Pollutant migration from two sanitary landfill sites near Sarnia, Ontario
Pollutant migration from two sanitary landfill sites near Sarnia, Ontario
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DOI：
10.1139/t77-023
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发表时间：
1977-05
影响因子：
3.6
通讯作者：
D. Goodall;R. Quigley
中科院分区：
文献类型：
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作者：
D. Goodall;R. Quigley
通过从谢尔比管样品中挤压孔隙水，并通过吸收火焰光度法分析这些水中的Ca++， Mg++， Na+和K+，获得了位于安大略省萨尼亚附近的两个年轻的垃圾填埋场的污染概况。在这两个地点都观察到污染锋，污染物阳离子浓度随着距离正常背景值的距离而衰减。较老的垃圾填埋场约有7年的历史，建立在风化壳下5.6 m深的完整粉质粘土上，其特征是从填充物底部向下流动梯度。污染（阳离子）向下迁移了30厘米的距离，而计算出的渗流锋的最大可能推进距离仅为4厘米。较年轻的垃圾填埋场大约有2.5年的历史，建立在风化和裂隙土壤的地壳中2.3 m的深度，其特征是由于大堆废物产生的重物向上流入垃圾填埋场。污染迁移有过程……
Contamination profiles below two youthful landfills founded on thick silty clay deposits near Sarnia, Ontario were obtained by squeezing pore water from Shelby tube samples and analyzing this water by absorption flame photometry for Ca++, Mg++, Na+, and K+. Pollution fronts were observed below both sites, the contaminant cation concentrations attenuating with distance to normal background values.The older landfill was about 7 years old, was founded at 5.6 m depth below the weathered crust on intact silty clays, and was characterized by a downward flow gradient from the base of the fill. Pollution (cation) migration had proceeded downwards for a distance of 30 cm compared to the calculated maximum possible advance of the seepage front of only 4 cm.The younger landfill was about 2.5 years old, was founded at 2.3 m depth within the crust on weathered and fissured soils, and was characterized by upward flow into the landfill due to heavy loads created by the large mound of waste. Pollution migration had proce...