Identification in 1982 on the Dutch Frisian Island of Ameland of beach
sand with;ln enhanced level of natural radioactivity, due to concentr
ations of heavy minerals, inspired a multi-disciplinary research proje
ct. A joint research effort in geochemistry, sedimentology, hydrodynam
ics, solid-state physics and nuclear physics has revealed new aspects
in the use of natural radioactivity in heavy-mineral exploration and p
rocessing, as well as in understanding sediment transport processes in
the coastal zone. This paper describes radiometric methods and techni
ques, such as thermoluminescence dating and a method known as radiomet
ric fingerprinting. Initially our focus was on relationships between n
atural radioactivity and grain size, and between radioactivity and min
eral species. Additionally the distribution of heavy minerals along th
e Dutch coast was mapped. One of the first substantial findings was th
at the concentrations of K, U and Th in light and heavy minerals diffe
r by two orders of magnitude. Thus the total heavy-mineral mass fracti
on (THM) could be accurately determined radiometrically. Attempts to d
etermine THM radiometrically resulted in identifying regions of proven
ance, or origin for coastal sand minerals. This stimulated studies of
transport processes and their selectivity. Investigations were conduct
ed on the beach, under laboratory conditions and on the seafloor. More
over, the enhanced radionuclide concentrations in, e.g., zircons make
them particularly suitable for thermoluminescence dating young dune an
d beach sediments. This knowledge may aid better management of coastal
zones, and may help to identify the genesis conditions of heavy-miner
al placers. The instrumentation development has resulted in MEDUSA a t
owed detector system used for radiometric seafloor mapping. MEDUSA rev
ealed unknown large quantities of heavy minerals on the Dutch seafloor
. These minerals are present in layers up to 40% in thickness and with
concentrations up to 20%. Radiometric fingerprinting of minerals allo
ws a quantitative assessment of mineral suites during various stages o
f wet and dry separation. This industrial application of MEDUSA is bei
ng considered in Australia and South Africa. (C) 1998 Elsevier Science
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