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The effect of solid phase transformations is taken into account by using temperature and phase dependent material properties and the continuous cooling transformation (CCT) diagram.
kCalculated by using temperature and humidity.
To assess average climate (as a potential factor in physician location preference), the discomfort index, developed by the US Weather Bureau (currently the National Weather Service) and widely used in previous studies [ 36, 37], was calculated by using temperature and humidity.
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In this work, the relationship between the structural mechanisms and macroscopic electrical properties of the Nb-modified 0.96(Bi0.5Na0.84K0.16TiO3)–0.04SrTiO3 (BNKT ST) system were elucidated by using temperature dependent and in situ synchrotron X-ray diffraction (XRD) techniques.
Finite difference method is used to solve the governing equations for each case by using temperature, relative humidity and solar radiation measurements for three climate conditions: Hot sub-humid, hot humid and warm sub-humid.
We previously reported on the excellent heat generation ability of PSi and the ability of PSi to irreversibly destroy cancer cells under NIR laser irradiation by using temperature rise measurement and MTT assay results, respectively [27, 28].
The high temperature behavior is investigated by using temperature cycles between 90 and 120 °C without adjustment of the gases dew points, to simulate a short-period temperature increase, possibly caused by an extended power demand and/or limited heat removal.
The effective magnetic anisotropies were determined by using temperature dependence of magnetization experiments and Stoner-Wohlfarth theory.
In line with this hypothesis, previous investigators provided structural description of the crystals similar to that presented in this study, and morever, by using temperature-sensitive (ts) mutants, suggested that the crystals were derived from fibers, with a proviso that penton base might also be involved [28].
Because seasons vary by our study sites, primary analyses used temperature and barometric pressure to adjust for seasonality.
By using these temperature and grain size data, and supposing a SRF of 6 (an average value from considering the results of Wolff-Boenisch et al. (2004)), the model presented in this study indicates that 200,000 years are necessary to alter 30%% of the protolith.
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