KBS-3

KBS-3 (an abbreviation of kärnbränslesäkerhet, nuclear fuel safety) is a technology for disposal of high-level radioactive waste developed in Sweden by Svensk Kärnbränslehantering AB (SKB) by appointment from Statens Strålskyddsinstitut (the government's radiation protection agency). The technology was developed by studying different natural storage facilities such as the natural reactor in Oklo, Gabon, and the uranium mine in Cigar Lake, Canada. The general theory is that radioactive rock in these sites has been present for thousands of years, and has not affected the health and well-being of human populations. KBS-3 is also to be used in Finland at the Onkalo spent nuclear fuel repository, being built by Posiva.

The disposal method consists of the following steps:

If the holes into the rock from the cave are drilled vertically, the method is called KBS-3V and if they are drilled horizontally it is called KBS-3H. The only method considered so far is KBS-3V.

The overall theory is that radioactive rock has always been present in the earth, and it is generally harmless to human populations. Further, Cigar Lake and Oklo have proven that actinides do not easily migrate via ground water or other means. Spent fuel consists of radioactive ceramic, cooled until its short-half-life radioactives have decayed, so its heat-production is negligible. When initially made, the ceramic fuel is also wrapped in sealed tubes of corrosion-resistant zirconium alloy. Therefore, spent fuel is not water-soluble in any conventional sense, and is mechanically sturdy. The other elements: crystalline bedrock, corrosion-resistant copper cylinders, etc. have been scientifically proven to reduce the exposure to ground water, and the rate at which it can penetrate to the fuel and dissolve it. Further, if correctly sited, any leakage will enter seawater, providing a safe dilution to decay. Geological stability against earthquakes and other extreme events can be further reduced by careful site-selection. These safety factors multiply, extending the containment lifetime until most radioactive elements in the fuel have decayed, and only the longest-lived, least-radioactive isotopes remain. At this point, the contents of the repository are at least as safe as natural deposits of uranium. The process has been extensively studied and depends on well-understood chemistry and geology.

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