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Road-impacted sediment and water in a Lake Ontario watershed and lagoon, City of Pickering, Ontario, Canada: An example of urban basin analysis

机译:加拿大安大略省皮克林市,安大略湖流域和泻湖中受道路影响的沉积物和水:城市流域分析的示例

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The world is increasingly urban but there are few studies of how contaminated water and sediment move through urban basins with their built landscapes and complexly disturbed geology. The central Canadian city of Pickering, Ontario sprawls across a small (27 km~2) densely urbanized (pop: 53,000) watershed and is underlain by Pleistocene glacial sediments and thick artificial fill deposits. Almost 80% of the area is hardened by impervious cover; road and rail lines cover 40% and include Canada's busiest highway (12-lane Highway 401:177,000 vehicles per day in 2003). The basin discharges to Lake Ontario through a small (85 ha) shallow (<3.5 m) lagoon (Frenchman's Bay). A 3-D steady state finite element groundwater numerical model (FEFLOW) was applied to 200 cored and geophysically-logged (gamma and resistivity) boreholes and 3400 digital water wells. It identifies the subsurface stratigraphy and hydrostratigraphic function of deposits and the rates of groundwater flow. Year-round monitoring of groundwater, creek and lagoon water quality shows that transportation infrastructure is the primary source of contaminated water and sediment. Some 7600 tonnes of de-icing salt are applied to watershed roads each year; 52% accumulates in groundwater where it continues to be released as brackish baseflow to creeks in summer. The remainder is rapidly delivered by surface runoff to Frenchman's Bay where chloride contents are more than double the average values in waters across the Great Lakes. Highway 401 is the largest single source of salt contamination to the lagoon; it receives 26% of all road salt applied to the watershed but covers just 1.3% of its area. Prominent spikes in chloride content (>2000 mg L~(-1)) occur during winter thaws in creeks downstream of the highway. Enhanced stream bank erosion as a consequence of flashy storm runoff from road surfaces moves ~ 100 tonnes of contaminated sediment to Frenchman's Bay each year. Instantaneous suspended sediment concentrations in storm runoff are as high as 1600gm~(-3) and loadings of sulphate (SO_4~(-2)) nutrients reach 594 kg h~(-1). Metals and E. coli in road runoff are all elevated well above Canadian water quality standards. These findings underscore findings from other urban areas regardless of regional climate, that transportation corridors are a major global source of contaminated water and sediment.
机译:这个世界越来越城市化,但是很少有关于受污染的水和沉积物如何通过其建筑景观和复杂扰动的地质条件流经城市盆地的研究。加拿大中部安大略省的皮克林市遍布一个很小的(27 km〜2)密集的城市化(人口:53,000)分水岭,其下是更新世的冰川沉积物和厚厚的人工填充沉积物。几乎80%的区域都被不透水的覆盖层硬化了;公路和铁路线占40%,其中包括加拿大最繁忙的高速公路(2003年每天有12条车道的401:177,000辆车)。该盆地通过一个小的(85公顷)浅(<3.5 m)泻湖(法国人湾)排放到安大略湖。将3-D稳态有限元地下水数值模型(FEFLOW)应用于200个有芯和地球物理测井(伽马和电阻率)的钻孔和3400个数字水井。它确定了沉积物的地下地层和水文地层功能以及地下水流量。全年对地下水,小河和泻湖的水质进行监测表明,运输基础设施是污染水和沉积物的主要来源。每年在流域道路上使用约7600吨除冰盐; 52%的水蓄积在地下水中,并在夏季以微咸的底流继续向小河排放。其余部分通过地表径流迅速输送到法国湾,那里的氯化物含量是五大湖中海水平均值的两倍以上。高速公路401是泻湖中最大的盐污染源。它获得了流域所有道路盐分的26%,但仅占其面积的1.3%。公路下游小溪的冬季解冻过程中,氯化物含量明显增加(> 2000 mg L〜(-1))。每年由于路面暴雨径流而导致的河岸侵蚀加剧,每年将约100吨受污染的沉积物运到法国人湾。暴雨径流中的瞬时悬浮沉积物浓度高达1600gm〜(-1),硫酸盐(SO_4〜(-2))养分含量达到594kgh〜(-1)。道路径流中的金属和大肠杆菌的含量都大大高于加拿大的水质标准。这些发现强调了无论区域气候如何,其他城市地区的发现,即运输走廊是全球受污染的水和沉积物的主要来源。

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