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Calculations of automatic chamber flux measurements of methane and carbon dioxide using short time series of concentrations

机译:用短时间序列计算甲烷和二氧化碳自动腔室通量测量的计算

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The closed chamber technique is widely used to measure the exchange of methane (CHsub4/sub) and carbon dioxide (COsub2/sub) from terrestrial ecosystems. There is, however, large uncertainty about which model should be used to calculate the gas flux from the measured gas concentrations. Due to experimental uncertainties the simple linear regression model (first-order polynomial) is often applied, even though theoretical considerations of the technique suggest the application of other, curvilinear models. High-resolution automatic chamber systems which sample gas concentrations several hundred times per flux measurement make it possible to resolve the curvilinear behavior and study the information imposed by the natural variability of the temporal concentration changes. We used more than 50?000 such flux measurements of CHsub4/sub and COsub2/sub from five field sites located in peat-forming wetlands ranging from 56 to 78°?N to quantify the typical differences between flux estimates of different models. In addition, we aimed to assess the curvilinearity of the concentration time series and test the general applicability of curvilinear models. Despite significant episodic differences between the calculated flux estimates, the overall differences are generally found to be smaller than the local flux variability on the plot scale. The curvilinear behavior of the gas concentrations within the chamber is strongly influenced by wind-driven chamber leakage, and less so by changing gas concentration gradients in the soil during chamber closure. Such physical processes affect both gas species equally, which makes it possible to isolate biochemical processes affecting the gases differently, such as photosynthesis limitation by chamber headspace COsub2/sub concentrations under high levels of incoming solar radiation. We assess the possibility to exploit this effect for a partitioning of the net COsub2/sub flux into photosynthesis and ecosystem respiration as an example of how high-resolution automatic chamber measurements could be used for purposes beyond the estimation of the net gas flux. This shows that while linear and curvilinear calculation schemes can provide similar net fluxes, only curvilinear models open additional possibilities for high-resolution automatic chamber measurements.
机译:封闭的腔室技术被广泛用于测量甲烷(CH <亚> 4 )和二氧化碳(CO 2 )的交换从地面生态系统。然而,存在大的不确定性关于哪种模型应该用于计算来自测量的气体浓度的气体通量。由于实验性不确定性,即使技术的理论考虑因素建议应用其他曲线模型,通常应用简单的线性回归模型(一阶多项式)。每个通量测量的样品气体浓度几百次的高分辨率自动腔室系统使得可以解决曲线行为并研究通过时间浓度变化的自然变化而施加的信息。我们使用超过50 000 000 000 000 000 000次的CH 4 和CO 2 ,其五个场地位于泥炭形成湿地的五个场地,范围为56至78°(以量化)不同模型的磁通估计之间的典型差异。此外,我们旨在评估浓度时间序列的曲线性并测试曲线模型的一般适用性。尽管计算出的磁通估计之间存在显着的情节差异,但总体差异通常被发现小于绘图规模上的局部通量变异性。腔室内的气体浓度的曲线行为受风室泄漏的强烈影响,并且通过在室内闭合期间改变土壤中的气体浓度梯度而较少。这种物理过程同样影响两种气体物质,这使得可以分离不同地影响气体的生物化学过程,例如在高水平的进入的太阳辐射下的腔室顶空CO 2浓度的光合作用限制。我们评估了利用这种效果的可能性,将净CO 2 通量分配到光合作用和生态系统呼吸中,作为高分辨率自动腔室测量的示例,可以用于超出估计的目的净气体通量。这表明,虽然线性和曲线计算方案可以提供类似的净磁通,但只有曲线模型开启了高分辨率自动腔室测量的其他可能性。

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