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AN ALTERNATIVE APPROACH TO MULTISCALE THERMOHYDROLOGIC MODELING

机译:多尺度热力学建模的替代方法

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摘要

The Yucca Mountain Project computes futurernsubsurface temperatures by running a series of models thatrnoperate on different spatial scales. These models are allrnparameterized in terms of time and areal mass loading; thernoutput of some of the models is used to adjust the time andrnmass loading scales in other models in order to obtain thernfinal results. Inaccuracies arise when these adjustments arernmade. An alternative approach is suggested here tornimprove accuracy. In the alternative approach, early-timerncalculations use the same models as the current YuccarnMountain Project approach, without adjusting time or massrnloading. Late-time calculations use a steady-state model ofrnlocal heat transfer parameterized in terms of instantaneousrnheat output and a local-average rock temperature, with thernlatter quantity derived from a mountain-scale transientrnmodel. Intermediate-time results are interpolated betweenrnthe other two approaches. The alternative approach isrnmore amenable to error analysis because none of itsrnvariables are defined implicitly in nonlinear equations.
机译:尤卡山项目(Yucca Mountain Project)通过运行一系列在不同空间尺度上变化的模型来计算未来的地下温度。这些模型在时间和面积质量负荷方面都进行了参数化。一些模型的输出用于调整其他模型中的时间和质量加载比例,以获得最终结果。进行这些调整时会出现不准确之处。在此建议另一种方法来提高准确性。在替代方法中,早期时间计算使用与当前YuccarnMountain Project方法相同的模型,而无需调整时间或质量负荷。后期计算使用局部传热的稳态模型,该模型根据瞬时热量输出和局部岩石平均温度进行参数化,其离散量来自山地尺度的瞬变模型。在其他两种方法之间插入中间时间结果。替代方法更适合误差分析,因为其变量都不是在非线性方程中隐式定义的。

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