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4.0
Solids; Nonmetallic or Composite Solids
4.3.2.3
V en tin g of P ressurized G ases O ver S olid s
No significant airborne release is postulated. The potential releases for loose surface
contamination on the solid are covered in Chapter 5.
4.3.3
F ree-F all S p ill an d I mp action S tres s
Brittle materials (e.g. glass, aggregate such as mechanically-compacted UO2, concrete,
limestone) can be fragmented when impacted or crushed. Jardine et al. (1982) performed
experiments to measure the fraction and size distribution generated by the impact of various
materials resting on a unyielding surface. Figure 4-12 reproduced from the reference
documents illustrates that the size distribution of UO2 pellets to an impact energy density of
1.2 J/cm3 is linear. Note that both the sieve and Coulter Counter data shown are physical
the average grain size shown corresponds to a particle ~ 29 m AED. The degree of
fragmentation and the size distribution are a function of the material, the strength/age of the
material, and the energy input per volume (Mecham et al., October 1981). The fraction in
the size range 10 m AED and less is relatively uniform as shown in Figure 4-13 reproduced
from the reference document and was empirically correlated with the energy input (J/cu-cm)
in subsection 5.1.3, Appendix F in Vol. 4 of SAND (September 1987) as:
ARF X RF = (A)(P)(g)(h)
(4-1)
where:
ARF X RF = (Airborne Release Fraction)(Respirable Fraction)
= empirical correlation, 2E-11 cm3 per g-cm2/s2
A
= specimen density, g/cm3
P
g
h
= fall height, cm.
Use of this correlation to estimate the ARF x RF value is considered very conservative, and
may be excessively so if large debris from substantial heights is considered.
4.3.4
A erod yn am ic E n train m en t an d R esus pen sion
No significant airborne release is postulated. Potential releases for loose surface
contamination on metal are covered in Chapter 5.
Page 4-52
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