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Multi-year water balance assessment of a newly constructed wetland, Fort McMurray, Alberta

机译:新建湿地艾伯塔省麦克默里堡的多年水平衡评估

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Oil sands mining in Alberta transforms the boreal landscape of forests and wetlands into open pits, tailings ponds and overburden piles. Whereas reclamation efforts have primarily focused on upland forests, rebuilding wetland systems has recently become a motivation for research. Wetland creation and sustainability in this region is complicated by the sub-humid climate and salinity of underlying mining material. In 2012, Syncrude Canada Ltd. completed the construction of the Sandhill Fen Watershed (SFW), a 52-ha upland-wetland system to evaluate wetland reclamation strategies on soft tailings. SFW includes an active pumping system, upland hummocks, a fen wetland and underdrains. To evaluate the influence of management practices on the hydrology of the system, this study reports the water balance from January 2013 to December 2014, the first 2 years after commissioning. A semi-distributed approach was taken to examine the fluxes and stores of water in uplands and lowlands. Natural and artificial inputs and outputs were measured using a series of precipitation gauges and pumps, and evapotranspiration was quantified using three eddy covariance towers. A series of near surface wells recorded water table position. Both 2013 and 2014 were normal rainfall years, with 2013 having more and 2014 less snow than normal. In 2013, inflow/outflow from pumping was the predominant hydrological fluxes, resulting in considerable variability in water table position and storage changes throughout the summer. In 2014, the artificial addition of water was negligible, yet the water table remained near the surface in lowland locations, suggesting that wetland conditions could be maintained under current conditions. Evapotranspiration rates between uplands and lowlands were similar between years and sites, ranging from 2.2 ± 1.8 to 2.5 ± 1.2 mm/day and were largely controlled by climate. These rates were less than nearby older upland systems, suggesting that water balance partitioning will change as vegetation develops. Comparison between years and with natural systems provides insight on how management practices influence hydrologic dynamics and the overall water balance of the SFW. Copyright © 2016 John Wiley & Sons, Ltd.
机译:艾伯塔省的油砂开采将森林和湿地的北方景观转变为裸露的矿坑,尾矿池和覆土堆。尽管开垦工作主要集中在陆地上的森林,但重建湿地系统最近已成为研究的动力。亚湿气候和底层采矿材料的盐度使该地区的湿地创造和可持续发展变得复杂。 2012年,加拿大Syncrude Ltd.公司完成了52公顷的高地湿地系统Sandhill Fen分水岭(SFW)的建设,以评估软尾矿的湿地开垦策略。 SFW包括一个主动抽水系统,高地山丘,一片芬湿地和暗地。为了评估管理实践对系统水文学的影响,本研究报告了调试后头2年的2013年1月至2014年12月的水平衡。采用半分布式方法来检查高地和低地的水通量和水位。使用一系列的降水量表和抽水机测量自然和人工的投入和产出,并使用三个涡流协方差塔对蒸散量进行量化。一系列近地表井记录了地下水位。 2013年和2014年均为正常降雨年份,2013年的降雪量高于2014年,而2014年的降雪量少于正常年份。 2013年,抽水的流入/流出是主要的水文通量,导致整个夏季的地下水位位置和储水量变化很大。在2014年,人工添加的水可以忽略不计,但地下水位仍然在低地位置附近的地表,这表明在当前条件下可以保持湿地条件。年份和地点之间,高地和低地之间的蒸散速率相似,范围为2.2±1.8至2.5±1.2 mm /天,并且很大程度上受气候控制。这些比率低于附近的较早的旱地系统,表明水平衡分配将随着植被的发展而变化。几年之间以及与自然系统之间的比较提供了有关管理实践如何影响水文学动态和SFW总体水平衡的见解。版权所有©2016 John Wiley&Sons,Ltd.

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