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草业学报 ›› 2012, Vol. 21 ›› Issue (3): 54-60.

• 研究论文 • 上一篇    下一篇

贺兰山不同海拔土壤颗粒有机碳、氮特征

杨益1,牛得草1*,文海燕1,张宝林2,董强2,陈菊兰3,傅华1   

  1. 1.兰州大学草地农业科技学院 草地农业生态系统国家重点实验室,甘肃 兰州 730020;
    2.内蒙古阿拉善盟草原总站,内蒙古 巴彦浩特 750306;
    3.内蒙古阿拉善盟畜牧研究所,内蒙古 巴彦浩特 750306
  • 出版日期:2012-06-20 发布日期:2012-06-20
  • 通讯作者: E-mail:xiaocao0373@163.com
  • 作者简介:杨益(1986-),女,重庆人,在读硕士。
  • 基金资助:
    中国科学院战略性先导科技专项-应对气候变化的碳收支认证及相关问题(XDA05050406-8),科技部科技支撑计划项目(2008BAD95B03),国家自然科学基金项目(31070412)和兰州大学中央高校基本科研业务费专项资金(lzujbky-2012-98)资助。

Responses of soil particulate organic carbon and nitrogen along an altitudinal
gradient on the Helan Mountain, Inner Mongolia

YANG Yi1, NIU De-cao1, WEN Hai-yan1, ZHANG Bao-Lin2, DONG Qiang2, Chen Ju-lan3, FU Hua1   

  1. 1. State Key Laboratory of Grassland Agro-ecosystems, College of Pastoral Agriculture Science and Technology, Lanzhou University, Lanzhou 730020, China;
    2.Alxa Alliance Grassland Station of Inner Mongolia, Bayinhaote 750306, China;
    3.Alxa Alliance Institute of Animal of Inner Mongolia, Bayanhot 750306, China)
  • Online:2012-06-20 Published:2012-06-20

摘要: 采用颗粒大小的物理分组方法,测定了贺兰山(西坡)不同海拔具有代表性的8个样地的草地土壤颗粒有机碳和颗粒有机氮含量,并且分析了土壤颗粒碳、氮分配比例与植被特征及环境因子的关系。结果表明,土壤颗粒碳、氮含量随海拔的降低而显著降低,随土层深度的增加而降低;在4个植被类型中,二者在高山草甸最高,在草原化荒漠最低。土壤颗粒碳、氮分配比例随海拔的降低表现出先降低后升高的趋势,在高山草甸最高,山地荒漠草原最低。土壤颗粒碳、氮分配比例与植被盖度、地上生物量、年均降水量呈极显著的正相关关系,与年均温呈极显著的负相关关系。

Abstract: The physical fractionation method was used to measure the contents of soil particulate organic carbon (POC) and particulate organic nitrogen (PON) in eight grassland sites along an elevation gradient on the Helan Mountain, Inner Mongolia. The relationships of POC, PON and their proportion with vegetation characteristics and environmental factors were analyzed. Both POC and PON declined significantly with altitude and with soil depth. Meanwhile, POC and PON changed significantly among vegetation types. The proportions of POC and PON reduced considerably with the altitude from 2 940 to 1 820 and 1 700 m. Among the four vegetation types, proportions of both POC and PON were the highest in the alpine meadow and lowest in the desert steppe. The proportions of POC and PON had significant positive correlations with vegetation cover, aboveground plant biomass and mean annual precipitation, but a significant negative correlation with mean annual temperature.

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