By Walid Elshorbagy and Rezaul Kabir Chowdhury
ISBN-10: 9535109286
ISBN-13: 9789535109280
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It was convenient to define dimensionless coefficient K for computation as follows: if t< τ then K = 0; if t> τ then K = 1. Numerous studies on longitudinal dispersion have been conducted over the past few decades. Fick's second law predicts how diffusion causes the concentration to change with time. In actuality, immobileflow zones (dead zones) may invalidate Fick’s law. Chatwin [12] developed a method for determining longitudinal dispersion intended to address the problem of non-Fickian behaviour.
In this situation, the stochastic constraints can be transferred to certain ones. The relationship between probability and b is shown in Fig. 6. 15, b = 100, b constrain, which contains probability the constraint, into a deterministic equivalent. 15, the answer is in the curve interval (mn), and the corresponding b is equal to 100; the solution is gi(x) ≥100, which is inconsistent with the original problem statement that gi (x) ≤Bi. Diagram (c) thus explains the conversion procedure. 15, the answer is equals 180; so the solution is gi (x) ≤180.
Netherlands. pp. 137-164. , Daněček J. Hydrol. , Vol. 50, No. 2, pp. C. (1971) On the interpretation of some longitudinal dispersion experiments. J. Fluid Mech. 48(4);689–702. [13] Field, M. (2002) The QTRACER2 program for Tracer Breakthrough Curve Analysis for Tracer Tests in Karstic Aquifers and Other hydrologic Systems. S. Environmental protection agency. deid=54930. , Koller, J. , Nesměrák, I. (1991) Čistota vod (Water Purity), Alfa Bratislava 264 pp. ISBN 80-05-00700-0 [18] Šajer, J. (2010) Modelová interpretace výsledků měření mísící zóny v Labi pod vypouštěním z ČOV Hradec Králové.