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Variations of mercury in the inflow and outflow of a constructed treatment wetland in south Florida, USA

机译:美国佛罗里达州南部人工湿地的流入和流出中汞的变化

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Variations of total mercury (THg) and methylmercury (MeHg) concentrations at the inflow and outflow of a constructed treatment wetland, Stormwater Treatment Area 2 (STA-2) in south Florida were investigated from 2000 to 2011. The linkages between inflow water quality parameters and outflow THg and MeHg concentrations were assessed. THg and MeHg concentrations at the outflow in 2001 (2.88 and 0.95 ng L~(-1)) and 2002 (2.33 and 0.87 ngL~(-1)) were significantly greater than those (1.14 and 0.14ngL~(-1), 1.16 and 0.12 ng L~(-1) , respectively) at the inflow during the same time period. This was due to dryout and rewetting which may lead to Hg release from soil and promote Hg methylation. The average concentrations (0.75 and 0.11 ngL~(-1)) of THg and MeHg at the outflow from 2005 to 2011 (except 2007) were lower than those (1.00 and 0.13 ngL~(-1)) at the inflow, indicating that net THg and MeHg retention occurred in STA-2 during those years, which ranged from 0.35% to 49% for THg and from 3.5% to 37% for MeHg, respectively. Stepwise regression identified several inflow water quality parameters which explained 68% and 58% of the variances in the outflow THg and MeHg concentrations from 2000 to 2011. Certain inflow quality parameters were strong predictors of the variations in outflow THg and MeHg concentrations. These parameters included sulfate, chloride, dissolved organic carbon (DOC), dissolved oxygen (DO), pH, and temperature for outflow THg; and sulfate, chloride, DOC, and DO for outflow MeHg. Inflow sulfate and DO concentrations separately exhibited significant correlations with outflow THg and MeHg concentrations only prior to 2004. The results indicate that STA-2 was a source of THg and MeHg during early years of operation and a sink for THg and MeHg when the wetland passed the initial operation period and especially as water management improved to prevent dryout from occurring. Findings from this study also underscore the important role of inflow water quality to the variations of the outflow THg and MeHg concentrations.
机译:研究了2000年至2011年佛罗里达州南部的人工处理湿地雨水处理区2(STA-2)的流入和流出处总汞(THg)和甲基汞(MeHg)浓度的变化。流入水质量参数之间的联系并评估流出的THg和MeHg浓度。在2001年(2.88和0.95 ng L〜(-1))和2002(2.33和0.87 ngL〜(-1))流出时的THg和MeHg浓度显着高于(1.14和0.14ngL〜(-1)),在同一时间段的流入量分别为1.16和0.12 ng L〜(-1)。这是由于干燥和重新润湿可能导致汞从土壤中释放出来并促进汞甲基化。 2005年至2011年(2007年除外)出水的THg和MeHg的平均浓度(0.75和0.11 ngL〜(-1))低于入流的THg和MeHg的平均浓度(1.00和0.13 ngL〜(-1)),表明在这些年中,STA-2的净THg和MeHg保留率分别为THg的0.35%至49%和MeHg的3.5%至37%。通过逐步回归确定了几个流入水水质参数,这些参数解释了2000年至2011年流出THg和MeHg浓度的68%和58%。某些流入水质参数是流出THg和MeHg浓度变化的有力预测指标。这些参数包括硫酸盐,氯化物,溶解有机碳(DOC),溶解氧(DO),pH和流出温度THg。硫酸盐,氯化物,DOC和DO用于流出MeHg。仅在2004年之前,硫酸盐和溶解氧的流入浓度才分别与流出的三价汞和甲基汞显着相关。结果表明,STA-2在运行初期是湿气和甲基汞的来源,而当湿地通过时则是三价汞和甲基汞的汇。初始运行期间,尤其是随着水管理的改善,以防止发生干透。这项研究的结果还强调了流入水水质对流出水THg和MeHg浓度变化的重要作用。

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