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Natural minerals, such as widespread quartz and feldspars, have physical properties which enable them to be used as radiation
dosimeters. The underlying luminescence phenomena have made it possible in recent decades to determine the age of a variety
of materials important for quaternary geochronometry and archaeochronometry. We present a new luminescence dating method based
on radioluminescence measurements of potassium feldspar. For the first time we have been able to investigate the light-emitting
transition of electrons from the conduction band to an optically sensitive electron trap. Many advantages can be derived from
such direct measurements of the metastable electron density in this particular trap, which produces the age-dependent signal.
The method can be used to date the last light exposure of feldspar grains within a range of a few hundred to more than 200,000 years.
Examples are presented of age determination of various waterlaid quaternary sands. The results of a basic study of feldspar
radioluminescence also shed light on effects not sufficiently understood in conventional dating by luminescence techniques,
especially in infrared optically stimulated luminescence dating of feldspar.
Received: 6 August 1998 / Accepted in revised form: 14 April 1999 相似文献
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The Science of Nature - 相似文献
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The optical properties (reflectance and transmittance) of selected leaves from a tropical mountain rainforest in southern Ecuador are determined to parametrize optical traits of plant functional types (PFT) of a state of the art land model (Community Land Model, CLM). 46 spatially dominating species are selected from 4 different forest types, the subpáramo and a succession stage of pasture areas representing ecologically predefined functional types within the study area. Measurements are conducted under a standardized experimental setup with a field spectrometer covering the radiation between 305 and 1305 nm. The results of the optical properties of all species are checked for similarity by cluster analysis and are compared to the composition of species of the predefined PFTs. Furthermore the results are compared to other studies, the default values for the globally defined PFT of tropical evergreen trees in the CLM and another forest growth model operated in the same study area. The results show that the clusters aggregated by the reflectance, transmittance or combined properties do not represent the predefined PFTs. The values of the other studies suggest a reassessment of the experimental setup for the transmittance measurements. Nevertheless, new reflectance values for the regionalized PFTs can be determined. The optical values differ from the CLM-PFT of tropical evergreen trees, and new values for the reflectance are recommended. 相似文献