Abstract
This paper describes the form of a number of limestone drainage systems on the Gower Peninsula, South Wales. The effect of system morphology on seasonal variation in flow pattern and solute load at spring sites is examined and the systems ordered according to the degree of development of the conduit flow component and the integration of percolation inputs. Reference is made to the development of flow systems in other areas and a projection of the effect of system form on the discharge hydrograph is attempted. Reference is made not only to chemical characteristics but also to mode of operation and system definition.
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