Desert Research Institute, Division of Atmospheric Sciences, 2215 Raggio Parkway, Reno, NV 89512, United States.
Desert Research Institute, Division of Hydrologic Sciences, 2215 Raggio Parkway, Reno, NV 89512, United States.
Sci Total Environ. 2016 Oct 15;568:522-535. doi: 10.1016/j.scitotenv.2015.11.104. Epub 2016 Jan 8.
A synthesis of published vegetation mercury (Hg) data across 11 contiguous states in the western United States showed that aboveground biomass concentrations followed the order: leaves (26μgkg(-1))~branches (26μgkg(-1))>bark (16μgkg(-1))>bole wood (1μgkg(-1)). No spatial trends of Hg in aboveground biomass distribution were detected, which likely is due to very sparse data coverage and different sampling protocols. Vegetation data are largely lacking for important functional vegetation types such as shrubs, herbaceous species, and grasses. Soil concentrations collected from the published literature were high in the western United States, with 12% of observations exceeding 100μgkg(-1), reflecting a bias toward investigations in Hg-enriched sites. In contrast, soil Hg concentrations from a randomly distributed data set (1911 sampling points; Smith et al., 2013a) averaged 24μgkg(-1) (A-horizon) and 22μgkg(-1) (C-horizon), and only 2.6% of data exceeded 100μgkg(-1). Soil Hg concentrations significantly differed among land covers, following the order: forested upland>planted/cultivated>herbaceous upland/shrubland>barren soils. Concentrations in forests were on average 2.5 times higher than in barren locations. Principal component analyses showed that soil Hg concentrations were not or weakly related to modeled dry and wet Hg deposition and proximity to mining, geothermal areas, and coal-fired power plants. Soil Hg distribution also was not closely related to other trace metals, but strongly associated with organic carbon, precipitation, canopy greenness, and foliar Hg pools of overlying vegetation. These patterns indicate that soil Hg concentrations are related to atmospheric deposition and reflect an overwhelming influence of plant productivity - driven by water availability - with productive landscapes showing high soil Hg accumulation and unproductive barren soils and shrublands showing low soil Hg values. Large expanses of low-productivity, arid ecosystems across the western U.S. result in some of the lowest soil Hg concentrations observed worldwide.
对美国西部 11 个相邻州发表的植被汞(Hg)数据进行综合分析表明,地上生物量浓度的顺序为:叶片(26μgkg(-1))~树枝(26μgkg(-1))>树皮(16μgkg(-1))>树干木材(1μgkg(-1))。未检测到地上生物量分布中 Hg 的空间趋势,这可能是由于数据覆盖范围非常稀疏且采样方案不同。灌木、草本物种和草等重要功能植被类型的植被数据基本缺失。从已发表的文献中收集的土壤浓度在美国西部很高,有 12%的观测值超过 100μgkg(-1),反映了偏向于在富含 Hg 的地点进行调查的倾向。相比之下,来自随机分布数据集(1911 个采样点;Smith 等人,2013a)的土壤 Hg 浓度平均值为 24μgkg(-1)(A 层)和 22μgkg(-1)(C 层),只有 2.6%的数据超过 100μgkg(-1)。土壤 Hg 浓度在不同的土地覆被之间存在显著差异,顺序为:林地>种植/栽培>草本林地/灌丛>贫瘠土壤。森林中的浓度平均比贫瘠地区高 2.5 倍。主成分分析表明,土壤 Hg 浓度与模型化的干和湿 Hg 沉积以及与采矿、地热区和燃煤电厂的接近程度无关或关系较弱。土壤 Hg 分布也与其他痕量金属关系不大,但与有机碳、降水、冠层绿色度和覆盖植被的叶片 Hg 库密切相关。这些模式表明,土壤 Hg 浓度与大气沉降有关,反映了植物生产力的巨大影响——由水分供应驱动——生产力高的景观显示出高的土壤 Hg 积累,而生产力低的贫瘠土壤和灌丛则显示出低的土壤 Hg 值。美国西部广大的低生产力、干旱生态系统导致了全球观察到的最低土壤 Hg 浓度之一。