A meshless solution of two-dimensional unsteady flow

The boundary element method (BEM) is a very useful numerical method for groundwater flow models. Particularly, this method was used to solve problems in homogeneous domains. However, it presents even greater difficulties than the other numerical methods when coping with non-homogeneities which are so characteristic in the groundwater hydraulics. Recently, meshless method which is based on a local boundary integral approach is introduced. It uses distributed nodal points, covering the domain. These points can be randomly spread over the domain. Every node is surrounded by a simple surface centered at the collocation point and the boundary integral equation is written on this local boundary. The unknown variables, in the local sub-domains, are approximated by some of the interpolation method. In this paper the combination of radial basis functions and the dual reciprocity method is used to solve the time-dependent groundwater flow.