Groningen gas field
|Operator||Nederlandse Aardolie Maatschappij BV|
|Start of development||1959|
|Start of production||1963|
|Current production of gas||93×106 m3/d|
3.3×109 cu ft/d
|Estimated gas in place||2.8×1012 m3|
100×1012 cu ft
The Groningen gas field is a giant natural gas field located near Slochteren in Groningen province in the northeastern part of the Netherlands. Discovered in 1959, it is the largest natural gas field in Europe and the tenth-largest in the world.
After two previous unsuccessful wells were commissioned to search for oil and gas, on 22 July 1959, the Slochteren 1 well, drilling to a depth of 3,000 metres (9,800 ft), discovered the huge 2.8 trillion cubic meters (100 trillion cubic feet) gas field in the porous Rotliegend sandstone formation, which is 130 metres (430 ft) to 140 metres (460 ft) thick and 45 kilometres (28 mi) long from north to south by 25 kilometres (16 mi) long from east to west. The field started production in 1963 and produced around 100 billion cubic meters (3.57 trillion cubic feet) per year in the first decade of production but gradually the annual production fell to around 35 billion cubic meters (1.25 trillion cubic feet) per year. As of 2009[update] the Groningen gas field has produced around 1,700 billion cubic meters (60.7 trillion cubic feet) which represents 60% of the total reserves of the field but the remaining 1,100 billion cubic meters (39.3 trillion cubic feet) are expected to last for another 50 years.
The Groningen gas field is operated by the Nederlandse Aardolie Maatschappij BV (NAM), a joint venture between Royal Dutch Shell and ExxonMobil with each company owning a 50% share. The field accounts for 50% of the natural gas production in the Netherlands, the other 50% being supplied by around 300 smaller gas fields, most of them located offshore in the North Sea.
After protests in Groningen because of the increase in induced earthquakes, whose event count shows an exponential growth in time,  the Dutch government decided on 17 January 2014 to cut output from the gas field and pay those affected by the earthquake a compensation worth 1.2 billion Euro, spread over a period of 5 years. The ministry said production would be cut in 2014 and 2015 to 42.5 bcm (billion cubic meters) and in 2016 to 40 bcm.
The State Supervision of Mines has brought forward that the production level should be cut back to 30 bcm to avoid the more severe quakes. Although it is technically possible to reduce Groningen's output to this level and still meet domestic demand, the ministry keeps production high (currently[when?] 39.4 bcm per year). Groningen officials are not satisfied with the measures. As of January 2015, no houses have been reinforced, nothing has been done about many seriously damaged buildings, and the risk of severe quakes, possibly resulting in collapsed buildings, injuries and death, is still too high. In June 2016, the Netherlands' National Mines Inspectorate advised the Dutch Government to reduce production even further to 24 bcm per year. On 23 September 2016 Dutch Prime Minister Mark Rutte confirmed that gas extraction from the northern Groningen gas field will be held at 24 bcm per year for the coming five years.
In September 2019, the Dutch government announced a further accelleration of the decommissioning of the field, stopping all regular production in 2022
The Groningen field lies within the Southern Permian Basin, which extends from the eastern coast of England to Poland. Within this area large volumes of gas have been discovered, mainly reservoired in the Rotliegend sandstone, with producing fields in England, the Netherlands, Germany, Denmark and Poland.
The main reservoir in the Groningen field is the Cisuralian (Lower Permian), Rotliegend Slochteren sandstone. The Rotliegend reservoir at Groningen is mainly an aeolian sand with local development of fluvial wadi sands.
The main source rock for the gas at Groningen are coals and carbonaceous shales within the Westphalian coal measures sequence that lies unconformably beneath the Rotliegend. These sources are dominated by type III kerogen.
The Groningen structure is a NNW-SSE trending intrabasinal high formed by normal faulting during the Mesozoic, particularly during the Late Jurassic to early Cretaceous. It has an overall horst geometry, lying between the Ems Graben to the east and the Lauwerszee Trough to the west.
The Rotliegend is covered by the Late Permian Zechstein evaporite sequence, consisting of carbonate, anhydrite and halite, which provides an effective seal to the gas accumulations within the underlying sandstone.
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