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Uniform depth channel flow keeps fluid depth consistent along channels such as irrigation canals. In natural channels, such as rivers, approximate uniform flow is often assumed. This condition occurs when the channel’s bottom slope matches the energy slope, balancing potential energy lost from gravity with head loss due to shear stress. This balance prevents depth changes along the channel length, resulting in a steady, uniform flow.Uniform flow in open channels with a constant cross-section...
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In concrete, the pore size distribution significantly influences the material's properties. Capillary pores, markedly larger than gel pores, form a vast network within partially hydrated cement paste, reducing the concrete's strength and increasing its permeability. This heightened permeability leads to a greater risk of damage from environmental factors like freeze-thaw cycles and chemical attacks, with the extent of vulnerability also being tied to the water-to-cement ratio.
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Understanding steady, laminar flow between parallel plates is essential for analyzing and designing flow in narrow rectangular channels, commonly found in various water conveyance and drainage systems. The Navier-Stokes equations govern fluid motion and are generally challenging to solve due to their nonlinearity. However, simplifications are possible in certain cases, like the steady laminar flow between parallel plates. For this scenario, we assume steady, incompressible, laminar flow.
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How Equivalent Are Equivalent Porous Media?

Ahmad Zareidarmiyan1,2,3, Francesco Parisio4, Roman Y Makhnenko5

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Simplifying fractured rock models with equivalent porous media can lead to inaccurate pore pressure distribution and fracture stability predictions. Explicitly modeling fractures is often necessary for reliable geoenergy simulations and induced seismicity forecasting.

Keywords:
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Area of Science:

  • Geosciences
  • Computational modeling
  • Energy resources

Background:

  • Geoenergy and geoengineering commonly involve fluid flow in fractured rock formations.
  • Accurate modeling of these processes requires understanding the interplay between pore pressure and rock deformation (poromechanics).

Purpose of the Study:

  • To assess the validity of using equivalent porous media as a simplification for modeling fluid flow in fractured rocks.
  • To compare the accuracy of equivalent porous media models against explicit fracture models in geoenergy applications.

Main Methods:

  • Numerical simulations comparing two modeling approaches: explicit fracture representation versus equivalent porous media.
  • Calibration of both models to match injection and production well data.

Main Results:

  • Significant differences in pore pressure distribution were observed between the two modeling approaches.
  • Equivalent porous media models failed to accurately capture changes in fracture stability.

Conclusions:

  • Explicitly modeling fractures is crucial for accurate coupled thermohydromechanical simulations in certain geoenergy contexts.
  • Accurate fracture modeling can enhance the reliability of tools used for induced seismicity forecasting.