From the patterns, very intense peaks were observed at the three most important peaks of In2O3 namely 〈222〉, 〈400〉, 〈440〉 reflections.
In both EI and ESI mass spectra, very intense peaks corresponding to piperazine ring fragmentation were observed.
However, it should be noted that the very intense peaks in the EI mass spectra correspond to the R substituent connected to the piperazine 4′ nitrogen atom (Fig. 1b, fragments a and b).
The PL spectrum of PS shows a very intense emission peak at around 625 nm.
The diffraction pattern of pure Gr (Fig. 1(a)) shows a very intense, sharp peak at 2θ = 26.27°, attributed to the diffraction of the (002) graphite plane composed of highly organized layers with an interlayer spacing of 0.34 nm [34, 35].
For this species, Loehr and Plane, [35] and also Pokrovski et al.[9] observed a very distinctive intense peak near 710 cm-1, with a shoulder near 655 cm-1.
The mass spectrum showed a very intense molecular ion peak at 361 (M++2) and a number of fragments support the proposed structure [37].
The next day, the MFR upgraded it to a very intense tropical cyclone, estimating peak 10 minute winds of 225 km/h (140 mph).
On April 1, the MFR upgraded it to a very intense tropical cyclone, estimating peak 10 minute winds of 225 km/h (140 mph).
The low temperature relaxation observed by TSDC and d.m.a. is a complex band and as the temperature increases there are three very sharp and intense peaks which are attributed, by comparing the results of the various techniques used here, to the primary glass transition of the amorphous zones of the material, to an additional crystallization process and to the crystal-liquid crystal transition.
