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1.
Sci Total Environ ; 919: 170633, 2024 Apr 01.
Article in English | MEDLINE | ID: mdl-38340865

ABSTRACT

Biogenic and anthropogenic organic vapors are crucial precursors of ozone and secondary organic aerosol (SOA) in the atmosphere. Here we conducted real-time measurements of gaseous organic compounds using a Vocus proton-transfer-reaction mass spectrometer (Vocus PTR-MS) at the Shanghuang mountain site (1128 m a.s.l.) in southeastern China during November 2022. Our results revealed a substantial impact of mixed biogenic and anthropogenic compounds at the mountain site, with oxygenated volatile organic compounds (OVOCs) comprising 74 % of the organic vapors. Two distinct periods, characterized by sunny days (P1) and persistent cloud events (P2), were observed. P1 exhibited higher concentrations of biogenic-related emissions compared to P2. For instance, isoprene, monoterpenes, and sesquiterpenes during P1 were 2.4-2.9 times higher than those during P2. OVOCs such as acetaldehyde, MVK + MACR, acetone, and MEK also showed higher concentrations during P1, indicating a dominant source from the photochemical oxidation of biogenic VOCs. Anthropogenic-related VOCs like benzene and toluene had higher concentrations during P2, displaying different diurnal cycles compared to P1. Our analysis identified four biogenic-related factors dominated by isoprene and sesquiterpene oxidation products, and two anthropogenic-related factors. During P1, biogenic sources contributed approximately 80 % to total organic compounds, while during P2, anthropogenic sources, particularly the aromatic-related factor, increased from 16 % to 35 %. Furthermore, a unique factor characterized by C2 amines and C3 amides and periodic plumes indicated the influence of industrial emissions from regional transport. The study highlights the significant variations in sources and compositions of gaseous organic compounds at regional mountain sites due to changes in meteorology and photochemical processing, potentially impacting regional ozone and SOA formation.

2.
Proc Natl Acad Sci U S A ; 115(34): 8541-8546, 2018 08 21.
Article in English | MEDLINE | ID: mdl-30082380

ABSTRACT

The signature of mass-independent fractionation of quadruple sulfur stable isotopes (S-MIF) in Archean rocks, ice cores, and Martian meteorites provides a unique probe of the oxygen and sulfur cycles in the terrestrial and Martian paleoatmospheres. Its mechanistic origin, however, contains some uncertainties. Even for the modern atmosphere, the primary mechanism responsible for the S-MIF observed in nearly all tropospheric sulfates has not been identified. Here we present high-sensitivity measurements of a fifth sulfur isotope, stratospherically produced radiosulfur, along with all four stable sulfur isotopes in the same sulfate aerosols and a suite of chemical species to define sources and mechanisms on a field observational basis. The five-sulfur-isotope and multiple chemical species analysis approach provides strong evidence that S-MIF signatures in tropospheric sulfates are concomitantly affected by two distinct processes: an altitude-dependent positive 33S anomaly, likely linked to stratospheric SO2 photolysis, and a negative 36S anomaly mainly associated with combustion. Our quadruple stable sulfur isotopic measurements in varying coal samples (formed in the Carboniferous, Permian, and Triassic periods) and in SO2 emitted from combustion display normal 33S and 36S, indicating that the observed negative 36S anomalies originate from a previously unknown S-MIF mechanism during combustion (likely recombination reactions) instead of coal itself. The basic chemical physics of S-MIF in both photolytic and thermal reactions and their interplay, which were not explored together in the past, may be another ingredient for providing deeper understanding of the evolution of Earth's atmosphere and life's origin.

3.
Br J Oral Maxillofac Surg ; 47(6): 461-5, 2009 Sep.
Article in English | MEDLINE | ID: mdl-19586694

ABSTRACT

We report our experience of the management of 53 patients with 57 carotid body tumours from two units of oral and maxillofacial surgery in China between 1995 and 2006. Digital subtraction angiography was used most often for the confirmation of diagnosis and preoperative assessment. Fifty-one patients with 55 tumours had their tumours resected and 2 patients had radiotherapy. Of the 55 excised tumours, 14 were resected successfully without injury to the carotid artery, 25 were resected with the external carotid artery, 5 had arteriorrhaphy, and 11 resulted in sacrificing the unilateral internal carotid artery (ICA). Six patients had interposition reconstruction of the ICA. Immediately after operation 14 patients (27%) had neurological damage, which was permanent in 3 (6%), and 2 (4%) developed stroke. There were no deaths. Once the ICA is resected, vascular reconstruction is recommended to minimise neurological morbidity.


Subject(s)
Carotid Artery, External/surgery , Carotid Artery, Internal/surgery , Carotid Body Tumor/surgery , Vascular Surgical Procedures/adverse effects , Adolescent , Adult , Aged , Angiography, Digital Subtraction , Carotid Body Tumor/diagnostic imaging , Carotid Body Tumor/radiotherapy , Child , Collateral Circulation , Cranial Nerve Injuries/etiology , Female , Humans , Male , Middle Aged , Retrospective Studies , Stroke/etiology , Treatment Outcome , Vascular Surgical Procedures/methods , Young Adult
4.
Zhonghua Kou Qiang Yi Xue Za Zhi ; 38(3): 213-6, 2003 May.
Article in Chinese | MEDLINE | ID: mdl-12887802

ABSTRACT

OBJECTIVE: To investigate the friction and wear behavior of different human enamels. METHODS: 24 enamel samples selected from aged, young permanent and faded deciduous teeth were classified into 3 groups and slid against artificial porcelain teeth in the presence of artificial saliva on an oscillating friction and wear test rig. The wear volume loss, microhardness and toughness of each group of the enamel specimens were measured, the wear scars were observed with a scanning electron microscope, and the elemental compositions of Ca, P, and Si of the wear scar and wear debris were determined with an energy dispersion spectrometer. RESULTS: The wear volume losses of aged, young permanent and deciduous tooth enamels are (2.40 +/- 1.10) x 10(-12) m(3), (3.50 +/- 1.83) x 10(-12) m(3) and (4.86 +/- 2.49) x 10(-12) m(3). The data of aged tooth enamels are statistically greater than that of deciduous tooth enamels (P < 0.05). There is no significant difference between the wear volume loss of aged and young permanent tooth enamels or between the young permanent and deciduous tooth enamels (P > 0.05). However, the friction and wear behavior of each group of enamel specimens is different from each other. CONCLUSIONS: In the present testing condition, the wear scars of each kind of enamel specimens is characterized by ploughing and cracking. The different wear resistance of the three kinds of enamels is attributed to the different microstructure of the enamel, while the hardness and toughness of the enamels are not correlated with the wear resistance.


Subject(s)
Dental Enamel/pathology , Tooth Abrasion/pathology , Adolescent , Age Factors , Aged, 80 and over , Child , Child, Preschool , Dentition, Permanent , Female , Humans , In Vitro Techniques , Infant , Infant, Newborn , Male , Middle Aged , Tooth, Deciduous
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