首页> 外文期刊>Science of the total environment >Sediment-adsorbed total mercury flux through Yolo Bypass, the primary floodway and wetland in the Sacramento Valley, California
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Sediment-adsorbed total mercury flux through Yolo Bypass, the primary floodway and wetland in the Sacramento Valley, California

机译:通过加利福尼亚州萨克拉曼多山谷的主要洪水道和湿地Yolo旁路的沉积物吸附的总汞通量

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The fate and transport of mercury are of critical concern in lowland floodplains and wetlands worldwide, especially those with a history of upstream mining that increases the mobility of both dissolved and sediment-bound Hg in watersheds. A mass budget of total mercury {THg) quantifies sources and storage for particular areas - knowledge that is required for understanding of management options in lowland floodplains. In order to assess contaminant risk in the largest flood-control bypass, prime wetland, and restoration target in the Sacramento River basin, we estimated empirical relationships between THg, suspended sediment concentration (SSC), and streamflow (Q) for each of the major inputs and outputs using data from various publicly available sources. These relationships were improved by incorporating statistical representations of the dynamics of seasonal and intra-flood exhaustion (hysteresis) of sediment and mercury. Using continuous records of Q to estimate SSC suspended sediment flux and SSC to estimate THg flux, we computed the net transfer of sediment-adsorbed mercury through the Yolo Bypass over a decade, 1993-2003. Flood control weirs spilling Sacramento River floodwaters into the bypass deliver -75% of the water and -50% of the river's suspended sediment load, while one Coast Range tributary of the bypass, Cache Creek, contributes twice the THg load of the mainstem Sacramento. Although estimated sediment flux entering Yolo Bypass is balanced by efflux to the Sacramento/San Francisco Bay-Delta, there is much evidence of deposition and remobilization of sediment in Yolo Bypass during flooding. These factors point to the importance of the bypass as sedimentary reservoir and as an evolving substrate for biogeochemical processing of heavy metals. The estimates of mercury flux suggest net deposition of -500 kg in the 24,000 ha floodway over a decade, dominated by two large floods, representing a storage reservoir for this important contaminant.
机译:在全世界的低地洪泛区和湿地中,尤其是那些上游开采历史悠久,增加了流域中溶解性汞和沉积物结合汞的迁移率的汞,其命运和运输受到了至关重要的关注。总汞预算(THg)量化了特定地区的来源和储存-了解低地洪泛区管理方案所需的知识。为了评估萨克拉曼多河流域最大的防洪旁路,主要湿地和恢复目标中的污染物风险,我们估算了每一个主要水体的总重,悬浮物浓度(SSC)和水流(Q)之间的经验关系。使用来自各种公开来源的数据进行输入和输出。通过结合季节性和洪水内沉积物和汞耗尽的动态(滞后性)的统计表示,改善了这些关系。使用Q的连续记录来估算SSC悬浮泥沙通量和SSC来估算THg通量,我们计算了1993-2003年十年间通过Yolo旁路的泥沙吸附汞的净转移量。萨克拉曼多河洪水溢流到防洪堤中的防洪堰输送了-75%的水和-50%河流的悬浮泥沙量,而旁路的一个海岸支流Cache Creek则贡献了萨克拉曼多主干的THg负荷的两倍。尽管估计的进入Yolo旁路的泥沙通量通过萨克拉曼多/旧金山湾三角洲的外流来平衡,但仍有很多证据表明洪水期间Yolo旁路的沉积物沉积和迁移。这些因素表明,旁路作为沉积物储层和作为重金属生物地球化学处理过程中不断发展的基质的重要性。汞通量的估计值表明,十年来在24,000公顷的洪水道中净沉积了-500千克,其中两次大洪水占主导地位,代表了这种重要污染物的储存库。

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