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冰川冻土 ›› 2014, Vol. 36 ›› Issue (5): 1298-1305.doi: 10.7522/j.issn.1000-0240.2014.0155

• 寒旱区生物学 • 上一篇    下一篇

青藏高原东缘高寒草甸退化过程中植物群落物种多样性、生产力与土壤特性的关系

罗亚勇1, 孟庆涛2, 张静辉1, 赵学勇1, 秦彧1   

  1. 1. 中国科学院 寒区旱区环境与工程研究所, 甘肃 兰州 730000;
    2. 内蒙古煤炭建设生态环境研究院, 内蒙古 呼和浩特 010020
  • 收稿日期:2014-02-11 修回日期:2014-06-06 出版日期:2014-10-25 发布日期:2014-11-19
  • 作者简介:罗亚勇(1983-), 男, 甘肃平凉人, 助理研究员, 2010年在中国科学院寒区旱区环境与工程研究所获博士学位, 现主要从事生理生态学方面的研究. E-mail:luoyy@lzb.ac.cn
  • 基金资助:
    国家自然科学基金项目(41201249);冻土工程国家重点实验室开放基金项目(SKLFSE201203);国家科技支撑计划项目(2011BAC07B02)资助

Species diversity and biomass in relation to soil properties of alpine meadows in the eastern Tibetan Plateau in different degradation stages

LUO Yayong1, MENG Qingtao2, ZHANG Jinghui1, ZHAO Xueyong1, QIN Yu1   

  1. 1. Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;
    2. Research Institute of Ecology Environment of Inner Mongolia Coal Mine, Hohhot 010020, China
  • Received:2014-02-11 Revised:2014-06-06 Online:2014-10-25 Published:2014-11-19

摘要: 为了阐明高寒草甸退化过程中植物群落物种多样性、生产力与土壤特性的关系, 在青藏高原东缘的玛曲县沿着高寒草甸退化梯度选取了轻度退化草甸、中度退化草甸、重度退化草甸和沙化草甸, 测定了高寒草甸退化过程中植物群落物种多样性、生产力与土壤理化性状. 结果表明: 从轻度退化到中度、重度和沙化草甸, 植被地下生物量分别降低了36%、48%和91%, 总生物量分别降低了34%、47%和91%, 土壤有机碳分别下降了18%、81%和97%, 全N分别下降了25%、82%和95%, 全P含量分别下降了14%、33%和41%. 随着高寒草甸的退化, 植被群落的生物多样性和地上生物量呈先稳定后降低的趋势, 土壤砂粒含量、pH值和全K含量呈增加趋势, 黏粉粒呈降低趋势, 速效N、速效P和速效K呈先增加后降低的趋势. 相关分析表明, 群落物种多样性和生产力与土壤有机碳、全N、全P、速效N、速效P、速效K、黏粒含量、粉粒含量、水分含量均呈显著正相关(P<0.01), 而与土壤砂粒、全K和pH值均呈显著负相关(P<0.05). 因此, 高寒草甸退化过程中, 土壤质地、养分和水分等的复杂变化及其相互关系共同决定着高寒草甸群落物种多样性和生产力的变化. 同时, 植被生产力和土壤碳、氮的降低产生明显的正反馈效应, 导致在重度退化阶段和沙化阶段, 植被生产力和土壤碳氮的急剧下降.

关键词: 高寒草甸, 物种多样性, 生产力, 土壤理化性质, 退化

Abstract: To clarify the changes of species diversity and biomass in relation to soil properties of alpine meadows in different degradation stages, mild degraded meadow, moderate degraded meadow, severe degraded meadow and serious sandy meadow were chosen to measure species diversity, biomass and soil properties. The changes of vegetation and soil properties, followed by degraded process of alpine meadow, show the following trends: 1) vegetation diversity and biomass decrease gradually; 2) contents of soil moisture, soil clay, silt, soil organic carbon, total nitrogen (N), total phosphorous (P), available N and available potassium (K) decrease consistently, while content of soil sand and total K as well as pH value increase consistently. The correlation between species diversity or biomass and soil factors such as soil moisture, soil clay, silt, soil organic carbon, total N, total N, available N, available P and available K is significant positive, while the correlation between species diversity or biomass and soil factors such as content of soil sand and total K as well as pH value is significant negative. Therefore, changes of species diversity and biomass are governed by soil texture, soil nutrients, soil water content, pH and electrical conductivity.

Key words: alpine meadow, species diversity, biomass, stiochiometry characteristics, degradation

中图分类号: 

  • S154.4