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Short Sharp Science: A New Scientist Blog

00.30 GMT, 13 March 2011

Fukushima_explosion.jpg
(Image: NHK)

Sumit Paul-Choudhury, editor, newscientist.com


Cooling systems have failed at a second reactor at the stricken Fukushima Daiichi nuclear power plant, where a massive blast ripped through a reactor building on Saturday. The Tokyo Electric Power Company, which operates the plant, said it was preparing to release mildly radioactive steam to reduce pressure in the plant's No. 3 reactor.

The move follows the decision to use seawater mixed with boric acid to cool the No.1 reactor, whose core container remained intact despite a dramatic explosion which destroyed the walls and ceiling of the reactor building. The expectation is that the boron will kill the nuclear reaction while the corrosive seawater will cool the core and render the reactor unusable. Tepco described the reactor as "stable" late on Saturday and the Japanese government said radiation levels around the plant had decreased.

Around 200,000 people have now been evacuated from the vicinity of the Fukushima Daiichi plant and the nearby Fukushima Daini plant, where a state of emergency has also been declared and plans to vent steam have also been prepared. Up to 160 people may have been exposed to radiation, and those arriving at evacuation centres are being scanned and given iodine supplements. Iodine is used to mitigate radiation sickness.

17:40 GMT, 12 March 2011

Roger Highfield, magazine editor, and Yuriko Nagano, contributor, Tokyo

A turning point in the efforts to avert a meltdown at Fukushima Daiichi nuclear power station came in the wake of the blast that destroyed the exterior walls of the crippled reactor.

The emergency began when the magnitude 8.9 earthquake which rocked the region on 11 March put the 439 MWe Boiling Water Reactor into shutdown mode.

Even after shut down, however, a reactor still requires cooling.

Diesel generators initially supplied cooling water but they failed about an hour after the quake as a result of the tsunami, prompting fears of a meltdown.

The pressure in Fukushima 1 started to rise, as the cooling water covering the core boiled into steam.

Malcolm Grimston, an associate fellow at Chatham House in London, said that the fuel began to overheat.

At around 1500 degrees Celsius, the zirconium metal cladding the uranium fuel would react with the steam to form hydrogen.

If any of the fuel rods have been compromised, there would be evidence of a small amount of other radioisotopes called fission fragments (specifically radio-caesium and radio-iodine), according to Paddy Regan of Surrey University.

Regan added that while the intergrity of the pressure vessel is secure, the vast majority of the fission fragments and radioactive fuel material is safely contained within the pressure vessel and should not escape.

However, the pressure in the steel vessel would have increased inexorably.

The Tokyo Electric Power Company, Tepco, had the flexibility to use pressure release valves to vent some steam, even though it was mildly contaminated, because it had taken the precaution of evacuating the local population within a 12 mile radius.

Grimston described this as "extraordinary forward planning".

The steam was released from the pressure vessel into the surrounding building and this was consistent with reports that radiation levels had soared to around 1000 times the background level. Officials also said they had detected caesium, an indication that some fuel was already damaged.

The blast occurred at 3:36 PM local time after a large aftershock shook the plant, though Grimston said that it was not clear the two were connected.

The shock wave that can be clearly seen in video of the blast suggests a point ignition source detonated the released hydrogen when it came into contact with oxygen in the air, he said.

Four workers were injured, according to Atsushi Sugimoto of Tepco.

"At this point, we don't know how much radiation has escaped," said Shinji Kinjo of the Nuclear and Industrial Safety Agency. "Should the situation change, the evacuation zone could become larger."

Yukio Edano, Japan's Chief Cabinet Secretary, said the cause of the explosion was a mixture of hydrogen, from steam escaping the core, and oxygen from the surrounding air.

He added that the pressure vessel was unaffected and the incident would not be a cause for a large amount of radiation to leak.

Although the concrete cladding disintegrated in a spectacular fashion, Grimston said that the fact that the metal frame of the building was left intact suggests that the explosion was not as violent as it looked.

Because the plant went into operation in 1971 and is due for decommissioning, the decision was taken by Tepco to flood it with seawater containing boric acid to kill the nuclear reaction.

This began just after 2pm UK time and would take up to ten hours.

The use of corrosive seawater would render the reactor unusable but would ensure that the risk of a meltdown had been averted, said Grimston.

He said that, if the information he had received was accurate, it looked a "textbook example" of how to deal with a nuclear emergency.

Tepco said Fukushima was stable but remained sketchy on key details.

More measures are under way to protect the local population. "The authorities also say they are making preparations to distribute iodine to residents," said the International Atomic Energy Agency.

Meanwhile, an official at Japan's nuclear safety agency rated the incident  a 4, according to the International Nuclear and Radiological Event Scale. Three Mile Island was rated a 5, while Chernobyl was rated 7 on the 1 to 7 scale.

The Kyodo news agency reported that some 10,000 people in the town on Minamisanrikucho, in Miyagi prefecture, are missing in the wake of yesterday's tsunami.


12:30 GMT, 12 March 2011

Jeremy Webb, editor-in-chief and Rowan Hooper, news editor


Details are emerging of the explosion at the nuclear power plant in Fukushima on the east coast of Japan, 240 kilometres north of Tokyo.

The blast blew off the outer concrete shell of a building housing one of the six reactors at the Fukushima Daiichi (number 1) nuclear power station, leaving behind a skeleton of metalwork. Four workers are reported to have been injured at the site and radiation is leaking into the environment. Japanese authorities have extended the evacuation zone around the plant to 20 kilometres.

Chief Cabinet Secretary Yukio Edano told a press briefing that the pressure vessel that houses the radioactive core of the plant is intact, and that a large amount of radiation leakage is not expected. He said that radiation is remaining at a low level. The Japanese news agency Kyodo earlier reported levels of 1050 micro Sieverts - within Japanese national safety levels - around the explosion at the Fukushima 1 reactor building.

Edano announced that the Tokyo Electric Power Company (TEPCO), which runs the Fukushima facility, will be allowed to use sea water to cool the reactor down.

The cause of the explosion is still unclear, but suggestions include a build up steam released from the reactor cooling system or by the ignition of hydrogen gas. That hydrogen could have been liberated by water "cracking" in the ultra high temperatures in the reactor.

Trouble at Daiichi began on March 11, when the earthquake struck offshore, northeast of Fukushima. The plant tripped out immediately, as it's designed to do, shutting down the chain reaction in the core.

The reactors at the Daiichi station are boiling water reactors built by US company GE in the 1960s. Water passes up through the core, turning into steam, which powers the turbines to generate electricity. The steam is then cooled and pumped back into the core.

When the reactor trips out, water needs to keep circulating to remove residual heat in the core. But, according to TEPCO, an hour after the earthquake, the diesel engines running the cooling system failed. This led to evaporation of water in the core and a build up of steam in the pressure vessel.

TEPCO managed this by releasing the steam from the pressure vessel into the large surrounding building. This appears to be the building that has exploded.

If heat continues to build up in the core, there is a possibility that it could melt, as happened in the Three Mile Island accident in the US in 1979.


11:30 GMT, 12 March 2011

Paul Marks, senior technology reporter

A massive explosion has ripped through a nuclear power plant in the city of Fukushima on the east coast of Japan, raising fears of a radioactive meltdown. Four workers are believed to have been injured in the blast, which has caused major structural damage. Radioactive caesium and iodine isotopes, by-products of nuclear fission, have been detected in the vicinity.

A state of nuclear emergency was declared yesterday at the Fukushima-Daiichi plant, 240 kilometres north of Tokyo, as its operator, the Tokyo Electric Power Company (Tepco), struggled to contain rising temperatures and pressures in the core of two reactors whose cooling systems failed after Friday's magnitude 9.0 earthquake shook Japan and sent tsunami waves across the Pacific. Tepco has also reported problems at the nearby at the neighbouring Fukushima Daini plant, meaning that a total of five nuclear reactors are now covered by the state of emergency.

It is not yet clear what has been destroyed, but Japan's public broadcaster NHK is reporting that the walls to reactor number 1 at the Fukushima Daiichi plant - also known as Fukushima I - have been blown apart. It is not yet known if the reactor's containment vessel was affected. Nor is the cause of the explosion yet known, although commentators for the BBC and for Reuters suggested it was more likely to be chemical in nature than nuclear.

Updates from the Tokyo Electric Power Company over the few hours preceding the explosion indicated an inexorable build up of pressure in a number of the reactor containment buildings at both Fukushima sites.

All six of Fukushima 1's reactors are shut down - reactors 1, 2 and 3 were closed for precautionary reasons as the quake struck, while reactors 4,5 and 6 had already been switched off for inspections. At 1pm local time on 12 March, TEPCO reported that pressure was increasing in the containment vessel of reactor 1 and that it was taking steps to vent the pressure at the direction of the national government. At the same time, water was being introduced in a bid to cool the core - but that creates steam and adds to the pressure.

It appears from the explosion that the TEPCO lost its battle to keep the lid on the pressure on that reactor. If the temperature is still rising the core could melt into an uncontrollable radioactive-particle-ejecting mass - a "meltdown".

At the nearby Fukushima II plant an alarm suggested that one of the control rods used to quench the fission reaction had not been fully inserted - perhaps meaning that fission could continue. The alarm was later called off and Tepco said that other control rods had been confirmed as fully inserted, but the pressure and temperature nonetheless increased enough for another radioactive steam venting operation to be prepared.

Japan's megaquake: what we know

0930 GMT, 12 March 2011

Sumit Paul-Choudhury, editor, newscientist.com

There has been a massive explosion at the Fukushima-Daiichi nuclear power plant, raising fears of a radioactive meltdown. Several workers are believed to have been injured in the blast, which seems to have caused major structural damage to the plant.

A state of nuclear emergency was declared at the plant yesterday as its operator, the Tokyo Electric Power Company, struggled to contain rising temperatures and pressures in the core of two reactors whose cooling systems failed after Friday's magnitude 9.0 earthquake. An emergency has now also been declared at the neighbouring Fukushima Daini plant.

Further details here.

1830 GMT, 11 March 2011

Paul Marks, senior technology reporter

The US Air Force is delivering a cargo of liquid coolant to the Tokyo Electric Power Company's Fukushima-Daiichi nuclear power plant - where one of six reactors seriously affected by today's quake is still alarmingly hot many hours after it was automatically shut down when the quake struck.

Electrical, mechanical and diesel generator failures are said to have combined to deprive the reactor of power for its coolant pumps.

The Tokyo Electric Power Co told Japanese news service Jiji News that pressure in the reactor vessel is rising and that the company intends to "take measures" to release it. CNN reports that activity around the plant hints at a "struggle" to cool down the facility. Indeed, Japan's trade minister said this evening that there could well be what he described as "small radiation leak" from the Fukushima plant.

US Secretary of State Hilary Clinton said local US air bases are helping deliver the coolant. The reactor - one of six - is thought to be a boiling water reactor, so the coolant is likely to be demineralised light water, meaning it is depleted of the hydrogen isotope deuterium. 

Some 3000 local residents living within a 3 kilometre radius of the Fukushima plant have been evacuated by the Japanese defence force.


0240 GMT, 12 March 2011

Michael Reilly, senior technology editor

The latest figures on the earthquake that struck Japan on Friday suggest that, despite all the headlines, it was actually surprisingly small.

That is, the area of fault that ruptured was small - somewhere between 300 and 400 kilometres long. By comparison, the magnitude 9.1 Sumatra earthquake in 2004 broke along an area of fault 1300 km long.

How then, did today's quake get so powerful? What the fault lacked in size, it made up for when the two adjoining tectonic plates slipped a whopping 40 metres. This calculation comes from Chen Ji of the University of California, Santa Barbara (in the figure below, red colouring indicates areas of 40 metres' slip).

JapanQuake.jpg
(Image: Guangfu Shao / UCSB)

To arrive at this astounding figure, he downloaded information about when seismic waves arrived at listening stations around the world, and then reverse-engineered the data - earthquake geeks call it an inversion - to see where along the fault the seismic energy was generated.
 
It's early days, and Ji stresses that his work is preliminary. But his calculations suggest that an area of fault between 300 and 400 kilometres long by 100 kilometres wide slipped some 40 metres. The US Geological Survey puts their estimate closer to 20 metres. Consider those upper and lower boundaries on where the final figure will likely fall.

Either way, it's apparent that this is one of the largest fault movements the world has ever seen.  And it has implications for future quakes in the region as well, as the stress released during the quake is likely to have transferred to other faults nearby.

"There is no doubt this quake increased stress conditions and the potential for the fault to break both to the south and north of this event," Ji told New Scientist. "It could be a few months, or it could be a few years."

Once Japan and its researchers are back on their feet, data from the country's thousands of seismic monitors will emerge that will provide a look in unprecedented detail at how the quake that spawned this disaster unfolded.

Peter Aldhous, San Francisco bureau chief

The surge of water that inundated the coast of northeast Japan was triggered by the largest quake in the nation's history. But Japan is no stranger to devastating earthquakes and tsunamis, as this map of seismic events since 1900 shows. Use the slider to view quakes for a narrower range of dates, roll over the points to see data on each earthquake, and use the radio buttons to reveal the deadly quakes featured in the table.

Dashboard blog
Dashboard blog

Caitlin Stier, contributor

dickinson1HR.jpg
(Image: Daniel Dickinson)

Single-celled slime moulds work together to improve their chances for survival. Now Daniel Dickinson and his colleagues at Stanford University in Palo Alto, California, have discovered that the humble slime Dictyostelium discoideum forms a specialised tissue known as a polarised epithelium that rivals forms found in multicellular animals. The findings suggest the building blocks for multicellularity existed long before the first animals evolved.

When food is scarce for the slime mould, a fungus-like creature that lurks in damp soils, they join up to create a stalk and cap structure that spreads their spores to a new home. The tip of this fruiting body is made up of the polarised epithelium (pictured above). Proteins similar to the animal equivalents of alpha- and beta-catenins (in orange) help the slime mould organise components within each cell to specialise the function of the overall tissue.

Journal reference: Science, DOI: 10.1126/science.1199633

All today's stories on NewScientist.com, including: Japan earthquake, motion capture kangaroos, and a lost world under the sea

Full text RSS feed Full text RSS - You can now subscribe to the full text of Today on New Scientist.

Japan's quake updated to magnitude 9.0

A 9.0-magnitude earthquake struck off the coast of Japan today, triggering a tsunami - more tsunamis are expected around the Pacific

Eight extremes: The biggest things in the universe

The mightiest planet, star, galaxy, artefact - and hole

Nuke test sensors could hear tsunamis coming

At the moment it's a matter of guesswork whether a submarine earthquake is going to produce a tsunami. But a treaty banning nuclear tests may change that

Sea level's rise and rise is down to melting ice sheets

Greenland and Antarctic ice sheets could bump up sea levels by 56 centimetres this century

Lost world hints at life in the Mesozoic

A seamount of the Antarctic coast has a fauna that appears to be a throwback to the end of the Mesozoic, over 65 million years ago

Motion capture could reveal how kangaroos hop

See how a technique typically used in animated movies is being used to study kangaroo movement

Feedback: Amazing achievement of peak performer

One man who's consulted 3 million people, when an automatic door isn't, meet the googlegang, and more

PS3 no longer hackable?

The security hole in Sony's Playstation 3 appears to have been patched. What does that mean for their lawsuit against the hacker that exploited it?

Tumours could be the ancestors of animals

Cancers could be "living fossils" with a genetic code laid down 600 million years ago, giving hope that modern therapies will eventually prevail

High-tech remixes vs low-tech originals: You decide

See what happened when Intel commissioned 13 artists to reinterpret 13 masterpieces, using new technologies to bring them into the digital age

Eight extremes: The densest thing in the universe

Try working out the density of a black hole

US navy faces up to a new enemy - climate change

A National Research Council report for the US navy identifies weaknesses on the warming Arctic frontier and the threat of rising sea levels

Inflight Wi-Fi hits more turbulence

A new breed of brighter cockpit displays went blank when an inflight Wi-Fi system was turned on

Fluid societies powered human evolution

Human hunter-gatherer societies swap members more flexibly than groups of other animals do - could that have driven the rise in brainpower?

Drug-carrying robot roams through eye

A tiny robotic implant could better target drugs to treat conditions like macular degeneration

Remastered masterpieces given a new lease of life

Reinterpretations of iconic artworks in a London exhibition sometimes miss the mark, but many are excellent pieces in their own right

Debora MacKenzie, Brussels correspondent

At the moment it's a matter of guesswork whether a submarine earthquake is going to produce a tsunami. But a treaty banning nuclear tests - or at least, trying to - may change that, if the treaty doesn't die first.

The Comprehensive Nuclear Test-Ban Treaty was signed in 1996 but has not yet come into effect, mostly because the US has not yet ratified it - though President Obama wants to.

Meanwhile a worldwide network of seismographs and other sensors designed to detect nuclear blasts listens for any tests. But it also gives fast, reliable warnings of earthquakes. The Comprehensive Nuclear Test-Ban Treaty Organization monitoring centre in Vienna, Austria, spotted today's Japanese quake, and alerted Indonesia and other governments to the quake off Sumatra that caused the 2004 Boxing Day tsunami. And it can also do other tricks too.

All today's stories on NewScientist.com, including: smart wingtips, missing Martian carbon dioxide, and the darkest thing in the universe

Full text RSS feed Full text RSS - You can now subscribe to the full text of Today on New Scientist.

Eight extremes: The darkest thing in the universe

The least bright thing in the universe is dark matter - one day, perhaps we'll see it

Born to be viral: Computer fights hacker attack

A stunning visualisation shows a hacker break into a server and the battle that ensues

Momentous quantum milestones

Jim Baggott's The Quantum Story: A history in 40 moments goes from Max Planck to Richard Feynman in discrete quanta

Quit-smoking apps perform dismally in tests

In tests, smartphone apps designed to help people stop smoking received a dismal 7.8 out of 60 points on average

Cigarette packets stripped bare and hidden away

The UK government has plans to hide cigarettes behind shop counters and to strip colours from the packets in a bid to curb smoking. But will it work?

Smarter wingtips speed record-breaking solar drone

Adding a miniature tail to an aircraft wingtip will allow the wing to made from lighter materials - and boost speed

One pill or two? The weather can help doctors decide

Doctors may soon look out of the window before setting drug doses - it seems sunlight can affect how fast we metabolise drugs

Eight extremes: The roundest thing in the universe

Does anything live up to the medieval notion of the music of the spheres?

Mars's missing carbon dioxide could be underground

The Red Planet's carbon-dioxide atmosphere was probably much thicker in the past - some of it may have gone into carbonate minerals that were later buried

Jessica Hamzelou, reporter

Cigarettes will be hidden behind shop counters and their packets stripped of suggestive colours and wording, according to recent UK government white paper. 

But will the changes have an effect on smokers? The Department of Health has published its tobacco control plan for England - a series of promises to change the way tobacco products are sold with the aim of cutting the number of the country's adult smokers by 210,000 by the end of 2015. 

The plan was released yesterday to coincide with the UK's national no smoking day. In the document, the government says it will bring in legislation to end tobacco displays in large stores by April 2012 and other stores by April 2015. It also promises to:

Consult on options to reduce the promotional impact of tobacco packaging, such as using plain packaging by the end of the year 

Caitlin Stier, contributor

Thumbnail image for marscarbon.jpg

(Image: NASA/JPL-Caltech/Univ. of Arizona)

Carbonate minerals buried beneath the Martian surface could help explain the disappearance of carbon dioxide from Mars's atmosphere.

A thin, CO2-dominated atmosphere surrounds Mars today. But in the past, it was likely much thicker, allowing liquid water to remain stable on the planet's surface. Where did that carbon dioxide go?

It may have gone towards forming carbonate minerals, which on Earth arise when oceans absorb carbon dioxide from the atmosphere and deposit it as carbonate rock. A similar process involving liquid water may have happened on ancient Mars.

A mineral-mapping instrument aboard NASA's Mars Reconnaissance Orbiter has spotted the minerals (shown in lighter shades) in rocks that had once been buried beneath the planet's surface but were later brought to the surface by impacts. A crater on the raised rim of an even larger, 470-metre-wide crater called Huygens reveals these iron and calcium carbonates.

James Wray of Cornell University in Ithaca, New York, presented the findings this week at the Lunar and Planetary Science Conference in Texas.

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