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首页> 外文期刊>Journal of Hydrology >Fully coupled heat and water dynamics modelling of a reclamation cover for oil sands shale overburden
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Fully coupled heat and water dynamics modelling of a reclamation cover for oil sands shale overburden

机译:完全耦合的热水和水动力学建模油砂岩覆盖物的垦区

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摘要

Numerical models of soil-water dynamics have been widely used in the design of soil cover systems for mine site reclamation; however, in most cases these models only consider water dynamics without consideration of heat dynamics. For cover systems in northern climates, such as those associated with oil sands mines in northern Alberta, Canada, freezing conditions exist for approximately 6 months of the year and snow melt comprises approximately 25% of annual precipitation. This study attempts to assess whether a fully coupled water and heat flow model (CM) provides additional insights into cover performance as compared with a water flow model (FM). The CM and FM are developed for a monitored reclamation cover constructed over oil sands shale overburden. The validated results indicated that the key limitation of the CM was its inability to simulate frozen ground infiltration. This limitation results in an overestimate of snow melt runoff and does not replicate the development of perched conditions on the shale overburden surface as a result of snow melt infiltration. The FM is also unable to simulate the observed infiltration of snow melt deep into the cover when snow melt is re-presented simply as surface precipitation in early spring following ground thaw. Both models are improved if snow melt infiltration is represented in the model by the preferential filling of macropores across the full depth of the cover and oxidized shale prior to ground thaw. This methodology is incorporated with the CM to produce a coupled water and heat model with enhanced infiltration (CM-EI), and with the FM to produce a flow model with enhanced infiltration (FM-El). The CM-EI provided an improved simulation of soil temperature dynamics under frozen and unfrozen conditions, as well as soil water dynamics under unfrozen conditions, including the improved representation of the annual water balance components over each water year. Given the small difference in annual water balance components between the CM-EI and FM-EI modelling approaches (similar to 5 mm/year), it is concluded that a FM-EI provides the best tool with which to assess the performance of these reclamation covers.
机译:土壤水动力学的数值模型已广泛应用于矿山场地填海区土壤覆盖系统的设计;然而,在大多数情况下,这些模型仅考虑水动态而不考虑热动态。对于北部气候的覆盖系统,例如与艾伯塔北部的油砂矿相关的覆盖物,加拿大冻结条件约6个月的年份,雪熔融占年降水量的约25%。该研究试图评估完全耦合的水和热流模型(CM)是否与水流量模型(FM)相比提供了覆盖性能的额外洞察。 CM和FM是为由油砂岩覆盖物构建的监测填充盖开发的。验证的结果表明,CM的关键限制是无法模拟冷冻的地渗透。由于雪熔融渗透,这种限制导致雪熔体径流过度高估了雪熔融径流,并不会复制页岩覆盖表面上的栖息状况的发展。所述FM也不能模拟的雪被观察者浸润熔融深入到盖时融雪是重新呈现以下地面解冻仅仅作为表面沉淀在早春。如果在模型中,通过优于覆盖在地面解冻之前的覆盖物的全部深度和氧化页岩的宏观中,可以提高两种模型。该方法掺入CM以产生具有增强的渗透(CM-EI)的偶联水和热模型,并用FM产生具有增强渗透(FM-EL)的流模型。 CM-EI提供了在冷冻和未变化条件下的土壤温度动态的改进模拟,以及在未冷却条件下的土壤水动力学,包括每年水中的年度水平衡成分的改善。鉴于在CM-EI和FM-EI建模之间的年度水量平衡分量小差接近(类似于至5毫米/年),可以得出结论,一个FM-EI提供与评估这些回收的性能的最佳工具盖子。

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