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Soil-atmosphere modelling of an engineered soil cover for acid generating mine waste in a humid, alpine climate

机译:工程土壤覆盖层的土壤-大气模型,用于在潮湿的高山气候下产生酸的矿山废料

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A research program studying the performance of soil covers at the Equity Silver Mine was initiated in 1992. This site is situated in the humid, alpine climate of north central British Columbia. A one-dimensional, fully coupled heat and water transport, soil-atmosphere flux model was developed as part of this research program to simulate the movement of liquid water and water vapour within a soil cover in response to rainfall and evapotranspiration. Predicted and measured conditions in the cover showed good agreement for a five-month period from June to November 1993. The modelling exercise showed that vapour flow was the dominant flow mechanism near the surface of the cover within a few days after the start of drying. This points out the necessity of being able to couple heat and water transport in soil cover analyses and design. The numerical modelling demonstrated that input parameters are readily attainable through field and laboratory measurement. Model predictions of extreme and mean climate conditions indicated that percolation through the cover system would be limited to approximately 2% of the annual precipitation and that oxygen flux through the cover would be reduced by approximately 98% from uncovered conditions. [References: 54]
机译:1992年启动了一项研究项目,研究Equity银矿的土壤覆盖层性能。该地点位于不列颠哥伦比亚省中北部的潮湿高山气候中。作为该研究计划的一部分,开发了一种一维,完全耦合的热与水传输,土壤-大气通量模型,以模拟响应于降雨和蒸散作用的土壤覆盖物中的液态水和水蒸气的运动。从1993年6月到1993年11月的5个月期间,覆盖层的预测和测量条件显示出良好的一致性。建模工作表明,开始干燥后几天内,蒸汽流是覆盖层表面附近的主要流动机制。这指出了在土壤覆盖物分析和设计中必须能够将热和水的传输耦合起来的必要性。数值模型表明,通过现场和实验室测量可以轻松获得输入参数。极端和平均气候条件的模型预测表明,通过覆盖系统的渗流将被限制在年降水量的2%左右,而通过覆盖层的氧气通量将比未发现的条件降低约98%。 [参考:54]

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