Why the rock makes lining matter
Carboniferous limestone is riddled with joints and solution channels. Rivers such as the Lathkill and the Manifold run partly underground in dry weather, which shows how freely water moves through it. An unlined or cracked earth store on that ground can lose effluent into the rock with little warning at the surface.
Further south, on the clays and gravels of the Dove valley around Ashbourne and Hilton, the risk shifts to the watercourses beside the fields. Either way, a welded liner over protection fleece removes the ground from the question.


