4.7 Article

An Approach to Include Hydrogeologic Barriers With Unknown Geometric Properties in Groundwater Model Inversions

期刊

WATER RESOURCES RESEARCH
卷 58, 期 7, 页码 -

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1029/2021WR031458

关键词

groundwater; hydrogeology; model calibration; geological structure; faulting; groundwater age

资金

  1. Australian Government Research Training Program
  2. Australian Research Council [LP150100395, LP180101153]
  3. Rio Tinto Iron Ore
  4. Australian Research Council [LP150100395, LP180101153] Funding Source: Australian Research Council

向作者/读者索取更多资源

This study demonstrates that sharp hydrogeological barriers can be included in groundwater model inversion even when their presence is uncertain. The use of phantom structures improves the identification of barriers and successfully infers their location and properties.
Hydrogeological barriers can significantly impact groundwater model predictions. They are, however, often excluded from, or misrepresented in, groundwater models if their presence is unknown or their properties are poorly constrained. Here we show that sharp barriers can be included in groundwater model inversion, even where their presence is uncertain. We describe an approach utilizing phantom structures-randomly located, linear groups of model cells assigned a unique hydraulic conductivity value-to improve identifiability of barriers. Algorithmic parameter estimation using model-independent parameter estimation code (PEST) is implemented to determine model structures that best match the hydraulic head and groundwater age observation data from a hypothetical aquifer. Our results show that for a series of case studies, this method was successful in inferring the appropriate location and properties of hydrogeological barriers, when that barrier was not aligned with the dominant flow direction. We compare these results to model inversion using traditional pilot points. The phantom structures approach shows promise in identifying hydrogeological structures and in reproducing groundwater flow across a model domain. Our results demonstrate that the geometric properties of geological structures can remain flexible in a model inversion. This is a step toward reducing conceptual model uncertainty where the presence and properties of hydrogeologic barriers are undefined.

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