Scientists probe the Pacific to determine how far the damage from one of the largest nuclear meltdowns in history extends.
Between 2012 and 2014, Yoshida et al. analyzed the abundance of two cesium (Cs) isotopes—134Cs and 137Cs—at various locations throughout the North Pacific Ocean. These radioactive elements were released in relatively equal abundance during the Fukushima disaster, but 137Cs already existed in low levels in the Pacific Ocean as a leftover product of nuclear weapons testing over the years. Any discovery of 134Cs, however, could be directly attributed to the Fukushima disaster.
At the end of 2012, samples of surface water taken along the 30°N parallel—which runs approximately from San Diego to southern Japan—showed 134Cs had migrated as far east as 174.3°W longitude. (For reference, Hawaii is located at 157.8°W.) Similar measurements taken in 2013 show that the cesium appeared to be traveling about 5 centimeters per second: It had migrated to 160.6°W—approximately 1580 kilometers closer to North America.
The team also took depth measurements to track how deep the cesium was penetrating the water. Again, no 134Cs was found farther east than 160.6°W, but closer to Japan the radioactive isotopes were observed as far down as 600 meters—a surprising finding that showed the rapid and deep progression only 2 years after the accident. Physical processes responsible for the deep signal could be explained by the distinct water mass formation or deep wintertime mixing; however, it has yet to be clarified.
Although the full environmental impact of the Fukushima disaster may not be fully understood for years to come, the 134Cs present in the oceans won’t stay there for long; its half-life is only about 2 years, meaning that since the 2012 measurements, more than half of the isotopes have decayed. However, the radioactive 137Cs released from the plant won’t see a similar 50% reduction until around the year 2040.