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Air Pollution
EIA uses its unique investigative skills to tackle one of the greatest threats to global ecological security - depletion of the ozone layer. Life on Earth depends on the fragile ozone layer to screen out harmful ultraviolet radiation. In the mid-1980s scientists first observed a 'hole’ in this ozone layer over the Antarctic – resulting from widespread use of a range of ozone-depleting substances (ODS). Chemicals containing chlorine and bromine are the culprits causing damage to the ozone layer. These include chlorofluorocarbons (CFCs) mostly used for refrigeration and air-conditioning, and halons, used to extinguish fires. In 1987 the international community came together to sign the Montreal Protocol convention, under which ozone-depleting substances will eventually be phased out. Yet by the mid-1990s the gradual phase-out schedule had prompted the emergence of a thriving illegal trade in CFCs and halons. EIA is the only international NGO working to expose the smuggling of ozone-depleting substances, and is the acknowledged expert group on the subject. EIA’s detailed evidence on the global illegal trade in CFCs and halons has been presented to Montreal Protocol member countries, as well as enforcement agencies around the world.
Editorial: Fluoride Versus Sulfur Oxides in Air Pollution
Dr. George L. Waldbott
For several decades, extensive investigations have been under way regarding airborne sulfur oxides and their effects on human health. Sulfur oxides are a major atmospheric contaminant derived from the burning of fossil fuels, particularly of soft coal.
In the two London, England, smoke disasters in 1940 and in 1952, sulfur oxides received understandably much attention because the smoke could be seen coming out of the many chimneys of London homes where soft coal was being burned. Furthermore, their characteristic odor, their bluish-white color, and the relative ease of demonstrating their presence in the air accounted for their identification with coal smoke. Nevertheless, some investigators (1-3) questioned the role of sulfur oxides in smoke disasters, because the officially reported concentrations in the air were not sufficiently elevated to induce serious damage to health. In the 1952 London disaster, the average concentration of sulfur dioxide was 1.7 ppm which is well within the industrial threshold limit of 5 ppm (4).
In contrast to the London disaster, in the Donora, Pennsylvania (1948), and the Meuse Valley (1930) pollution episodes, where zinc smelters and fertilizer plants contributed significantly to the atmospheric contamination, sulfur oxides played a minor role. These industries are notorious sources for fluoride emission. Indeed, the official investigators failed to establish a major contaminant to which the disastrous effect could have been attributed since knowledge on airborne fluorides was very sparse at that time. Independent studies in both areas, in Donora by Sadtler (5) and in the Meuse Valley in retrospect by Roholm (6) produced considerable evidence indicating that fluoride was primarily responsible for illness and death in these two disasters.
In reviewing the effects of the two pollutants on vegetation and domestic animals there can be no doubt that airborne fluoride is far more harmful than sulfur oxides. Guinea pigs exposed to sulfur oxides continuously for one year at a concentration of 5 ppm failed to develop respiratory disorders (7). Fluoride, on the other hand, reaches the blood stream both through inhalation and by ingestion with contaminated food. Similarly, in plants the translocation of fluoride throughout the plant structure and its damaging effect on leaves, blossoms and fruit is much more pronounced than that of sulfur oxides (8). In comparing the effects of sulfur oxides on plants with that of fluorides, Bohne (9) showed that greater amounts of fluoride had accumulated and that fluoride had caused more damage than sulfur oxides.
In humans, more than 90% of inhaled sulfur oxides are absorbed in the airways above the larynx (10). With the moisture of the air, they form sulfuric acid and sulfates which, although irritating to the respiratory membranes, are of low toxicity.
Thus sulfur oxides irritate, primarily, the upper respiratory tract. They rarely, if ever, enter the distal portions of the lungs and the alveolar system. They never enter the bloodstream. Fluoride, on the other hand - a systemic poison - is promptly absorbed into the blood stream from the upper respiratory tract. It affects primarily the calcified tissue but can also induce considerable damage to many other organs, especially the arteries and the heart.
In the London episode, the delayed effects and subsequent deaths from respiratory diseases differed materially from effects in Donora and in the Meuse Valley where heart failure played a major role in the afflicted persons. Sulfur compounds are associated with a general increase in the total white male mortalities (11). These authors were not aware that sulfur oxides are not likely to reach beyond the respiratory tract. The simultaneous presence of fluoride and other toxic agents in coal and other fossil fuel could well account for their findings.
Recent studies by Dassler and others (see page 223), from the German Democratic Republic, tend to shed considerable light on the explanation of the cause of casualties in the London disaster. They found that the fluoride content of soft coal may reach a level as high as 1400 ppm (ashed) and that between 70 and 100 percent of gaseous fluoride is airborne when coal is burned. In other words, where there is smoke from burning coal there is also fluoride. Thus, the systemic damage to humans believed to have been induced by sulfur oxides is likely to be primarily brought on by fluoride in conjunction with such other toxic agents as arsenic, cadmium and mercury present in coal (4). Further studies on this problem are indicated.
To learn more about fluoride pollution, see http://www.fluoridealert.org/f-pollution.htm
Invasive species means an alien species whose introduction does
or is likely to cause economic or environmental harm or harm to human health.
Invasive species are one of the largest threats to our terrestrial, coastal and
freshwater ecosystems, as well as being a major global concern. Invasive species
can affect aquatic ecosystems directly or by affecting the land in ways that
harm aquatic ecosystems. Invasive species represent the second leading cause of
species extinction and loss of biodiversity in aquatic environments worldwide.
They also result in considerable economic effects through direct economic losses
and management/control costs, while dramatically altering ecosystems supporting
commercial and recreational activities. Effects on aquatic ecosystems result in
decreased native populations, modified water tables, changes in run-off dynamics
and fire frequency, among other alterations. These ecological changes in turn
impact many recreational and commercial activities dependent on aquatic
ecosystems. Common sources of aquatic invasive species introduction include
ballast water, aquaculture escapes, and accidental and/or intentional
introductions, among others.
A major concern is the introduction of invasive species through ship ballast water carrying viable organisms from one water body to another. All mainland coasts of the United States – East, West, Gulf, and Great Lakes, as well as the coastal waters of Alaska, Hawaii, and the Pacific Islands – have felt the effects of successful aquatic species invasions. Over two-thirds of recent non-native species introductions in marine and coastal areas are likely due to ship-borne vectors, and ballast water transport and discharge is the most universal and ubiquitous of these. EPA is working in conjunction with our Federal and State partners to address this source of aquatic invasive species both domestically and internationally.
They suggest that the buildup of carbon dioxide and other greenhouse gases in the atmosphere has fed a 30-year trend of stronger winds encircling the Arctic and bringing warmer winters to the Northern Hemisphere.
Natural causes can't be ruled out, but computer-based climate models cannot simulate the effect unless they include the influence of the buildup of such gases, says David Thompson of the University of Washington at Seattle. Indeed, the trend "seems to be unprecedented," noted Seattle colleague John Wallace at a recent meeting here of the American Geophysical Union.
The shift is in what is called Arctic Oscillation. Arctic Oscillation refers to two patterns of atmospheric pressure that occur in the region between the north pole and north mid-latitudes.
The "weak" phase of the oscillation occurs when the average Arctic pressure is higher than normal while the mid-latitude average pressure is below normal. The "strong" phase occurs when Arctic pressure is relatively low and mid-latitude pressure relatively high. In this mode, winds between the mid-latitudes and the Arctic tend to form a pattern called the Polar Vortex. This usually confines colder air to high latitudes. Warmer, wetter conditions then prevail over Scandinavia, Siberia, and North America east of the Rockies. The Seattle scientists have found, to their surprise, that the Arctic
Oscillation has been increasingly favoring this strong mode during the past 30 years. Something seems to be biasing its fluctuations. They suspect greenhouse gases are forcing this bias, but they can't yet prove it.
The oscillation operates independent of other major weather factors such as El Niño, and changes in the oscillation can explain much of what has been happening in the Northern Hemisphere climate.
The change in the oscillation can account for half of the 5.4 degree F. rise in Eurasian average surface temperature during the past 30 years. It accounts for nearly all of the small drop in Arctic average sea level atmospheric pressure. It accounts for three-quarters of the 45 percent rise in Norwegian rainfall.
Other scientists have identified such trends with swings in Atlantic and Pacific sea-surface temperatures. Dr. Wallace says these are just part of the oscillation.
In a perplexing discovery, scientists also discovered that these oscillations begin six miles up in the stratosphere and move downward - instead of starting low and moving upward like all other known weather phenomena.
Moreover, Mark Baldwin of Northwest Research Associates Inc. in Bellevue, Wash., notes that the stratosphere is relatively cold in the strong phase of
the oscillation. This provides further evidence that greenhouse gases could be influencing the oscillations, he says, because greenhouse gases cool the stratosphere as they warm the surface.
In another announcement at the meeting with major implications for climate-change study, researchers said new data indicate that the dirt and soot humans put in the air are as important as greenhouse gases in driving global warming.
Climatologists don't yet know whether they enhance the warming or tone it down, but the find suggests that efforts to curb the emission of greenhouse gases are not enough to control human-induced climate change. A global effort will have to be made to control aerosol pollution as well.
"This is a sort of new thing thrown at us," says climatologist V. Ramanathan with the Scripps Institution of Oceanography in La Jolla, Calif. It introduces unexpected complexity into the climate-change puzzle.
Scientists had thought aerosols would have a cooling effect because they reflect incoming sunshine. But the haze layers contained so much soot they absorbed some of the radiation and warmed up.
Scientists say they want to study whether the haze is having an effect on tiny marine algae that underlie the ocean food chain. But the main
effect of aerosols may be on rainfall and clouds, says Dr. Ramanathan. They may change cloud structure in ways that significantly change - probably reduce - rainfall.
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