植物生态学报 ›› 2006, Vol. 30 ›› Issue (3): 450-456.DOI: 10.17521/cjpe.2006.0060

所属专题: 碳水能量通量

• 研究论文 • 上一篇    下一篇

川中丘陵区水稻田土壤呼吸及其影响因素

韩广轩1,2(), 朱波2,*, 江长胜3   

  1. 1中国科学院成都山地灾害与环境研究所,成都 610041
    2中国科学院植物研究所植被数量生态学重点实验室, 北京 100093
    3中国科学院大气物理研究所, 北京 100029
  • 接受日期:2005-09-08 发布日期:2006-05-30
  • 通讯作者: 朱波
  • 作者简介:*E-mail: bzhu@imde.ac.cn
    E-mail: gxhan@ibeas.ac.cn
  • 基金资助:
    国家重点基础研究发展计划项目(2005CB121108);国家自然科学基金重点项目(40331014);中国科学院知识创新工程重大项目(KZCX1-SW-01-01B)

SOIL RESPIRATION AND ITS CONTROLLING FACTORS IN RICE FIELDS IN THE HILL REGION OF THE CENTRAL SICHUAN BASIN

HAN Guang-Xuan1,2(), ZHU Bo2,*, JIANG Chang-Sheng3   

  1. 1Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, China
    2Laboratory of Quantitative Vegetation Ecology, Institute of Botany, Chinese Academy of Sciences, Beijing 100093, China
    3Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
  • Accepted:2005-09-08 Published:2006-05-30
  • Contact: ZHU Bo

摘要:

基于川中丘陵区2003年4~9月水稻田土壤呼吸、土壤温度和水稻(Oryza sativa)生物量的测定,研究了水稻田土壤呼吸日变化和季节变化特征以及影响稻田土壤呼吸的主要因素。结果表明,水稻田土壤CO2排放通量的日变化为单峰型,其最小值和最大值分别出现在当地时间7∶00和15∶00;在水稻生长期内,稻田土壤CO2排放通量在18.00~269.69 mg·m-2·h-1之间波动,平均排放通量为121.76 mg·m-2·h-1。在日的时间尺度上,水稻田土壤CO2排放通量与5 cm土壤温度存在显著的指数函数关系;而从整个生长期时间尺度上看,水稻田土壤CO2的排放通量主要受到5 cm土壤温度和水稻地下生物量的影响。在水稻生长初期,水稻地下生物量与稻田土壤CO2排放通量之间存在着显著的相关关系;水稻拔节中后期到成熟期,土壤温度则是制约稻田土壤CO2排放的关键因素。CO2排放通量与稻田地表水层深度的相关关系不显著。

关键词: 土壤呼吸, 稻田, 影响因素

Abstract:

Measurements of soil respiration, soil temperature and rice biomass were made during the rice growing season in the hill region of the central Sichuan Basin from April to September 2003. Characteristics of the daily and seasonal variations of soil respiration and their controlling factors are presented. The results showed that daily variations of soil respiration could be modeled with a single peak curve. The minimum and maximum soil respiration values from rice fields occurred at 7∶00 and 15∶00, respectively. Daily soil respiration rates were highly correlated with 5 cm depth soil temperature measurements. The mean rate of soil respiration was 121.76 mg·m-2·h-1, ranging from 18.00 to 269.69 mg·m-2·h-1 during the growing season. Rice root biomass and 5 cm depth soil temperatures were the major factors influencing soil CO2 emissions during the entire growing season. There was a significant relationship between the rate of soil respiration and root biomass of rice during the initial growing season. From the middle/late stages to mature stage, 5 cm depth soil temperatures played a key role in regulating soil CO2 emissions from rice fields, while the relationship between the rate of soil respiration and water levels in the rice fields was not obvious.

Key words: Soil respiration, Rice field, Controlling factors