E.16.0 VITRIFIED HLW TRANSPORT TO THE POTENTIAL GEOLOGIC REPOSITORY
Under the ex situ treatment alternatives the HLW streams would be vitrified or calcined and eventually shipped to a geologic repository assumed to be located 2,140 km (1,330 mi) offsite by a dedicated train of 10 railcars per train. The nonradiological and radiological transportation impacts associated with this activity are evaluated in this section.
E.16.1 NONRADIOLOGICAL TRANSPORTATION IMPACTS
The nonradiololgical impacts are injuries and fatalities resulting from rail accidents. The number of injuries and fatalities were calculated by multiplying the total distance traveled in each zone shown in Table E.16.1.1 by the appropriate unit risk factors shown in Table E.1.3.1. The expected injuries and fatalities resulting from transportation accidents associated with each ex situ stabilization alternative are summarized in Table E.16.1.2.
Table E.16.1.1 Distance Traveled in Population Zones
Table E.16.1.2 Injuries and Fatalities from Rail Transportation Accidents
E.16.2 RADIOLOGICAL CONSEQUENCES
Radiological exposures resulting from routine exposures and accidents while the waste is in transit were analyzed using RADTRAN 4 (Neuhauser-Kanipe 1992).
Travel fractions and population densities for the offsite rail shipments were determined using a computer code (Peterson 1985, Green 1995). For shipments to the geologic repository in the western United States, the following travel fractions were used:
- Rural population zones - The population density was assumed to be 3.4 persons/km2 (8.8 persons/mi2). The fraction of the route spent in rural zones was 0.936 (i.e., nearly 94 percent of the route would be rural);
- Suburban population zone - The population density was assumed to be 406 person/km2 (1,051 persons/mi2). The fraction of the route spent in suburban zones was 0.055; and
- Urban population zone - The population density was assumed to be 1,959 persons/km2 (5,074 persons/mi2). The fraction of the route spent in urban zones was 0.009.
For routine risk, the key variable in the code was the dose rate from the vehicle package. The radioactive shipments in this analysis were assumed to be less than the regulatory maximum dose rate of 10 mrem per hour at 1 m (3.3 FT) (Jacobs 1996).
For accidents, the population doses calculated by RADTRAN 4 were dependent on the accident probability, release quantities, atmospheric dispersion parameters, population distribution parameters, human uptake, and dosimetry models (Jacobs 1996).
The routine exposures were addressed as onsite population LCF risk and offsite population LCF risk. The analysis addressed radiological accident impacts as both integrated population LCF risk (i.e., accident frequencies times consequences integrated over the entire shipping campaign) and urban population LCF risk. The routine and accident LCF risks resulting from transporting vitrified or calcined HLW to a potential geologic repository are presented in Table E.16.2.1 for each of the ex situ treatment alternatives.
A main uncertainty associated with calculating the radiological doses resulting from transporting HLW to a potential geologic repository is the location of the repository. The analysis was based on the assumption that the waste would be transported to Yucca Mountain, should that site be shown to be acceptable and approved as a potential geologic repository. If Yucca Mountain should not be approved, the LCF risks could increase or decrease depending on the distance and population pathways of the alternative site.
Other uncertainties that would impact the LCF risk is the percent of the waste by weight that could be mixed with the glass matrix. To demonstrate these uncertainties, a sample scenario for the Ex Situ Intermediate Separations alternative is presented in Table E.16.2.2. The baseline analysis used in the EIS assumed a 20 weight percent waste loading. A range from the base line from as little as 15 weight percent to as much as 40 weight percent are used in the uncertainty evaluation (Jacobs 1996).
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