l by:
calcium CA ++ 0.050 20
magnesium Mg ++ 0.083 12
sodium Na + 0.043 23
chloride Cl - 0.029 35
sulfate SO 4 -- 0.021 48
carbonate CO 3- - 0.033 30
bicarbonate HCO 3 - 0.016 61
Appendix 4. Classification of Irrigation Waters, USDA Agriculture Handbook 60

Low Salinity Water (C1) can be used for irrigation of most crops with little likelihood that soil salinity will develop. Some leaching is required, but this occurs under normal irrigation practices except in soils of extremely low permeability.

Medium Salinity Water (C2) can be used if a moderate amount of leaching occurs. Plants with moderate \salt tolerance can be grown in most cases without special practices for salinity control.

High Salinity Water (C3) cannot be used on soils with restricted drainage. Even with adequate drainage, special management for salinity control may be required, and plants with good salt tolerance should be selected.

Very High Salinity Water (C4) is not suitable for irrigation under ordinary conditions, but may be used occasionally under very special circumstances. The soils must be permeable, drainage must be adequate, irrigation water must be applied in excess to provide considerable leaching, and very salt-tolerant crops should be selected.

Low Sodium Water (S1) can be used for irrigation on most soils with little danger of the development of harmful levels of exchangeable sodium. However, sodium-sensitive crops such as stonefruit trees and avocados may accumulate injurious concentrations of sodium.

Medium Sodium Water (S2) will present an appreciable sodium hazard in fine-textured soils having high cation exchange capacity, especially under low leaching conditions, unless gypsum is present in the soil. This water may be used on coarse-textured soils or organic soils with good permeability.

High Sodium Water (S3) may produce harmful levels of exchangeable sodium in most soils and will require special soil management – good drainage, high leaching, and organic matter additions. Gypsiferous soils may not develop harmful levels of exchangeable sodium from such waters. Chemical amendments may be required for replacement of exchangeable sodium, except that amendments may not be feasible with waters of very high salinity.

Very High Sodium Water (S4) is generally unsatisfactory for irrigation purposes except at low and perhaps medium salinity, where the solution of calcium from the soil or use of gypsum or other amendments may take the use of these waters feasible.

Sometimes the irrigation water may dissolve sufficient calcium from the calcareous soils to decrease the sodium hazard appreciably, and this should be taken into account in the use of C1-S3 and C1-S4 waters. For calcareous soils with high pH values or non-calcareous soils, the sodium status of water in classes C1-S3, C1-S4, and C2-S4 may be improved by the addition of gypsum to the water. Similarly, it may be beneficial to add gypsum to the soil periodically when C2-S3 and C3-S2 waters are used.

Source: Agriculture Handbook 60, U.S. Department of Agriculture.

For more information visit the Plant Materials Program website.

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Last Modified: 08/21/2008