|Foreword| |Route map| |Atomic bomb|
|Damge| |Effects of blast| |Effects
of fire| |Immediate effects of radiation| |Delayed effects of radiation| |Statistics| |Sociological destruction| |
Effects of Thermal Radiation
(1) Human damage
The fireball that developed in the air simultaneously with the
detonation attained a maximum temperature of 300,000 degrees Centigrade at the instant of
the explosion, a diameter of about 180 meters and a surface temperature of about 1,700
degrees; 1/100 of a second later, a surface temperature of about 7,000 degrees - ... -
rising again; 0.3 second later, a maximum diameter of about
280 meters and surface temperature of about 5,000 degrces; 1 second later, a surface
temperature of 1,700 degrees again; 3 seconds later, and thereafter, it gradually dropped.
Ninety-nine percent of the thermal radiation from the fireball had strong effect on the
ground only during the time from 1/100 to about 3 seconds after the detonation. The
thermal radiation of ultraviolet rays caused fire, and loss of eyesight and heat burns on
the human body. Thermal radiation heat burns of the exposed human skin were observed to
about 3.5 kilometers from the hypocenter.
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The temperature of the heat rays in the hypocenter is estimated to have been from 3,000 degrees Centigrade to 4,000 degrees Centigrade, which may be compared with the melting point of an iron bar, 1,5360 C. Anythi~g near the hypocenter, both human and other materials was supposedly tumed to ashes. Persons located without shielding within about 1.2 kilometers from the hypocenter sustained fatal heat burns and 20% to 30% deaths were due to this injury.
(2) Damage done to materials
The uniqueness of thermal radiation effects on materials was vividly shown in such
phenomena as spontaneous combustion, charring, and the imprinting of shadows of things.
Since there was spontaneous combustion on clothes of persons outdoors or laundry drying in
the sun about 1.8-2 kilometeis from the hypocenter, the vast range of spontaneous
combustion due to the direct thermal radiation may be easily conceived.
Railroad ties and wooden fences along railroads even 2.1 kilometers from
the hypocenter spontaneously ignited and burnt. The surface of granite stones within one
kilometer of the hypocenter melted in the heat. Glass-like bubbles formed on the surface
of roof-tiles within 600 meters of the hypocenter.
There was also spontaneous combustion on plants and trees. Many old and huge trees were
left with their insides burnt.
Shadow of valve imprinted on a gas tank: Coal tar on the surface of the tank absorbed enough heat to make a clear shadow on the tank even though there was some distance between the valve and the side of the tank. The tar completely melted away. (2,000 meters from the hypocenter. Photographed by Shunkichi Kikuchi.)