[Aluminum dissolution and changes of pH in soil solution during sorption of copper by aggregates of paddy soil].
Size fractions of soil aggregates in Lake Tai region were collected by the low-energy ultrasonic dispersion and the freeze-desiccation methods. The dissolution of aluminum and changes of pH in soil solution during sorption of Cu2+ and changes of the dissolution of aluminum at different pH in the solution of Cu2+ by aggregates were studied by the equilibrium sorption method. The results showed that in the process of Cu2+ sorption by aggregates, the aluminum was dissoluted and the pH decreased. The elution amount of aluminum and the decrease of pH changed with the sorption of Cu2+, both increasing with the increase of Cu2+ sorption. Under the same conditions, the dissolution of aluminum and the decrease of pH were in the order of coarse silt fraction > silt fraction > sand fraction > clay fraction, which was negatively correlated with the amount of iron oxide, aluminum and organic matter. It suggested that iron oxide, aluminum and organic matters had inhibitory and buffering effect on the aluminum dissolution and the decrease of pH during the sorption of Cu2+.
Hai-Bo
HB
Xu
Dao-Yuan
DY
Zhao
Chao
C
Qin
Yu-Jiao
YJ
Li
Chang-Xun
CX
Dong
D000327:Adsorption; D000535:Aluminum / Q000737:chemistry*; D000538:Aluminum Silicates; D000077215:Clay; D003300:Copper / Q000737:chemistry*; D005290:Ferric Compounds; D006863:Hydrogen-Ion Concentration; D012275:Oryza; D012822:Silicon Dioxide; D012987:Soil / Q000737:chemistry*; D012995:Solubility
D000538:Aluminum Silicates; D005290:Ferric Compounds; D012987:Soil; C000499:ferric oxide; D012822:Silicon Dioxide; D003300:Copper; D000535:Aluminum; D000077215:Clay