Makó Gas Field
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Makó Gas Field
The Makó gas field (Makó Trough of the Pannonian Basin Gas Accumulation) is a large natural gas field next to Makó, in southeastern Hungary. Formation The worldwide interest in unconventional hydrocarbon accumulations has increased continuously a growing demand for natural gas, and equally important, because of the availability of a growing range of advanced oilfield technologies. For these reasons the thermally mature, shaly sediments of the deep Makó Trough of the Pannonian Basin have become a new target for exploration companies looking for unconventional natural gas resources.http://epa.niif.hu/01600/01635/00335/pdf/EPA01635_foldtani_kozlony_2011_141_1_023-040.pdf Research Since the 1960s it was well known that a large gas field existed next to Makó. The disadvantages are the depth of the gas deposit at about as well as the very high pressures and temperatures, the large thermal increase with depth in Hungary about per degree Celsius compared to a world-average ...
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Hungary
Hungary ( hu, Magyarország ) is a landlocked country in Central Europe. Spanning of the Carpathian Basin, it is bordered by Slovakia to the north, Ukraine to the northeast, Romania to the east and southeast, Serbia to the south, Croatia and Slovenia to the southwest, and Austria to the west. Hungary has a population of nearly 9 million, mostly ethnic Hungarians and a significant Romani minority. Hungarian, the official language, is the world's most widely spoken Uralic language and among the few non- Indo-European languages widely spoken in Europe. Budapest is the country's capital and largest city; other major urban areas include Debrecen, Szeged, Miskolc, Pécs, and Győr. The territory of present-day Hungary has for centuries been a crossroads for various peoples, including Celts, Romans, Germanic tribes, Huns, West Slavs and the Avars. The foundation of the Hungarian state was established in the late 9th century AD with the conquest of the Carpat ...
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Natural Gas Field
A petroleum reservoir or oil and gas reservoir is a subsurface accumulation of hydrocarbons contained in porous or fractured rock formations. Such reservoirs form when kerogen (ancient plant matter) is created in surrounding rock by the presence of high heat and pressure in the Earth's crust. Petroleum reservoirs are broadly classified as ''conventional'' and '' unconventional'' reservoirs. In conventional reservoirs, the naturally occurring hydrocarbons, such as crude oil or natural gas, are trapped by overlying rock formations with lower permeability, while in unconventional reservoirs, the rocks have high porosity and low permeability, which keeps the hydrocarbons trapped in place, therefore not requiring a cap rock. Reservoirs are found using hydrocarbon exploration methods. Oil field An oil field is an area of accumulation of liquid oil underground in multiple (potentially linked) reservoirs, trapped as it rises by impermeable rock formations. In industrial terms, an o ...
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Makó
Makó (, german: Makowa, yi, מאַקאָווע Makowe, ro, Macău or , sk, Makov) is a town in Csongrád County, in southeastern Hungary, from the Romanian border. It lies on the Maros River. Makó is home to 23,272 people and it has an area of , of which is arable land. Makó is the fourth-largest town in Csongrád County after Szeged, Hódmezővásárhely and Szentes. The town is from Hódmezővásárhely, from Szeged, from Arad, from Gyula, from Timișoara (Temesvár), and from Budapest. The climate is warmer than anywhere else in Hungary, with hot, dry summers. The town is noted for its onion which is a hungarikum, the spa and the thermal bath. The Makó International Onion Festival, the largest of its kind, is held annually. Makó is a popular tourist destination in Hungary. The Makó gas field, located near the town, is the largest natural gas field in Central Europe. The gas volume is more than 600 billion cubic metres (21 trillion cubic feet), according to a ...
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Unconventional (oil & Gas) Reservoir
Unconventional (oil & gas) reservoirs, or unconventional resources (resource plays) are accumulations where oil & gas phases are tightly bound to the rock fabric by strong capillary forces, requiring specialised measures for evaluation and extraction. Conventional reservoir Oil and gas are generated naturally at depths of around 4 or 5 kms below Earth’s surface. Being lighter than the water, which saturates rocks below the water table, the oil and gas percolate up through aquifer pathways towards Earth's surface (through time) by buoyancy. Some of the oil and gas percolate all the way to the surface as natural seepages, either on land or on the sea floor. The rest remain trapped underground where the oil and gas are prevented from reaching the surface by geological barriers, in a range of trap geometries. In this way, underground pockets of oil & gas accumulate by displacing water in porous rock, which, if permeable, are referred to as ''conventional reservo ...
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