What are soluble salts and how are they measured?
The term soluble salts
refers to the inorganic soil constituents (ions) that are dissolved in the
soil water. Pure water is a very poor conductor of electric current, whereas
water containing dissolved salts conducts current approximately in
proportion to the amount of salt present. Thus, measurement of the
electrical conductivity of a soil extract gives an indication of the total
concentration of soluble salts in the soil. The electrical conductivity
measurement is usually reported in units of millimhos per centimeter (mmhos/cm),
although some labs report decisemens per meter (dS/m). One decisemen per
meter is equal to one mmhos/cm.
Why are they important?
Soluble salt levels in
the soil are important, because high soluble salts can reduce water uptake
by plants, restrict root growth, cause burning of the foliage, inhibit
flowering, and limit fruit and vegetable yields. Sensitivity to soluble
salts differs among plant species/cultivars and their stage of growth. Seed
germination and seedling growth are more sensitive to salt stress than the
growth of mature plants, so greenhouse growers routinely test their growing
media for soluble salt levels. A soluble salt test can be useful when
investigating the cause of poor plant growth, determining the suitability of
a new planting site, or monitoring the quality of "black dirt" for use on
landscaped areas.
Where
do they come from?
Excessive rates of
fertilizer application and placing fertilizer too close to seeds or plant
roots creates soluble salt problems. Pet urine and feces can increase
soluble salts in localized areas resulting in plant damage or death. The use
of deicing salts (primarily in the form of sodium chloride) on streets and
sidewalks frequently results in high soluble salt levels in adjacent areas
that restrict the growth of turfgrass, flowers, and shrubs.
Correcting Soluble Salt
Problems
Salts can be leached out
of soil with salt-free water, and rain will naturally reduce soil salt
levels in time. In soils where internal
drainage is poor, prevention may be the only feasible approach for reducing
salt problems. In well-drained soils, incorporation of gypsum (calcium
sulfate) at the rate of 10 to 15 lbs.100 sq. ft. followed by leaching with
good quality water can be an effective means of correcting soluble salt
problems. Gypsum is most effective in situations where sodium is the cause
of high soluble salts. High levels of sodium in the soil will tend to
disperse soil particles resulting in poor soil structure and making water
infiltration difficult. The calcium in gypsum will displace sodium and the
sodium will then move (leach) out of soil profile with irrigation water
and/or rainfall. Soils high in calcium have better structure than those high
in sodium. Use of gypsum on soils where sodium is not high has generally not
been shown to be effective in improving soil structure. Thus, on low sodium
soils, topdressing lawns with gypsum is not an effective way to improve soil
structure and therefore not a recommended practice.