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In both cases however, the corresponding H2O peak evolving around the same temperature can be observed.
The second H2O peak evolving at 750°C can be attributed to the hydrogen species associated the polyaromatic hydrocarbons.
This suggests that the CO2 peak evolving from the n-hexadecane deposits between 400 and 500°C may be hidden by the offset in the baseline of the CO2 evolution profile.
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This peak evolves into a background at low frequencies and high temperature.
At intermediate temperatures a stress-dependent peak evolves in both the maximum strain and polarization.
The CO peak evolves with time on stream, gradually increasing in intensity from ∼20min to 5 h.
The spectra consist of three emission peaks evolving in time.
The peaks evolved with cycles and changed significantly when the plastic strain amplitude was increased.
f Inorganic perovskite PL peaks evolved with their anions.
The right two conductance peaks evolve into a single conductance peak, and the height of the conductance peak is suppressed.
The left two conductance peaks evolve into a single conductance peak, and the right conductance peak moves in the right direction in the case of ε3 > 0. We also find the height of the left conductance peak is suppressed.
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