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dimensional finite difference groundwater flow model MODFLOW (McDonald 1988).

The model presented in this paper is called SMILE (an acronym for Simple Macropore Infiltration, Leakage and Evaporation) and it consists of a spatially explicit model of saturated groundwater flow and a lumped conceptual model of vertical unsaturated flow. The model concentrates on the dominant processes that control recharge and salt load discharge at the catchment scale. Model development of the unsaturated flow processes proceeded from the simple to the more complex, where additional complexity was only retained where it could be shown that it yielded a significant improvement. While there are (arguably) a number of physically-based models that have the potential to model the coupled processes of interest, it was considered that there was not the data available to validate model response at the required spatial and temporal scales. The amount of calibration data available for this model application is typical of many catchment investigations, and is representative of the fundamental limitations imposed on physically-based models that has been discussed by such authors as Klemes (1986) and Beven (1989). The process of model development adopted here follows the suggestions of Grayson and Nathan (1993), in which the model was developed for a specific problem at a complexity commensurate with the available data.

The developed conceptual model simulates a well connectedsurface water/groundwater system dominated by either matrix or macropore flow. As such, the classical matrix flow approximations described by the Richards Equation were not used. The simplified conceptual model approximates one-dimensional vertical soil moisture movement which recharges a three-dimensional finite difference groundwater model. The vertical soil moisture model simulates soil infiltration, recharge to a underlying groundwater system and evapotranspiration on a daily timestep for each active cell within the model domain. Sub-surface lateral flow within each soil column is not permitted. A detailed description of the conceptual model is provided below.

Evapotranspiration

Evapotranspiration is a function of soil moisture and an assigned crop factor as defined by:

IMAGE imgs/SMILE02.gif


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