植物生态学报 ›› 2007, Vol. 31 ›› Issue (3): 380-385.DOI: 10.17521/cjpe.2007.0046 cstr: 32100.14.cjpe.2007.0046
所属专题: 生态系统碳水能量通量
收稿日期:2006-09-08
接受日期:2006-11-14
出版日期:2007-09-08
发布日期:2007-05-30
作者简介:E-mail: wenxf@igsnrr.ac.cn
基金资助:
WEN Xue-Fa1(
), SUN Xiao-Min1, LIU Yun-Fen1, LI Xiao-Bo2
Received:2006-09-08
Accepted:2006-11-14
Online:2007-09-08
Published:2007-05-30
摘要:
理论上,土壤呼吸通量的量值可以通过观测土壤呼吸CO2扩散速率(∂c/∂t)计算得到。但是为获得∂c/∂t,通常须允许土壤呼吸箱内CO2浓度升高,因此,如何估算外界大气CO2浓度条件下的∂c/∂t是土壤呼吸观测技术的关键,关系到观测结果的准确性。通常∂c/∂t的估算会受土壤表层大气CO2扩散梯度(即土壤呼吸箱内CO2扩散梯度和大气CO2浓度昼夜变化)的影响。目前,线性回归方法是土壤呼吸观测中估算∂c/∂t的基本方法。然而,常用的线性回归方法会低估∂c/∂t,而指数回归方法则可以准确地估算∂c/∂t。夜间∂c/∂t的变化与大气CO2浓度之间存在非常明显的负相关关系。夜间土壤表层大气CO2扩散梯度的减小导致线性回归方法明显低估∂c/∂t。∂c/∂t的昼夜变化过程存在明显的非对称性现象,而指数回归方法可以更好地描述∂c/∂t昼夜变化的非对称性响应。
温学发, 孙晓敏, 刘允芬, 李晓波. 线性和指数回归方法对土壤呼吸CO2扩散速率估算的影响. 植物生态学报, 2007, 31(3): 380-385. DOI: 10.17521/cjpe.2007.0046
WEN Xue-Fa, SUN Xiao-Min, LIU Yun-Fen, LI Xiao-Bo. EFFECTS OF LINEAR AND EXPONENTIAL FITTING ON THE INITIAL RATE OF CHANGE IN CO2 CONCENTRATION ACROSS THE SOIL SURFACE. Chinese Journal of Plant Ecology, 2007, 31(3): 380-385. DOI: 10.17521/cjpe.2007.0046
图1 指数和线性回归方法对土壤呼吸CO2扩散速率(?c/?t)的影响
Fig.1 Impacts of exponential and linear fit on the initial rate of change in the CO2 concentration across the soil surface a: 土壤呼吸箱内CO2浓度的变化过程 Variations of CO2 concentration in the soil respiration chamber b: 材料与方法中试验处理1) Experiment 1) described in Material and Methods
图2 测量时间对土壤呼吸CO2扩散速率(?c/?t)的影响
Fig.2 Impacts of different measuring periods on the initial rate of change in CO2 concentration (?c/?t) across the soil surface
图3 指数和线性回归估算的土壤呼吸CO2扩散速率(?c/?t)和大气CO2浓度的日变化特征
Fig.3 Diurnal variation of CO2 concentration and the initial rate of change in the CO2 concentration (?c/?t) by the exponential and linear fit across the soil surface
图4 昼夜CO2扩散梯度变化对土壤呼吸CO2扩散速率(?c/?t)的影响 a和c指白天数据 b和d指夜间数据
Fig.4 Impact of the diurnal CO2 diffusion gradient on the initial rate of change in CO2 concentration (?c/?t) across the soil surface a and c refer to daytime data b and d refer to nighttime data
图5 土壤呼吸CO2扩散速率(?c/?t)对温度昼夜变化响应的非对称性响应特征 a、b和c分别代表图3中第一天、第二天和第三天的日变化数据 d代表图3中所有的日变化数据
Fig.5 Diurnal asymmetry of the initial rate of change in CO2 concentration (?c/?t) in response to air temperature across the soil surface a, b and c refer to the data on the 1st, 2nd and 3rd day, respectively, in Fig. 3 d refers to all data in Fig. 3
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