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Both PL and PLE spectra of the samples demonstrate vibronic oscillations which were attributed to the ground and excited states of sulfur- and oxygen-related molecular species.
This peak can be attributed to the ground energy level transition in the quantum ring, which corresponds to the photoresponse peak at 1.52 eV measured at 300 K.
According to the excitation power variable experiments, the three peaks can be attributed to the ground states (GS), the first excited states (ES1), and the second excited states (ES2), respectively.
As indicated in the inset in Fig. 1, the EL spectrum for the QD-only test sample shows a series of well-defined features at 1293, 1200, and 1116 nm, which are attributed to the ground state, the first excited state, and the second excited state of the QD transitions.
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In the region of the shortest wavelengths (below 500 nm), the positive signal decreases significantly showing that different processes take place which we can attribute to the ground-state bleaching [32].
The 1560 cm 1 signal decayed with a lifetime of 100 ns, forming another transient species (main feature 1626 cm 1), which decayed with a lifetime of 200 ns and was attributed to the singlet ground state of the cation (41).
Both the fluorescence and phosphorescence emission spectra are composed of a monomeric-like component and a red-shifted emission attributed to the formation of ground state dimers.
Gray points show the signals that can be attributed to the ordinary daytime ground backscatter signals.
Consequently, the long-term FW PG variation at our site, which is a typical continental site in the Northern Hemisphere, is attributed to the seasonality of ground aerosol concentration.
Considering the dependence of the quantum confinement potentials on the dot size, the most intense peak located at 1.06 eV is attributed to the emission from the ground states of larger QDs (LQDs), while the higher energy peak at 1.11 eV refers to the emission from the ground states of smaller QDs (SQDs) [15].
Tan et al. [29] estimated that YRB wildfires resulted in the total emission of 81 ± 14 Tg C yr-1 in 2004 alone, of which 73%and27%7% could be attributed to the consumption of the ground layer and aboveground biomass, respectively.
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