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Neumayer-Station III


Neumayer-Station III, also known as Neumayer III after geophysicist Georg von Neumayer, is a German Antarctic research station of the Alfred-Wegener-Institut. It is located on the approximately 200 metres (660 ft) thick Ekstrom Ice Shelf several kilometres south of Neumayer-Station II. The station's assembly kit was transported to its current position early in November 2007. It is moving with the shelf ice at about 200 meters per year towards the open sea.

After almost ten years of work on the project, beginning in October 1999, including conception, environmental impact assessment, planning and construction phases, regular operation of the station began on 20 February 2009. The station replaces the Neumayer-Station II and the Georg-von-Neumayer-Station that preceded it. The expected lifespan of the station is 25 to 30 years and the entire project is estimated to cost 39 million.

The station was constructed 6 m (20 ft) above ground on a temporary two-level platform, and it now rests on 16 hydraulic columns set on a solid snow surface. A garage and further technical equipment are located within a subsurface snow cavern at the front of the station. The moving concrete supporting feet are powered by hydraulic machinery. Through an annual lifting procedure of 80 to 100 cm (31 to 39 in) it is expected to prevent new snow from causing the platform to sink.

The station runs all year round and includes 210 m2 (2,300 sq ft) of laboratory surface, divided into 12 compartments. It has twice the floor area of previous stations. Within the 15 living compartments there is room for 40 occupants to sleep. All inner rooms of the platform are built as self-contained units, some of which have aligned connecting passages, depending on their size. The compartmentalized interior of the station is enclosed in sheet metal with an interior polyurethane rigid foam insulation. The green metal girders in the “structure section” image indicate snow level; they are not part of the final structure. All items below the girders will later be embedded in the Antarctic snow.


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