Protonated leucine enkephalin (YGGFL) was studied by ultraviolet photodissociation (UVPD) from 225 to 300 nm utilizing an optical parametric oscillator tunable wavelength laser system (OPO). Fragments were identified by absolute mass measurement in a 9.4 T Fourier transform ion cyclotron resonance mass spectrometer (FT-ICR MS). Bond cleavage was preferred in the vicinity of the two aromatic residues, resulting in high ion abundances for a, a, b, y and y fragments. a, b and y ions dominated the mass spectrum, and full sequence coverage was achieved for those types. Photodissociation was most effective at the short wavelength end of the studied range, which is assigned to the onset of the L π-π* transition of the tyrosine chromophore, but worked well also at the L π-π* chromophore absorption maxima in the 35 000-39 000 cm region. Several side-chain and internal fragments were observed. H atom loss is observed only above 41 000 cm, consistent with the requirement of a curve crossing to a repulsive πσ* state. It is suggested that the photochemically generated mobile H atom plays a role in further backbone cleavages, similar to the mechanism for electron capture dissociation. The b fragment is most intense at the L chromophore absorptions, undergoing additional fragmentation at higher photon energies. The high resolution of the FT-ICR MS revealed that out of all x and z-type fragments only x and x were formed, with low intensity. Other previously reported x- and z-fragments were re-assigned to internal fragments, based on exact mass measurement.
Although marine aerosols undergo extensive photochemical processing in the troposphere, a molecular level understanding of the elementary steps involved in these complex reaction sequences is still missing.
Understanding the intrinsic properties of the hydrated carbon dioxide radical anions CO2.−(H2O)n is relevant for electrochemical carbon dioxide functionalization. CO2.−(H2O)n (n=2–61) is investigated by using infrared action spectroscopy in the 1150–2220 cm−1 region in an ICR (ion cyclotron resonance) cell cooled to T=80 K. The spectra show an absorption band around 1280 cm−1, which is assigned to the symmetric C−O stretching vibration νs. It blueshifts with increasing cluster size, reaching the bulk value, within the experimental linewidth, for n=20. The antisymmetric C−O vibration νas is strongly coupled with the water bending mode ν2, causing a broad feature at approximately 1650 cm−1. For larger clusters, an additional broad and weak band appears above 1900 cm−1 similar to bulk water, which is assigned to a combination band of water bending and libration modes. Quantum chemical calculations provide insight into the interaction of CO2.− with the hydrogen‐bonding network.
Electronic
absorption spectra of water cluster anions (H2O)n–, n ≤
200, at T = 80 K are obtained by photodissociation
spectroscopy and compared with simulations from literature and experimental
data for bulk hydrated electrons. Two almost isoenergetic electron
binding motifs are seen for cluster sizes 20 ≤ n ≤ 40, which are assigned to surface and partially embedded
isomers. With increasing cluster size, the surface isomer becomes
less populated, and for n ≥ 50, the partially
embedded isomer prevails. The absorption shifts to the blue, reaching
a plateau at n ≈ 100. In this size range,
the absorption spectrum is similar to that of the bulk hydrated electron
but is slightly red-shifted; spectral moment analysis indicates that
these clusters are reasonable model systems for hydrated electrons
near the liquid–vacuum interface.
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