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Modeling the biogeochemical cycle of selenium in the San Francisco Bay.

机译:模拟旧金山湾中硒的生物地球化学循环。

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Due to recent concerns about selenium toxicity in the San Francisco Bay and the roles of refinery and San Joaquin River inputs on the selenium cycle, the model ECoS 3 (distributed from Plymouth Marine Laboratory, United Kingdom) was modified to simulate the biogeochemical cycle of selenium in the Northern Reach. The model is designed to simulate salinity, total suspended material, phytoplankton concentrations, dissolved selenium and its speciation (selenite, selenate, and organic selenide), and particulate selenium and its speciation (selenite + selenate, elemental selenium, and organic selenide). Actual data from 1999 were used to calibrate the model, while data from other sampling periods (1986–1988 and 1997–1998) were then compared to model simulations to verify its accuracy. The sensitivity of the model to specific inputs of selenium was also determined. These results indicate that dissolved selenium is largely controlled by riverine and refinery inputs, while particulate selenium is a function of phytoplankton productivity and riverine inputs of sediment. Forecasting simulations included increasing the San Joaquin River discharge to the Delta and varying refinery discharges to the Bay. These simulation results indicate that total particulate selenium concentrations may increase in the entire Bay to 1 μg g−1 if the San Joaquin Flow is increased. This concentration is twice as high as the current estuarine average particulate selenium and at the level where the concentration of selenium in Potomocorbula amurensis becomes problematic for estuarine predators. Furthermore, simulations suggest that doubling the current refinery loads as selenate have little effect on the particle-associated selenium in the estuary. Simulated data from the model can be used in other models to predict selenium concentrations in higher trophic levels. Furthermore the model can be used as a template to study the biogeochemical cycle of other elements in well-mixed estuaries, and in restoration projects, pollution control and other trophic transfer scenarios.
机译:由于最近对旧金山湾中硒的毒性以及精炼厂和圣华金河投入物在硒循环中的作用的担忧,因此对模型ECoS 3(由英国普利茅斯海洋实验室分配)进行了修改,以模拟硒的生物地球化学循环。在北部河段。该模型旨在模拟盐度,总悬浮物,浮游植物的浓度,溶解的硒及其形态(硒,硒酸盐和有机硒化物),颗粒硒及其形态(硒+硒酸盐,元素硒和有机硒)。使用1999年的实际数据来校准模型,然后将其他采样期间(1986-1988年和1997-1998年)的数据与模型仿真进行比较,以验证其准确性。还确定了模型对特定硒输入的敏感性。这些结果表明,溶解的硒在很大程度上受河流和精炼厂投入的控制,而硒颗粒则是浮游植物生产力和河流沉积物投入的函数。预测模拟包括增加圣华金河到三角洲的排放量以及改变炼油厂到海湾的排放量。这些模拟结果表明,如果增加圣华金流量,整个海湾中的总硒颗粒浓度可能会增加到1μgg -1 。该浓度是当前河口平均颗粒硒的两倍,并且在<斜体> Potomocorbula amurensis 中的硒浓度对河口捕食者造成问题的水平。此外,模拟表明,将当前精炼厂负荷(含硒量)增加一倍,对河口与颗粒相关的硒影响不大。来自该模型的模拟数据可用于其他模型,以预测较高营养水平的硒浓度。此外,该模型可以用作研究在充分混合的河口以及修复项目,污染控制和其他营养转移方案中其他元素的生物地球化学循环的模板。

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