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草业学报 ›› 2014, Vol. 23 ›› Issue (6): 61-68.DOI: 10.11686/cyxb20140608

• 论文 • 上一篇    下一篇

不同种植年限紫穗槐根际非根际土壤磷组分含量特征

李金辉,卢鑫,周志宇*,赵萍,金茜,周媛媛   

  1. 草地农业生态系统国家重点实验室 兰州大学草地农业科技学院,甘肃 兰州730020
  • 收稿日期:2012-09-07 出版日期:2014-12-20 发布日期:2014-12-20
  • 通讯作者: E-mail:zyzhou@lzu.edu.cn
  • 作者简介:李金辉(1986-),女,甘肃武威人,在读硕士
  • 基金资助:
    国家科技支撑计划资助项目(2007BAD80B05)和国家自然科学基金项目(31201849)资助

Phosphorus contents in the rhizosphere and bulk soil under Amorpha fruticosa established in different years

LI Jin-hui,LU Xin,ZHOU Zhi-yu,ZHAO Ping,JIN Qian,ZHOU Yuan-yuan   

  1. State Key Laboratory of Grassland Agro-ecosystems, College of Pastoral AgricultureScience and Technology, Lanzhou University, Lanzhou 730020, China
  • Received:2012-09-07 Online:2014-12-20 Published:2014-12-20

摘要: 以不同种植年限的紫穗槐根际和非根际土壤为试验对象, 采用Tiessen等修正后的Hedley土壤磷素分级方法,对其有效磷、全磷及不同形态磷组分进行了分析研究。结果表明,不同年限根际土壤有效磷含量均高于非根际土壤。从无机磷含量特征可以看出除了H2O-Pi(水溶磷)和Conc.HCl-Pi(浓 HCl提取无机磷)外,其余无机磷均是Y60的含量最高。不同形态磷:除Y28的NaHCO3-Po(0.5 mol/L NaHCO3提取有机磷)外,其他株龄的NaHCO3-Pi(0.5 mol/L NaHCO3提取无机磷),NaOH-Pi(0.1 mol/L NaOH提取无机磷),NaHCO3-Po,NaOH-Po(0.1 mol/L NaOH提取有机磷),Conc.HCl-Po(浓 HCl提取有机磷)含量均是根际高于非根际土壤相应磷指标含量。根际土壤有效磷与Dil.HCl-Pi和Conc.HCl-Po含量显著相关(P<0.05),H2O-Pi与Total-P含量显著相关(P<0.05),根际和非根际土壤有效磷与pH值和根际全磷含量相关性均不显著(P>0.05)。

Abstract: The rhizosphere and bulk soil of Amorpha fruticosa established in different years were studied. Available phosphorus (P), total P and P fractions were analysed using the method of Hedley which was a soil P classification method revised by Tiessen. Available P levels in the rhizosphere were higher than those out of the rhizosphere. The Y60 had the highest inorganic P content than the other except for H2O-Pi and Conc. HCl-Pi. The NaHCO3-Pi, NaOH-Pi, NaHCO3-Po, NaOH-Po, and Conc. HCl-Po in the rhizosphere were higher than those in bulk soil in different aged Amorpha except for NaHCO3-Po in Y28. Available P in the rhizosphere had a significant relationship with Dil. HCl-Pi and Conc. HCl-Po. H2O-Pi and total P had a significant relationship. Available P and pH in the rhizosphere and out of the rhizosphere did not have a significant relationship with total P in the rhizosphere.

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