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The lack of wet-weather sampling made 2010 ideal for study of dry-weather exceedance events.
Perkins and Foster[11] also observed Se(IV) species in weathered samples.
Next, the terahertz (THz) spectra of the weathering samples in the study area were measured using a terahertz time-domain spectrum system (THz-TDS).
To minimize damage to the relics, three small weathering samples were collected from the ultrasonic testing regions (Fig. 1c) and then ground evenly with an agate mortar.
The treatments were tested on artificially weathered samples of Globigerina limestone ("Franka" type), a highly porous stone typically used in historical architecture in Malta and severely affected by decay processes.
Chemical surface modifications were induced by UV-irradiation in a specially designed climatic chamber and were investigated through comparative tests on untreated and artificially weathered samples using X-ray photoelectron spectroscopy (XPS).
During the dry weather studies, samples were collected once per week for 5 weeks.
During 1971, British weather ships sampled the upper 500 m of the ocean to investigate plankton distribution by depth.
After weathering the samples, they presented depleted photocatalytic properties.
Some weathered carving samples as small as such could be obtained outside of the main body of the stone relics.
U Th Ra disequilibria, cosmogenic in situ 10Be concentrations and major and trace element concentrations have been analyzed in a 2 m-deep weathering profile sampled at the summit of the granitic Strengbach catchment (France).
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