A Monte Carlo Method without Grid to Compute the Exchange Coefficient in the Double Porosity Model Part I : From the Matrix to the Fissures

Once we have decided that the particle is “significantly” in the matrix, we have to compute its coordinate at this time by simulating the longitudinal component, and using the

Since the gradient of the trial wave function ∇Ψ(R) (and of the exact wave function) does not generally vanish at the location of the nodes, the drift velocity v(R) diverges at

On the right, the ambiguity in the inferred pose of the true camera is shown: its position can lie anywhere on the circle that is centered in the fixed-axis rotation axis,

Risk factors associated with acute respiratory distress syndrome and death in patients with coronavirus disease 2019 pneumonia in Wuhan, China. Hyperglycemia and the novel

This is not true for ssGBLUP because new genomic relationships may modify old pedigree relationships; however, the ef- fect of genotypes of young animals on GEBV of other

For this purpose it presents the analysis of a bar with random elastic modulus and prescribed boundary conditions, say, fixed at one end and attached to a punctual mass and two

Pour ´eviter d’avoir `a faire une hypoth`ese sur la valeur de la vitesse non-thermique, on peut se pencher sur la variation de largeur avec l’altitude. Or mettre en ´evidence

The scaling of results is an integral part of the testing process, and is presented here as a means to identify if the testbed can be used as a risk- reduction step