ON THE CALIBRATION AND VALIDATION OF MATHEMATICAL-MODELS FOR THE INTERPRETATION OF TRACER EXPERIMENTS IN GROUNDWATER

被引:57
作者
MALOSZEWSKI, P
ZUBER, A
机构
[1] GSF-Institut für Hydrologie, D-8042 Neuherberg
[2] Institute of Nuclear Physics, PL-31342 Cracow
关键词
D O I
10.1016/0309-1708(92)90031-V
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Calibration and validation processes of mathematical models applied to the interpretation of tracer experiments in groundwater are reviewed and exemplified by a number of case studies. Definitions of basic terms related to those processes are given and adapted to specific problems of groundwater tracing. The calibration procedures commonly used are often ambiguous, due to the interplay of parameters, and then a proper validation is unavailable. The number of fitting parameters may sometimes be reduced by using information available from independent observations, or by calibration of a multi-tracer experiment. Even if a unique calibration is achieved, an ideal validation process is usually impossible or uneconomical to perform. Therefore, indirect validation methods must be used. A satisfactory agreement of the values of parameters obtained by calibration with those known from independent observations may be regarded as an indirect validation. Direct or indirect validation is often obtained only with respect to some parameters and in such cases it should be regarded as a partial validation only.
引用
收藏
页码:47 / 62
页数:16
相关论文
共 53 条
[1]  
Bibby, Mass transport of solutes in dual-porosity media, Water Resources Research, 17, pp. 1075-1081, (1981)
[2]  
Bullivant, O'Sullivan, Matching a field tracer test with some simple models, Water Resources Research, 25, pp. 1879-1891, (1989)
[3]  
Cacas, Ledoux, Marsily, Tillie, Barbreau, Durand, Feuga, Peaudecerf, Modeling fracture flow with a stochastic discrete fracture network: Calibration and validation, 1. The flow model, Water Resources Research, 26, pp. 479-489, (1990)
[4]  
Cacas, Ledoux, Marsily, Barbreau, Calmels, Gaillard, Margritta, Modeling fracture flow with a stochastic discrete fracture network: Calibration and validation, 2. The transport model, Water Resources Research, 26, pp. 491-500, (1990)
[5]  
Carlier, Nouvelles equations de propagation d'un dand une nappe souteraine, Journal of Hydrology, 103, pp. 189-197, (1988)
[6]  
Dagan, Stochastic modeling of groundwater flow by unconditional and conditional probabilities, 2. The solute transport, Water Resources Research, 18, pp. 835-848, (1982)
[7]  
Dagan, Solute transport in heterogeneous porous formations, Journal of Fluid Mechanics, 145, pp. 151-177, (1984)
[8]  
Egboka, Cherry, Farvolden, Frind, Migration of contaminants in groundwater at a landfill: a case study, 3. Tritium as an indicator of dispersion and recharge, Journal of Hydrology, 63, pp. 51-80, (1983)
[9]  
Freiberg, A natural gradient experiment on solute transport in a sand aquifer: 2. Spatial moments and the advection and dispersion of nonreactive tracers, Water Resources Research, 22, pp. 2031-2046, (1986)
[10]  
Garnier, Crampon, Preaux, Porel, Vreulx, Traçage par <sup>13</sup>C, <sup>2</sup>H, I<sup>−</sup> et uranine dans la nappe de la craie sènonienne en écoulement radial convergent (Béthune, France), Journal of Hydrology, 78, pp. 379-392, (1985)