首页> 外文期刊>Hydrological ProcHydrological Processesrnesses >SULPHATE DYNAMICS IN RELATION TO GROUNDWATER–SURFACE WATER INTERACTIONS IN HEADWATER WETLANDS OF THE SOUTHERN CANADIAN SHIELD
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SULPHATE DYNAMICS IN RELATION TO GROUNDWATER–SURFACE WATER INTERACTIONS IN HEADWATER WETLANDS OF THE SOUTHERN CANADIAN SHIELD

机译:与加拿大南部盾构源湿地地下水-地表水相互作用相关的硫酸盐动力学

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The spatial and temporal distribution of sulphate (SO) concentrations in peat pore water and the outlet streams of two forested swamps was related to variations in the magnitude of upland runoff, wetland water levels and flow path. The swamps were located in headwater catchments with contrasting till depths typical of the southern Canadian Shield. Inputs of SO from shallow hillslope tills and streams showed little seasonal variation in either source or concentration in both swamps. Sulphate dynamics at the outlet stream reflected hydrological and biogeochemical processes within the valley wetlands, which in turn were partly controlled by catchment hydrogeology. During high runoff, maximum water table elevations and peak surface flow in the swamps resulted in upland inputs largely bypassing anoxic peat. Consequently, SO concentrations of 8–10 mg/l at the swamp outlets were similar to stream and groundwater inputs. During periods of low flow, concentrations of SO at the swamp outlets declined to less than 3 mg/l. At this time lower water table elevations resulted in increased interaction of input water with anoxic peats, and therefore, SO reduction. Contrasts in till depth and the nature of groundwater flow between catchments resulted in differences in SO dynamics between years and swamps. In dry summers the absence of groundwater inputs to the swamp in the catchment with thin till resulted in a large water table drawdown and re-oxidation of accumulated S, which contributed to maximum SO concentrations (up to 35 mg/l) during storm runoff. Continuous groundwater input to the swamp in the catchment with deeper till was critical to maintaining saturated surfaces and efficient SO retention during both dry and wet summers. A conceptual model of wetland SO retention and export, based on catchment hydrogeology, is developed to generalize the SO dynamics of valley bottom wetlands at the landscape scale. © 1997 by John Wiley & Sons, Ltd.
机译:泥炭孔隙水和两个森林沼泽的出口溪流中硫酸盐(SO)浓度的时空分布与山地径流大小,湿地水位和流径的变化有关。沼泽位于源头流域,与加拿大南部盾构的典型深度形成对比。在两个沼泽中,来自浅坡耕作和溪流的SO的输入在来源或浓度上均显示出很小的季节性变化。出口处的硫酸盐动力学反映了山谷湿地内的水文和生物地球化学过程,而这些反过来又部分受流域水文地质控制。在高径流期间,沼泽中最大的地下水位高程和峰值地表流量导致高地投入物很大程度上绕过缺氧泥炭。因此,沼泽出口处的SO浓度为8-10 mg / l,与溪流和地下水输入量相似。在低流量期间,沼泽出口处的SO浓度降至3 mg / l以下。此时较低的地下水位高度导致进水与缺氧泥炭的相互作用增加,因此SO降低。集水区之间的耕作深度和地下水流性质的对比导致年份和沼泽之间SO动态的差异。在干燥的夏季,缺乏流向沼泽地的沼泽的地下水输入不足,导致地下水位下降,积累的S重新氧化,这导致暴雨径流中的最大SO浓度(高达35 mg / l)。在干旱和潮湿的夏季,连续不断地向集水区的沼泽中不断输入地下水对于维持饱和表面和有效地保留二氧化硫至关重要。建立了基于集水区水文地质学的湿地SO保留和输出的概念模型,以概括景观尺度下谷底湿地的SO动力学。 ©1997,John Wiley&Sons,Ltd.版权所有。

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