期刊文献+

锡林河流域羊草草原暗栗钙土矿质氮动态变化 被引量:14

Mineral nitrogen dynamics in Dark Chestnut soil of Leymus chinensis grassland in the Xilin River Basin, China
下载PDF
导出
摘要 通过野外采样,分析了内蒙古锡林河流域三个不同放牧强度羊草草原0~30cm表层土壤中矿质氮(NH4+-N+NO3--N)的浓度特征,研究了它们在生长季期间的含量变化情况。结果表明:羊草草原暗栗钙土中矿质氮主要以NH4+-N形式存在,矿质氮含量仅占土壤全氮的0·20%~0·92%;土壤矿质氮含量随草地放牧强度升高而降低,围封禁牧多年的羊草样地矿质氮含量高于轮牧地和自由放牧地;生长季期间0~10cm、10~20cm和20~30cm各层次土壤NH4+-N和NO3--N含量随土壤温度、水分和植物生长吸收的变化而波动明显,不同深度土壤矿质氮的季节变化趋势基本一致,表层0~10cm土壤矿质氮含量波动幅度最大:在4月和7、8月份,NO3--N和NH4+-N浓度分别出现峰值;NH4+-N和NO3--N含量随采样深度增加而降低,各采样点0~30cm土壤中NH4+-N含量均高于NO3--N。 In the paper, the dynamic features of mineral nitrogen (SMN, NH^+_4-N+NO^-_3-N) of the 0-30cm Dark Chestnut soil were studied, its seasonal variations during growing season and the SMN content differences among different research points were analyzed. All the samples were taken randomly from three different managed Leymus chinensis grasslands of Xilin River Basin in Inner Mongolia of China. The results showed that in Dark Chestnut soil the prevailing form of SMN was NH^+_4-N,the plant available nitrogen only takes a very small part of the soil total nitrogen, always below 1%(0.20%~0.92%).With the increase of grassland grazing intensity, the SMN content changed oppositely. The sequence of SMN content from high to low was: fenced grassland﹥rotational grazing grassland﹥random grazed grassland. During the growing season, the contents of NH^+_4-N and NO^-_3-N in different soil layers of three different managed grasslands changed evidently with the changes of soil temperature, moisture and plant absorbance, the trends of seasonal change were similar in different soil layers. The mineral nitrogen content of 0-10cm surface soils fluctuated most significantly, the content of NO^-_3-N was the highest in April and that of NH^+_4-N was higher in July and August. The content of NH^+_4-N was higher than that of NO^-_3-N in three different soil layers, and their contents decreased with the increase of sampling depth. The SMN content changed just the same order as the soil total nitrogen, organic carbon and soil water content with the increase of the depth, but there were no significant correlations between SMN content and anyone of them.
出处 《地理研究》 CSCD 北大核心 2005年第3期387-393,共7页 Geographical Research
基金 国家重点基础研究发展规划项目(2002CB412503) 中国科学院知识创新重大项目(KZVX1-SW-01-04) 中国科学院地理科学与资源研究所知识创新项目(CXIOG-E01-03-01)。
  • 相关文献

参考文献20

  • 1Ingestad T. Plant growth in relation to nitrogen supply. In: Clark F E, Rosswall T (eds.). Terrestrial Nitrogen Cycles. Ecology Bulletin, Stockholm, 1981, 33(303): 268~271.
  • 2齐玉春,董云社.土壤氧化亚氮产生、排放及其影响因素[J].地理学报,1999,54(6):534-542. 被引量:82
  • 3Zhang Q. Effects of soil extracts from repeated plantation woodland of Chinese-fir on microbial activities and soil nitrogen mineralization dynamics. Plant and Soi1,1997, (191):205~212.
  • 4Hartemink A E, Buresh R J, Bodegom P M, et al. Inorganic nitrogen dynamics in fallows and maize on an Oxisol and Alfisol in the highlands of Kenya. Geoderma, 2000, (98): 11~33.
  • 5Koschorreck M, Darwich A. Nitrogen dynamics in seasonally flooded soils in the Amazon floodplain. Wetland Ecology and Management, 2003, (11):317~330.
  • 6Bluefield T J, Xu Z H, Chen C. Mineral nitrogen dynamics following soil compaction and cultivation during hoop pine plantation establishment. WWW. elsevier, com/locate/foreco. 2004. 9.9.
  • 7Mazzarino M J, Bertiller M B, Sain C. Soil nitrogen dynamics in northeastern Patagonia Steppe under different precipitation regimes. Plant and Soil, 1998, (202):125~131.
  • 8范世华,李培芝,王力华,许思明.杨树人工林下根系的氮素循环与动态特征[J].应用生态学报,2004,15(3):387-390. 被引量:18
  • 9李香真.放牧对典型草原土壤-植物系统中碳、氮、磷库特征的影响[Z].中国科学院文献情报研究中心:中国科学院植物研究所,1999..
  • 10李博 雍世鹏 等.锡林河流域植被及其利用[J].草原生态系统研究,1988,(3):84-183.

二级参考文献102

共引文献492

同被引文献327

引证文献14

二级引证文献170

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部