| 
 Radioecology 
 and the Chernobyl Disaster 
 By: J.N.B. Bell 
 Radioecology 
 is the study of the pathways of radionuclides in the environment and their 
 impact on biota. It is a relatively young science, having been born following 
 the development of nuclear weapons. Initially concern was related to the fate 
 of radionuclides discharged into the stratosphere following the testing of 
 nuclear bombs aboveground, with subsequent long-term deposition to the earth's 
 surface on a global scale. Subsequently, interest switched to the consequences 
 of releases from nuclear installations, such as power stations and reprocessing 
 plants, arising routinely or as a result of accidents. In terms of accidents, 
 the Chernobyl Disaster of 1986 had the most widespread and serious 
 environmental consequences, which led to a major boost in research into a wide 
 range of radioecological topics. 
 It is now 
 over 16 years since the accident at the Chernobyl nuclear power station in the 
 northern Ukraine, then part of the USSR, yet the ensuing environmental problems 
 remain to this day and will continue into the future. The accident occurred on
 26 
 April 1986 
 (a date which I remember well, because it is my birthday!), as a result of an 
 unauthorized experiment coupled with a design fault, which rendered the reactor 
 inherently unsafe. The accident resulted in a massive surge of power, which 
 could not be controlled, due to removal or switching off of control devices, 
 causing a steam explosion, which blew the top off the reactor. This was 
 followed by a major fire, which burned for 10 days before becoming 
 extinguished. The fires resulted in discharge of vast quantities of a cocktail 
 of radionuclides to the atmosphere. A large amount of the radioactivity was 
 deposited in the surrounding regions of both Ukraine and Byelorussia, this 
 being often associated with the larger particles arising from the fire, but the 
 plume containing smaller particles and gases was dispersed a very long 
 distance, ultimately circling the northern hemisphere. 
 The human 
 consequences of the accident were appalling. Some 150,000 people had to be 
 evacuated from the nearfield contaminated area and a large amount of farmland 
 taken out of production. To this day much of the surrounding area is a 
 permanent exclusion zone and the city of Prypiat, which formerly contained 
 c.55,000 people is the largest ghost town in the world, with a population of 
 zero. An immediate ecological effect of the accident was the radiation-induced 
 death of trees close to the reactor, resulting in the so-called "Red Forest". 
 Subsequently abnormalities were observed in the form of very large pine needles 
 and oak leaves. These heavily contaminated trees were disposed of by burial on 
 the site of the 
 Red 
 Forest. Around the reactor the topsoil was scraped off for disposal and the 
 reactor itself was entombed in concrete to form a sarcophagus in order that the 
 other reactors in the complex could continue to operate. 
 As was 
 normal in the Soviet Union the authorities failed to publicise bad news and it 
 was not until the plume had been detected abroad that the first announcement 
 was made. Thus on 28 April at 21.00 Radio Moscow reported "An accident has 
 occurred at the Chernobyl nuclear power plant - one of the atomic reactors has 
 been damaged. Measures are being taken to liquidate the consequences of the 
 accident. Those affected are being given aid, and a government commission has 
 been created". This was essentially a standard USSR statement and could be 
 described as the understatement of the century! 
 The first 
 detection of the radioactive plume outside the USSR occurred at the Forsmark 
 nuclear power station on the east coast of Sweden, when the alarms sounded. 
 When it was determined that no accident had taken place on site it was realised 
 that a massive nuclear disaster had occurred in some place east of Sweden. This 
 initial plume passed over central 
 Europe, 
 depositing radioactivity largely as a result of interception by rain. Then in 
 early May the plume moved northwards, passing over the United Kingdom, with 
 deposition of radioactivity primarily being associated with rainstorms. 
 Immediately the countries concerned started to take measurements of the 
 radionuclides of concern in environmental samples, such as air, water and soil 
 and in foods, such as vegetables, milk and meat, as the isotopes concerned - 
 iodine - 131, caesium - 134 and caesium - 137 entered food chains. The 
 half-life of I131 is only 8 days, but values for Cs134 
 and Cs137 are 2 and 30 years, respectively, so that a longer term 
 problem should have been anticipated. 
 Different 
 countries reacted very differently in terms of countermeasures taken to 
 reduce radioactive dose to humans. In Germany different states also gave 
 varying advice, including not allowing children to play in sand and avoiding 
 the consumption of certain vegetables, while in The Netherlands the sale of 
 sheepsmilk cheese was prohibited for some time. Particular problems arose in 
 Arctic Scandinavia, where the Lapps are heavily reliant on their reindeer herds 
 as a source of food. Reindeer feed on reindeer moss, which is in fact a lichen 
 and, as such is adapted to take up nutrients from the atmosphere. The latter 
 fact and the absence of the protective cuticle found in higher plants resulted 
 in the reindeer moss accumulating an extremely high level of radiocaesium, 
 which is then passed through the food chain to reindeer. In view of highly 
 elevated levels of caesium in reindeer the authorities took action by 
 slaughtering large numbers of the animals, thereby resulting in considerable 
 social hardship to the people concerned. In the UK it was decided that any 
 immediate countermeasures, such as a ban on sale of milk from heavily 
 contaminated areas, would cause more social disruption and stress than was 
 warranted by any hypothetical life saved by reduction in collective dose. So 
 the only advice given in the immediate aftermath of the accident (other than 
 "do not panic"!) was not to drink rainwater in certain parts of Scotland. 
 Thus it was 
 apparent that radioactivity was entering food-chains. In fact the behaviour of 
 radiocaesium in this respect had been studied back to the days of bomb-testing, 
 when regular measurements were made of levels in air and milk across the UK. 
 Another radionuclide, strontium-90 had similarly been studied in milk and air, 
 and as an undergraduate I remember newspaper cartoons of housewifes testing 
 milk bottles with Geiger counters and people making jokes about drinking their 
 daily dose of radioactivity! In the UK the government was extremely reassuring 
 and it is worth noting what was said at the time. On 
 6th
 May 1986 
 the Secretary of State for the Environment stated in the House of Commons that 
 "The effects of the cloud have already been assessed and none presents a risk 
 to health in the UK". On 13th May he reiterated "As long as there 
 are no further discharges from the Chernobyl accident, the incident may be 
 regarded as over for this country by the end of the week, although its traces 
 will remain". Further reassurance was given by the Minister of Agriculture on 
 the 19th May when he told the House of Commons "We have always been 
 a long way from the stage when we might need to contemplate imposing any sort 
 of restriction". 
 One month 
 later from this last statement the Ministry of Agriculture, Fisheries and Food 
 suddenly imposed a wide scale ban on the movement and slaughter of sheep over a 
 large area of North West England, surrounding the mountainous Lake District, 
 and in North Wales, including the mountainous Snowdonia area. Then 4 days later 
 the Secretary of State for Scotland announced a similar ban in 3 regions of 
 that country. 
 The 
 disruption caused by these actions was severe in the extreme, in view of the 
 paramount importance of sheep farming in the local economies. The ban was 
 imposed, because radiocaesium levels in sheep meat were being found to exceed 
 the regulatory threshold of 1000 Bq kg-1. The only way of testing if 
 this threshold was being exceeded was by killing the animal concerned and a 
 sample of meat being sent off to a laboratory for analysis. 4,200,000 sheep out 
 of a national flock of 24,600,000 were affected in this manner and, clearly, it 
 was not possible to determine the level of radioactivity in each of these. Thus 
 during the summer of 1986 there was a race to develop a "live monitor", which 
 could be used to measure the level of radioactivity in sheep without the need 
 for slaughter. By the autumn this monitor had been used to assess precisely 
 where the sheep exceeded the threshold level and it was possible to lift the 
 ban on large areas of land. The latter were essentially in lowlands, with the 
 remaining banned areas being in the uplands, with rough grazing of natural 
 vegetation. 
 Why did the 
 government fail to predict that in many upland areas sheep would show rising 
 radiocaesium levels, rather than falling ones, as had been predicted? The 
 problem lay essentially in the fact that advice by Ministry of Agriculture, 
 Fisheries and Food Scientists was based on experiments involving measurement of 
 uptake by crops of caesium from agricultural lowland soils. Such soils contain 
 a significant proportion of clay particles onto which caesium rapidly becomes 
 more or less irreversibly fixed and thus is unavailable for uptake into plants. 
 An example of such an experiment was carried out at Imperial College in the mid 
 1980s. Winter wheat was grown over two successive growing seasons in two 
 agricultural soils - a sandy loam and a silty clay - which had been 
 contaminated with Cs137 before the start of the experiment. The 
 uptake was measured at maturity in each year: in 1984 and 1985, the wheat 
 growing in the sandy loam contained 105 and 38 Bq kg-1, 
 respectively, while the corresponding figures for the silty clay were 180 and 
 29 Bq kg-'. This fall was not due to depletion of radiocaesium in 
 the soil, but rather by fixation on clay particles. In lowland agricultural 
 areas of the UK this is precisely what happened, with a sharp fall in caesium 
 levels in agricultural grasses, from the time of initial contamination. Indeed 
 the areas derestricted after the first live monitoring exercise were all places 
 with normal agricultural soils. 
 The upland 
 areas where restrictions remained were very different from lowland agricultural 
 systems. They contain semi-natural habitats, with peaty soils with very low 
 clay contents. In addition they are invariably highly acidic and often 
 waterlogged, both characteristics tending to render metals more available for 
 uptake through the roots. The vegetation in these places is very different from 
 lowland grasses. It consists of coarse grasses, sedges and Ericaceous species, 
 as well as other plants adapted to these harsh conditions. The plants concerned 
 are adapted to maximise nutrient uptake from these very poor quality soils. It 
 should be remembered that caesium is an analogue of potassium, which is a 
 macronutrient, and thus it is hardly surprising that the radionuclide was 
 accumulated to extremely high levels in the upland vegetation. Sheep graze this 
 wild vegetation and thus radiocaesium enters the food chain. The effect of 
 growing plants on simulated upland and agricultural soils was demonstrated in a 
 further experiment at Imperial College. In this case artificial soils were 
 constructed containing either 18% clay and 10% peat or 2% clay and 90% peat and 
 Cs137 mixed into these. Heather (Calluna vulgaris), one of 
 the species grazed in uplands, was then grown in these soils for 25 days and 
 the uptake of the radionuclide measured at the end of this period. The results 
 of this study were dramatic, with the high peat/low clay soil plants containing 
 11395 Bq g-1 compared with 177 Bq g-1 in the high 
 clay/low peat soil. Current thinking is that the high organic matter content, 
 rather than low clay levels, is the predominant factor leading to the high 
 mobility of radiocaesium in upland ecosystems. 
 The problems 
 of contamination of ecosystems in Europe after the Chernobyl accident led to 
 extensive research programmes into environmental pathways of radiocaesium in 
 the countries concerned. These concentrated on a whole range of 
 natural/semi-natural ecosystems, which had largely been ignored in earlier 
 research. Besides soil characteristics, a range of vegetation related factors 
 were examined, such as absorption through the foliage, rooting depth and 
 seasonal growth patterns, as well as the influence of grazing by sheep and soil 
 ingestion. A study at Imperial College showed that heather could absorb large 
 quantities of caesium through the foliage, with subsequent translocation to 
 elsewhere in the shoot, whereas two other ericaceous species - bilberry (Vaccinium 
 myrtilus) and cross-leaved heath (Erica tetralix)- showed lower 
 uptake. Research in Scotland with artificial contamination of a grassland 
 showed a high level of variability in uptake of caesium between species, with 
 an insignificant species which represented a tiny fraction of cover in the 
 sward, the mouse-eared chickweed (Cerastium fontanum), showing a 
 particularly high level of accumulation. 
 Chernobyl 
 caused a major rethink in the world of radioecology, with the realisation that 
 there were many potential food-chain pathways to humans other than via 
 agriculture. Thus interest developed into uptake of radiocaesium into wild 
 fruits, game birds and animals and edible fungi. The latter are highly 
 effective in taking up caesium from the soil. This caused particular problems 
 in contaminated areas, where hunting of deer takes place. These animals have a 
 strong liking for the macrocarps of fungi and in the autumn these can form a 
 substantial part of their diet, thus resulting in high levels of radiocaesium 
 in their flesh. In Sweden active consideration was given to altering the 
 hunting season to avoid the major times of fungal fruiting body production, and 
 Prussian blue was introduced into saltlicks in the forest to act as an 
 antagonist to uptake of caesium. 
 It is now 
 nearly 17 years since the Chernobyl disaster. What is the situation in 
 contaminated areas at the present time and what is the prognosis for the 
 future? In the UK there continue to be restrictions on sheep in parts of the 
 contaminated uplands, although the number of farms affected continues to fall, 
 year by year. Thus in Cumbria 867,000 sheep on 1670 farms were restricted in 
 June 1986, with this failing by January 1998 to 14,000 sheep on 10 holdings. 
 The corresponding figures in Wales fell from 2,000,000 sheep on 5,100 farms to 
 180,000 sheep on 359 farms. Extrapolating into the future it has been estimated 
 that the last restrictions are likely to be lifted as long as 30 years into the 
 future, demonstrating the long-term influence of the Chernobyl accident at 
 locations very remote from the scene of the accident. 
 Around 
 Chernobyl itself large areas remain as an effectively permanent exclusion zone, 
 representing a vast radioactive nature reserve, where human influence has been 
 removed. This now teams with wildlife, including rare species, enjoying the 
 absence of interference by humans. The Red Forest has been replaced by new 
 growth of pine and birch trees, which contain large quantities of "Sr. At this 
 location there are concerns about downward migration of radioactivity into the 
 groundwater, with appropriate monitoring programmes having been established. 
 The exclusion zone represents a large open-air laboratory, with enormous 
 potential for research into radioecology, biogeochemical cycling and ecosystem 
 recovery after removal of human influence. A particularly important mechanism 
 for research in the Chernobyl area is the establishment of the Chernobyl 
 International Radioecology Laboratory. This is based in the city of Slavutych, 
 located outside the heavily contaminated area, which was constructed after the 
 accident to house the workers who operated the remaining reactors. This 
 laboratory is supported primarily by funds from the USA, but with contributions 
 also from the UK, France, Germany and Japan. It aims to provide facilities for 
 the international community of radioecologists to carry out research in the 
 exclusion zone. It has a second location, for more field-based work, in the 
 city of Chernobyl, which is still inhabited, but with the population living 
 there for 2 weeks on and 2 weeks off to reduce their dose. Much of the research 
 at the Laboratory is by radioecologists from the USA. This includes studies on 
 small mammals, which are particularly vulnerable, in view of their bodies being 
 in very close proximity to contaminated soil, so that they receive a 
 high dose of radioactivity. The results of this research are extremely 
 interesting. These animals are surviving at locations where they are exposed to 
 potentially lethal doses. At first it was thought that they might be wandering 
 into the most contaminated areas or else were not breeding. However, research 
 indicated that neither of these situations applied and that the animals 
 appeared to be adapting to these very high levels of radioactivity. Such 
 adaptation flies in the face of conventional wisdom and possibly should cause 
 us to re-examine the effects of radiation on biota, including humans. 
 The story of 
 Chernobyl is a tragic one and has represented a major set-back for the nuclear 
 power industry. The last operational reactor at 
 Chernobyl 
 closed around two years ago, with serious consequences for employment in this 
 remote region, although there are jobs concerned with the massive 
 decommissioning activities that will continue into the future. There are 
 salutary lessons to be learned from the UK government's misguided response to 
 contamination of the food chain. Any upland ecologist could have told the 
 agricultural scientists that radiocaesium could be expected to remain highly 
 mobile in the upland organic soils of the UK. This is a classic example of the 
 need to understand how the natural environment works in order to provide good 
 environmental protection and management. 
 Nigel Bell 
 is Professor of Environmental
 
 Pollution at Imperial College, London
 based 
 in the Department of Biological
 
 Sciences and the Department of
 
 Environmental Science & Technology |