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Kızıldere Geothermal Power Plant
The Kızıldere Geothermal Power Plant () is a geothermal power plant located at Kızıldere village of Sarayköy district in Denizli Province, southwestern Turkey. The initial power plant with 15 MW installed capacity was expanded in the second phase about 80 MW to 95 MW in total, making the facility Turkey's biggest geothermal power plant. It is planned to expand the power plant in a third and fourth phase. History The power plant began its operation as a prototype system with the installation of a 500 kW turbine generator group in 1974. The facility generated electricity and distributed it to the households of villages in the vicinity for four years free of charge. In 1984, the state-owned company Elektrik Üretim A.Ş. (EÜAŞ) built a power plant with 17.4 MW installed capacity and put it into service. However, the geothermal power plant has produced 10 MW on average since its opening in 1984. In September 2008, Zorlu Energy Inc. (Zorlu Doğal Elektrik Üretim A.Ş.), a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sarayköy
Sarayköy is a municipality and district of Denizli Province, Turkey. Its area is 379 km2, and its population is 30,834 (2022). It is 20 km west of the city of Denizli, on a plain between mountains and watered by Büyük Menderes River. Sarayköy is at a high altitude inland from the Mediterranean and thus has hot dry summers and very cold winters. The mountain sides are mostly bare but there are ongoing forestry projects. History The town was previously a village named ''Sarıbey'' after the Turkmen lord that settled his tribe here in the 14th century. Sarayköy was an important point of resistance to the Greek Army in the Turkish War of Independence. Volunteers assembled here were able to defend the bridge across the River Menderes and thus prevent the Greeks from occupying the city of Denizli. There is a statue in the town of a fighter in local efe costume to commemorate this struggle. Composition There are 32 neighbourhoods in Sarayköy District: [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dry Ice
Dry ice is the solid form of carbon dioxide. It is commonly used for temporary refrigeration as CO2 does not have a liquid state at normal atmospheric pressure and Sublimation (phase transition), sublimes directly from the solid state to the gas state. It is used primarily as a cooling agent, but is also used in fog machines at theatres for dramatic effects. Its advantages include lower temperature than that of Ice, water ice and not leaving any residue (other than incidental frost from moisture in the atmosphere). It is useful for preserving frozen foods (such as ice cream) where Refrigeration, mechanical cooling is unavailable. Dry ice sublimes at at Earth atmospheric pressure. This extreme cold makes the solid dangerous to handle without protection from frostbite injury. While generally not very toxic, the outgassing from it can cause hypercapnia (abnormally elevated carbon dioxide levels in the blood) due to a buildup in confined locations. Properties Dry ice is the soli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Demister (vapor)
A demister is a device often fitted to vapor–liquid separator vessels to enhance the removal of liquid droplets entrained in a vapor stream. Demisters may be a mesh-type coalescer, vane pack or other structure intended to aggregate the mist into droplets that are heavy enough to separate from the vapor stream. Demisters can reduce the residence time required to separate a given liquid droplet size by reducing the volume and associated cost of separator equipment. Demisters are often used where vapor quality is important in regard to entrained liquids, particularly where separator equipment costs are high (e.g., high-pressure systems) or where space or weight savings are advantageous. For example, in the process of brine desalination on marine vessels, brine is flash-heated into vapor. In flashing, vapor carries over droplets of brine, which have to be separated before condensing, otherwise the distillate vapor would be contaminated with salt. This is the role of the demist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limescale
Limescale is a hard, chalky deposit, consisting mainly of calcium carbonate (CaCO3). It often builds up inside kettles, boilers, and pipework, especially that for hot water. It is also often found as a similar deposit on the inner surfaces of old pipes and other surfaces where hard water has flowed. Limescale also forms as travertine or tufa in hard water springs. The colour varies from off-white through a range of greys and pink or reddish browns, depending on the other minerals present. Iron compounds give the reddish-browns. In addition to being unsightly and hard to clean, limescale can seriously damage or impair the operation of various plumbing and heating components.Hermann Weingärtner, "Water" in ''Ullmann's Encyclopedia of Industrial Chemistry'', December 2006, Wiley–VCH, Weinheim. Descaling agents are commonly used to remove limescale. Prevention of fouling by scale build-up relies on the technologies of water softening or other water treatment. Limescale can als ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calcium Carbonate
Calcium carbonate is a chemical compound with the chemical formula . It is a common substance found in Rock (geology), rocks as the minerals calcite and aragonite, most notably in chalk and limestone, eggshells, gastropod shells, shellfish skeletons and pearls. Materials containing much calcium carbonate or resembling it are described as calcareous. Calcium carbonate is the active ingredient in agricultural lime and is produced when calcium ions in hard water react with carbonate ions to form limescale. It has medical use as a calcium supplement or as an antacid, but excessive consumption can be hazardous and cause hypercalcemia and digestive issues. Chemistry Calcium carbonate shares the typical properties of other carbonates. Notably, it: *reacts with acids, releasing carbonic acid which quickly disintegrates into carbon dioxide and water: : *releases carbon dioxide upon heating, called a thermal decomposition reaction, or calcination (to above 840 °C in the case of ), t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carbon Dioxide
Carbon dioxide is a chemical compound with the chemical formula . It is made up of molecules that each have one carbon atom covalent bond, covalently double bonded to two oxygen atoms. It is found in a gas state at room temperature and at normally-encountered concentrations it is odorless. As the source of carbon in the carbon cycle, atmospheric is the primary carbon source for life on Earth. In the air, carbon dioxide is transparent to visible light but absorbs infrared, infrared radiation, acting as a greenhouse gas. Carbon dioxide is soluble in water and is found in groundwater, lakes, ice caps, and seawater. It is a trace gas Carbon dioxide in Earth's atmosphere, in Earth's atmosphere at 421 parts per million (ppm), or about 0.042% (as of May 2022) having risen from pre-industrial levels of 280 ppm or about 0.028%. Burning fossil fuels is the main cause of these increased concentrations, which are the primary cause of climate change.IPCC (2022Summary for pol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly Dolomite (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marble
Marble is a metamorphic rock consisting of carbonate minerals (most commonly calcite (CaCO3) or Dolomite (mineral), dolomite (CaMg(CO3)2) that have recrystallized under the influence of heat and pressure. It has a crystalline texture, and is typically not Foliation (geology), foliated (Layered intrusion, layered), although there are exceptions. In geology, the term ''marble'' refers to metamorphosed limestone, but its use in stonemasonry more broadly encompasses unmetamorphosed limestone. The extraction of marble is performed by quarrying. Marble production is dominated by four countries: China, Italy, India and Spain, which account for almost half of world production of marble and decorative stone. Because of its high hardness and strong wear resistance, and because it will not be deformed by temperature, marble is often used in Marble sculpture, sculpture and construction. Etymology The word "marble" derives from the Ancient Greek (), from (), "crystalline rock, shin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lithological
The lithology of a rock unit is a description of its physical characteristics visible at outcrop, in hand or core samples, or with low magnification microscopy. Physical characteristics include colour, texture, grain size, and composition. Lithology may refer to either a detailed description of these characteristics, or a summary of the gross physical character of a rock. Examples of lithologies in the second sense include sandstone, slate, basalt, or limestone. Lithology is the basis of subdividing rock sequences into individual lithostratigraphic units for the purposes of mapping and correlation between areas. In certain applications, such as site investigations, lithology is described using a standard terminology such as in the European geotechnical standard Eurocode 7. Rock type The naming of a lithology is based on the rock type. The three major rock types are igneous, sedimentary, and metamorphic. Igneous rocks are formed directly from magma, which is a mixture of m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
General Directorate Of Mineral Research And Exploration (Turkey)
The General Directorate of Mineral Research & Exploration of Turkey (Turkish language, Turkish: ''Maden Tetkik ve Arama Genel Müdürlüğü'', commonly known as MTA) is a scientific institution established by the Ministry of Energy and Natural Resources (Turkey), Ministry of Energy and Natural Resources in 1935. MTA conducts Geological survey, geological and Geophysical survey, geophysical surveys all around Turkey in order to explore natural resources, like ore deposits and energy raw materials. The institution has 6 divisions with many different analysis labs, and a training facility for geologists and Geophysicist, geophysical engineers in Ankara. Apart from focusing on fieldwork for mining research, MTA also has remote sensing facilities since 1975. Remote sensing unit operates under MTA Geophysics Research Division and TUBITAK has a cooperation since early 1970s. MTA publishes ''Bulletin of the Mineral Research and Exploration'' twice a year since 1936. Papers are publish ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Graben
In geology, a graben () is a depression (geology), depressed block of the Crust (geology), crust of a planet or moon, bordered by parallel normal faults. Etymology ''Graben'' is a loan word from German language, German, meaning 'ditch' or 'trench'. The first known usage of the word in the geologic context was by Eduard Suess in 1883. The plural form is either ''graben'' or ''grabens''. Formation A graben is a valley with a distinct escarpment on each side caused by the displacement of a block of land downward. Graben often occur side by side with Horst (geology), horsts. Horst and graben structures indicate tensional forces and crustal stretching. Graben are produced by sets of normal faults that have parallel fault traces, where the displacement of the hanging wall is downward, while that of the footwall is upward. The faults typically dip toward the center of the graben from both sides. Horsts are parallel blocks that remain between graben; the bounding faults of a horst t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taner Yıldız
Taner Yıldız (born 3 April 1962 in Devecipınar, Boğazlıyan, Yozgat Province) is a Turkish politician. He is a member of the Justice and Development Party and served as the Minister of Energy and Natural Resources between 2009 and 2015. Taner Yıldız graduated from the Istanbul Technical University as an electrical engineer and worked for the Kayseri Electricity Generation Company. He was elected to the Parliament in 2002. Yıldız served as an energy adviser to the prime minister Recep Tayyip Erdoğan Recep Tayyip Erdoğan (born 26 February 1954) is a Turkish politician who is the 12th and current president of Turkey since 2014. He previously served as the 25th prime minister of Turkey, prime minister from 2003 to 2014 as part of the Jus .... On 1 May 2009, after a reshuffle of the cabinet, he took the post of Minister of Energy and Natural Resources. Yıldız is married and has four children. References CitationsTurkish Energy Minister to visit Azerbaijan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
