欢迎访问《草业学报》官方网站,今天是 分享到:

草业学报 ›› 2010, Vol. 19 ›› Issue (1): 42-49.

• 研究论文 • 上一篇    下一篇

黄土高原不同地形封育草地的土壤呼吸日动态与影响因子分析

李志刚,侯扶江*   

  1. 农业部草地农业生态系统学重点开放实验室西部草业工程研究中心 兰州大学草地农业科技学院,甘肃 兰州 730020
  • 收稿日期:2009-02-17 出版日期:2010-01-25 发布日期:2010-02-20
  • 作者简介:李志刚(1985-),男,宁夏海原人,硕士。E-mail:lizhg06@lzu.cn
  • 基金资助:
    国家自然科学基金项目(30771529),公益性行业计划项目(nyhyzx07-022)和十一五科技支撑项目(2006BAD16B01)资助。

Analysis of soil respiration diurnal dynamics and factors influencing it in enclosednatural grasslands under different topographies in the Loess Plateau

LI Zhi-gang, HOU Fu-jiang   

  1. College of Pastoral Agriculture Science and Technology, Lanzhou University;
    Key Laboratory
    of Grassland and Agro-ecosystem, Ministry of Agriculture, Lanzhou 730020, China
  • Received:2009-02-17 Online:2010-01-25 Published:2010-02-20

摘要: 采用动态密闭气室红外CO2分析法(IRGA)对黄土高原丘陵沟壑区不同地形的封育草地土壤呼吸速率日动态进行了测定,并分析了土壤呼吸与土壤温度、土壤水分、地下生物量和地形间的关系。研究结果显示,草地的土壤呼吸日动态呈单峰曲线,最小值为0.393~1.103 μmol/(m2·s),出现在凌晨;最大值为1.034~1.405 μmol/(m2·s),出现在14时左右,可以用正弦曲线拟合;而且不同样地间土壤呼吸速率与土壤温度间的关系均可用指数函数描述。土壤日均呼吸速率在不同地形的草地间存在差异,平坦草地为1.229 μmol/(m2·s),东北坡15°, 30° 和45° 草地分别为1.138, 1.033和0.890 μmol/(m2·s);西南坡15°, 30° 和45° 草地分别为1.036, 0.859和0.379 μmol/(m2·s);土壤呼吸速率随坡度的增大而减小,东北坡土壤呼吸速率小于西南坡,与不同样地间土壤水分和地下生物量的变化趋势一致,而且研究结果表明土壤呼吸的这种差异主要是受地形影响的土壤水分和地下生物量空间分布差异性决定的,而不同样地间土壤平均温度差异不显著(P>0.05)。

Abstract: The diurnal dynamics of soil respiration in enclosed grasslands of gullied-hilly areas of the Loess Plateau, were measured by closed chamber infrared CO2 gas analyzer and the relationships between soil respiration and soil temperature, soil water content, underground biomass and topography were analyzed. Diurnal soil respiration showed a single-peak curve with the lowest value of 0.393-1.103 μmol/(m2·s) in the early hours of the morning and a peak value of 1.034-1.405 μmol/(m2·s) at 14:00. A sine curve could be fitted to the data and all relationships between soil respiration rate and soil temperature could be depicted by an exponential function. There were differences in soil daily average respiration rate between plots: In flat grassland it was 1.229 μmol/(m2·s); on north-east facing grassland slopes of 15°, 30°, and 45° it was 1.138 ,1.033 and 0.890 μmol/(m2·s), respectively, while on similar south-west facing slopes it was 1.036, 0.859, and 0.379 μmol/(m2·s), respectively. Soil respiration rate declined as slope increased, and that of south-west facing grassland was lower than that of north-east facing grassland, changes that were consistent with soil water content and underground biomass. These differences were determined by spatial distribution differences of soil water content and underground biomass which were affected by topography, but there was no effect of temperature between plots.

中图分类号: