基于土壤浓度剖面的地表CO2通量估算

Salmawati, K. Sasaki, S. Yuichi
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引用次数: 2

摘要

目的:估算由CO2浓度曲线得到的地表CO2通量,并利用先前使用封闭室法测量得到的地表CO2通量数据验证结果。研究设计:采用推导的质量平衡方程模型,测量土壤CO2浓度剖面、土壤性质和土壤温度,估算地表CO2通量。结果随后与使用封闭室法测量的表面CO2通量进行了比较。学习地点和时间:2015年11月至2016年3月,INAS位于日本九州大学伊藤校区。方法:在四个不同深度取样二氧化碳气体,分析其在土层内的浓度。在整个测量过程中监测土壤温度,并测量土壤的密度、孔隙率和含水量等特性,以估计扩散速率。从质量平衡方程出发,估算了地表CO2通量。利用以前在同一地点采用封闭室法进行的表面CO2通量测量数据进行了验证。结果:7次测得的土壤CO2浓度剖面显示,CO2浓度随土壤深度的增加而增加,且符合对数趋势(平均r2 = 0.981)。在每个深度测量了一系列CO2浓度值,即在0.1 m深度测量了1300至8700 ppm;在0.2 m深度2500 ~ 10800 PPM;0.3 m深度4200 ~ 13200 PPM;原创研究论文Salmawati et al.;生物工程学报,7(4):214-222,2017;条款no.BJECC.2017.017 215 5800至16500 ppm在1.0 m深度。0.1 m土壤深度CO2浓度高,地表CO2通量高。结论:INAS农田土壤CO2浓度呈对数增长趋势。基于这一趋势,利用质量平衡方程和气体扩散模型的推导模型,提出了估算地表CO2通量的方程。对估算的地表CO2通量进行了比较,结果与实测值吻合较好。本文提出的方程可能适用于估算地表CO2通量。
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Estimating surface CO2 flux based on soil concentration profile
Aims: To estimate the surface CO2 flux derived from CO2 concentration profiles and to validate the results by previous data of surface CO2 flux obtained from the measurements using close-chamber method. Study Design: The measurement of soil CO2 concentration profile, soil properties, and soil temperature was carried out to estimate surface CO2 flux using the derived model of mass balance equation. The results were subsequently compared with measurements of surface CO2 flux using close-chamber method. Place and Duration of Study: INAS field located in Ito Campus of Kyushu University (Japan) from November 2015 to March 2016. Methodology: CO2 gas was sampled in four different depths to analyze its concentration within the soil layer. Soil temperature was monitored throughout the measurement and soil properties such as density, porosity and moisture content were measured as well to estimate the diffusion rate. Derived from mass balance equation, the surface CO2 flux was estimated. It was validated using the previous measurement data of surface CO2 flux using close-chamber method that had been conducted formerly at the same location. Results: A total of seven measurements of soil CO2 concentration profile showed that the CO2 concentration increased with soil depth and it was fitted with logarithmic trend (R 2 = 0.981 in average). A range of CO2 concentration values was measured at each depth, i.e., 1300 to 8700 ppm at 0.1 m depth; 2500 to 10800 ppm at 0.2 m depth; 4200 to 13200 ppm at 0.3 m depth; and Original Research Article Salmawati et al.; BJECC, 7(4): 214-222, 2017; Article no.BJECC.2017.017 215 5800 to 16500 ppm at 1.0 m depth. High CO2 concentration in 0.1 m soil depth indicated high surface CO2 flux. Conclusions: Soil CO2 concentration in INAS field increased following a logarithmic trend. Based upon this trend, an equation to estimate the surface CO2 flux was proposed using derived model from mass balance equation and gas diffusion model. The estimated surface CO2 flux was compared and showed a good agreement with measured one. The equation presented herein is potentially suitable to estimate the surface CO2 flux.
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