Hidden Reserves

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- Jurassic argillaceous rock on the coast of England is similar in build as the underground shale gas systems. Photo: TU Clausthal
A new term is spreading amongst Europe’s energy experts: “Shale gas” could be translated “Schiefergas” in German. This denotes a natural gas located in dense, ancient clay formations yet which cannot be extracted with the usual methods. These long since known gas deposits can be economically exploited only since a few years ago. Their exploitation makes sense also Jura ssic arg illaceous rock on the coast of England is similar in build as the undergr ound shale ga s systems. Photo: TU Clausthal because the transition to sustainable sources of energy will require many years more, during which fossil fuels will continue to be used. In such a case, natural gas is the first choice as it yields the same net energy as coal yet with 40 to 50 percent less of the climate gas carbondioxide.
In the US today, nearly every tenth cubic metre of natural gas comes from such rock formations. Here, Europe still is far behind. Only in 2009, two research projects started: Professor Dr. Brian Horsfield of the GFZ heads „Gas Shales in Europe“ (GASH) and GFZ scientist Dr. Hans-Martin Schulz coordinates the core topic „Shale Gas“ within the context of the compound project GeoEnergy. “In these projects, we investigate how shale gas is formed and what typical deposits in Europe look like” explains Hans-Martin Schulz. Presumably, there is a whole series of such deposits in England, Poland and Sweden, the Vienna Basin as well as in Lower Saxony and in the south of Germany.
The reserves then are accessed by a vertical bore hole. Once the boring cutter reaches the natural gas layer, it turns horizontal and possibly bores horizontally for some kilometres more. Then water is pressed into the layer, opening up fissures in the rock, which are permanently stabilised by small quartz spheres within the solution. The natural gas then can escape from these fissures.










