Location
It neighbors the Nevada Test and Training Range and the Nevada Test Site. The Nevada Test Site was home to 904 atomic bomb tests between 1945 and 1992.[2] Although the Department of Energy is planning to consider other options to Yucca Mountain, it remains the only legal site in the United States for development as a deep geologic repository. The Yucca Mountain Development Act was passed by the Congress and signed by President Bush in 2002 making development of Yucca Mountain the Law. Until Congress amends or changes the law, the Secretary of Energy is charged with pursuing development of Yucca Mountain as the Nation's geologic repository.[3]
In 2010 the future of the proposed waste site was threatened by government action which could leave the United States without any long term solution for its nuclear waste, currently stored on-site at various facilities around the country.[4]
[edit] Geology
The formation that makes up Yucca Mountain was created by several large eruptions from a caldera volcano and is composed of alternating layers of ignimbrite (welded tuff), non-welded tuff, and semi-welded tuff. Tuff has special physical, chemical and thermal characteristics[vague] that some experts[who?] believe make it a suitable material to entomb radioactive waste for the hundreds of thousands of years required for the waste to become safe through radioactive decay.
The volcanic units have been tilted along fault lines, thus forming the current ridge line called Yucca Mountain. In addition to these faults, Yucca Mountain is criss-crossed by fractures, many of which formed when the volcanic units cooled. While the fractures are usually confined to individual layers of tuff, the faults extend from the planned storage area all the way to the water table 600 to 1,500 ft (180 to 460 m) below the surface.[5]
The volcanic tuff at Yucca Mountain is appreciably fractured and movement of water through an aquifer below the waste repository is primarily through fractures.[6] Future water transport from the surface to waste containers is likely to be dominated by fractures. There is evidence that surface water has been transported down through the 700 ft (210 m) of overburden to the exploratory tunnel at Yucca Mountain in less than 50 years.[7][8]
Some site opponents assert that, after the predicted containment failure of the waste containers tens of thousands of years from now, these cracks may provide a route for movement of radioactive waste that dissolves in the water flowing downward from the desert surface.[9]
Officials state that the waste containers will be stored in such a way as to minimize or even nearly eliminate this possibility. Even without faults and fractures, tuff is slightly permeable to water, but due to the depth of the water table it is estimated that by the time the waste enters the water supply it will be safe.[9]
Map of the Location of the Mountain
The area around Yucca Mountain received much more rain in the geologic past and the water table was consequently much higher than it is today, though well below the level of the repository. Critics contend that future climate cannot be predicted to 10,000 years so it is optimistic to assume that the area will always be as arid as it is today. Most geologists who have worked at the site still maintain that the geology will adequately slow the rate of waste seepage to protect water supplies even if the local climate becomes much wetter.[9]