The Chemistry of Salinity in Soils Naomi Waissman Assadian Texas A&M Research and Extension Center at El Paso September 4, 2002
Introduction Salinity concentrations in soils have profound effects on soil properties Poor drainage, nutrient deficiencies, and crop toxicity Factors in soil salinity include: Arid climates Erosion of primary minerals Saline irrigation and drainage waters High water table High potential Evapotranspiration Additions of inorganic and organic fertilizers Sludges and sewage effluents 2
The term Salinity refers to the presence of the major dissolved inorganic solutes, essentially Na +, Mg 2+, Ca 2+, K +, Cl, SO 2 4, HCO 3, CO 2 3 SSSA BOOK SERIES: 5, METHODS OF SOIL ANALYSIS PT 3 CHEMICAL METHODS. (It could also include NH 4+, NO 3, PO 4, and charged organic particles in aqueous (soil) samples when determined by electrical conductance) 3
Dissolved Solids (Salts) Intensity Factor salt concentration in soil solution Capacity Factor the ability of solid phases to replenish elements as it is depleted from solution 4
5
Salt Measurement Intensity Factor Electrical Conductance EC Electrical current carried by a salt solution. EC increases as salt concentrations increase. Soil Characteristics ph is generally below 8.5 EC is more than 4 ds/m 6
Calculations Total Dissolved Solids=(~640)(EC) Ionic Strength= (0.013)(EC)=Σc i Z 2 Single-Ion Activity α j =γ j m j m=molar concentration Extended Debye Huckle Equation (estimate activity coefficients) Logγ=-AZ 2 [(I) 1/2 /(1+Bå(I) 1/2 )] A=0.512 for water @ 25 o C, B~0.33 in water @ 25 o C å=adjustable parameter corresponding to ion size and charge (6) 7
Factors Affecting Salt Dissolution Salt Effect or Ionic Strength Effect Addition of an inert salt can increase the solubility of an ionic compound Added NaCl can increase CaSO 4 dissolution Increased ionic strength affects ph Ion pairing effect Weak bonds between hydrated ions Common Ion Effect a salt will be less soluble if one of its constituent ions is already present in the solution 8
Osmotic Potential (kpa) =40EC 9
The Physiochemical EffectThe + + Electric Double Layer + + + ++ + Na Ca 2+ + + + + + (Soil solution) 10
Sodium Adsorption Ratio (SAR): Defined as being related to the adsorption of sodium by the soil SAR=Na + / (Ca ++ +Mg ++ )/2 Na +, Ca ++, and Mg ++ in milliequivalent/l (Allison, 1954) Sodicity occurs when the ratio of sodium is much higher to that of other soluble salts. Soil Characteristics ph ranges between 8.5 to 10, ESP>15 Plastic and sticky when wet, forming hard clods and crusts Impermeable to all water. Impermeable to all water. Specific Ion Effect Na ion can be inhibitory to certain plant processes 11
Surface Salt Pattern Low salt accumulation Moderate salt accumulation High salt accumulation Very high salt accumulation 12
Current Research 13
Study #1 Salt conc. (mg/kg) 40000 30000 20000 10000 0 Salt conc. vs. Extraction Ratios-Aerobically Digested Sludge paste 1:5 1:10 1:25 1:50 Extraction ratios Ca K Mg Na salt conc. (mg/kg) 2500 2000 1500 1000 500 0 Salt Conc. vs Extraction Ratios-Anerobically Digested Sludge K Mg Na paste 1:5 1:25 1:50 ratio Ca 14
Extraction Ratio's impacts on EC-Aerobically Digested Sludge EC (ds) 12 10 8 6 4 2 0 paste 1:5 1:10 1:25 1:50 Extraction Ratio Sodium Adsorption Ratio-Aerobically Digested Biosolids SAR, ratio 7 6 5 4 3 2 1 0 paste 1:5 1:10 1:25 1:50 Extraction Ratio 15
Log of Soluble (Ca) y = -0.5248x + 6.7474 R 2 = 0.6891 8.60 8.50 8.40 8.30 8.20 ph 8.10 Study #2 8.00 7.90 7.80 7.70-3.300-3.100-2.900-2.700-2.500-2.300-2.100-1.900-1.700-1.500 Log (Ca) 7.60 16
Study #3 - Objectives Determine if minimum tillage is possible on irrigated soils with a high potential for salt hazard. Determine if biosolids remediate accumulation of salts at the soil surface. Evaluate the impact of ammonium on soil salinity. 17
Treatment Design Tillage Maximum Minimum Soil Texture Ge Glendale silty clay loam. Gs Glendale silty clay. Hs Harkey silty clay loam. Tg Tigua silty clay. Subplots Bed Row Position Furrow Side Top Center 18
Minimum versus Maximum Tillage 7 6 5 4 3 2 1 0 EC Min v Max Tillage Tillage Max. Tillage Min. June July August December 120 100 80 60 NH 4 + Content - Min v Max Tillage Tillage Max. Tillage Min. 40 20 0 June July August December 19
Soil Texture 120 100 NH4+ Content - Soil Texture 12 10 8 EC- Soil Texture Ge Gs Ha Tg 80 60 40 20 Ge Ha Gs Tg E C, d S / m 6 4 0 June July August December 2 0 June July August December 20
Furrow Position EC, ds/m 7 6 5 4 3 2 1 0 EC Furrow Position Furrow Side Top Center Top Depth 120 100 80 60 40 NH 4 + Content - Furrow Position Furrow Side Top Center Top Depth nh4+, mg/kg June July August December 20 0 June July August December 21
The Future in the Upper Rio Grande Basin 22
Potential Salt Management Strategies Develop a consistent and detailed salt monitoring program Miyamoto and Iglesias Crop Selection Halophytes Miyamoto and USSL Pretreatment of alternative water sources for irrigation Relatively new, site-specific Irrigation delivery systems Enciso Integrated Soil Management to maintain soil structure and permeability (organic enrichment) 23