CNR-Institute of Atmospheric Pollution Research, c/o: UNICAL-Polifunzionale, 87036 Rende, Italy.
Environ Res. 2013 Aug;125:69-74. doi: 10.1016/j.envres.2013.02.004. Epub 2013 Mar 8.
Atmospheric mercury emissions from mine-waste enriched soils were measured in order to compare the mercury fluxes of bare soils with those from other soils covered by native grasses. Our research was conducted near Mt. Amiata in central Italy, an area that was one of the largest and most productive mining centers in Europe up into the 1980s. To determine in situ mercury emissions, we used a Plexiglas flux chamber connected to a portable mercury analyzer (Lumex RA-915+). This allowed us to detect, in real time, the mercury vapor in the air, and to correlate this with the meteorological parameters that we examined (solar radiation, soil temperature, and humidity). The highest mercury flux values (8000ngm(-2)h(-1)) were observed on bare soils during the hours of maximum insulation, while lower values (250ngm(-2)h(-1)) were observed on soils covered by native grasses. Our results indicate that two main environmental variables affect mercury emission: solar radiation intensity and soil temperature. The presence of native vegetation, which can shield soil surfaces from incident light, reduced mercury emissions, a result that we attribute to a drop in the efficiency of mercury photoreduction processes rather than to decreases in soil temperature. This finding is consistent with decreases in mercury flux values down to 3500ngm(-2)h(-1), which occurred under cloudy conditions despite high soil temperatures. Moreover, when the soil temperature was 28°C and the vegetation was removed from the experimental site, mercury emissions increased almost four-fold. This increase occurred almost immediately after the grasses were cut, and was approximately eight-fold after 20h. Thus, this study demonstrates that enhancing wild vegetation cover could be an inexpensive and effective approach in fostering a natural, self-renewing reduction of mercury emissions from mercury-contaminated soils.
为了比较裸露土壤和覆盖有本地草的土壤的汞通量,测量了富含矿山废物的土壤中的大气汞排放。我们的研究在意大利中部的阿米亚塔山附近进行,该地区是 20 世纪 80 年代以前欧洲最大、生产力最高的采矿中心之一。为了确定原地汞排放,我们使用了一个与便携式汞分析仪(Lumex RA-915+)相连的有机玻璃通量室。这使我们能够实时检测空气中的汞蒸气,并将其与我们检查的气象参数(太阳辐射、土壤温度和湿度)相关联。在最大绝热时间,裸露土壤上的汞通量值最高(8000ngm(-2)h(-1)),而覆盖有本地草的土壤上的汞通量值较低(250ngm(-2)h(-1))。我们的结果表明,两个主要的环境变量影响汞排放:太阳辐射强度和土壤温度。本地植被的存在可以使土壤表面免受入射光的影响,从而减少汞排放,我们将这一结果归因于汞光还原过程效率的降低,而不是土壤温度的降低。这一发现与在多云条件下,汞通量值下降到 3500ngm(-2)h(-1)的情况一致,尽管土壤温度较高。此外,当土壤温度为 28°C 且从实验地点除去植被时,汞排放增加了近四倍。这种增加几乎是在草被切断后立即发生的,20 小时后约增加了八倍。因此,这项研究表明,增加野生植被覆盖率可能是一种廉价且有效的方法,可以促进受汞污染土壤的自然、自我更新的汞排放量减少。