Evacuation Policy Versus Radiation Level Measurements In Japan
Sunday, March 18th, 2012Here are some of the latest measurements of radiation levels in the Fukushima region of Japan, these were made just last month.

There is something very striking about this image even at first glance. Notice that the no-entry zone has absolutely no correspondence whatsoever to radiation levels. It’s simply a circle drawn around the nuclear plant. Much of the area has quite low radiation levels and some of the area outside the exclusion zone has higher radiation levels than the area within it. Since there’s now no real danger of the reactors being further damaged or experiencing uncontrolled discharges, there’s absolutely no reason to enforce a no-entry zone based on such a blind method of drawing the map. If a no-entry zone is to exist at all (which it really, at this point, does not need to)
Actual Doses experienced:
Few areas exceed 20 uSv per hour by very much. The red area signifies areas with higher than this level, but most of this area is only slightly above 20 uSv/hr. Areas with 20 uSv/hr or more exist in a relatively narrow strip running northwest from the area of the nuclear plant.
A person lives in an area where the external radiation dose rate is 20 uSv/hr. Of course, this is really only outdoors and inside there will be less contamination, but for the sake of argument, lets assume the worst: They get 20 uSv/hr and they stay in that are all the time. There are 8760 hours in a year, so if they spend all their time outdoors in the 20 uSv/hr area, they receive 175,200 uSv per year or about 175 mSv per year.
This is still a bit unreasonable for what a person would actually be exposed to because it assumes they are always outdoors and standing over ground that has not been in any way cleaned of contamination. Indoors, the level will be a lot lower. If they travel outside the area of highest radiation, their dose is also reduced. As time goes on, both radioactive decay and natural weathering and erosion will reduce levels further. Therefore, after a year in such an area, it’s more reasonable to expect a total exposure of something like 100-150 mSv and maybe quite a bit less.
Most of the no-entry zone is far bellow this. The yellow areas would produce only about half the dose of the highest regions and the areas shaded green would result in an annual dose of only about 10-30 mSv her year. That’s hardly a lot of radiation.
How much radiation a person is exposed to in a year from background sources varies greatly depending on things like location, diet, travel and things like whether they happen to cook with natural gas, live in a granite structure or have radon seeping into their home’s foundation. About 3 mSv is a normal average for those living at sea level in much of the world. Of course, it’s quite common for it to be much higher than this. Areas with background radiation in excess of 10 mSv per year are quite common. A few areas have much higher. In the Guarpari region of Brazil, background levels can exceed 175 mSv per year due to local deposits of uranium and thorium. Residents of Kerala India experience doses of over 70 mSv per year. Ramsir Iran is famous for having some of the highest levels in the world at over 260 mSv per year. Locations across Africa and Australia may produce levels above 40 mSv per year.
Studies have been done of the populations of these areas and no ill effects have been documented as a result of the high radiation exposure. Of course, the expected radiation exposure from living in such an area for an extended period of time would be much higher than for those in the Fukushima area. Since the radioactivity in the Fukushima region is mostly limited to the surface and includes many relatively short-lived radioisotopes, it will diminish significantly in the years to come. Natural sources, on the other hand, are constantly replenished. So a person who lives in an area with increased radiation levels as a result of the Fukushima incident will not experience the same dose next year as they will this year. It will be less.
And no, there have been no calls that high background areas of the world be evacuated and declared off limits.

Despite these dangers, radium-226 was once far more valuable than gold. For the first half of the 20th century, radium and its decay products were the most widely used radioisotope source for any purpose that required radioactive materials. It was used for cancer treatment, in the form of radium needles, external sources and devices that collected radon for use in irradiating tissue. Radium was commonly used in any circumstance where calibration sources were required, with many earth geiger counters coming with a radium-based test source. It was used in ion and moisture gauges, cold cathode vacuum tubes and combined with beryllium to produce small neutron sources. Radium was well known for its use in radiolumonescent paints. The paint was commonly used for clock and watch faces, allowing them to glow brightly without first having to be exposed to light. Larger concentrations were used for aircraft instrument dials, illuminated markers and
Radium-226 exists in small concentrations in uranium ore. To recover a single gram of the material, several tons of uranium ore must be processed. Still, because the material had so many uses and was so valuable, large operations existed all over the world to produce it.
Remote areas of Alaska are off the wider electrical grid and are far from natural gas pipelines or railways to deliver coal. Heat may be provided, at least in part, by wood burning stoves that can use local fuel, although wood supplies may also be limited. However, by far the most important source of energy is oil. Diesel oil is the only way for these communities to generate electricity and provides most of the heat. Petroleum also powers local transportation and powers the vital systems of the communities, either directly or by generating electricity. Communications, drinking water wells, sanitary systems, heat and lighting all require energy provided by oil.
The choice of isotope for space missions has always been, and continues to be
There are other isotopes that can also be used to provide power for RTG’s, but none are as desirable as Pu-238. 
There’s only one problem with these amazing little glowing key chains: nobody in the US sells them, at least not directly. Technically, these are not approved for sale or ownership in the United States, although I’ve never heard of anyone getting in trouble for owning one. Many people do own them and talk about them openly online and elsewhere. It might just be one of those things that hasn’t shown up on the radar of a bureaucrat who was asinine enough to bother to do something about it.
Fission was recognized as a potential energy source after the possibility of a fission chain reaction was realized. A chain reaction occurs when neutrons produced by nuclear fission strike other fissile nuclei, releasing more energy in a self-sustaining reaction.
All this changed in 1972, when an unusual discrepancy in the concentration of uranium-235 from a mine in Gabon Africa was detected










