6 THE SHORTER-TERM BIOLOGICAL HAZARDS OF A FALLOUT FIELD 1 hererhe ot Held tnvte isl? METEOROLOGY-~FALLOUT AND WEATHERING | | | with time and location through a very large 7 sizes as far as radioactivity is concerned are easily moved by moderate winds. Smaller particles may be eroded by a process known as saltation, in which the impact of larger, erodible, particles jars them loose and allows the wind range. The movement of various particles by the action of wind is shown in Figure 6 (from a paper by G. R. Hilst of the Hanford Atomic Products Operation). The table shows that to carry them away. the particles most easily moved by wind are those in the range of 50-800 microns in diameter. A wind of only about 10 knots (measured at the meter level) is sufficient to pick up particles in the 60 to 130-mieron level (A. Sund- The particles whictt are lifted by the wind will, of course, settle elsewhere. However, in general, (he importance of this dispersal process is the diluting of the higher radietion intensities. Furthermore, particles initially or sub- so it is apparent that. the important particle most apt to remain. borg, Geagrafiska Annaler NRXVIL (1955) ). eneft sequently settling inte crevices will be the ones Radiation from these 7 so deed be ot H4I2 7 'W.8. HAND COMPUTATION (WINDS PREDICATED AT 2) so nu mp Ye OH & ellen STATUTE MILES. Frours 2.—-Sample Fallout Computation— Predicted Winds. WEATHERING Tae radioactive particles deposited on the ground may be transported or modified in their into the ground—carrying some particles with it. Once the air space in the soil is filled with water, most of the additional rainfall will run off along the surface andinto streams—-carrying along more of the radioactive particles. To this must be addedthe action of raindrops effect on man by the action of wind and precipitation. Three types of weathering can be imagined: 1, Particles can be washed away. 2. Particles can be blown away. 3. Particles can be covered. In the first case, particles embedded in rain- in dislodging the particles by their striking force. With light winds or on level ground this the initial part of even heavyrain tends to soak tremendous variability in rainfall can differ water or snow melt can be washed into the ground or carried away by runoff. Light rainor WB. HAND COMPUTATION {SHOT- TIME WINDS) is unimportantbutin strong winds or on slopes with as little as 10 percent grade, there will be significant transport, This qualitative picture combined with the o © 2 © © © Swasi STATUTE MILES Fioure 3.—Sample Fallout Computation—Observed Winds at Test Site.