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东北地区不同纬度农田土壤碱解氮的剖面分布

Profile distribution of alkali-hydrolyzed nitrogen in farmland soils of Northeast China along a latitudinal gradient

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【作者】 施春健庄秋丽李琪梁文举姜勇

【Author】 SHI Chun-jian1,2, ZHUANG Qiu-li1,2, LI Qi1,2, LIANG Wen-ju1, JIANG Yong1 (1Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China; 2Graduate University of Chinese Academy of Sciences, Beijing 100039, China).

【机构】 中国科学院沈阳应用生态研究所中国科学院沈阳应用生态研究所 沈阳110016中国科学院研究生院北京100039沈阳110016中国科学院研究生院沈阳110016

【摘要】 为研究农田土壤碱解氮的含量及其分布,以东北玉米带不同纬度农田土壤为对象,研究了100cm深度范围内碱解氮含量垂直分布及纬向分异特征。结果表明:土壤碱解氮主要分布在0~60cm土层中,各样点碱解氮含量随土壤深度的增加而减少;除公主岭点外,其它各点0~60cm的3个土层间碱解氮含量差异显著(P<0.05);碱解氮含量与有机碳、全氮含量极显著正相关(P<0.01),说明土壤碱解氮含量及其分布主要受土壤有机质和氮素水平的影响。0~20cm土层碱解氮含量具有随纬度增加而增加的趋势,气候条件和土壤类型的差异是导致其纬向分布差异的主要原因。

【Abstract】 The vertical distribution and latitudinal differentiation of alkali-hydrolyzed nitrogen in the profile down to 100 cm depth of maize soils in Northeast China was investigated along a latitudinal gradient. The results showed that soil alkali-hydrolyzed N was mainly distributed at the depth of 0—60 cm, and decreased with soil depth. Except for the Gongzhuling site, the soil alkali-hydrolyzed N content in other sampling sites was significantly different (P<0.05) among the 3 layers at the depth of 0—60 cm. Soil alkali-hydrolyzed N had a significant positive correlation (P<0.01) with soil organic carbon and total N, indicating that its content and distribution was mainly affected by soil organic matter and total N levels. Soil alkali-hydrolyzed N content increased with increasing latitude, and climate condition and soil type were considered as the main reasons that induced the latitudinal differentiation of soil alkali-hydrolyzed N.

【基金】 国家重点基础研究发展计划项目(2005CB121105);国家自然科学基金资助项目(30670379)
  • 【文献出处】 生态学杂志 ,Chinese Journal of Ecology , 编辑部邮箱 ,2007年04期
  • 【分类号】S153
  • 【被引频次】55
  • 【下载频次】745
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