Kinetics of Dissolution of Phosphate Rock, Partial Acidulated Phosphate Rock and Tri Super Phosphate in Calcareous Soil

被引:0
|
作者
Al-Rubaye, M. A. [1 ]
Nasir, K. M. [1 ]
Munaf, D. F. [1 ]
机构
[1] Baghdad Univ, Coll Agr, Dept Soil Sci & Water Resources, Baghdad, Iraq
关键词
Elovich equation; rate of p release constant (Kd); Bach equilibrium technique;
D O I
暂无
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
A study was conducted to evaluate kinetics of phosphorus release from dissolution of phosphate rock (PR), partial acidulated phosphate rock (40%-PAPR) and tri super phosphate (TSP) in calcareous soil by using Batch equilibrium technique for five incubation times. The water soluble phosphorus was measured at end of each incubation times. Six kinetic equations were tested to know which one is the best in description of phosphorus release to soil. The results showed that were gradual increases in the released p from the dissociated 40%-PAPR and TSP. Liberation of p from phosphate rock was so weak with time. The accumulated amount of the released phosphorus at end of incubation time (720h.) was higher in TSP. The phosphorus release curves showed good liberation of phosphorus in PAPR and TSP. The Elovich equation was the best in explaining successfully phosphorus release and the rate of phosphorus release constant (kd) values were 4.38 h(-1) and 15.11 h(-1) in PAPR and TSP respectively.
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页码:886 / 890
页数:5
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