TRANSFER FUNCTION APPROACH FOR ARTIFICIAL TRACER TEST INTERPRETATION IN KARSTIC SYSTEMS

[4] Cruz J.V., Amaral C.S., Major ion chemistry of groundwater from perched-water bodies of the Azores Portugal volcanic archipelago, Applied Geochemistry 2004, 19, 445–459 [5]

In this study, we proposed to run the inverse problem based on artificial tracer tests with a numerical procedure composed of the following three main steps: (1) conduit

La circulaire du 13 septembre 2005 relative à l’échange d’information entre les officiers de l’état civil et l’Office des étrangers à l’occasion d’une déclaration de

Comparison of the residual oil saturation estimates uncertainty ranges resulting from a 50 (left column) or 25 ppm (right column) error in the alcohol and ester outlet

(B) At birth few fat cells are present; fat cell number rapidly grows during childhood and cell number is set afterwards, cells are replaced at a constant rate.. (C) Like B,

Nous proposons dans cet article d'étudier par traçages artificiels l'unité géologique carbonatée du Beausset, constituant un aquifère à forte valeur patrimoniale

Based on the fact that the H ∞ norm of an an- alytic transfer function is defined as the supremum of its maximal singular value on the imaginary axis, the matching of the rational

Poznyak, “Unified Lyapunov function for a finite- time stability analysis of relay second-order sliding mode control systems,” IMA Journal of Mathematical Control and Information,