A new inorganic phosphorus (IP) fractionation scheme developed by Jiang and Gu was used in an incubation experiment to investigate the transformation of applied P in a calcareous fluvisol. The results show that after ...A new inorganic phosphorus (IP) fractionation scheme developed by Jiang and Gu was used in an incubation experiment to investigate the transformation of applied P in a calcareous fluvisol. The results show that after addition of common superphosphate (CSP), the Ca2-P in the soil decreased gradually and transformed largely to the less available Fe-P, Al-P and Ca8-P, rather than to the unavailable forms of Ca10-P and O-P. The different IP fractions ranked in the following order with respect to the increment by addition of CSP after 120 days of incubation: Fe-P> Al-P>Ca8-P>Ca2-P. After addition of pig manure, the content of Ca2-P in the soil increased rapidly at first and then decreased slowly, and the amount of different IP fractions accumulated after 120 days of incubation ranked in the following order: Ca2-P > Fe-P > Ca8-P > Al-P. Evidently, the variation in content of Ca2-P and the order of increase in different IP fractions in incubation induced by application of pig manure were quite different from that of CSP. The increase in IP fractions in the incubation of broad bean green manure (BBGM)for 120 days was in the rank of Fe-P > Ca2-P > Ca8-P > Al-P; but because organic phosphorus (OP) of BBGM degraded relatively slowly, the increment in IP fractions was lower than that of pig manure. Wheat straw was difficult to mineralize and induced a strong biological fixation of soil P, resulting in a decrease of the content of Ca2-P, even Ca8-P, Fe-P and Al-P.展开更多
文摘A new inorganic phosphorus (IP) fractionation scheme developed by Jiang and Gu was used in an incubation experiment to investigate the transformation of applied P in a calcareous fluvisol. The results show that after addition of common superphosphate (CSP), the Ca2-P in the soil decreased gradually and transformed largely to the less available Fe-P, Al-P and Ca8-P, rather than to the unavailable forms of Ca10-P and O-P. The different IP fractions ranked in the following order with respect to the increment by addition of CSP after 120 days of incubation: Fe-P> Al-P>Ca8-P>Ca2-P. After addition of pig manure, the content of Ca2-P in the soil increased rapidly at first and then decreased slowly, and the amount of different IP fractions accumulated after 120 days of incubation ranked in the following order: Ca2-P > Fe-P > Ca8-P > Al-P. Evidently, the variation in content of Ca2-P and the order of increase in different IP fractions in incubation induced by application of pig manure were quite different from that of CSP. The increase in IP fractions in the incubation of broad bean green manure (BBGM)for 120 days was in the rank of Fe-P > Ca2-P > Ca8-P > Al-P; but because organic phosphorus (OP) of BBGM degraded relatively slowly, the increment in IP fractions was lower than that of pig manure. Wheat straw was difficult to mineralize and induced a strong biological fixation of soil P, resulting in a decrease of the content of Ca2-P, even Ca8-P, Fe-P and Al-P.
