环境地球化学国家重点实验室知识库

Dynamic flux chambers (DFCs) and micrometeorological (MM) methods are extensively deployed for gauging air-surface Hg-0 gas exchange. However, a systematic evaluation of the precision of the contemporary Hg-0 flux quantification methods is not available. In this study, the uncertainty in Hg-0 flux measured by the relaxed eddy accumulation (REA) method, the aerodynamic gradient method (AGM), the modified Bowen ratio (MBR) method, as well as DFC of traditional (TDFC) and novel (NDFC) designs, are assessed using a robust data set from two field intercomparison campaigns.

The absolute precision in Hg-0 concentration difference (Delta C) measurements is estimated at 0.064 ng m(-3) for the gradient-based MBR and AGM systems. For the REA system, the parameter is Hg-0 concentration (C) dependent at 0.069 + 0.022C. During the campaigns, 57 and 62% of the individual vertical gradient measurements are found to be significantly different from 0, while for the REA technique, the percentage of significant observations is lower. For the chambers, non-significant fluxes are confined to a few night-time periods with varying ambient Hg-0 concentrations. Relative bias for DFC-derived fluxes is estimated to be similar to +/- 10, and similar to 85% of the flux bias is within +/- 2 ng m(-2) h(-1) in absolute terms. The DFC flux bias follows a diurnal cycle, which is largely affected by the forced temperature and irradiation bias in the chambers. Due to contrasting prevailing micrometeorological conditions, the relative uncertainty (median) in turbulent exchange parameters differs by nearly a factor of 2 between the campaigns, while that in Delta C measurement is fairly consistent. The estimated flux uncertainties for the triad of MM techniques are 16-27, 12-23 and 19-31% (interquartile range) for the AGM, MBR and REA methods, respectively. This study indicates that flux-gradient-based techniques (MBR and AGM) are preferable to REA in quantifying Hg-0 flux over ecosystems with low vegetation height. A limitation of all Hg-0 flux measurement systems investigated is their inability to obtain synchronous samples for the calculation of 1 C. This reduces the precision of flux quantification, particularly in the MM systems under non-stationarity of ambient Hg-0 concentration. For future applications, it is recommended to accomplish Delta C derivation from simultaneous collected samples.