Particulate Matter (PM) and AerosolPropertiesExposure EffectsExisting GuidelinesVolcanic Examples and IncidentsReferencesVolcanic Gases and Aerosols Index
PropertiesAn aerosol is a suspension of a solid or liquid particle in the air. For health purposes, aerosol or particulate matter (PM) is typically defined by size, with the smaller particles having more health impact. Commonly quoted values for PM are total particulate matter (TPM) or total suspended particles (TSP); particles with a diameter <10 µm (PM10); and particles with a diameter <2.5 µm (PM2.5). The effects and guidelines given here apply only to the size of the aerosol, but surface properties, chemical composition, and multi-species interactions may also be important in governing impacts and these require further study. Halogen and some sulphate aerosols are acidic, and it is thought that acidic PM may pose a greater risk to health than non-acidic. Metals contained in volcanic plumes, such as mercury, iridium, arsenic, and others, can catalyse reactions, and particularly in combination with acid gases and aerosols, increase health effects. In addition, volcanic aerosols are typically PM2.5 (e.g. Allen et al., 2002), a size fraction that is able to penetrate into the deepest parts of the lung. Fine ash is an aerosol and may also be acidic if it has adsorbed acid gases in the plume. Certain types of ash also may have an associated silicosis risk (e.g. Baxter et al., 1999). These extended impacts are not considered here. Exposure EffectsCAUTION: Most studies of exposure effects are based on urban pollution and so are not representative of volcanic pollution. A high proportion of volcanic aerosol is acidic and there is concern that acidic aerosol may be more severe on the respiratory system than non-acidic aerosol. The effects and guidelines provided here should thus be taken as indicative only. Since the depth to which particulate matter can penetrate the respiratory system is dependent on size, fine particles (PM2.5) have a higher probability of deposition in the alveoli of the lungs and are associated with a greater health risk than larger particles. Particles of this small size also have residence times of days to weeks in the troposphere and can travel distances of hundreds to thousands of kilometres allowing them to be widely dispersed. The effects of even smaller "ultrafine" particles (<0.1 µm in diameter) on health are not well understood, but are of current concern. Recent studies suggest that, even at low levels (<100 µg m-3), short-term exposure to PM of any size range is associated with health effects (WHO, 1999), and that strong aerosol acidity or high sulphate content may contribute to the effects associated with PM2.5. Epidemiological studies have shown that both daily mortality and hospital admissions increase with increasing PM in the surface boundary layer and that the effects for PM2.5 are amplified over those for PM10 (e.g. Braga et al., 2001). The scale of these increases is only on the order of half to a few percent and these associations are only valid over a period of a few days. Once the exposure to air pollution has finished there are generally no long-term effects unless the initial dosage was very high (this is more likely in an industrial accident than in a volcanic context). The short-term impacts of PM are on the respiratory and pulmonary systems of the body. Asthmatics and people with existing respiratory problems may experience reactions at lower concentrations than others. Existing GuidelinesAmbient and occupational guidelines exist for particulate matter. Some guidelines are for total particulate matter (TPM), whereas others are for particular size fractions - usually PM10 or PM2.5. Guidelines for acidic aerosol do not exist. In 1971, the USA Environmental Protection Agency (EPA) set the level of particulate matter that could cause significant harm to the health of persons at 1000 µg m-3 (24-hour average). Importantly, this level is reduced when sulphur dioxide is also present at elevated concentrations. The tables show that this EPA value is considerably lower than the present USA occupational guidelines. Inhalation of aerosol can be prevented using respirators of an appropriate standard.
Ambient air quality guidelines for particulate matter/aerosol
Ambient Guidelines SummaryThe ambient particulate matter guidelines table above demonstrates the tremendous range of international guidelines that exist. Difference between country's guidelines may be explained by the age of the guideline, the practical achievement of a standard based on current and predicted pollution levels or the data from which the standard was set (e.g. epidemiological study versus actual pollution levels). The table below summarises the range of main guideline values for each particle size.
Summary of the ranges of ambient particulate matter guideline levels
Occupational guidelines for particulate matter/aerosol
Volcanic Examples and IncidentsVolcanic particulate emissions cause problems over a range of distances from the vent and the highest levels of particulate matter may be found in areas tens of km away from the volcano (e.g. Yano et al., 1990). In addition, at degassing volcanoes, levels of sulphate aerosol (SO42-) close to the vent can be dangerously high:
In some cases, in-plume aerosol concentrations can be quite low. For instance, plume concentrations of SO42- 10-300 km downwind of Etna, Italy in September 1983 were of order of magnitude 0.1-10 µg m-3 (Bergametti et al., 1984; Martin et al., 1986) and in 1989-90 mean PM10 levels tens of km downwind of the active Kilaeua vent on the Island of Hawaii were 11.1 µg m-3. Both of these examples are within ambient levels. However, one-hour averages of PM2.5 >80 µg m-3 have been measured at the popular National Park Visitor Center at the summit of Kilauea, during specific wind conditions (National Park Service, 2003 unpublished data). From 1987-1991, during the continuous phase of the Kilauea eruption, emergency room visits and hospital admissions for chronic obstructive pulmonary disease and asthma increased on the Island of Hawaii (Mannino et al., 1996), as compared to rates from 1981-1986, but a direct link between this increase and volcanic PM or gas emissions could not be established. The presence of metals and acid aerosol in the Kilauea plume also raises concerns regarding the health effects of volcanic pollution. The acidic mixture of volcanic gas and aerosol produced by Kilauea has been named "vog". Further downwind of active volcanoes particulate levels can be raised intermittently depending on the activity of the volcano and weather conditions.
Large eruptions cause problems due to the amount of fine ash they erupt; these health impacts have been reviewed by Horwell & Baxter, 2006:
Anecdotal evidence from many volcanoes shows that ash and acid aerosol in the vicinity of volcanic plumes can be an irritant to the eyes, skin and respiratory system, but relatively few studies have examined the impacts of volcanic particulate matter on human health. These studies include investigations of health effects related to the eruptions of Kilauea, Hawaii (e.g. Mannino et al., 1996); Mount St. Helens, USA (e.g. Baxter et al., 1981; Baxter et al 1983; Bernstein et al., 1986); Mt. Spurr (Choudhury et al., 1997; Gordian et al., 1996); Popocatepetl, Mexico (Rojas-Ramos et al., 2001); Ruapehu, New Zealand (Hickling et al., 1999); Sakurajima, Japan (e.g. Wakisaka et al., 1988, Yano et al., 1986); Soufrière Hills, Montserrat (e.g. Forbes et al. 2003); and Soufriere, St Vincent (e.g. Leus et al., 1981). In some of these studies, positive associations between increased volcanic particulate and certain health outcomes have been found for both acute and chronic exposure. However, it is difficult to separate the effects of ash, gas, and aerosols of various chemical compositions. In addition, the health measures examined in the studies were variable, with some more appropriate for discerning effects than others. Further work is required to determine the direct contribution of volcanic aerosol to ill health. ReferencesAllen, A.G., Oppenheimer, C., Ferm, M., Baxter, P.J., Horrocks, L.A., Galle, B., McGonigle, A.J.S. and Duffell, H.J., 2002. Primary sulfate aerosol and associated emissions from Masaya Volcano, Nicaragua. Journal of Geophysical Research 107(D23). Baxter, P.J., Ing, R., Falk, H. and Plikaytis, B., 1983. Mount St. Helens eruptions: the acute respiratory effects of volcanic ash in a North American community. Archives of Environmental Health, 38(3): 138-143. Baxter, P.J., Ing, R., Falk, H., French, J., Stein, G.F., Bernstein, R.S., Merchant, J.A. and Allard, A., 1981. Mount St Helens eruptions, May 18 to June 12, 1980. Journal of the American Medical Association, 246(22): 2585-2589. Baxter, P.J., Bonadonna, C., Dupree, R., Hards, V.L., Kohn, S.C., Murphy, M.D., Nichols, A., Nicholson, R.A., Norton, G., Searl, A., Sparks, R.S.J. and Vickers, B.P., 1999. Cristobalite in volcanic ash of the Soufrière Hills volcano, Montserrat, British West Indies. Science, 283: 1142-145. Bergametti, G., Martin, D., Carbonnelle, J., Faivre-Pierret, R. and Vie Le Sage, R., 1984. A mesoscale study of the elemental composition of aerosols emitted from Mt. Etna Volcano. Bulletin of Volcanology, 47(4(2)): 1107-1114. Bernstein, R.S., Baxter, P.J., Falk, H., Ing, R., Foster, L. and Frost, F., 1986. Immediate public health concerns and actions in volcanic eruptions: lessons from the Mount St. Helens eruptions, May 18 - October 18, 1980. American Journal of Public Health, 76(Supplement): 25-37. Braga, A.L.F., Zanobetti, A. and Schwartz, J., 2001. The lag structure between particulate air pollution and respiratory and cardiovascular deaths in 10 US cities. Journal of Occupational and Environmental Medicine, 43(11): 927-933. Choudhury, A.H., Gordian, M.E. and Morris, S.S., 1997. Associations between respiratory illness and PM10 air pollution. Archives of Environmental Health, 52(2): 113-117. Delmelle, P., Stix, J., Baxter, P.J., Garcia-Alvarez, J. and Barquero, J., 2002. Atmospheric dispersion, environmental effects and potential health hazard associated with the low-altitude gas plume of Masaya volcano, Nicaragua. Bulletin of Volcanology 64(6), 423-434. Forbes, L., Jarvis, D., Potts, J. and Baxter, P.J., 2003. Volcanic ash and respiratory symptoms in children on the island of Montserrat, British West Indies. Occupational and Environmental Medicine, 60(3): 207-211. Gordian, M.E., Özkaynak, H., Xue, J., Morris, S.S. and Spengler, J.D., 1996. Particulate air pollution and respiratory disease in Anchorage, Alaska. Environmental Health Perspectives, 104(3): 290-297. Hickling, J., Clements, M., Weinstein, P. and Woodward, A., 1999. Acute health effects of the Mount Ruapehu (New Zealand) volcanic eruption of June 1996. International Journal of Environmental Health Research, 9(2): 97-107. Horwell, C.J. and Baxter, P.J., 2006. A critical review of the studies on the respiratory health hazards of volcanic ash. Bulletin of Volcanology. Leus, X., Kintanar, C. and Bowman, V., 1981. Asthmatic bronchitis associated with a volcanic eruption in St. Vincent, West Indies. Disasters, 5: 67-69. Mannino, D.M., Ruben, S., Holschuh, F.C., Holschuh, T.C., Wilson, M.D. and Holschuh, T., 1996. Emergency department visits and hospitalizations for respiratory disease on the island of Hawaii, 1981 to 1991. Hawaii Medical Journal, 55: 48-54. Martin, D., Ardouin, B., Bergametti, G., Carbonnelle, J., Faivre-Pierret, R., Lambert, G., Le Cloarec, M.F. and Sennequier, G., 1986. Geochemistry of sulfur in Mount Etna plume. Journal of Geophysical Research, 91(B12): 12,249-12,254. Mason, B., 2002. Pinatubo dust is still a killer. New Scientist, 175(2351): 7. Mather, T.M., Allen, A.G., Oppenheimer, C., Pyle, D.M. and McGonigle, A.J.S., 2003. Size-resolved characterisation of soluble ions in the particles in the tropospheric plume of Masaya volcano, Nicaragua: origins and plume processing. Journal of Atmospheric Chemistry 46(3), 207-237. Miranda, J., Zepeda, F. and Galindo, I., 2004. The possible influence of volcanic emissions on atmospheric aerosols in the city of Colima, Mexico. Environmental Pollution, 127: 271-279. Moya, M., Castro, T., Zepeda, M. and Baez, A., 2003. Characterization of size-differentiated inorganic composition of aerosols in Mexico City. Atmospheric Environment, 37(25): 3581-3591. Raga, G.B., Kok, G.L., Baumgardner, D., Baez, A. and Rosas, I., 1999. Evidence for volcanic influence on Mexico City aerosols. Geophysical Research Letters, 26(8): 1149-1152. Rojas-Ramos, M., Catalan-Vazquez, M., Martin - Del Pozzo, A.L., Garcia-Ojeda, E., Villalba-Caloca, J. and Perez-Neria, J., 2001. A seven months prospective study of the respiratory effects of exposure to ash from Popocatepetl volcano, Mexico. Environmental Geochemistry and Health, 23: 383-396. Searl, A., Nicholl, A. and Baxter, P.J., 2002. Assessment of the exposure of islanders to ash from the Soufrière Hills volcano, Montserrat, British West Indies. Occupational and Environmental Medicine, 59(8): 523-531. Wakisaka, I., Yanagihashi, T., Tomari, T. and Ando, T., 1988. Effects of volcanic activity on the mortality figures of respiratory disease. Japan Journal of Hygiene, 42(6): 1101-1110. WHO, 1999. Guidelines for Air Quality, World Health Organisation, Geneva. Yano, E., Yokoyama, Y. and Nishii, S., 1986. Chronic pulmonary effects of volcanic ash: an epidemiological study. Archives of Environmental Health, 41(2): 94-99. Yano, E., Yokoyama, Y., Higashi, H., Nishii, S., Maeda, K. and Koizumi, A., 1990. Health effects of volcanic ash: a repeat study. Archives of Environmental Health, 45(6): 367-373.
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We are proud to announce the publication of two pamphlets on volcanic ash fall hazards. They are designed for mass distribution at the onset of new eruptions. They are now avaiable in English, Japanese, French Spanish, Portuguese and Swahili with Italian versions being available shortly. Please see our Pamphlets page for further infomation.
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