The impact of a disused mine on uranium transport in the River Fal, South West England

Abstract

Unfiltered and filtered (0.45 and 0.2 μm) water samples and sediment samples (sieved to <180 μm and 180–1000 μm) were collected along a ∼15 km transect of the River Fal, Cornwall, UK, to examine the impact of the disused South Terras uranium mine on the uranium concentrations of the river water and underlying sediments. The uranium concentration of the water samples fluctuated along the river, with the 0.45 μm filtered water showing the largest, seven-fold, difference between minimum (0.19 μg L⁻¹) and maximum (1.34 μg L⁻¹) concentrations. The historical uranium mine and spoil heaps were not a significant source of uranium to the river water, as water concentrations were low next to the site, but a highly elevated uranium concentration (1000 mg kg⁻¹) was found in sediment below an outflow pipe from this mine. Operationally defined “colloidal” (0.2–0.45 μm) and “dissolved” (<0.2 μm) uranium were the predominant forms of the element in the river water (35 and 45% respectively). The uranium concentration in the dissolved phase showed a correlation coefficient of 0.83 (n = 9) with the total cation concentration, suggesting that the uranium concentration in this fraction is directly linked to weathering of rocks and minerals. The observation that weathering is the dominant mechanism delivering uranium to the river water explains the low uranium concentrations in the river water close to South Terras mine, despite the proximity of the spoil heaps, and the maximum uranium concentrations close to a china clay mining area.