首页> 外文期刊>Hydrological ProcHydrological Processesrnesses >ROAD SALT ACCUMULATION IN HIGHWAY SNOW BANKS AND TRANSPORT THROUGH THE UNSATURATED ZONE OF THE OAK RIDGES MORAINE, SOUTHERN ONTARIO
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ROAD SALT ACCUMULATION IN HIGHWAY SNOW BANKS AND TRANSPORT THROUGH THE UNSATURATED ZONE OF THE OAK RIDGES MORAINE, SOUTHERN ONTARIO

机译:安大略省南部橡树岭冰SAT的未饱和带中公路雪岸中的盐分积累和运输

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摘要

Pathways and fate of road deicing salt (NaCl) applied during the 1994–1995 winter were studied for a 14-km section of a major highway that crosses the Oak Ridges Moraine in southern Ontario. Total salt applications over the winter ranged from 29 to 74 kg m of highway, and NaCl concentrations in snow banks adjacent to the roadway reached 9400 mg l during the later stages of snow cover development. This salt was released to the ground surface during snowmelt. Sodium chloride (NaCl) loadings to soil from snow cover during the final melt phase were relatively uniform along the study section (3–5 kg NaCl m of highway). However, the snowpack at all transects retained <50% of applied NaCl, and this shortfall probably reflected direct runoff and infiltration of saline meltwater from the road surface into the adjacent shoulder and right-of-way. Cation exchange with Ca in near-surface soils most likely resulted in preferential retention of Na relative to Cl, although total storage of NaCl in upper soil horizons by winter's end was <15% of deicing salt applications. An environmental tracer (O) was used to trace movement of saline meltwater through the unsaturated zone underlying the highway. Average meltwater particle velocities at a site underlain by loam soils were 0.02 m d, and 280 mm of water was displaced below a depth of 1.86 m over a 78-day period in the spring and summer of 1995. Sodium ion and chloride ion concentrations in water sampled in late summer 1995 at depths >2 m exceeded 500 mg l and 1000 mg l, respectively. Approximately 75% of the net flux of NaCl below the upper soil was retained in the 0–2.8 m depth interval at this site, and results from more permeable soils traversed by the highway indicate an even greater penetration of the annual NaCl application into the unsaturated zone along the moraine. This saline water likely recharges groundwater in this portion of the Oak Ridges Moraine.
机译:研究了1994-1995年冬季使用的道路除冰盐(NaCl)的路径和结局,该道路横穿安大略省南部Oak Ridges冰Ridge的一条主要公路长达14公里。整个冬季,盐的总施用量为29至74 kgkg·m的高速公路,在雪盖发育的后期,与道路相邻的雪堆中的NaCl浓度达到9400 mg / l。在融雪期间,该盐释放到地面。在最终的融化阶段,从雪盖到土壤中的氯化钠(NaCl)在研究区域内相对均匀(3-5 kg kg NaCl m公路)。但是,所有断面的积雪都保留了施用的NaCl的<50%,这一不足可能反映了盐水融水的直接径流和渗透,从路面到相邻路肩和通行道路。尽管到冬季结束时,上部土壤层中NaCl的总储存量不到结冰盐施用量的15%,但在近地表土壤中与Ca进行阳离子交换最有可能导致Na相对于Cl的优先保留。使用环境示踪剂(O)跟踪盐水融化水通过高速公路下方的非饱和区的运动。在1995年的春季和夏季,在壤土覆盖的某个地点的平均融水颗粒速度为0.02μm·d,并且在长达78天的时间里,有280μm的水被置换到1.86μm的深度以下。 1995年夏末,>2μm深度的水分别超过500μg/ l和1000μg/ l。在该位置,上部土壤下面的NaCl净通量的大约75%保留在0-2.8μm的深度区间内,并且高速公路横穿的渗透性更强的土壤的结果表明,年度NaCl施用量甚至更多地渗透到非饱和土壤中。沿冰ora带。这种咸水很可能在Oak Ridges冰a的这一部分补充地下水。

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