Using Homogenized Models to Explore the Effect of Fracture Densities on Weathering

IF 1.9 3区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
M. Lebedeva, S. Brantley
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引用次数: 0

Abstract

Despite its importance, only a few researchers have incorporated the effects of fracturing into models of reactive transport for rock weathering. Here we explore 2D simulations that describe weathering under conditions of diffusive and advective transport within heterogeneous media consisting of rocky blocks and fractures. In our simulations, the Darcy velocities vary in space and time and depend on weathering processes within the rock matrix. We explore simulations with saturated and unsaturated flow for weathering bedrock that consists of blocks separated by inert or weathered material. The simulations show that a simplified homogenized model can approximate exact solutions for some of the simulated columns and hills and can allow exploration of coupling between flow and reaction in fractured rock. These hillslope simulations document that, even in the presence of 2D water flow, i) an increase in fracture density results in faster weathering advance rates; and ii) the water table locates deeper for a rock system that is weathered and fractured rather than weathered and unfractured. Some of these patterns have also been observed for natural systems. But these simulations also highlight how simplified models that do not use appropriate averaging of heterogeneities can be inaccurate in predicting weathering rate for natural systems. For example, if water flows both vertically and laterally through the vadose zone of a hill, then a prediction of the depth of regolith that is based on modeling strictly unidirectional downward infiltration will be unrealistically large. Likewise, if the fracture density observed near the land surface is used in a model to predict depth of weathering for a system where the fracture density decreases downward, the model will overestimate regolith depth. Learning how to develop accurately homogenized models could thus enable better conceptual models and predictions of weathering advance in natural systems.
利用均匀化模型探讨断裂密度对风化的影响
尽管它很重要,但只有少数研究人员将压裂的影响纳入岩石风化反应输运模型。在这里,我们探索二维模拟,描述在由岩块和裂缝组成的非均质介质中扩散和平流输送条件下的风化。在我们的模拟中,达西速度随时间和空间的变化而变化,并取决于岩石基质内的风化过程。我们探索了由惰性或风化物质分开的块组成的风化基岩的饱和和不饱和流动的模拟。模拟结果表明,简化的均匀化模型可以近似解出部分模拟柱和丘的精确解,并可以探索裂隙岩体中流动与反应之间的耦合关系。这些山坡模拟表明,即使在二维水流存在的情况下,1)裂缝密度的增加导致更快的风化推进速率;ii)风化和破裂的岩石系统的地下水位较风化和未破裂的岩石系统的地下水位较深。其中一些模式也在自然系统中被观察到。但是,这些模拟也突出表明,没有适当地平均非均质性的简化模型在预测自然系统的风化速率时可能是不准确的。例如,如果水沿垂直方向和横向方向通过山丘的渗透带,那么基于严格单向向下入渗建模的风化层深度预测将会不切实际地大。同样,如果将在地表附近观测到的裂缝密度用于预测裂缝密度向下减小的系统的风化深度的模型,则该模型将高估风化层深度。因此,学习如何开发精确的均质模型可以实现更好的概念模型和自然系统中风化进展的预测。
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来源期刊
American Journal of Science
American Journal of Science 地学-地球科学综合
CiteScore
5.80
自引率
3.40%
发文量
17
审稿时长
>12 weeks
期刊介绍: The American Journal of Science (AJS), founded in 1818 by Benjamin Silliman, is the oldest scientific journal in the United States that has been published continuously. The Journal is devoted to geology and related sciences and publishes articles from around the world presenting results of major research from all earth sciences. Readers are primarily earth scientists in academia and government institutions.
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