Faraji Maryam, Pourpak Zahra, Naddafi Kazem, Nodehi Ramin Nabizadeh, Nicknam Mohammad Hossein, Shamsipour Mansour, Osornio-Vargas Alvaro R, Hassanvand Mohammad Sadegh, Alizadeh Zahra, Rezaei Soheila, Mazinani Marzieh, Soleimanifar Narjes, Mesdaghinia Alireza
1School of Public Health, Tehran University of Medical Sciences, Enqelab Square, Tehran, Iran.
2Immunology, Asthma and Allergy Research Institute, Tehran University of Medical Sciences, Tehran, Iran.
J Environ Health Sci Eng. 2019 Feb 2;17(1):493-502. doi: 10.1007/s40201-018-00327-w. eCollection 2019 Jun.
This study aimed to investigate chemical composition of PM (particulate matter with aerodynamic diameter ≤ 10 μm) during dust storm and inversion in Tehran and hemolysis effects.
PM was sampled in Tehran, Iran, during dust storm and inversion conditions. Water soluble ions (F¯, Cl¯, NO¯, NO¯, SO¯, Na, K, NH , Ca, Mg) and elements (Al, Ba, Cd, Co, Cr, Cu, Fe, Li, Mn, Mo, Ni, Pb, Se, Sn, Sr, V, Zn, Pt, Rh, Pd, As and Si) were analyzed by ion chromatograph (IC) and inductively coupled plasma optical emission spectrometer (ICP-OES), respectively. Hemolysis was examined as in vitro at PM concentrations of 50-300 μg/ml.
Daily average of PM concentrations in dusty and inversion days were 348.40 and 220.54 μg/m, respectively. Most prevalence ionic components were NO¯, Cl¯, SO¯ and Ca during dust storm and SO¯, NO¯, Cl¯ and NH during inversion. Si, Fe and Al had the maximum values in both conditions. Particles associated with both conditions induced hemolytic responses. PM from dusty day showed a higher hemolysis percent (10.24 ± 4.67%) than inversion (9.08 ± 5.47%), but this difference was not significant ( = 0.32). Hemolytic effects were significantly intensified by increased PM concentrations ( < 0.001) in a dose-response manner.
As the results, chemical composition of sampled particles from inversion days and dust storm was different from each other. Hemolytic effects of particles during dust storm were more than inversion days. However, this difference was not statistically significant.
本研究旨在调查德黑兰沙尘暴和逆温期间细颗粒物(空气动力学直径≤10μm的颗粒物)的化学成分及其溶血效应。
在伊朗德黑兰沙尘暴和逆温条件下采集细颗粒物。分别采用离子色谱仪(IC)和电感耦合等离子体发射光谱仪(ICP-OES)分析水溶性离子(F⁻、Cl⁻、NO₃⁻、NO₂⁻、SO₄²⁻、Na⁺、K⁺、NH₄⁺、Ca²⁺、Mg²⁺)和元素(Al、Ba、Cd、Co、Cr、Cu、Fe、Li、Mn、Mo、Ni、Pb、Se、Sn、Sr、V、Zn、Pt、Rh、Pd、As和Si)。在体外以50 - 300μg/ml的细颗粒物浓度检测溶血情况。
沙尘日和逆温日细颗粒物浓度的日平均值分别为348.40和220.54μg/m³。沙尘暴期间最普遍的离子成分是NO₃⁻、Cl⁻、SO₄²⁻和Ca²⁺,逆温期间是SO₄²⁻、NO₃⁻、Cl⁻和NH₄⁺。Si、Fe和Al在两种条件下的值均最高。与两种条件相关的颗粒物均诱导溶血反应。沙尘日的细颗粒物溶血百分比(10.24±4.67%)高于逆温日(9.08±5.47%),但差异不显著(P = 0.32)。溶血效应随细颗粒物浓度增加以剂量反应方式显著增强(P < 0.001)。
结果表明,逆温日和沙尘暴采样颗粒物的化学成分彼此不同。沙尘暴期间颗粒物的溶血效应大于逆温日。然而,这种差异无统计学意义。