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This paper presents an overview of the current developments on modelling of subsurface flow CWs based on the modelling work and model developments presented at the WETPOL 2007 symposium.
Numerical modelling of subsurface flow constructed wetlands (CWs) gained increasing interest during the last years.
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Our work could provide a workflow linking outcrop fracture observations to the 3D model of subsurface fracture prediction and extend modeling capability in other outcrop studies.
Fig. 2 Model of subsurface structure.
Structural restoration and reconstruction is a methodology for building and improving structural models of subsurface geology.
Additionally, the Pacific Northwest National Laboratory PNNLL) has developed a numerical model of Subsurface Transport Over Multiple Phases (STOMP-CO2) to provide a practical tool of subsurface injection and long-term storage of carbon dioxide in deep subsurface reservoirs [38, 39].
These illustrate the type of insights that can be obtained from process-based modeling of subsurface fluvial architecture, and highlight potential applications of stratigraphic simulation.
The information gain maximization can suggest data collection locations to reduce uncertainties in the conceptual models of subsurface flow and transport.
Wavelet decomposition of surface measurements of SWC could improve modeling of subsurface SWC by segregating features at different temporal scales and projecting them to the subsurface.
Generating a realistic model of subsurface stratigraphy that fits data from multiple well locations is a well-established problem in the field of aquifer characterisation.
A model of subsurface heat generation and transport helps elucidate the contribution of microbial and infrastructure heating to observed temperature increases at this site.
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