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应用生态学报 ›› 2011, Vol. 22 ›› Issue (03): 665-672.

• 研究报告 • 上一篇    下一篇

祁连山中段土壤有机碳和氮素的剖面分布

耿增超,姜林,李珊珊,佘雕,侯磊   

  1. 西北农林科技大学资源环境学院| 陕西杨凌 712100
  • 出版日期:2011-03-18 发布日期:2011-03-18

Profile distribution of organic carbon and nitrogen in major soil types in the middle of Qilian Mountains.

GENG Zeng-chao, JIANG Lin, LI Shan-shan, SHE Diao, HOU Lei   

  1. College of Resources and Environment, Northwest A &F University, Yangling 712100, Shaanxi, China
  • Online:2011-03-18 Published:2011-03-18

摘要: 以祁连山中段地区主要土壤类型(棕钙土、灰褐土、栗钙土、高山草甸土)为对象,研究了不同土壤剖面上有机碳、全氮、铵态氮和硝态氮含量的分布规律.结果表明:在祁连山中段地区,随剖面深度增加,不同土壤类型的有机碳、全氮、铵态氮和硝态氮含量均逐渐降低,且其有机碳、氮素的累积和分解存在差异.其中,有机碳含量的全剖面平均值在14.01~41.17 g·kg-1,大小顺序为灰褐土>高山草甸土>栗钙土>棕钙土;全氮含量在1.28~2.73 g·kg-1,为高山草甸土>灰褐土>栗钙土>棕钙土;铵态氮含量在5.80~8.40 mg·kg-1,为棕钙土>高山草甸土>栗钙土>灰褐土;硝态氮含量在6.57~15.11 mg·kg-1,为栗钙土>高山草甸土>棕钙土>灰褐土;土壤C/N在11.33~19.22,为灰褐土>栗钙土>高山草甸土>棕钙土;硝铵比在1.00~2.69,为灰褐土>栗钙土>高山草甸土>棕钙土.在不同的气候、植被和地形(坡位、坡向等)条件下,同一土壤类型的有机碳和氮素含量有很大差别.土壤有机碳、全氮和铵态氮含量之间存在极显著正相关,而这三者与硝态氮之间相关性不显著.土壤速效钾含量与铵态氮、硝态氮呈极显著正相关,速效磷含量与土壤有机碳、全氮和铵态氮呈极显著、显著正相关,而pH值、全钾、全磷含量与有机碳和氮素之间无明显相关性.

关键词: 祁连山, 土壤剖面, 有机碳, 氮素

Abstract: This paper studied the distribution patterns of organic carbon (OC), total nitrogen (TN), NH4+-N, and NO3--N in the profiles of brown calcic soil, grey cinnamon soil, chestnut soil, and alpine meadow soil in the middle of Qilian Mountains. In all test soils, the contents of OC, TN, NH4+-N, and NO3--N decreased with increasing soil depth, and the accumulation and decomposition of OC and various N forms differed with soil types. The average content of OC in different soil profiles changed from 14.01 to 41.17 g·kg-1, and was in the order of grey cinnamon soil > alpine meadow soil > chestnut soil > brown calcic soil; the average content of TN changed from 1.28 to 2.73 g·kg-1, with a sequence of alpine meadow soil > grey cinnamon soil > chestnut soil > brown calcic soil. The C/N ratio was from 11.33 to 19.22, with the order of grey cinnamon soil > chestnut soil > alpine meadow soil > brown calcic soil. NH4+-N content changed from 5.80 to 8.40 mg·kg-1, and was in the order of brown calcic soil > alpine meadow soil > chestnut soil > grey cinnamon soil; NO3--N content changed from 6.57 to 15.11 mg·kg-1, being in the order of chestnut soil > alpine meadow soil > brown calcic soil > grey cinnamon soil. The ratio of NO3--N to NH4+-N was 1.00-2.69, with the sequence of grey cinnamon soil > chestnut soil > alpine meadow soil > brown calcic soil. The OC and N contents in the same soil types differed significantly with the conditions of climate, vegetation, and topography (e.g., slope aspect and slope position). Correlation analysis showed that there were highly significant positive correlations between OC, TN, and NH4+-N, but these three items had no significant positive correlations with NO3--N. Furthermore, there were highly significant positive correlations between available K, NH4+-N, and NO3--N and between available P and OC, significant positive correlations between available P, TN, and NH4+-N, but no significant correlations between pH, total K, and total P and OC and N.

Key words: Qilian Mountains, soil profile, organic carbon, nitrogen