STEADY-STATE GROUNDWATER-FLOW SIMULATION WITH IMPRECISE PARAMETERS

Citation
Ch. Dou et al., STEADY-STATE GROUNDWATER-FLOW SIMULATION WITH IMPRECISE PARAMETERS, Water resources research, 31(11), 1995, pp. 2709-2719
Citations number
43
Categorie Soggetti
Limnology,"Environmental Sciences","Water Resources
Journal title
ISSN journal
00431397
Volume
31
Issue
11
Year of publication
1995
Pages
2709 - 2719
Database
ISI
SICI code
0043-1397(1995)31:11<2709:SGSWIP>2.0.ZU;2-#
Abstract
A methodology based on fuzzy set theory is developed to incorporate im precise parameters into steady state groundwater flow models. In this case, fuzzy numbers are used to represent parameter imprecision. As su ch, they are also used as a measure for the uncertainty associated wit h the hydraulic heads due to the imprecision in the input parameters. The imprecise input parameters may come from indirect measurements, su bjective interpretation, and expert judgment of available information. In the methodology, a finite difference method is combined with level set operations to formulate the fuzzy groundwater flow model. This fu zzy modeling technique can handle imprecise parameters in a direct way without generating a large number of realizations. Two numerical solu tion methods are used to solve the fuzzy groundwater flow model: the g roundwater model operator method proposed in this methodology and the iterative algorithm based on conventional interval arithmetics. The it erative method is simple but may overestimate the uncertainty of hydra ulic heads. The groundwater model operator method not only provides th e hull of the solution set for the hydraulic heads but also considers the dependence of hydraulic head coefficients which are functions of i mprecise parameters. Sensitivity analysis shows that the dependence of hydraulic head coefficients has a critical impact on the model result s, and neglecting this dependence may result in significant overestima tion of the uncertainty of hydraulic heads. A numerical model based on the methodology is tested by comparing it with the analytical solutio n for a homogeneous radial flow problem. It is also applied to a simpl ified two-dimensional heterogeneous flow case to demonstrate the metho dology.