A deep geological repository, (DGR), is a radioactive waste repository excavated deep within a stable geologic environment (typically below 300 m or 1000 feet). Deep geological repository may be used as the final disposal of untreated spent nuclear fuel or vitrified high-level waste arising from fuel reprocessing. Deep disposal in a mined repository is now the preferred option for HLW final disposal in most countries. The Waste Isolation Pilot Plant (WIPP) deep geological waste repository is in operation in the US for the disposal of transuranic waste – long-lived ILW from military sources, contaminated with plutonium.
Deep geological repository entails a combination of waste form, waste package, engineered seals and geology that is suited to provide a high level of long-term isolation and containment without future maintenance. Crystalline rock (granite, welded tuff and basalt), salt and clay are the most suitable formations for geological disposal. For example, the once-through cycle considers the spent nuclear fuel to be high-level waste (HLW) and, consequently, it is directly disposed of in a storage facility without being put through to any chemical processes, where it will be safely stored for millions of years until its radiotoxicity reaches natural uranium levels or another safe reference level.
This strategy is favored by several countries: the United States, Canada, Sweden, Finland, Spain and South Africa. Some countries, notably Finland, Sweden and Canada, have designed repositories to permit future recovery of the material should the need arise, while others plan for permanent sequestration in a geological repository like the Yucca Mountain nuclear waste repository in the United States.
Natural precedents for geological disposal – Oklo Reactor
It must be noted, nature has already proven that geological isolation of radioactive material is possible through several natural examples (or ‘analogues’). One of the most important case is the natural nuclear reactor in Oklo. The world’s first nuclear reactor operated about two billion years ago (at that time the concentration of U-235 in all natural uranium was about 3%). The natural nuclear reactor formed at Oklo in Gabon, Africa, when a uranium-rich mineral deposit became flooded with groundwater that acted as a neutron moderator, and a nuclear chain reaction started. These fission reactions were sustained for hundreds of thousands of years, until a chain reaction could no longer be supported. This was confirmed by existence of isotopes of the fission-product gas xenon and by different ratio of U235/U238 (enrichment of natural uranium).
During this spontaneous fission, all the radionuclides found in HLW were also produced, including over 5 tonnes of fission products and 1.5 tonnes of plutonium, all of which remained at the site and eventually decayed into non-radioactive elements. The study of such natural phenomena is important for any assessment of geologic repositories, and is the subject of several international research projects.