植物生态学报 ›› 2006, Vol. 30 ›› Issue (4): 553-562.DOI: 10.17521/cjpe.2006.0073

• 论文 • 上一篇    下一篇

内蒙古草地样带植物群落生物量的梯度研究

韩彬1,2(), 樊江文1,*(), 钟华平1   

  1. 1 中国科学院地理科学与资源研究所,北京 100101
    2 中国科学院研究生院,北京 100039
  • 收稿日期:2005-01-25 出版日期:2006-01-25 发布日期:2006-07-30
  • 通讯作者: 樊江文
  • 作者简介:*E-mail:jwfan@cem.ac.cn
    E-mail:hanb@igsnur.ac.cn
  • 基金资助:
    科技部973项目(2002CB412501);中国科学院地理科学与资源研究所知识创新工程项目(CX100G-101-02-05)

GRASSLAND BIOMASS OF COMMUNITIES ALONG GRADIENTS OF THE INNER MONGOLIA GRASSLAND TRANSECT

HAN Bin1,2(), FAN Jiang-Wen1,*(), ZHONG Hua-Ping1   

  1. 1 Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
    2 Graduate School of Chinese Academy of Sciences, Beijing 100039, China
  • Received:2005-01-25 Online:2006-01-25 Published:2006-07-30
  • Contact: FAN Jiang-Wen

摘要:

采用样带法对内蒙古草地植物群落生物量沿水热梯度的变化特征进行了研究,并对几种回归方法进行了比较。一元回归结果表明:在本样带的限定范围内,生物量与年均温、≥0 ℃年积温、≥10 ℃年积温、年实际日照总时数等热量因子呈负相关(年均温的相关性最高),而与年降水量、年均相对湿度等水分因子呈正相关(年均相对湿度的相关性最高),其中年均温和年均相对湿度对生物量的影响最为显著,二者对生物量的空间变异起着互为消长的作用,而海拔高度的影响则不显著。多元回归结果表明,作为半干旱区植物生长的主要限制因子,年降水量在大尺度上对生物量产生影响的途径更为复杂,但其作用不可低估。生物量和地下地上生物量比值会因不同的气候区、不同的植被类型和物种组成,对环境因子的响应程度不同,在经向、纬向和草地类型梯度上的变化特征也不同。水热的配比关系要比单一的水分和温度与植物的生长具有更紧密的关系,地下地上生物量比随着水热配比关系的变化也会呈现出不同的变化规律,其驱动因子并不一定始终都是降水。也许可以认为:半干旱/干旱的划分界限是本研究所涉及的草地样带上生物量和地下地上生物量比值沿草地类型梯度变化的一个转折界限,在此界限前后,气候对生物量的主导因素和生物量对此关键因子的响应程度都有所变化。

关键词: 内蒙古, 草地样带, 地下生物量, 地上生物量, 地下生物量/地上生物量, 梯度分析

Abstract:

Background and Aims Vegetation transect is an effective method to study the relationship between global change and terrestrial ecosystem. However there are few researches on biomass gradient characters of grassland vegetation and their environmental driving mechanism. The transect measurement was used in this study to analyze biomass gradient change of grassland vegetation in Inner Mongolia. The following questions were tried to answer: (a) How does grassland biomass change along with longitude and latitude as well as water and thermal gradients? (b) Which climate factors will produce pivotal effect to grassland biomass change? (c) How do climate factors control material production process of grassland ecosystem?
Methods The selection of 49 sample sites was principally defined by a 1 900 km long×150 km wide transect across the grasslands of Inner Mongolia. Aboveground and belowground biomasses were measured in the sample sites. The correlativity between biomass and climate factors was analyzed using China climate grid database which constructed by Chinese Ecosystem Research Network.
Key results Grassland biomass was found to be negatively correlated to mean annual temperature, ≥0 ℃ accumulated temperature, ≥10 ℃ accumulated temperature and annual hours of sunshine. Contrarily it was positively correlated with mean annual precipitation and mean annual relative humidity. Among climate factors, mean annual temperature and mean annual relative humidity effected grassland biomass the most obvious.
Conclusions Aboveground and belowground biomasses present visible change regulation along with longitude and latitude as well as climate gradients. Mean annual precipitation was shown as a key role to grassland biomass although its effect ways were complicated. The study suggested combined and integrated relationships of environment factors should be considered in researches of biomass forming and changing.

Key words: Inner Mongolia, Grassland transect, Aboveground biomass, Belowground biomass, Below-aboveground biomass ratio, Gradient