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草业学报 ›› 2009, Vol. 18 ›› Issue (4): 111-116.

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甘肃永昌县放牧草地土壤脲酶活性与土壤肥力的关系初探

侯彦会1,周学辉2,焦婷1,刘荣堂1*,李兴福3   

  1. 1.甘肃农业大学草业学院,甘肃 兰州 730070;
    2.中国农业科学院兰州畜牧与兽药研究所,甘肃 兰州 730050;
    3.永昌县农业局,甘肃 永昌 737200
  • 收稿日期:2008-09-27 出版日期:2009-08-20 发布日期:2009-08-20
  • 作者简介:侯彦会(1982-),男,山东泰安人,在读硕士。E-mail: houyanhui1983@163.com
  • 基金资助:
    世界银行全球环境基金(GEF)项目(052456 CHA-GS-Y-2)资助。

A preliminary study on the relationship between soil urease activity and soil fertility in the grazing grasslands of Yongchang county, Gansu province

HOU Yan-hui1, ZHOU Xue-hui2, JIAO Ting1, LIU Rong-tang1, LI Xing-fu3   

  1. 1.College of Pratacultural Science, Gansu Agricultural University, Lanzhou 730070, China; 2.Lanzhou
    Institute of Animal Science and Veterinary Pharmaceutics Science of Chinese Academy
    of Agricultural Science, Lanzhou 730050, China; 3.Farming Office of
    Yongchang County, Yongchang 737200, China
  • Received:2008-09-27 Online:2009-08-20 Published:2009-08-20

摘要: 2007-2008年对甘肃永昌县放牧草地土壤脲酶活性与土壤肥力因子之间的关系进行了初步研究。结果表明,2种放牧草地土壤脲酶活性不同,土壤剖面中脲酶活性的变化趋势是表层明显高于下层。土壤脲酶活性与有机质、全氮、速效氮、速效钾呈极显著正相关,与土壤pH值呈极显著负相关。通径分析结果表明,土壤肥力因子对脲酶活性的直接作用系数大小顺序为全氮>速效钾>速效氮>速效磷>pH值>有机质。有机质对脲酶活性的直接效应较小,主要通过全氮表现为较强的间接效应。全氮对脲酶活性具有显著的直接效应。土壤速效氮、速效磷和速效钾对脲酶活性的直接作用不大,主要通过全氮对脲酶活性产生间接影响。土壤pH值对脲酶活性所起的直接效应和间接效应均较小,不是影响土壤脲酶活性的主要因素。

Abstract: The relationship between soil urease activity and soil fertility in the grazing grasslands of Yongchang county of Gansu province was studied from 2007 to 2008. There were significant differences in the urease activities of different grazing grasslands, and these activities were more intense in the surface layer than in the deeper layers. The soil urease activities showed significant positive correlations with organic matter content, total nitrogen, available nitrogen, and available potassium, but a significant negative correlation with soil pH value. Path analysis showed that the sequence of soil fertilities based on their direct acting coefficients to soil urease activity was: Total nitrogen>available potassium>available nitrogen>available phosphorus>soil pH value>organic matter. The organic matter does not affect urease activities directly, but acts indirectly through its effect on total nitrogen. Total nitrogen directly affects urease activity. Other factors like soil available nitrogen, available phosphorus, and available potassium do not directly affect urease activity, but indirectly affect ti through total nitrogen. Both direct and indirect effects of soil pH value are limited and soil pH value is not a major factor affecting urease activity.

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