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农业和管理湿地中的汞循环:综合野外研究中甲基汞生成、水文输出和生物累积的综合分析。

Mercury cycling in agricultural and managed wetlands: a synthesis of methylmercury production, hydrologic export, and bioaccumulation from an integrated field study.

机构信息

U.S. Geological Survey, Western Region Branch of Regional Research, 345 Middlefield Road/MS 480, Menlo Park, CA 94025, USA.

U.S. Geological Survey, California Water Science Center, 6000 J St, Placer Hall, Sacramento, CA 95819, USA.

出版信息

Sci Total Environ. 2014 Jun 15;484:221-31. doi: 10.1016/j.scitotenv.2014.01.033. Epub 2014 Feb 14.

DOI:10.1016/j.scitotenv.2014.01.033
PMID:24530187
Abstract

With seasonal wetting and drying, and high biological productivity, agricultural wetlands (rice paddies) may enhance the conversion of inorganic mercury (Hg(II)) to methylmercury (MeHg), the more toxic, organic form that biomagnifies through food webs. Yet, the net balance of MeHg sources and sinks in seasonal wetland environments is poorly understood because it requires an annual, integrated assessment across biota, sediment, and water components. We examined a suite of wetlands managed for rice crops or wildlife during 2007-2008 in California's Central Valley, in an area affected by Hg contamination from historic mining practices. Hydrologic management of agricultural wetlands for rice, wild rice, or fallowed - drying for field preparation and harvest, and flooding for crop growth and post-harvest rice straw decay - led to pronounced seasonality in sediment and aqueous MeHg concentrations that were up to 95-fold higher than those measured concurrently in adjacent, non-agricultural permanently-flooded and seasonally-flooded wetlands. Flooding promoted microbial MeHg production in surface sediment of all wetlands, but extended water residence time appeared to preferentially enhance MeHg degradation and storage. When incoming MeHg loads were elevated, individual fields often served as a MeHg sink, rather than a source. Slow, horizontal flow of shallow water in the agricultural wetlands led to increased importance of vertical hydrologic fluxes, including evapoconcentration of surface water MeHg and transpiration-driven advection into the root zone, promoting temporary soil storage of MeHg. Although this hydrology limited MeHg export from wetlands, it also increased MeHg exposure to resident fish via greater in situ aqueous MeHg concentrations. Our results suggest that the combined traits of agricultural wetlands - slow-moving shallow water, manipulated flooding and drying, abundant labile plant matter, and management for wildlife - may enhance microbial methylation of Hg(II) and MeHg exposure to local biota, as well as export to downstream habitats during uncontrolled winter-flow events.

摘要

受季节性湿润和干燥以及高生物生产力的影响,农业湿地(稻田)可能会促进无机汞(Hg(II))向甲基汞(MeHg)的转化,后者是毒性更强的有机形式,通过食物网进行生物放大。然而,由于需要对生物群、沉积物和水成分进行年度综合评估,因此对季节性湿地环境中 MeHg 源和汇的净平衡仍了解甚少。我们在 2007-2008 年期间检查了加利福尼亚中央山谷中一系列用于种植水稻或野生动物的湿地,该地区受到历史采矿作业造成的汞污染的影响。为种植水稻、野生水稻或休耕(用于田地准备和收获的干燥以及用于作物生长和收获后稻草腐烂的洪水)而对农业湿地进行的水文管理导致沉积物和水相中 MeHg 浓度出现明显季节性,其浓度比相邻非农业永久性洪水湿地和季节性洪水湿地中同时测量的浓度高 95 倍。洪水促进了所有湿地表层沉积物中微生物 MeHg 的产生,但延长的水停留时间似乎优先增强了 MeHg 的降解和储存。当输入的 MeHg 负荷增加时,个别田地通常充当 MeHg 汇,而不是源。农业湿地中浅层水的缓慢水平流动导致垂直水文通量的重要性增加,包括地表水 MeHg 的蒸发浓缩和蒸腾作用驱动的向根区的平流,促进了 MeHg 在土壤中的临时储存。尽管这种水文学限制了 MeHg 从湿地中的输出,但它也通过增加原位水相中 MeHg 浓度,增加了 MeHg 对当地生物的暴露。我们的研究结果表明,农业湿地的综合特征——缓慢移动的浅水、人为的洪水和干燥、丰富的易生物降解植物物质以及对野生动物的管理——可能会促进 Hg(II)的微生物甲基化和 MeHg 暴露当地生物群以及在不受控制的冬季水流事件期间向下游栖息地的输出。

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