4 research outputs found
Supplementary document for Optofluidic Tunable Filters using Ionic Liquid Electrolyte Capacitors - 6829960.pdf
Supplemental Document
Sesquiterpenoids with Phytotoxic and Antifungal Activities from a Pathogenic Fungus <i>Aspergillus alabamensis</i>
Five
new carotane sesquiterpenoids (asperalacids A–E (1–5)), one new tricyclic sesquiterpenoid
(4-hydroxy-5(6)-dihydroterrecyclic acid A (6)), and two
known analogues (7–8) were obtained
from a seagrass-derived fungus Aspergillus alabamensis, which was speculated to be a phytopathogenic fungus, isolated from
the necrotic leaves of Enhalus acoroides. The structures of 1–6 were established
by a combination of spectroscopic methods, including comprehensive
NMR analysis, mass spectrometry, conformational analysis, NMR computational
methods, and ECD calculations. Compound 4, with higher
inhibitory activity on wheat (Triticum aestivum L.) root and shoot elongation than the positive control terbutryn,
a broad-spectrum systemic herbicide, is a new natural plant growth
inhibitor. Compound 5, belonging to the rare glycosylated
sesquiterpenoid class, represents the first example of glycosylated
carotane sesquiterpenoid whose sugar moiety was identified as α-d-glucose. Compounds 1–4 and 6 displayed weak to potent antimicrobial activity against
the plant pathogenic fungi Fusarium oxysporum, Fusarium graminearum, and Penicillium italicum and the Gram-positive bacteria Bacillus subtilis and Staphylococcus
aureus
Comparison of Daytime and Nighttime New Particle Growth at the HKUST Supersite in Hong Kong
Particles larger than 50–100
nm in diameter have been considered
to be effective cloud condensation nuclei (CCN) under typical atmospheric
conditions. We studied the growth of newly formed particles (NPs)
in the atmosphere and the conditions for these particles to grow beyond
50 nm at a suburban coastal site in Hong Kong. Altogether, 17 new
particle formation events each lasting over 1 h were observed in 17
days during 8 Mar–28 Apr and 1 Nov–30 Dec 2011. In 12
events, single-stage growth of NPs was observed in daytime when the
median mobility diameter of NPs (<i>D</i><sub>p</sub>) increased
up to ∼40 nm but did not increase further. In three events,
two-stage particle growth to 61–97 nm was observed at nighttime.
The second stage growth was preceded by a first-stage growth in daytime
when the <i>D</i><sub>p</sub> reached 43 ± 4 nm. In
all these 15 events, organics and sulfuric acid were major contributors
to the first-stage growth in daytime. Ammonium nitrate unlikely contributed
to the growth in daytime, but it was correlated with the second-stage
growth of ∼40 nm NPs to CCN sizes at nighttime. The remaining
two events apparently showed second-stage growth in late afternoon
but were confirmed to be due to mixing of NPs with pre-existing particles.
We conclude that daytime NP growth cannot reach CCN sizes at our site,
but nighttime NP growth driven by organics and NH<sub>4</sub>NO<sub>3</sub> can
Double-Edged Role of VOCs Reduction in Nitrate Formation: Insights from Observations during the China International Import Expo 2018
Aerosol nitrate (NO3–) constitutes
a significant component of fine particles in China. Prioritizing the
control of volatile organic compounds (VOCs) is a crucial step toward
achieving clean air, yet its impact on NO3– pollution remains inadequately understood. Here, we examined the
role of VOCs in NO3– formation by combining
comprehensive field measurements conducted during the China International
Import Expo (CIIE) in Shanghai (from 10 October to 22 November 2018)
and multiphase chemical modeling. Despite a decline in primary pollutants
during the CIIE, NO3– levels increased
compared to pre-CIIE and post-CIIENO3– concentrations decreased in the daytime (by −10 and −26%)
while increasing in the nighttime (by 8 and 30%). Analysis of the
observations and backward trajectory indicates that the diurnal variation
in NO3– was mainly attributed to local
chemistry rather than meteorological conditions. Decreasing VOCs lowered
the daytime NO3– production by reducing
the hydroxyl radical level, whereas the greater VOCs reduction at
night than that in the daytime increased the nitrate radical level,
thereby promoting the nocturnal NO3– production.
These results reveal the double-edged role of VOCs in NO3– formation, underscoring the need for transferring
large VOC-emitting enterprises from the daytime to the nighttime,
which should be considered in formulating corresponding policies