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Kriku kirjutas:

sass2401 kirjutas:Ja pärast lähevad sinna siiverteid koguma? Hakkavad kohe helendama või punetama.

Lähevad põllu pealt ringi, linnast tule alla ei jää. Kõlbas Punasesse metsa kaevikuid kaevata, kõlbab selline sõdimisviis ka. Territooriumit kasima saadetakse pärast filtratsioonilaagrite elanikud.

Kohalikest tahetakse nii või teisiti lahti saada.

sass2401 kirjutas:Huvitaks siiski jääkradiatsiooni info ütleme, pärast 10 ktn pommi viskamist.

A nuclear explosion produces a complex mix of more than 300 different isotopes of dozens of elements, with half-lifes from fractions of a second to millions of years. The total radioactivity of the fission products is extremely large at first, but it falls off at a fairly rapid rate as a result of radioactive decay. Seven hours after a nuclear explosion, residual radioactivity will have decreased to about 10 percent of its amount at 1 hour, and after another 48 hours it will have decreased to 1 percent. (The rule of thumb is that for every sevenfold increase in time after the explosion, the radiation dose rate decreases by a factor of 10.)

319. Residual Radiation.

The residual radiation hazard from a nuclear explosion is in the form of radioactive fallout and neutron-induced activity. Residual ionizing radiation arises from:

a. Fission Products. These are intermediate weight isotopes which are formed when a heavy uranium or plutonium nucleus is split in a fission reaction. There are over 300 different fission products that may result from a fission reaction. Many of these are radioactive with widely differing half-lives. Some are very short, i.e., fractions of a second, while a few are long enough that the materials can be a hazard for months or years. Their principal mode of decay is by the emission of beta and gamma radiation. Approximately 60 grams of fission products are formed per kiloton of yield. The estimated activity of this quantity of fission products 1 minute after detonation is equal to that of 1.1 x 1021 Bq (30 million kilograms of radium) in equilibrium with its decay products.

b. Unfissioned Nuclear Material. Nuclear weapons are relatively inefficient in their use of fissionable material, and much of the uranium and plutonium is dispersed by the explosion without undergoing fission. Such unfissioned nuclear material decays by the emission of alpha particles and is of relatively minor importance.

c. Neutron-Induced Activity. If atomic nuclei capture neutrons when exposed to a flux of neutron radiation, they will, as a rule, become radioactive (neutron-induced activity) and then decay by emission of beta and gamma radiation over an extended period of time. Neutrons emitted as part of the initial nuclear radiation will cause activation of the weapon residues. In addition, atoms of environmental material, such as soil, air, and water, may be activated, depending on their composition and distance from the burst. For example, a small area around ground zero may become hazardous as a result of exposure of the minerals in the soil to initial neutron radiation. This is due principally to neutron capture by sodium (Na), manganese, aluminum, and silicon in the soil. This is a negligible hazard because of the limited area involved.

Kõigepealt peab Venemaa saatma käsu - lasta tuumarakett - see toimib raadio teel kosmosest või merelähedaste saatjatega.

Bonnie kirjutas: ja ka kodeeringu lakkamine ise võib tähendada lahinguolukorda, kus allveelaeva kapten võtab luku tagant ümbriku ja loeb sealt mida kodeeritud signaali lakkamine x ajaks tähendab. Eeldatavasti kui NSVL-t oleks sattunud tuumarünnaku alla ja signaalid katkevad ning x ajal taastu (tehniline rike)
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Bonnie kirjutas:Juba nõukogude ajast olid neil mingid pikalaine saatjad mis saadavad 24/7 kodeeritud signaali välja. Need pidavat tänini töötama