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Dependence of Zeta Potential and Soil Hydraulic Conductivity on Adsorbed Cation and Aqueous Phase Properties

^a Faculty of Agriculture, Dep. of Soil Science, Mustafa Kemal Univ., Antakya, 31040 Turkey
^b Arid Land Research Center, Tottori Univ, 1390 Hamasaka, Tottori, 680-0001 Japan

View larger version (30K): [in a new window]   Fig. 1. Schematic diagram of electrophoresis apparatus (U-tube).

View larger version (21K): [in a new window]   Fig. 2. Variation of electrophoretic mobility (EM) and corresponding zeta potential (p ) of Ariake soil (AS) and Kzyl-Orda soil (KS) clays as a function of Na percentage (the complementary ion was Ca).

View larger version (19K): [in a new window]   Fig. 3. Effect of pH on electrophoretic mobility (EM) and corresponding zeta potential (p) of Ariake soil (AS) and Kzyl-Orda soil (KS) clay particles in 0.01 M NaCl-treated suspensions.

View larger version (22K): [in a new window]   Fig. 4. Electrophoretic mobility (EM) and corresponding zeta potential (p) of Ariake soil (AS) and Kzyl-Orda soil (KS) clays versus electrolyte concentration of NaCl.

View larger version (16K): [in a new window]   Fig. 5. Hydraulic conductivity versus exchangeable sodium percentage for Ariake (AS) and Kzyl-Orda (KS) clay/sand mixtures (distilled water was applied to columns).

View larger version (15K): [in a new window]   Fig. 6. Hydraulic conductivity as a function of pH for Ariake (AS) and Kzyl-Orda (KS) Na-clay/sand mixtures under 0.01 M NaCl solution.

View larger version (15K): [in a new window]   Fig. 7. Hydraulic conductivity versus electrolyte concentration of NaCl for Ariake (AS) and Kzyl-Orda (KS) clay/sand mixtures at exchangeable sodium percentage 100.

View larger version (22K): [in a new window]   Fig. 8. Relationship between zeta potential (p ) of clay particles and hydraulic conductivity of clay/sand mixtures for Ariake (AS) and Kzyl-Orda (KS) samples.