TY - JOUR
T1 - A Lagrangian‐Eulerian Method with zoomable hidden fine‐mesh approach to solving advection‐dispersion equations
AU - Yeh, G. T.
PY - 1990/6
Y1 - 1990/6
N2 - A Lagrangian‐Eulerian method with zoomable hidden fine‐mesh approach (LEZOOM), that can be adapted with either finite element or finite difference methods, is used to solve the advection dispersion equation. The approach is based on automatic adaptation of zooming a hidden fine mesh in regions where the sharp front is located. Application of LEZOOM to four bench mark problems indicates that it can handle the advection‐dispersion/diffusion problems with mesh Peclet numbers ranging from 0 to ∞ and with mesh Courant numbers well in excess of 1. Difficulties that can be resolved with LEZOOM include numerical dispersion, oscillations, the clipping of peaks, and the effect of grid orientation. Nonuniform grid as well as spatial temporally variable flow pose no problems with LEZOOM. Both initial and boundary value problems can be solved accurately with LEZOOM. It is shown that although the mixed Lagrangian‐Eulerian (LE) approach (LEZOOM without zooming) also produces excessive numerical dispersion as the upstream finite element (UFE) method, the LE approach is superior to the UFE method.
AB - A Lagrangian‐Eulerian method with zoomable hidden fine‐mesh approach (LEZOOM), that can be adapted with either finite element or finite difference methods, is used to solve the advection dispersion equation. The approach is based on automatic adaptation of zooming a hidden fine mesh in regions where the sharp front is located. Application of LEZOOM to four bench mark problems indicates that it can handle the advection‐dispersion/diffusion problems with mesh Peclet numbers ranging from 0 to ∞ and with mesh Courant numbers well in excess of 1. Difficulties that can be resolved with LEZOOM include numerical dispersion, oscillations, the clipping of peaks, and the effect of grid orientation. Nonuniform grid as well as spatial temporally variable flow pose no problems with LEZOOM. Both initial and boundary value problems can be solved accurately with LEZOOM. It is shown that although the mixed Lagrangian‐Eulerian (LE) approach (LEZOOM without zooming) also produces excessive numerical dispersion as the upstream finite element (UFE) method, the LE approach is superior to the UFE method.
UR - http://www.scopus.com/inward/record.url?scp=0025680793&partnerID=8YFLogxK
U2 - 10.1029/WR026i006p01133
DO - 10.1029/WR026i006p01133
M3 - 期刊論文
AN - SCOPUS:0025680793
SN - 0043-1397
VL - 26
SP - 1133
EP - 1144
JO - Water Resources Research
JF - Water Resources Research
IS - 6
ER -