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This current study only focused on tropic's different summer temperature and humidity steps to explore the adaptive comfort range.
A sample submitted to multiple relative humidity steps (ϕ = 10 75 33 75%) with a sensor placed at X∘= 5cm was found as the best option for determining both properties with the same experiment.
The advantage of classic methods is that salt standards are well characterized [104], the experiment can be performed with very small humidity steps, over long periods of time and that a large number of crystals can be treated at the same time.
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A parallel exponential kinetics model (PEK-model) was used to evaluate the change in mass during the adsorption process of each relative humidity step.
The experimental results show, that although both the time constants for temperature and humidity step changes are dependent on Reynolds number, the temperature response time constant (35 1300 s) is much larger than the humidity response time constant (4 25 s) for the Reynolds number range of 300 5.
SI Figure 6, Supporting Information, also compares the MS spectra from these methods, showing the increased detection of higher m/ z metabolites when the humidity step was employed.
Open image in new window Fig. 10 Fit parameter V 2 plotted against resistance change for low- to mid-humidity step increase data.
The absolute differences between sensor output and criterion values of temperature, humidity, and step count were also determined.
Unlike the results described above, adding the humidity chamber step did not increase the metabolite detection and only served to diffuse analytes in the lower mass region.
For DHB, the sublimation method shows some analyte diffusion in the lower mass range due to the humidity chamber step, but there are also some metabolites detected in the higher mass range that would not have been detected without the humidity chamber step.
Significantly more metabolite peaks were observed using gradual heating with the humidity chamber step (Method 4), in comparison with gradual heating and no humidity (Method 1), especially in the higher mass region (above m/ z 500).
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