| Literature DB >> 34158493 |
M Said Alghabra1, Rami Ali1,2, Vyacheslav Kim1, Mazhar Iqbal1, Philipp Rosenberger3,4, Sambit Mitra3,4, Ritika Dagar3,4, Philipp Rupp3, Boris Bergues3,4, Deepak Mathur5, Matthias F Kling3,4, Ali S Alnaser6.
Abstract
Regarded as the most important ion in interstellar chemistry, the trihydrogen cation, [Formula: see text], plays a vital role in the formation of water and many complex organic molecules believed to be responsible for life in our universe. Apart from traditional plasma discharges, recent laboratory studies have focused on forming the trihydrogen cation from large organic molecules during their interactions with intense radiation and charged particles. In contrast, we present results on forming [Formula: see text] from bimolecular reactions that involve only an inorganic molecule, namely water, without the presence of any organic molecules to facilitate its formation. This generation of [Formula: see text] is enabled by "engineering" a suitable reaction environment comprising water-covered silica nanoparticles exposed to intense, femtosecond laser pulses. Similar, naturally-occurring, environments might exist in astrophysical settings where hydrated nanometer-sized dust particles are impacted by cosmic rays of charged particles or solar wind ions. Our results are a clear manifestation of how aerosolized nanoparticles in intense femtosecond laser fields can serve as a catalysts that enable exotic molecular entities to be produced via non-traditional routes.Entities:
Year: 2021 PMID: 34158493 PMCID: PMC8219811 DOI: 10.1038/s41467-021-24175-9
Source DB: PubMed Journal: Nat Commun ISSN: 2041-1723 Impact factor: 14.919
Fig. 1Emitted ions from the surfaces of nanoparticles.
a Comparison between two TOF spectra from two experiments (red/green lines) with different conditions including size of nanoparticles (100 and 300 nm), concentration of sample (3 and 1.5 g/L), and laser intensity at 2 × 1014 W/cm2 serving as an evidence for the formation of . b Comparison between ions emitted from the surfaces of 100 nm silica nanoparticles inhabited by H2O and D2O molecules at 3 g/L concentration and irradiated by a laser intensity of 2 × 1014 W/cm2. The presence of and peaks in the ToF spectrum of D2O adsorbed on nanoparticles presents unequivocal evidence about the source of the trideuterium ions (for extended TOF spectra, cf. Supplementary Fig. 4). Source data are provided as a Source Data file.
Fig. 2Ion emission from D2O in gas phase and on nanoparticles.
a Comparison between time-of-flight spectra for D2O in the gas phase for different laser intensities as indicated. The observed H+ ions originate from background gas. b Comparison between TOF spectra taken for D2O in the gas phase at 9.5 × 1014 W/cm2 laser intensity and ions emitted from the surface of 100 nm nanoparticles inhabited by D2O molecules at a laser intensity of 1 × 1014 W/cm2. Only the spectrum associated with nanoparticles demonstrates the formation of , , and ions. Source data are provided as a Source Data file.
Fig. 3Momentum and energy of .
a 2D momentum image demonstrating the angular distribution in the plane of laser propagation vs. nanoparticles jet where the laser polarization is perpendicular to this plane and b energy distribution of emitted from the surface of 300 nm silica nanoparticles inhabited by H2O molecules at a laser intensity of 2 × 1014 W/cm2. Source data are provided as a Source Data file.
Fig. 4Bimolecular reaction to form from water molecules on nanoparticles.
An illustration of two potential processes responsible from the formation of from water molecules on the surface of silica nanoparticles. The bottom panel demonstrates a nanoparticle in an intense laser field. The orange dashed line depicts the formation of from two separate water molecules through a roaming on the surface mechanism. The green dashed line depicts the roaming mechanism within a water dimer. In both cases, there exist four stages. Stage 1 shows the ground state. Stage 2 shows the migration mechanism leading to the formation of a hydrogen molecule. Stage 3 is roaming close to another water ion. Stage 4 is the formation of .
Fig. 5Experimental setup.
Illustration of the experimental setup showing the nanoparticle solution (Np Solution) that is aerosolized by an atomizer with the help of Ar as carrier gas. The aerosol is then collimated using the aerodynamic lens producing a jet that is admitted to the ultrahigh vacuum chamber. The nanoparticles interact with the laser field in the center of a constant-field (E) spectrometer. The ions generated from the interaction are accelerated towards a microchannel plate (MCP) and delay-line detector (DLD). As for the electrons, they are accelerated towards a channeltron and are used to discriminate between nanoparticles and background ions. The inset shows a scanning electron microscope (SEM) image of the silica nanoparticles (NanoComposix) used in the experiments.
Fig. 6Channeltron signal for gas-phase and nanoparticle targets.
Figure 6 displays accumulated distributions from ~1 billion pulses in the experiment. A considerable difference in channeltron signal between gas phase and nanoparticles D2O targets. The red line represents the channeltron signal for D2O in the gas phase, whereas the blue curve demonstrates the signal associated with nanoparticles. Both measurements were performed at a laser intensity of 2 × 1014 W/cm2. The vast majority of laser shots result in no channeltron signal as indicated by the black dashed line. The orange dashed line highlights how laser shots associated with irradiating nanoparticles generate a significantly larger channeltron signal, which in turn is used in coincidence with the time-of-flight spectra to extract the time of flight for ions associated with nanoparticles. Source data are provided as a Source Data file.