Abstract

'&8;0454 The presence of coal in the Springbok Flats Coalfield (SFC) has been known since the beginning of the 1900s. However, the SFC has not been mined to any degree of economic profit, mostly due to the presence of uranium in the coal. Five boreholes were drilled in the SFC (BH1 to BH5); BH5 intersected two coal zones, the other boreholes intersected one coal zone. Coal samples were collected, selected, and characterized using proximate, ultimate, and calorific value analyses. X-ray fluorescence, instrumental neutron activation analysis, and inductively coupled plasma mass spectrometry were used to determine uranium content. The BH1 intersection and the upper coal zone in BH5 had ash contents higher than 50% and were considered to be primarily carbonaceous shale. BH2 was observed to have better coal quality, resembling typical South African bituminous coal used in local electricity generation. The highest uranium content was found in BH3 (up to 199 mg kg -1, followed by BH2 and BH1. BH4, the upper coal zone in BH5, and the lower coal zone in BH5 all had uranium contents averaging less than 10 mg kg-1. Uranium in the SFC samples was found both in the coal and carbonaceous shale. For all boreholes except BH5, uranium is concentrated within the uppermost 1 m of the coal zone. X-ray fluorescence was the preferred analytical technique since the analysis gave consistent results that compared well with instrumental neutron activation analysis results.

Highlights

  • Coal in South Africa is found in 19 coalfields located in the middle and northern sections of the country (Jeffrey, 2005)

  • There is limited public domain research pertaining to the quality of coal present in the Springbok Flats Coalfield (SFC) as well as the uranium associated with the coal and carbonaceous horizons

  • Eleven samples that revealed an uranium content higher than 10 mg kg-1 were subjected to instrumental neutron activation analysis (INAA) to confirm the results obtained from Inductive coupled plasma–mass spectrometry (ICP-MS) and Xray fluorescence (XRF)

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Summary

Introduction

Coal in South Africa is found in 19 coalfields located in the middle and northern sections of the country (Jeffrey, 2005). The average ash content for BH1 peaked at 88.4%, indicative of carbonaceous shale horizons or partings in the coal zone (Table I). The proximate analysis and CV results for the upper coal zone of BH5 are below the limits of typical South African coals, and the results resemble those of carbonaceous shale instead of coal (Martins et al, 2010).

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