Institute of Environmental and Occupational Health Sciences, College of Medicine, National Yang-Ming University, Taipei, Taiwan.
Environ Res. 2010 Aug;110(6):536-43. doi: 10.1016/j.envres.2010.05.009. Epub 2010 Jun 18.
Several studies have demonstrated that millions of people globally are potentially exposed to volcanic gases. Hydrogen sulfide is a typical gas in volcanic and geothermal areas. The gas is toxic at high concentrations that predominantly affects the nervous, cardiovascular, and respiratory systems. The WHO air quality guideline for hydrogen sulfide is 150 microg m(-3) (105 ppb). The northwest part of Taipei is surrounded by sulfur-rich geothermal and hot springs. Active fumaroles and bubbling springs around the geothermal area emit acidic gases. In combination with automobile emissions, the pollution of acid aerosols is characteristic of the metropolis. This study considered sulfur-rich geothermal, suburban and downtown locations of this metropolis to evaluate geothermally emitted acid aerosol and H(2)S pollution. Acid aerosols were collected using a honeycomb denuder filter pack sampling system (HDS), and then analyzed by ion chromatography (IC). Results indicated that long-term geothermal emissions, automobile emissions and photochemical reactions have led to significant variations in air pollution among regions of metropolitan Taipei. The highest H(2)S concentration was 1705 ppb in the geothermal area with low traffic density and the mean concentration was 404.06 ppb, which was higher than WHO guideline and might cause eye irritation. The SO(2) concentrations were relatively low (mean concentration was 3.9 ppb) in this area. It may partially result from the chemical reduction reaction in the geothermal emission, which converted the SO(2) gas into SO(4)(2-) and H(2)S. Consequently, very high sulfate concentrations (mean concentration higher than 25.0 microg m(-3)) were also observed in the area. The geothermal areas also emitted relatively high levels of aerosol acidity, Cl(-), F(-), PO(4)(3-), and N-containing aerosols. As a result, concentrations of HNO(3), NO(2)(-), PO(4)(3-), and SO(4)(2-) in metropolitan Taipei are significantly higher than those in other urban areas considered in other studies. These results provide evidence that geothermal emissions represent a significant source of acid aerosols in metropolitan Taipei. Therefore, in this metropolitan area, the combined health effects of air pollutants from automobiles and geothermal emissions should be particular concern.
几项研究表明,全球有数百万人可能接触到火山气体。硫化氢是火山和地热地区的一种典型气体。这种气体在高浓度下是有毒的,主要影响神经系统、心血管系统和呼吸系统。世卫组织的硫化氢空气质量指导值为 150 微克/立方米(105 皮克/立方英尺)。台北西北部被富含硫磺的地热和温泉环绕。地热区周围的活动喷气孔和冒泡温泉会排放酸性气体。再加上汽车排放的污染物,使得这个大都市的酸气溶胶污染具有特征性。本研究考虑了该大都市的富硫地热区、郊区和市区,以评估地热排放的酸气溶胶和 H₂S 污染。采用蜂窝状浓缩器过滤器采样系统(HDS)收集酸气溶胶,然后用离子色谱(IC)进行分析。结果表明,长期的地热排放、汽车排放和光化学反应导致了台北大都会不同地区空气污染的显著变化。在交通密度较低的地热区,H₂S 的最高浓度为 1705 皮克/立方英尺,平均值为 404.06 皮克/立方英尺,高于世卫组织的指导值,可能会引起眼睛刺激。该地区的 SO₂浓度相对较低(平均值为 3.9 皮克/立方英尺)。这可能部分是由于地热排放物中的化学还原反应,将 SO₂气体转化为 SO₄²⁻和 H₂S。因此,在该地区还观察到非常高的硫酸盐浓度(平均值高于 25.0 微克/立方米)。地热区还排放出相对较高水平的气溶胶酸度、Cl⁻、F⁻、PO₄³⁻和含氮气溶胶。因此,与其他研究中考虑的其他城市地区相比,台北大都会的 HNO₃、NO₂⁻、PO₄³⁻和 SO₄²⁻浓度明显更高。这些结果表明,地热排放是台北大都会酸气溶胶的一个重要来源。因此,在这个大都市地区,汽车和地热排放污染物的综合健康影响应该特别关注。