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作 者:林利红[1] 韩晓日[1] 刘小虎[1] 战秀梅[1]
机构地区:[1]沈阳农业大学土地与环境学院,辽宁沈阳110161
出 处:《土壤通报》2006年第1期80-83,共4页Chinese Journal of Soil Science
基 金:辽宁省自然科学基金项目(972119)资助
摘 要:对沈阳地区棕壤定位试验地各施肥处理土壤按Hed ley等建议的分级方法进行测定。结果表明,棕壤磷中残留态含量最高,无机磷主要以NaOH-P i和HC l-P i形态存在,有机磷主要以NaOH-Po形态存在,NaHCO3-Po在各组分中所占比例最小。施用有机肥能明显增加潜在活性有机磷(NaOH-Po)的数量。1.0mol L-1HC l浸提的Ca-P i存在着缓慢的动态转化过程,是棕壤中的潜在磷源。Changes in inorganic and organic phosphorus fractions resulted from 24 years of long - term fertilization in Brown soil were studied by using a sequential extraction method. The results showed: Residual - P was the largest fraction of phosphate in Brown soil. NaOH - Pi and HC1 - Pi were the two main fractions of inorganic phosphorus, and NaOH - Po was the main form of organic phosphorus, proportion of NaHCO3 - Po was the smallest in all the fractions . Application of organic fertilizers could obviously raise the contents of the potentially labile organic fraction extracted by NaOH. Calcium associated inorganic phosphorus (Ca- Pi), extracted by HC1 was potential phosphorus, having a slow dynamic transformation process .
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