Wednesday, 20 April 2011

Cherry blossom season



My lost two posts have been rather sober (earthquakes and radiation!) so I thought it was time I mentioned some of the many pleasant things in Japan. At the top of the list right now would be cherry blossoms.

If I drew up a list of iconic images of Japan, somewhere on there would be a park decked with cherry blossoms. For the last week that is precisely how many parks, rivers and lane ways around Tokyo have been – decked with cherry blossoms. The cherry blossoms don't last long - perhaps only a week or two before they are shaken from the trees by the breeze - but in that short time the Japanese certainly make the most of them. Right now, the national sport seems to be gazing at the cherry blossoms at one of the prime viewing locations.

On a Sunday, the parks will be packed with picnickers taking part in Hanami. Hanami (花見), meaning "flower viewing", is simply a picnic where you gaze upon the cherry blossoms. The picnic lasts for most of the day and involves alcohol since you can drink in public here. It is a way of acknowledging the changing of the seasons which I'm told is important in Japan.

I had my first Hanami on Sunday in Yoyogi Park. It was a great day even though the weather turned a little cold towards the end. Here are some photos from the Hanami as well as some photos of cherry blossoms I took around Tokyo and a person I came across in Yoyogi Park who was walking their pet rabbit, Flopsy!

Take care

Our Man in Japan








Wednesday, 13 April 2011

Can you fell it in your bones? The presence of Strontium-90


[Summary: Much has been reported about the presence of radioactive Iodine-131 and Caesium-137 following the problems at the Fukushima nuclear plant. However, nothing has been said about the arguably more dangerous isotope, Strontium-90, which accumulates in the body's bones. I have been puzzled by this for the last month. Strontium-90 is produced by nuclear plants at about double the volume of Iodine-131. As Iodine-131 levels have been reported as very high around Fukushima, I was sure that Strontium-90 must be present as well. You could say that I had a feeling in my bones! I have been following up the issue with the IAEA and ARPANSA. Today, they got back to me confirming that elevated levels of Strontium-90 have been detected around the Fukushima region.]


Walking around Tokyo you cannot help but notice that a significant number of people are wearing face masks. At a guess, I would say about 10% of people but that is just a guess. I had seen this in other Asian countries and knew that it was because the wearer of the mask:
  1. had a cold and didn't want to spread it;
  2. suffered hay fever and didn't want to breath in pollen;
  3. didn't want to catch other people's germs; or
  4. all of the above.
    Still, there were more masks than I expected. So I asked a few mask wearers why they were wearing them. They said that it was for the above reasons (particularly (2) since it's Spring time in Tokyo) but also because they were concerned about radioactive material in the air from the Fukushima nuclear plant.

I was surprised by this. Despite some sensational reports, I always thought the risk of background radiation was minimal. The background radiation levels increased in Tokyo a few weeks ago before falling away again. Even at their peak, they were still far less than the background radiation levels in many other parts of the world and definitely beneath harmful levels. From my calculations, the background radiation in Tokyo peaked at around 0.95mSV per yeari. In parts of India and Brazil, the background radiation is 35mSV per year while in parts of Iran it is 260mSV per year. The average background radiation worldwide is around 3mSV per yearii. So at its peak, Tokyo's background radiation was less than a third of what the average person is exposed to.


One thing which has been puzzling me is the presence of Strontium-90 in Japan. There has been a lot said about the presence of two other isotopesiii, Iodine-131 and Caesium-137, around the Fukushima region but nothing about Strontium-90. I found this strange because Strontium-90 is in fact more dangerous than both Iodine-131 and Caesium-137. Please bear with me while I explain why.


There are three factors to consider when determining how dangerous a particular isotope is:
  1. its half-life;
  2. where it accumulates in the human body; and
  3. whether we can stop it accumulating in the human body.

Half-life

Iodine-131 has a “half-life” of around 8 days. This means that in 8 days approximately half of a sample of Iodine-131 will convert itself into another element and in the process emit a set amount of radiation. This conversion is called “decay”. This decay process is continuous. So after 16 days, 1/4th of a sample of Iodine-131 will remain and after a further 8 days 1/8th will remain. After a few weeks, a sample of Iodine-131 will have largely disappeared. Caesium-137, on the other hand, has a half-life of around 30 years. 

So what does this mean? In short, a sample of Caesium-137 will remain in the environment emitting radiation for generations while a sample of Iodine-131 will have largely vanished after a few months. The longer an isotope remains in the environment, the greater the probability of it being consumed by a human. But what would happen if you consumed Iodine-131 or Caesium-137? This leads us to the second factor mentioned above: Where does an isotope accumulate in the human body?

Where does an isotope accumulate in the human body?

Different elements accumulate in different parts of the human body. Where they accumulate depends on their chemical properties rather than their nuclear properties (please see the explanation of the difference between chemical and nuclear properties at foot note ii at the end of this post). All of the isotopes of a particular element will accumulate in the same part of the body because they all have the same chemical properties.

Iodine-131 accumulates in the thyroid gland where it can increase the risk of developing thyroid cancer. 

The human body mistakes Caesium-137 for Potassium and absorbs it into the electrolyte system. From there, it spreads throughout the body. It remains in the body for a relatively short time as it is excreted through urine.

Can we stop an isotope accumulating in the human body?

We have all probably read about Iodine tablets which prevent Iodine-131 from accumulating in the thyroid gland.

The thyroid gland can only absorb so much Iodine. If it is “saturated” with a non-radioactive isotope of Iodine, there is simply no room for it to absorb the radioactive Iodine-137. Iodine tablets contain a non-radioactive isotope of Iodine, being Iodine-127. Provided sufficient iodine tablets are taken, the thyroid gland will be saturated with this non-radioactive isotope and there will be no room for Iodine-131. This is particularly helpful for protecting human health because Iodine-131 is very dangerous once it is absorbed into the thyroid gland. Because Iodine-131 decays at a fast rate (remember that it only has a half-life of 8 days) it will emit a large amount of radiation in a short period of time. This high rate of emission can significantly increase your risk of developing thyroid cancer. 

Alternatively, Caesium-137 decays slowly (remember that is has a half life of 30 years) and will be largely excreted before it emits much radiation. That said, there is no equivalent to iodine tablets for Caesium-137.

So what does this all mean for Strontium-90?

It's taken a while but I'm now finally getting to what this all has to do with Strontium-90. If you're still with me, thank you for reading all the background information. I think this information is important to understanding the dangers of Strontium-90.

Strontium-90 has a half-life of around 29 years. So it remains in the environment for generations. What is particularly concerning about Strontium-90 is that the human body mistakes it for calcium and therefore absorbs it into your bones where it will stay increasing your risk of bone cancer and leukaemia. About 20-30% of Strontium-90 which is ingested will be retained in your bones while the remainder will pass out of your bodyiv. As far as I am aware, there is no equivalent to iodine tablets for preventing Strontium-90 accumulating in the human body.

So why have we heard nothing about Strontium-90 levels following the Fukushima nuclear plant incident? It is certainly dangerous enough. In fact, it is regarded as one of the most dangerous isotopes due to the fact it is absorbed into your bones. After the Chernobyl incident, it was one of the most problematic isotopes.

Further, Strontium-90 is very likely to be present in Japan right now. Of all the isotopes produced by a nuclear plant, the percentage concentrations of Iodine-131, Caesium-137 and Strontium-90 are as follows:

  1. Iodine-131 – 2.8%
  2. Caesium-137 – 6.1%
  3. Strontium-90 – 5.8%

As you can see, the amount of Strontium-90 produced is over double that of Iodine-131. So every time you read a report about an elevated level of Iodine-131, just think that the level of Strontium-90 may well be double that. Yet we still hear nothing about Strontium-90.

The silence regarding Strontium-90 has been puzzling me for the last month. I have written to the International Atomic Energy Agency (IAEA) and the Australian Radiation Protection and Nuclear Safety Agency (ARPANSA) to get answers. This morning I received a response from the IAEA (which took some weeks) and a response from ARPANSA.

The IAEA agreed with my concerns and agreed that Strontium-90 has “an important (radiological significance for) impact on human health”. The IAEA also said that the reason there has been no reports on Strontium-90 is that the laboratory techniques required to detect it take several weeks to complete and for that reason Strontium-90 could not be detected … that is until now.

Yes, the IAEA told me that they have detected Strontium-90 levels in Japan. Apparently, they took soil and plant samples from the Fukushima region on March 16. On April 12, the lab results came through and detected Strontium-90 levels up to 32 times the normal level in soil. The IAEA gave no indication as to whether these levels are dangerous. They simply said that they are “up to now” less significant than the levels for Iodine-131 and Caesium-137 which had been detected at much higher levels.

After receiving this information from the IAEA, I noticed that they had released information on their website about the detection of Strontium-90. Some foreign news agencies have also started reporting Strontium-90 today.

As for ARPANSA, they agreed with me that Strontium-90 is a high yield product of nuclear plants. ARPANSA said the reason Strontium-90 has not been detected until now is:
(1) it is less volatile than Caesium-137 and Iodine-131 and for that reason more likely to be retained in the fuel rods of the Fukushima plant rather than released to the environment; and
(2) it is harder to detect than Caesium-137 and Iodine-131.

What does this mean going forward?

As far as I can tell, this means that there is about a one month delay in detecting Strontium-90 levels. Until recently, radioactive water was being dumped into the ocean from the Fukushima plant by the Tokyo Electric Power Company. Given this one month delay time, we may have to sit tight and see what levels of Strontium-90 are actually out there.

So what will I do in the mean time? Simple, live life as usual. If you read my previous post on earthquakes, you probably realised that I'm not a particularly alarmist individual. Ever since arriving in Tokyo I've been drinking the water, drinking the milk and eating whatever I please. If this stuff does turn out to be radioactive, hey, I might gain radioactive superpowers! I've always wanted to be able to see in the dark!

Seriously, although Strontium-90 is a dangerous isotope, I am not presently concerned. I trust the Japanese government. I trust them to impose adequate restrictions on produce from the Fukushima region and generally watch out for me. Still, the whole Strontium-90 issue (which has gone largely ignored until now) intrigues me and I'll keep monitoring it.

Take care

Our Man in Japan

i.        I base this yearly dosage on a radiation level of 0.109 microsieverts per hour which I found in this article: http://www.bloomberg.com/news/2011-04-01/hong-kong-radiation-exceeds-tokyo-even-after-japan-crisis.html



iii.      For those of us who avoided high school and university physics, “isotopes” are different variants of a particular element. For example, the element Uranium has several isotopes, the most famous being Uranium-238, Uranium-235 and Uranium-236. The numbers after the name of the element indicate which isotope we are dealing with.

Isotopes of the same element all have the same chemical properties. Chemical properties include things such boiling temperature, melting temperature and solubility in water. However, different isotopes of the same element have different nuclear properties. Nuclear properties include things such as whether the isotope emits radiation and its half-life. Because different isotopes can have very different nuclear properties, we must be careful to distinguish between different isotopes of the same element when discussing radiation.

iv.     http://www.epa.gov/rpdweb00/radionuclides/strontium.html#properties

Tuesday, 12 April 2011

Earthquakes for the uninitiated



Japan is notorious for earthquakes. It experiences thousands per year. We are all aware of the terrible devastation they can cause after the major quake of 11 March 2011. But what is it like to feel a quake for the first time or be in a country which is so prone to them? Well, here are the first impressions of one of the uninitiated, being me.

Before I moved to Japan, I was incredibly keen to feel a quake. I'd never felt one in my life apart from the time I strapped myself into an earthquake simulator in Nara. It wasn't long until I got my wish. It was all a bit of an anti-climax, though. Before I arrived, I had read of “major aftershocks” of magnitudes 6 and 7 striking Japan and “rocking buildings in Tokyo”. It was only after sitting through a few of these “major aftershocks” that I realised you barely notice them unless you are located in a building several levels up and sitting perfectly still.

The best aftershock I've felt so far was at 8.08 am (Japan Standard Time) on Tuesday, 12 April. I was lying in bed at the time in my 9th storey apartment. My room gently swayed for a few moments, there was a slight creaking sound and a book I had left teetering on the edge of my desk fell to the floor. That was it. I didn't feel any need to rush from the building. In fact, I didn't even feel the need to get out of bed. It was as if a strong gust of wind had rocked the building or a heavy truck had driven by outside.

After a minute or so I summoned up the motivation to get out of bed (it was not a work day) and logged on to the earthquake section of the Japanese Meteorological Agency website to check where the quake had occurred and its magnitude. As it turned out, a magnitude 6.3 quake had occurred about 200 km away from Tokyo at a depth of about 30 km. Its epicentre was at sea. In Tokyo, it was felt as a magnitude 4.0 quake.

I looked out my window. The workman on the scaffolding outside were still working, people were walking to work, cars were driving by … it was business as usual. In fact, all of these people probably wouldn't have even realised that a quake had occurred.

It wasn't long before the first foreign news reports of this quake emerged. Reuters were first to the punch. According to Reuters “another major aftershock [had] rocked eastern Japan, swaying buildings in central Tokyo”. Technically, Reuters were correct. A magnitude 6.3 quake is “major”; eastern Japan had “rocked” to some extent and yes, buildings swayed in Tokyo albeit slightly. However, the impression you would get from reading this report is that people had frozen in abject terror contemplating whether to evacuate from the swaying building or whether the very walls around them would crumble at any moment. Nothing could be further from the truth.

The previous day I had been shopping in IKEA when a magnitude 7.1 quake struck off Eastern Honshu, once again, about 200 km away from Tokyo. According to foreign news agencies, buildings in Tokyo were “rattled” by this “serious” aftershock. If I'd read about this quake back in Australia, I would have imagined items falling off shelves in IKEA and people fleeing the store in terror. A few people from home actually emailed me asking about the quake. So what did happen? Well, nothing actually. Myself and the other shoppers didn't even notice the quake as it was only felt as a magnitude 3.0 in Tokyo, we were on the ground level of IKEA and we were far too enthralled by what piece of chipboard furniture we could buy next.

The two quakes I've mentioned illustrate an important point which is rarely reported by foreign news agencies: The magnitude of the quake at its epicentre is not that important. What matters is the magnitude it is felt at where you live. As the epicentre may be hundreds of kilometres from a densely inhabited area, the magnitude it is felt at by people is often far less than what it was at its epicentre.

A useful indication of how a quake feels is given at the bottom of this post. Based on my limited experience, it seems pretty accurate. As you can see, it is not until a quake reaches magnitude 5.0 that you are likely to realise that a quake has actually occurred. The major earthquake of 11 March 2011 (which was originally reported as magnitude 7.9 by the Japan Meteorological Agency but later upgraded to magnitude 9.0) was apparently felt as a 5 magnitude quake in Tokyo. In other words, you know it is quake but there is very little damage. In the regions closest to the epicentre, it was in the 6s. As we know, it was the tsunami which caused the catastrophic damage more than the quake itself. Take a look at the link at the bottom of this post from the Japanese Meteorological Agency which gives you some useful data on how the 11 March 2011 quake was felt across Japan.


So next time you read about a “major aftershock” in Japan, visit the Japan Meteorological Agency website and check the magnitude it was felt at in Tokyo, Osaka, Nagoya or another heavily populated area. If it was not felt as at least magnitude 5.0, assume that no-one noticed it and if they did, they probably didn't care.

Take care

Our Man in Japan

~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~

The earthquake section of the Japan Meteorological Agency website


The Japan Meteorological Agency report on the earthquake of 11 March 2011


How earthquakes of different magnitudes feel

9.0 and above — Causes complete devastation and large-scale loss of life.
8.0 — Very few buildings stay up. Bridges fall down. Underground pipes burst. Railroad rails bend. Large rocks move. Smaller objects are tossed into the air. Some objects are swallowed up by the earth.
7.0 — It is hard to keep your balance. The ground cracks. Roads shake. Weak buildings fall down. Other buildings are badly damaged.
6.0 — Pictures can fall off walls. Furniture moves. In some buildings, walls may crack.
5.0 — If you are in a car, it may rock. Glasses and dishes may rattle. Windows may break.
4.0 — Buildings shake a little. It feels like a truck is passing by your house.
3.0 — You may notice this quake if you are sitting still, or upstairs in a house. A hanging object, like a model airplane, may swing.
2.0 — Trees sway. Small ponds ripple. Doors swing slowly. But you can't tell that an earthquake is to blame.
1.0 — Earthquakes this small happen below ground. You can't feel them.

(Source: www.scholastic.com)