Fig. 2From: Effect of humic substances and clay minerals on the hydrosorption capacity of clay particles in meadow soils (Middle Priamurje, Far East of Russia)X-ray diffraction patterns of WDC (I) and AC (II). 1 Air-dry samples; 2 samples after solvation with ethylene glycol; 3 samples after incineration at 550 °C; a Ag horizon; b Elcg horizon; c Btg1 horizon. The peak numbers do not correspond to 2Θ values, but d spacing valuesBack to article page