Numerical simulation
Numerical simulation consists of the use of specialized software to understand and analyze the behavior of groundwater.
Software used
Hydro-Ressources uses cutting-edge software, including the latest version of FEFLOW (7), which utilizes an unstructured mesh. We also use Leapfrog software to construct the geometry of faults and lithological units.
The various software tools we employ, such as FEFLOW and MODFLOW, are based on the principle of mass conservation. FEFLOW is particularly efficient because it uses the finite element method, making it more flexible when topography is highly variable across a site.
A digital model can be compared to a physical model, but displayed on a computer. The validity of the model, commonly referred to as calibration, allows us to assess its effectiveness in relation to real-world conditions. This primarily involves comparing certain field observations with those simulated by the model.
What is a digital model?
A digital model can be compared to a physical model, but displayed on a computer. The validity of the model, commonly known as calibration, allows us to assess its effectiveness in relation to reality. This primarily involves comparing certain observed field results with those simulated by the model.
How to use a digital model?
Once the model is built, an infinite number of simulations can be run, such as estimating the recharge area and protection zones of a catchment well, or modeling the future transport of a contaminant. A numerical model is an important, even essential, tool for municipalities that rely on groundwater. It enables quick and precise responses to various questions from managers.
Profile Tracing Test (PTT)
Patented methodology
A profile tracing test is an application recently adopted by our firm. The concept is simple: it involves mixing a tracer as uniformly as possible into a single open hole (for example, a diamond drill hole used for exploration). Once the tracer is mixed into the hole, its concentration is measured at various time intervals within the same vertical borehole. Concentration profiles are created, and the variations in concentration indicate the location of the naturally active flow zone. In fact, when the concentrations decrease, it indicates the presence of flow.
Our achievements
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