Nuclear weapons
A nuclear weapon is a bomb whose destructive power is mainly based on the pressure wave and thermal radiation created by the explosion. Another threat is radiation from both radioactive substances released by the explosion and neutron radiation released immediately in the explosion.
The effects of a nuclear explosion depend significantly on whether the bomb explodes on the surface, underground or in the air. The extent of the radiation hazard area depends on the size and especially the explosion height of the nuclear weapon. If the explosion occurs so low that it creates a risk of significant deposition, protection against the radiation caused by the nuclear weapon explosion is provided by civil defence shelters.
A nuclear weapon does not go off accidentally, even if it is dropped or the vehicle carrying the weapon crashes. However, a fire or chemical explosion can damage a nuclear weapon so that the uranium or plutonium it contains is exposed and released into the environment. As a result, the radiation situation near the accident site could be harmful to health up to tens of kilometres away.
Nuclear weapon construction is a demanding process that requires weapons-grade material, such as highly enriched uranium or plutonium.
Air detonation of a nuclear weapon
In an air detonation, the nuclear weapon explodes so high that the fireball of the explosion does not touch the ground. As a result, the areas of the destructive pressure effect and thermal radiation are biggest and the impact zone of the nuclear weapon is thus as wide as possible. Detonating a 100 kiloton nuclear weapon at an optimum height in the air, for example, would kill a large proportion of completely unprotected population within a radius of about four kilometres from the point of explosion. The radioactive substances created in an air explosion rise high up in the atmosphere, and a local fallout, which is particularly dangerous in terms of radiation, does not usually occur.
Surface detonation of a nuclear weapon
In surface detonation, a nuclear weapon explodes on or near ground surface. Shortly after the explosion, a large proportion of the resulting highly radioactive substances fall on ground as a local fallout. Outside the immediate impact zone, there is then a threat of radiation from the radioactive substances generated by the explosion.
The extent of the radiation hazard area depends on the size and explosion height of the nuclear weapon, as well as on the weather conditions. When a large, megaton nuclear weapon explodes, people even hundreds of kilometres away from the explosion site have to go to civil defence shelters in the direction of the spread of fallout. The corresponding impacts of the explosion of a smaller, kiloton tactical nuclear weapon might extend to tens of kilometres.
The strong heat immediately vaporises the structures of the bomb and the radioactive substances produced by the explosion. If the nuclear explosion occurs so low that the fireball of the explosion touches the ground, it will also cause the soil and materials to melt and evaporate. The material rises into the air by the force of the explosion and forms a mushroom-shaped cloud typical of a nuclear explosion.
The heat and pressure wave caused by a nuclear weapon is so strong that it kills and destroys living environments in a wide area. These are immediate impacts that occur within approximately one minute of the explosion.
Immediate impacts also include initial radioactive radiation, which is ionising gamma and neutron radiation generated in the initial phase of the nuclear explosion.
Electromagnetic pulses (EMP), on the other hand, propagate in the atmosphere and can damage electronics and electrical equipment over a wide area if the explosion occurs high in the atmosphere.
The after-effects include early fallout of radioactive radiation, i.e. fallout occurring on the ground within a day, delayed fallout and the radioactivity of the explosion site. The health hazards of the after-effects can appear after years and even decades.
Consequences of a radiation hazard situation caused by the use of a nuclear weapon
As a result of the use of a nuclear weapon, some areas would be completely destroyed and normal life and economic activities would be impossible. The conditions would be similar to those after a devastating earthquake. However, the thermal radiation generated by a nuclear explosion would cause many serious burns to those surviving the explosion, whose treatment would require a lot of attention. In the immediate vicinity of the explosion, people would also be exposed to intense direct radiation, which can cause conditions such as radiation sickness. In addition, possible radioactive fallout would cause a risk that does not occur in natural disasters.
The radioactive fallout resulting from a surface detonation differs in its composition from possible fallout resulting from a nuclear power plant accident. It causes an immediate radiation risk, especially through external radiation. The fallout also threatens the safety of rescue personnel and slows down rescue work and helping survivors.
As after a nuclear power plant accident, the fallout can contaminate food. Radioactive substances may find their way into cereals and other food or feed plants directly from the air, with rain or dry deposition or from the ground extracted by plant roots. Animals can breathe contaminated air, and some of the fallout that enters surface water is transferred to fish via water food chains.
A serious fallout situation would not only cause a radiation hazard. Long-term psychological consequences could be significant, especially for the survivors in the area who are concerned about long-term health effects. This would probably make it much more difficult to return to normal life than in a natural disaster of a corresponding scale. In addition, it is known from nuclear power plant accidents that the radiation effects of fallout may cause concern even far away from the actual accident area.
Food production would have to be restricted over a much wider area than where people are protected. The economic consequences would also be significant. The economic impacts would be considerable around the world, especially if the nuclear weapon were used in an area that is strongly linked to world trade. In addition to direct damage, the fallout and its threat would hinder economic activity and transport in extensive areas. The accident at the Fukushima nuclear power plant in 2011, for example, had such consequences much further away than would have been justified on the basis of mere radiation.
The need to perform radiation measurements on goods and people arriving from the presumed fallout area would probably also have a significant impact on international trade and the movement of people. Such an area can extend to thousands of kilometres. Following the Fukushima accident, pressure arose to ensure the cleanliness of all goods, vehicles and people arriving from or passing through the presumed fallout area.
The type of explosive, the yield of the explosion, explosion height and weather conditions all affect the radiation hazard situation and exposure caused by the use of nuclear weapons.
The explosive power of a nuclear weapon is based on nuclear fission or fusion.
In a fission explosion, the nuclear reaction releases large amounts of energy by splitting heavy atomic nuclei, such as uranium (U-233, U-235) or plutonium (Pu-239). The explosion generates radioactive substances and neutron radiation.
In a fusion explosion, energy is released when lighter atomic nuclei are fused. Fusion bombs always require a fission explosion as an igniter, but the fusion reaction itself produces much less radioactive products . On the other hand, neutrons created during fusion can transform the bomb’s structural materials and environmental substances into radioactive substances. Nuclear fusion requires a very high temperature. In practice, fissions determine the radiation hazard caused by radioactive substances in most fusion bombs. For this reason, the share of the total explosion intensity caused by fissions is important information when assessing consequences. Fusion is fuelled by tritium, deuterium and lithium or a mixture of these (H-3, H-2, Li-6, Li-7).
The yield of a nuclear explosion is described by comparing it to a TNT explosive. A one kiloton nuclear explosion is thus equivalent to 1,000 tonnes of TNT explosive. Explosion intensity is usually measured in kilotons (kt) or megatons (Mt). One kiloton corresponds to approximately 4.2 x 1012 joules of energy. A nuclear explosion of one kiloton, for example, releases as much energy as the complete fission of approximately 50–60 grams of uranium or plutonium.
Among others, the total yield and height of the explosion mainly determine how high the explosion cloud rises and how large it is at the beginning. The cloud caused by a ground surface explosion or a low-altitude air explosion reaches between 3 and 30 kilometres in about ten minutes, depending on the yield of the explosion.
If the fireball created by the explosion touches the ground below and/or various structures, it vaporises their materials. The materials are absorbed into the rising explosion cloud and form attachment points of different sizes for vaporised radioactive substances. The process produces radioactive particles of different sizes, the largest of which start to fall immediately around the explosion site. These particles form early fallout, i.e. fallout occurring on ground surface within 24 hours.
The finest materials rise high with the explosion cloud, even up to the stratosphere in the case of a large bomb or a bomb detonated at a high altitude. Particles that reach the stratosphere circulate around the globe with air currents and only settle on the ground over years. This will result in a delayed fallout occurring over the long term. Because the particles remain in the atmosphere for years before settling, their radioactivity decreases through multiple half-lives. As a result, the radiation effects of delayed fallout are significantly lower than those of early fallout. If the explosion occurs high enough in relation to the explosion intensity of the bomb, the fireball will not touch the ground at all and there will be little early fallout. Non-radiation effects are still significant (pressure, heat, electromagnetic pulse).
The radioactive cloud will travel and expand, at the same time diluting according to the prevailing wind conditions and atmospheric mixing conditions. Rainfall may bring radioactive substances to ground surface in large quantities compared to rain-free conditions.
Fifty per cent of the explosion energy of a fission bomb is pressure energy, 35 per cent thermal radiation, 5 per cent initial radiation and 10 per cent post-radiation. In a fusion bomb, where fission is always also required, half of the energy is assumed to come from fissions.
The estimates are averaged because the exact distribution of the explosion energy depends on the structure of the explosive. The share of fission in a fusion bomb, for example, may be considerably lower, resulting in less post-radiation in particular. The impact of the explosion also strongly depends on whether the bomb is exploded in the air, underground or in water. The higher in the atmosphere the bomb is detonated, the smaller the impact of the pressure surge or wave, for example. On the other hand, ground explosions cause significant radioactive contamination of soil and the living environment, which increases the effective total share of post-radiation (the share of radioactive fallout).
In the simplest consequence assessment models, the radiation hazard situation can be scaled according to the total explosion intensity, the share of fission in the explosion, average wind speed and explosion height.
Today, there are modern assessment models that take into account the prevailing weather conditions at different altitudes and distances, as well as the amounts of radioactive particles of different sizes in different parts of the cloud. However, despite the models, it is still necessary to make certain assumptions, at least with regard to the structure and composition of the bomb.
If a nuclear explosion occurs as a surface explosion, the effects of the fallout can at worst extend to the territories of several states hundreds, even thousands of kilometres away. This is influenced by the properties of the explosive, explosion height, the quality of ground surface and weather conditions. Experimental observations have shown that the intensity of fallout radiation decreases according to the seven-ten rule: radiation decreases to a ten-fold in seven hours from the intensity measured one hour after the explosion. This requires that nearly all of the fallout has already landed at the site. After that, the radiation declines further to a ten-fold of this in two days and so on.
Impact distances of nuclear explosions of different sizes | ||||
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Effects (explosion at optimum height) | Distance (km) | |||
Explosion intensity | ||||
1 kt | 10 kt | 100 kt | 1000 kt | |
Pressure | ||||
civil defence shelters are destroyed | 3 | |||
strong buildings become irreparably damaged | 0,4 | 0,8 | 1,6 | 3,5 |
weak buildings become irreparably damaged | 0,8 | 1,7 | 3,6 | 8 |
windows break, damage to doors and partitions | 3,5 | 7,5 | 16 | 34 |
Burn | ||||
2nd degree burns (blisters in burned areas); flammable substances ignite | 0,8 | 2,3 | 6,3 | 16 |
Radioactive initial radiation | ||||
almost all people get radiation sickness, some die | 0,9 | 1,3 | 1,8 | 2,5 |
Source: Ydinturvallisuus, 2013 (p. 333). Luku 8. Ydinmateriaalivalvonta kansainvälisen asevalvonnan edelläkävijänä (pdf).
Nuclear test ban
Nuclear weapons have been tested in nuclear tests conducted in air, water and underground since 1945. In 1963, nuclear tests were banned, with the exception of those conducted underground. There have been no nuclear tests in the atmosphere since 1980, although not all countries have committed to complying with the agreement. Tests in the atmosphere released radioactive substances into the environment, and small amounts of these substances can still be detected around the world. In 1996, a treaty banning all nuclear tests was signed, but it has not yet entered into force. However, compliance with the ban on nuclear testing is monitored with a global network of measurement stations.
Nuclear Material Regulation and the Non-Proliferation Treaty
The aim of safeguarding nuclear materials is to assure that nuclear materials and other nuclear products remain in peaceful use in accordance with permits and declarations and that nuclear facilities and nuclear technology are used only for peaceful purposes. Regulation aims to prevent the proliferation of nuclear weapons and to ensure that nuclear materials are not produced, used or transferred for the manufacture of nuclear weapons.
The international basis for regulation is the Treaty on the Non-Proliferation of Nuclear Weapons (NPT), which was ratified in 1969 and entered into force in 1970 and is monitored by the IAEA. Finland has been involved in the treaty from the very beginning.
In the EU, the use and procurement of nuclear materials is also supervised by the Commission’s Safeguards Department. The basis for supervision is the Euratom Treaty of 1957, the Treaty establishing the European Atomic Energy Community.
Nuclear material safeguards are a prerequisite for the peaceful use of nuclear energy. States have an undivided responsibility to ensure that no activities contrary to the Non-Proliferation Treaty are conducted in their territory.
International agreements
Disarmament is the most effective way to prevent the proliferation, testing and use of nuclear weapons. In addition to the Non-Proliferation Treaty, there are many other international agreements that support this goal: the Treaty Banning Nuclear Weapon Tests in the Atmosphere, In Outer Space and Under Water; also known as the Partial Test Ban Treaty (PTBT), and the Comprehensive Nuclear-Test-Ban Treaty, CTBT). The CTBT was signed in 1996, but it will not enter into force until all 44 countries using nuclear technology are involved in it.
Activities under the CTBT Treaty are monitored by CTBTO, which has a worldwide monitoring network for the detection of nuclear tests. The system measures radionuclides and also detects seismic, hydroacoustic and infrasound-based signals. Among other things, the system has detected all nuclear tests reported by North Korea.
Monitoring in Finland and the role of STUK
The Radiation and Nuclear Safety Authority (STUK) is an authority that sets requirements concerning nuclear and radiation safety and monitors their fulfilment. STUK also maintains and develops the national control system for nuclear materials, whose goal is to take care of fulfilling the obligations of the Treaty on the Non-Proliferation of Nuclear Weapons in Finland. The IAEA, on the other hand, monitors the functioning and results of the national control system also in Finland.
The monitoring targets are nuclear power plants and other nuclear facilities, nuclear materials and the final disposal of nuclear waste, based on the accounting and reporting of nuclear materials. Operators and STUK must always be aware of the number, location and use of all nuclear materials.
STUK also acts as the national data centre (FiNDC) required by CTBT. The FiNDC collects and analyses data produced by the CTBT monitoring network, for example, and reports suspected nuclear tests to the government.
When a radiation hazard is imminent, STUK carries out a situation assessment and evaluates the severity of the situation from the safety standpoint. STUK gives recommendations to other authorities regarding protective measures. STUK has 24-hour emergency preparedness for nuclear accidents and other radiation hazard situations.
Nuclear-weapon states
Of nuclear-weapon states, the Nuclear Non-Proliferation Treaty (NPT) has been signed by
- United States
- Russia
- The United Kingdom
- France
- China
Countries outside of the Nuclear Non-Proliferation Treaty that have declared that they own nuclear weapons:
- India
- Pakistan
- North Korea
In addition, Israel is estimated to have a significant number of nuclear weapons. North Korea has carried out several nuclear tests since 2009.
In addition to the current nuclear-weapon states, there are countries that have had a nuclear weapons programme or nuclear weapons:
- South Africa abandoned its programme and nuclear weapons and now has a nuclear power plant and other nuclear activity.
- Iraq had a nuclear weapons programme that was revealed during the Gulf War but did not make significant progress before the war broke out. The country has no nuclear weapons or nuclear activity.
- Syria secretly built a reactor suitable for the production of plutonium, which was bombed by Israel in 2007. The reactor was similar to the one in North Korea. Since then, it has been unclear where the other necessary facilities, nuclear material, etc., are. The programme ended soon after it had started, but the investigation has not progressed due to the state of war. Syria has minor nuclear activity.
- During the Gulf Wars, Iran had a preliminary nuclear weapons programme similar to a feasibility study, which it itself abandoned. The country secretly built two uranium enrichment plants using technology from secret networks, which later came under the control of the IAEA. Iran has a rather large nuclear power programme, which has also been suspected to prepare the ability to build a nuclear weapon, if necessary.
Q&A
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At its worst, nuclear fallout can extend to the territories of several countries hundreds, even thousands of kilometres away. This is influenced by the properties of the explosive, explosion height, the quality of ground surface and weather conditions. Explosion height in particular has a significant impact on whether or not local fallout occurs and, if so, how far it spreads.
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Nuclear material (Fin:ydinaineet) refers to specific fissionable substances and source materials suitable for producing nuclear energy. Specific fissionable substances include plutonium-239 (Pu-239) and uranium enriched with isotopes uranium-235 (U-235) or uranium-233 (U-233). The source materials are natural uranium, depleted uranium and thorium.
Nuclear use items (Fin:ydinmateriaali) refers to nuclear substances and other substances used in nuclear weapons or in their design and manufacture (e.g. deuterium and graphite), devices (e.g. fuel processing devices), equipment (e.g. enrichment and waste treatment plants), data materials and agreements.
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When a nuclear bomb explodes, a huge amount of thermal radiation is released, causing all the residues of the bomb parts to heat up to several tens of millions of degrees and vaporise. As all gases are created in the original volume of the bomb, evaporation creates enormous pressure that is about one million times that of the normal atmosphere. The thermal radiation of hot gases mainly consists of X-rays, which are absorbed into the surrounding air within a radius of a few metres in an air explosion. The fireball is created as a result of air and the chemical processes of the materials of the weapon's vaporised residues.
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The Radiation and Nuclear Safety Authority (STUK) monitors the use of nuclear material in Finland and is a national data centre in matters related to nuclear test monitoring. STUK also cooperates with international operators, such as the IAEA and CTBTO. STUK collects information and maintains situational awareness. STUK also has a standby task if a weapon explodes in a place that may threaten the population.
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Spent nuclear fuel is not the primary material for nuclear weapon construction. The plutonium isotope ratio of the spent fuel is unfavourable for the construction of a bomb, which makes the construction of an effective nuclear weapon more challenging than if actual weapons-grade plutonium were used. Separating plutonium from spent fuel also requires complicated chemical waste treatment. In addition, this would have major political and economic consequences, as such activity would violate the strict conditions of use of nuclear material safeguards and fuel purchase agreements.
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The greatest hazards of nuclear weapons arise from their actual use as a bomb, but there is also a minor risk of a nuclear weapon accident associated with manufacturing, storage and transport.
Nuclear bombs have been destroyed in accidents involving aircraft carrying them in Thule (1968) and Palomares (1966), for example. The accidents contaminated the environment. In 2012, the submarine Yekaterinburg with nuclear warheads caught fire during maintenance in Kola, Russia. If the warheads had also ignited, plutonium could have spread into the environment.
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Two nuclear bombs have been used in war. During the Second World War, the United States detonated nuclear bombs in Hiroshima and Nagasaki in 1945. In addition, more than 1,000 nuclear bombs have been detonated in nuclear tests, most of them much more powerful than the bombs used in Hiroshima and Nagasaki.