Open ventilated chamber system for measurements of H2O and CO2 fluxes from the soil surface

Zinaida Iritz , Anders Lindroth , Annemieke Gärdenäs
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引用次数: 38

Abstract

This paper describes the design of a ventilated ‘open’ chamber system for continuous measurement of fluxes of water and carbon dioxide from the soil surface. The system consists of four units: a chamber, an air switching unit, an infrared gas analyzer and a data logger. The chamber has the shape of a rectangular ‘box’ lying on the soil surface covering a ground area of 0.68 m−2. The wind speed through the chamber can be regulated with a fan from zero up to a maximum of about 0.9 m s−1. The soil evaporation measured by the chamber showed good agreement with evaporation measured by a balance. In situ measurement of evaporation by the chamber agreed well with evaporation estimated by a physically-based soil model. The soil water content under the chamber showed good agreement with the simulated values as well as with the water content measured outside the chamber. The magnitude of soil CO2 efflux was in good accordance with other data reported in literature. The main error with this technique was found in the measurement of the air flow through the chamber.

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用于测量土壤表面H2O和CO2通量的开放式通风室系统
本文介绍了一种通风“开”室系统的设计,用于连续测量土壤表面的水和二氧化碳通量。该系统由四个单元组成:一个腔室,一个空气开关单元,一个红外气体分析仪和一个数据记录器。该室的形状为一个矩形“盒子”,位于土壤表面,占地面积为0.68 m−2。风机可调节通过腔室的风速,从0到最大约0.9 m s−1。试验箱测得的土壤蒸发量与天平测得的土壤蒸发量吻合较好。室内测量的蒸发量与基于物理的土壤模型估算的蒸发量非常吻合。试验室内土壤含水量与模拟值及室外实测值吻合较好。土壤CO2外排量与文献报道的其他数据吻合较好。这种技术的主要误差是在测量通过腔室的空气流量时发现的。
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