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Soil CO2 evolution rates in the field - a comparison of three methods.

机译:田间土壤CO 2 的演化速率-三种方法的比较。

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摘要

In this field study, three methods for determining soil CO2 evolution rates were compared: (1) a static chamber method and (2) a dynamic chamber method, both with gas chromatographic (GC) analysis of air samples, and (3) a dynamic chamber system using a portable infrared gas analyzer (CIRAS). The mean CO2 evolution rate in the field increased in the order static chamber-GC < dynamic chamber-GC < dynamic chamber-CIRAS by 40%. The CO2 evolution rates obtained using the three methods were significantly correlated. None of the three methods was significantly affected by soil moisture or soil temperature. This has been repeatedly observed by others, but is still not fully understood. The difference between air and soil temperature had strong negative effects on both GC methods, but not on the CIRAS system.
机译:在此田间研究中,比较了确定土壤CO 2 释放速率的三种方法:(1)静态室法和(2)动态室法,均采用空气的气相色谱(GC)分析(3)使用便携式红外气体分析仪(CIRAS)的动态腔室系统。田间平均CO 2 演化速率按静态室-GC <动态室-GC <动态室-CIRAS的顺序增加了40%。三种方法获得的CO 2 释放速率具有显着的相关性。三种方法均未受到土壤水分或土壤温度的显着影响。其他人已经反复观察到这一点,但仍未完全理解。空气和土壤温度之间的差异对两种气相色谱方法都具有强烈的负面影响,但对CIRAS系统却没有。

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