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A multichannel automated chamber system for continuous measurement of forest soil CO2 efflux

机译:多通道自动室系统,可连续测量森林土壤二氧化碳排放量

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We developed a fast-response multi-chamber system for measuring soil-surface CO2 efflux (F.). The chambers (90 x 90 x 50 cm, L x W x H) had lids that opened and closed automatically, and were connected in parallel to a single CO2 analyzer equipped with a 16-channel gas sampler. Between measurements the chamber lids were raised to allow precipitation and leaf litter to reach the enclosed soil surface. When a chamber was closed, it was ventilated with well-buffered ambient air (125 1 min(-1)) that entered by an inlet on one chamber sidewall and exited through a large vent on the opposite sidewall. The pressure difference between the inside and outside of the chamber was less than 0.22 Pa. Two additional mixing fans maintained an air speed of 0.3 +/- 0.1 in s(-1) at 20 cm above the soil surface. Air was withdrawn continuously from the inlets and outlets of each chamber, and fed sequentially to an infrared CO2 analyzer. With this system, we measured F-c in a 40-year-old temperate Pinus densiflora Sieb. & Zucc. forest from February 8 to May 30, 2001. Mean F, increased steadily from 0.9 mumol m(-2) s(-1) at the beginning of February to 4.6 mumol m(-2) s(-1) by the end of May. There was a statistically significant correlation between F-c and surface soil temperature (r = 0.896; P < 0.0001), and the Q(10) value was 2.8. Spatial variation of F-c was higher in the non-growing season than in the growing season. Measurements were not interrupted by either rain or snow.
机译:我们开发了一种用于测量土壤表面CO2排放(F.)的快速响应多室系统。室(90 x 90 x 50厘米,长x宽x高)有自动打开和关闭的盖,并与配有16通道气体采样器的单个CO2分析仪并联连接。在两次测量之间,将室盖抬高以使降水和枯枝落叶到达封闭的土壤表面。当一个腔室关闭时,用缓冲良好的环境空气(125 1 min(-1))通风,该空气通过一个腔室侧壁上的入口进入,并通过相对侧壁上的大排气孔排出。室内和室外之间的压力差小于0.22 Pa。两个额外的混合风扇在土壤表面上方20 cm处保持s(-1)的空气速度为0.3 +/- 0.1 ins(-1)。从每个腔室的入口和出口连续抽出空气,然后依次送入红外CO2分析仪。借助该系统,我们在40岁的温带松柏(Pinus densiflora Sieb)中测量了F-c。 &Zucc。森林从2001年2月8日至5月30日。平均F值从2月初的0.9 mumol m(-2)s(-1)稳定增加到2000年底的4.6 mumol m(-2)s(-1)。可能。 F-c与地表土壤温度之间存在统计学上的显着相关性(r = 0.896; P <0.0001),并且Q(10)值为2.8。在非生长季节,F-c的空间变化高于生长季节。测量没有被雨或雪打断。

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