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Immediately prior to sampling the face should be scraped free of light-exposed grains on the surface.
Higher energy facies with erosion of previous deposited sediments and formation of new grains with clast percussion during saltation and creep at the base of the water column often yield a mixture of apparent grain ages.
If such inhomogeneities cannot be avoided field gamma spectrometry or collection of sediment from the disparate units is advised to document the in situ dose rate.
Also, care should be exercised in collection samples within 1 to 1.5 m of the surface, with likely pedogenic alterations.
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