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A combination of a low temperature of sample annealing and a high rate of its cooling may be considered as one of the most plausible factors responsible for its appearance.
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After reaching the desired low temperature of 2 K, the sample was warmed and magnetization recorded, called the "heating" process.
Sample #20 released a large amount of 4He, 7.4 × 10−3 cm3 STP/g, at the low temperature of 500°C, with a subsequent sharp decrease at higher temperatures.
XRD spectra of whole coal and low temperature ash samples of the Kasnau-Matasukh lignites are shown in Fig. 9a, b.
The lowest efficiency corresponds to the sample grown at lowest temperature of 520 °C, although its morphological characteristics are similar to other samples.
Table 1 Chemistry of low temperature vent fluid sample from Franklin Seamount, Woodlark Basin.
Transition from electrically discontinuous to electrically continuous layer in case of low temperature annealed samples is more gradual and occurs between the effective layer thicknesses from 10to2020 nm regarding the annealing temperature.
Sharp et al. [66] investigated Δ17O variations in low temperature quartz samples in an effort to constrain the temperature of the water from which the quartz precipitated.
Radiation of low temperature samples, such as those packaged with dry ice, must therefore take these dosimeter temperature effects into consideration.
In order to avoid any effect of low temperature, samples were maintained at 20°C prior to analysis.
Notably, there was no freeze-drying tendencies during the period of low temperature and the samples were wet and soft once they were warmed up after freezing.
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