长期施肥后简育湿润均腐土中磷素形态特征的研究
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*中国科学院知识创新工程项目(KZCX2-413-3);国家重点基础研究发展计划(973计划)(2005CB121108);国家自然科学基金重大项目(30390080)资助


FORMS OF PHOSPHORUS IN HAPLI-UDIC ISOHUMOSOLS SOILS AFTER LONG-TERM FERTILIZATION
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    摘要:

    对黑土(简育湿润均腐土)长期定位施肥15年后土壤磷素形态进行分析研究.结果表明:土壤中积累的Al-P、Ca2-P量与施磷量成正相关;只施NK能促进植物对Ca8-P的吸收;闭蓄态磷(Oc-P)含量均较低.施磷肥能增加黑土Fe-P含量,却未能增加Ca10-P含量.黑土各形态无机磷的含量大小顺序为:Fe-P>Ca10-P>Al-P>Ca8-P>Ca2-P>Oc-P.施磷能增加土壤中有机磷(O-P)的含量,但不能增加土壤有机质含量.土壤有机质含量均有不同程度的下降.本试验黑土中施入N112.5kghm-2a-1和P20kghm-2a-1能保持土壤中无机磷(I-P)平衡.

    Abstract:

    Change in forms of phosphorus in a typical Hapli-Udic Isohumosols(black soil) under a 15-year long-term fertilization experiment was studied.Results show that accumulation of soil Al-P and Ca2-P was positively related to P application rate;application of NK stimulated the plant to absorb Ca8-P;and the concentration of Occluded-P(Oc-P) was decreased.P application did increase the content of Fe-P in the black soil,but did not the content of Ca10-P.In terms of content in the black soil,the various forms of in-organic P were in the order of Fe-P>Ca10-P>Al-P>Ca8-P>Ca2-P>O-P.P fertilizer application increased organic P in the soil,but it did not increase the content of organic matter.Instead,the content of organic matter dropped to a varying degree in different treatments.Application of N 112.5 kg hm-2 a-1and P 20 kg hm-2 a-1 could keep I-P in balance in the soil.

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林德喜,范晓晖,胡锋,杨林章,韩晓增.长期施肥后简育湿润均腐土中磷素形态特征的研究[J].土壤学报,2006,43(4):605-610. DOI:10.11766/200504110411 Lin Dexi, Fan Xiaohui, Hu Feng, Yang Linzhang, Han Xiaozeng. FORMS OF PHOSPHORUS IN HAPLI-UDIC ISOHUMOSOLS SOILS AFTER LONG-TERM FERTILIZATION[J]. Acta Pedologica Sinica,2006,43(4):605-610.

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  • 收稿日期:2005-04-11
  • 最后修改日期:2005-12-26
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  • 在线发布日期: 2013-02-25
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