For many years now, scientists and
biologists tried to grasp the effect of the aftermath of the 1986
nuclear catastrophe on biological wildlife. One of the most
contaminated areas following the event is a strip of 10 to 15
km²
of Scots pine wood (lat. pinus silvestris) The most affected zone is
approximately 2 km away from the power station:
“(the) Zone
suffered a complete loss of conifers with partial damage to hardwoods
(the so-called "Red forest"). Scholars estimate that the
level of absorbed doses of external gamma radiation exposure in
1986–1987 was 8000–10000, with the maximum extent of the dose was
500 mR/h and more. The total area of this zone is approximately 400
hectares. In this zone, the pine tree trunks completely died and pine
needles exhibited a brick color. The entire forest was virtually
"burned down"—having accumulated a significant amount of
radioactive emissions. Heavy radioactive contamination of the dead
trees led to their burial. On the territory of the "Red Forest",
immediate actions were implemented to restore the forests” (1)
Inside
of that zone heavy mutations were imminent: Pine trees looked more
like bushes then trees, gigantism and also deformity in the branches
were very common. The less affected zones don't show as many
deformities, nevertheless, the trees suck up radionucleides and
especially wildfires are an important risk for releasing more
radioactivity trough smoke clouds that could easily affect all of
Europe.
In
1992, a large wildfire burnt down undetected and released massive
amounts of radioactivity into the atmosphere. To this date, nothing
is known about the consequences of the great fire of 1992. Sergiy
Zibtsev, a professor from the Forestry Institute at the Kiev
University of Life Sciences is one of the few international experts
on the issue. Recently dispatched to Japan to ascertain the risks of
the Fukushima Daiich'i Nuclear Meltdowns to the wildlife in the
region. Zibtsev has worked for almost 20 years in the concerned
Chernobyl region, trying to figure out the risks and development of
forest life. He also coordinates with the 100 firefighters
permanently stationed in the area to spot wildfires:
Firefighters in Chernobyl have one of the least enviable jobs in the world. They spend all day up rusty Soviet watchtowers, which sway in the wind like tin-box metronomes, and act as conductors to the huge lightning storms which swing across the land most afternoons in summer, often sparking fires. When they spot a wildfire, the firefighters triangulate its location by radio. Teams jump aboard big, red, Soviet fire trucks, and lumber along cracked, overgrown roads to the source of the blaze...They believe they know when they are fighting a radioactive fire - they experience a tingling, metallic sensation in their skin - but they do not fully understand the serious dangers of being exposed to superheated radioactive particles... Sergiy (Zbitsev) says more big wildfires in Chernobyl like the one in 1992 would be catastrophic for Ukraine's image, and potentially devastating for farmland right across Europe. (2)
During
a recent visit near the exclusion zone and the heavily contaminated
areas of Southern Belarus, I wanted to have a closer look on trees
and how they were affected by the 1986 Chernobyl catastrophe. I had
read in several studies, especially in Nesterenko & Yablokov's
“Consequences of Chernobyl on Environment (N.Y Academy of Sciences
2008) that even in trees far away from the powerplant in Ukraine,
Belarus and Russia, the affect of radiation can be seen directly with
a different color of the year ring in the tree trunk, showing that
the tree's growth rate and biological circle were heavily affected bt
the incident. Incidentally, trees outside of the heavily contaminated
areas of Southern Belarus show the same characteristics as the trees
that were studied by Nesterenko and Yablokov: The year 1986 is in
most trees visible and from that period their growth and the color of
their stem changes dramatically. On the following pictures this can
be observed very well:
Picture clearly showing the growth change and radiation marks on the year rings. Picture taken in Southern Belarus, Gomel Region 2012 CC SA 2.0 Share & give credit to blog & name
Sources:
James
D. Brownridge and Noel K. Yeh
Department
of Physics, Applied Physics and Astronomy
State
University of New York at Binghamton Binghamton,
NY
13902, U.S.A.
http://www.bbc.co.uk/news/magazine-18721292 (2)
thank you for sharing Phil!
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