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Brine mining

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20: 1210:, which, they concluded, could extract uranium at a cost of US$ 660/kg. While this was still five times the cost of uranium from ore, the amount of uranium dissolved in seawater would be enough to provide nuclear fuel for thousands of years at current rates of consumption. Bernard L. Cohen showed that all the world’s energy requirements for 5 billion years could be provided by breeder reactors fueled by uranium extracted from seawater without the cost of electricity rising by as much as 1% due to fuel costs. (Considering that rivers refill the oceans continuously and extraction would slightly lower the concentration and thus the rate lost to deposits) 199:
dissolved species are less mobile than the water, resulting in higher TDS concentrations than seawater. Bivalent species such as calcium (Ca) are less mobile than univalent species such as sodium (Na), resulting in calcium enrichment. The ratio of potassium to sodium (K/Na) may increase or decrease with depth, thought to be the result of ion exchange with the sediments.
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ropes, casing, and derricks since it was salt resistant. Iron wedges were hung from a bamboo cable tool attached to a lever on a platform constructed atop the tower. The derricks required two to three men jumping on and off the lever that moved the iron wedge pounded into the ground to dig a hole deep enough into the ground to hit the brine.
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Lithium mining from geothermal boreholes is a groving project in Europe. Potential sites are Cornwall (UK), Rhine Graben (France, Germany) and Cesano (Italy). All these sites have a lithium concentration of 200 mg/L or higher. Origin is due to interaction with mica minerals in the granite and/or
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varies from much less than seawater to ten times the total dissolved solids of seawater. In general, total dissolved solids (TDS) concentrations increase with depth. Most deep groundwaters classified as brines (having total dissolved solids equal to or greater than that of seawater) are predominantly
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Geothermal power plants often bring brine to the surface as part of the operation. This brine is usually re-injected into the ground, but some experiments have been made to extract minerals before re-injection. Brine brought to the surface by geothermal energy plants has been used in pilot plants as
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In 2016, MGX Minerals developed a proprietary design process (U.S. Provisional Patent #62/419,011) to potentially recover lithium and other valuable minerals from highly mineralized oilfield brine. The company has acquired development rights to over approximately 1.7 million acres of brine-bearing
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Starting in 2002, CalEnergy extracted zinc from brines at its geothermal energy plants at the Salton Sea, California. At full production, the company hoped to produce 30,000 metric tons of 99.99% pure zinc per year, yielding about as much profit as the company made from geothermal energy. But the
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is recovered from surface brine of the Dead Sea, at plants in Israel and Jordan. In 2013 Dead Sea brine provided 9.2% of the world production of potash. As of 1996, the Dead Sea was estimated to contain 2.05 million tons of potassium chloride, the largest brine reserve of potassium other than the
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Commercial brines include both surface water (seawater and saline lakes) and groundwater (shallow brine beneath saline or dry lakes, and deep brines in sedimentary basins). Brine brought to the surface by geothermal energy wells often contains high concentrations of minerals, but is not currently
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Several industries produce brines as by-products. Such industries are dairy, textile, leather, oil industries, etc. Thus, useful materials can be extracted and reused. However in industrial brine other chemicals and inhibitors might limit the ability to extract these useful materials. Innovative
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Around 500 BC, the ancient Chinese dug hundreds of brine wells, some of which were over 100 meters (330 feet) in depth. Large brine deposits under the earth's surface were drilled by drilling boreholes. Bamboo towers were erected, similar in style to modern-day oil derricks. Bamboo was used for
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By far the largest source of iodine from brine is Japan, where iodine-rich water is co-produced with natural gas. Iodine extraction began in 1934. In 2013 seven companies were reported to be extracting iodine. Japanese iodine brines are produced from mostly marine sediments ranging in age from
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The presence of groundwater with TDS higher than seawater is in some cases due to contact with salt beds. More often, however, the higher TDS of deep sediments is thought to be the result of the sediments acting as semi-permeable membranes. As the sediments compact under burial pressure, the
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Because metallic magnesium is extracted from brine by an electrolytic process, the economics are sensitive to the cost of electricity. Dow had located their facility on the Texas coast to take advantage of cheap natural gas for electrical generation. In 1951, Norsk Hydro started a
1045:. At the end of World War II, all shut down except the plant at Freeport, Texas, although the Velasco plant was reactivated during the Korean War. The magnesium plant at Freeport operated until 1998, when Dow announced that it would not rebuild the unit following hurricane damage. 290:) has been a valuable commodity since prehistoric times, and its extraction from seawater also goes back to prehistory. Salt is extracted from seawater in many countries around the world, but the majority of salt put on the market today is mined from solid 316:
Today, salt from groundwater brines is generally a byproduct of the process of extracting other dissolved substances from brines and constitutes only a small part of world salt production. In the United States, salt is recovered from surface brine at the
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magnesium-from-seawater plant at Heroya, Norway, supplied by inexpensive hydroelectricity. The two seawater magnesium plants, in Texas and Norway, provided more than half the world's primary magnesium through the 1950s and 1960s.
182:, California). Boron was recovered circa 1900 from geothermal steam at Larderello, Italy. Lithium recovery has also been investigated. But as of 2015, there is no sustained commercial-scale mineral recovery from geothermal brine. 817:
10 g/L) iodine, while subsurface brines contain as much as 1,560 mg/L (1.56 g/L), more than five orders of magnitude greater than seawater. The source of the iodine is thought to be organic material in
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The first commercial production of magnesium from seawater was recorded in 1923, when some solar salt plants around San Francisco Bay, California, extracted magnesium from the bitterns left after salt precipitation.
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The chemistry of shallow brines used for mineral extraction is sometimes influenced by geothermal waters. This is true of a number of shallow brines in the western United States, such as at Searles Lake, California.
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in Bolivia is thought to contain the world's largest lithium resource, often estimated to be half or more of the world's resource. As of 2015, no commercial extraction has taken place, other than a pilot plant.
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from seawater were common in the early 20th century. A number of people claimed to be able to economically recover gold from seawater, but they were all either mistaken or acted in an intentional deception.
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Brines brought to the surface by geothermal energy production often contain concentrations of dissolved silica of about 500 parts per million. A number of geothermal plants have pilot-tested recovery of
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production is derived from brine. The majority is recovered from Dead Sea brine at plants in Israel and Jordan, where bromine is a byproduct of potash recovery. Plants in the United States (
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As of 2014, the only producer of primary magnesium metal in the United States was U.S. Magnesium LLC, which extracted the metal from surface brine of the Great Salt Lake, at its plant in
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sodium chloride type. However, the predominance of chloride usually increases with increasing TDS, at the expense of sulfate. The ratio of calcium to sodium usually increases with depth.
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P. Evan Dresel and Athur W. Rose, Chemistry and Origin of Oil and Gas Well Brines in Western Pennsylvania, Pennsylvania Geological Survey, Open-File Report OFOG 10=01.0, 2010.
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with salinity greater than seawater, making them attractive for mineral extraction. Examples are the Dead Sea and the Great Salt Lake. In addition, some saline lakes, such as
1968:"Comments on "Lithium-rich geothermal brines in Europe: An up-date about geochemical characteristics and implications for potential Li resources" by Sanjuan etal. (2022)" 313:(Arab Salt Works). The total salt precipitated in solar evaporation at the Dead Sea plants is tens of millions of tons annually, but very little of the salt is marketed. 600:, which as of 2015 yielded about a third of the world's supply. The brine operations are primarily for potassium; extraction of lithium as a byproduct began in 1997. 585:
production. Whereas seawater contains about 0.17 mg/L (0.00017 g/L), subsurface brines may contain up to 4,000 mg/L (4.0 g/L), more than four
1370:"Minimal Liquid Discharge (MLD) and Zero Liquid Discharge (ZLD) strategies for wastewater management and resource recovery – Analysis, challenges and prospects" 1041:, to extract magnesium from the sea. A number of other plants to extract magnesium from brine were built in the US, including one near the Freeport plant at 958:), China, Turkmenistan, and Ukraine, recover bromine from subsurface brines. In India and Japan, bromine is recovered as a byproduct of sea salt production. 96:, and other materials, and are potentially important sources of a number of others. Brine mining supports waste minimization and resource recovery efforts. 813:. Iodine is recovered from deep brines pumped to the surface as a byproduct of oil and natural gas production. Seawater contains about 0.06 mg/L (6.0 61:
in that those methods inject water or chemicals to dissolve materials which are in a solid state; in brine mining, the materials are already dissolved.
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R. Gordon Bloomquist, "Economic benefits of mineral extraction from geothermal brines," 2006, Washington State University Extension Energy Program.
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ppb of gold in seawater, a commercially successful extraction seemed possible. After analysis of 4,000 water samples yielding an average of 0.004
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is recovered from shallow brines beneath Searles Lake, California, by Searles Valley Minerals. Although boron is the primary product,
1911:"Lithium-rich geothermal brines in Europe: An up-date about geochemical characteristics and implications for potential Li resources" 1760:
Dwight Bradley and others, "A preliminary deposit model for lithium brines," US Geological Survey, Open-File Report 2013–1006, 2013.
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P. B. Altringer and others, "Tungsten recovery from Searles Lake brines," US Bureau of Mines, Report of Investigation 8315, 1978.
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Jean E. Moran, "Origin of iodine in the Anadarko Basin, Oklahoma: an 129I study" AAPG Bulletin, May 1996, v.80 n.5 p.685–694.
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Sanjuan, Bernard; Gourcerol, Blandine; Millot, Romain; Rettenmaier, Detlev; Jeandel, Elodie; Rombaut, Aurélien (2022-05-01).
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Greta J. Orris, Deposit model for closed-basin potash-bearing brines, US Geological Survey, Open-File Report 2011-1283, 2011.
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J. R. Davis and J. D. Vine, "Stratigraphic and tectonic setting of the lithium brine field, Clayton Valley, Nevada," in
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greater than seawater. Typical commercial lithium concentrations are between 200 and 1,400 mg/L (1.4 g/L).
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In 2012 research for the US Department of Energy, building on Japanese research from the 1990s, tested a method for
57:, or hyper-saline solutions from several industries (e.g., textile industries). It differs from solution mining or 1856:"A revision of lithium minerals thermodynamics: Possible implications for fluids geochemistry and geothermometry" 611:
Commercial deposits of shallow lithium brines beneath dry lakebeds have the following characteristics in common:
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in East Africa, have chemistry very different than seawater, making them potential sources of sodium carbonate.
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since prehistoric times, and more recently of magnesium and bromine. Potassium is sometimes recovered from the
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Some near-surface brines in the western United States contain anomalously high concentrations of dissolved
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The brine beneath the Salar de Olaroz, Argentina, is a commercial source of boron, lithium, and potassium.
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for a pilot project aimed at showing the financial feasibility of extracting high-quality lithium from
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ppb, it became clear to Haber that the extraction would not be possible, and he stopped the project.
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brine. It uses brine from the 49.9 megawatt Featherstone geothermal power plant in California's
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Donald E. White, "Saline waters in sedimentary rocks", in Addison Young and John E. Galley (eds.),
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S. Warren Hobbs and James E. Elliottt, "Tungsten," in Donald A. Brobst and Walden P. Pratt (eds.)
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Operation of a mineral recovery unit on brine from the Salton Sea known geothermal resource area
1304:"Environmental impacts of desalination and brine treatment - Challenges and mitigation measures" 1436: 216:
Many brines contain more than one recovered product. For instance, the shallow brine beneath
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production was recovered from brine. Two plants in the US, at Searles Lake, California, and
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left after salt precipitation. The oceans are often described as an inexhaustible resource.
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Groundbreaking Scientific Experiments, Inventions, and Discoveries of the Ancient World
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began producing magnesium on a small scale in 1916, from deep subsurface brine in the
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zinc recovery unit did not perform as anticipated, and zinc recovery halted in 2004.
34: 1670:"Anson Resources experiences improved exploration success close to Long Canyon area" 1327: 2261: 2222: 1987: 1930: 1875: 1381: 1323: 593: 436: 375: 350: 338: 30: 2090: 1729:(Report). Bureau of Mines Report of Investigations. US Bureau of Mines. p. 3 1646: 1038: 646: 318: 287: 152: 69: 1483: 1269:) did research on the extraction of gold from seawater in an effort to help pay 1835:"Vulcan and Enel to jointly develop Cesano geothermal lithium project in Italy" 1510:"Lithium will fuel the clean energy boom. This company may have a breakthrough" 1385: 1042: 1034: 860: 604: 528: 510: 334: 306: 249: 130: 1628:, Rocky Mountain Association of Geologists, Utah Geological Association, 1979. 161:
often has brines with chemistry similar to that of the lakes or former lakes.
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Since 1977, iodine has been extracted from brine in the Morrow Sandstone of
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Circa 1900, boron was recovered from geothermal steam at Larderello, Italy.
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William H. Gross, "magnesium from the sea," in: Frank E. Firth (ed.)
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Panagopoulos, Argyris; Haralambous, Katherine-Joanne (2020-10-01).
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Panagopoulos, Argyris; Haralambous, Katherine-Joanne (2020-12-01).
1163: 832: 822:, which also form the source rock for the associated hydrocarbons. 524: 298: 281: 245: 175: 158: 126: 122: 46: 341:, recovered sodium sulfate from shallow brines beneath dry lakes. 1908: 1270: 1256: 948: 582: 237: 233: 93: 81: 73: 2140:
F. F. Wright, "Minerals of the ocean," in Frank E. Firth (ed.),
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F. F. Wright, "Minerals of the ocean," in Frank E. Firth (ed.),
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In 2010 Simbol Materials received a $ 3 million grant from the
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ECONOMIC BENEFITS OF MINERAL EXTRACTION FROM GEOTHERMAL BRINES
1642:"Cornish Lithium Releases Globally Significant Lithium Grades" 153:
Shallow groundwater brines associated with saline or dry lakes
108: 2106:, Washington State University Extension Energy Program, 2006. 1809:"Lithium de France: geothermal brines for lithium extraction" 1772:"Could Hawaii Geothermal Plant Become a Windfall for Public?" 819: 806: 717: 597: 225: 208:
solutions such as antiscalant deactivation technology (ASDT)
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The largest operations are in the shallow brine beneath the
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In 2015 subsurface brines yielded about half of the world's
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Salt is produced as a byproduct of potash extraction from
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https://www.rockstone-research.com/images/PDF/MGX20en.pdf
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in the 1890s. A British fraudster ran the same scam in
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Recovery of Minerals and Metals from Geothermal Fluids
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Stephen M. Jasinski, "Potash," US Geological Survey,
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Seawater, bittern remaining after salt precipitation
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Seawater, bittern remaining after salt precipitation
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formations in Canada and Utah. According to MGX, the
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Seawater, bittern remaining after salt precipitation
2119:, US Geological Survey Professional Paper 820, 1973. 1701:"142 ppm Li Assay Result from Artesian Flow Horizon" 1435:. Greenwood (published December 30, 2003). pp.  1422: 1420: 961: 185: 2195:(contains a chapter on gold-from seawater swindles) 1591: 1528: 1662: 1581: 1579: 1577: 1560: 1467:. Springer (published May 18, 2016). p. 1034. 1458: 1456: 724:and other salts are also recovered as byproducts. 211: 2154:“Record haul of uranium harvested from seawater,” 1720: 1718: 1695: 1693: 1691: 1689: 1687: 1549: 1547: 1417: 2277: 29:is the extraction of useful materials (chemical 1574: 1453: 321:, Utah, and from a shallow subsurface brine at 2169:“Breeder reactors: A renewable energy source,” 2032:, US Geological Survey, Minerals Yearbook 2013 1715: 1684: 1544: 915:5,000 to 6,000 mg/L (5.0 to 6.0 g/L) 190:The concentration of dissolved solids in deep 2136: 2134: 1724: 1374:Journal of Environmental Chemical Engineering 2205:Haber, F. (1927). "Das Gold im Meerwasser". 1427:Krebs, Robert E.; Krebs, Carolyn A. (2003). 2185:A Hole in the Ground with a Liar at the Top 1588:, Orocobre website, accessed 17 March 2016. 1408: 850: 109:Types of brines used for mineral extraction 2131: 1426: 805:supply worldwide. Major deposits occur in 2242:"Concentration of gold in natural waters" 1965: 1934: 1853: 1832: 1251:ran a gold-from-seawater swindle in the 618:Closed basin with a dry or seasonal lake 114:used for commercial mineral extraction. 18: 2187:(Salt Lake: Univ. of Utah Press, 2006) 2144:(New York: Van Nostrand, 1969) 406-407. 2073:(New York: Von Nostrand, 1969) 368-372. 1557:(New York: Van Nostrand, 1969) 406–407. 955:Bromine production in the United States 64:Brines are important sources of common 2278: 2239: 1769: 1725:Schultze, L. E.; Bauer, D. J. (1982). 1462: 1277:. Based on published values of 2 to 64 1059:The Dead Sea Works in Israel produces 2204: 1636: 1634: 1063:as a byproduct of potash extraction. 2142:The Encyclopedia of Marine Resources 2071:The Encyclopedia of Marine Resources 1555:The Encyclopedia of Marine Resources 1507: 1482:W. L. Bourcier, M. Lin, and G. Nix, 1363: 1361: 661:in the rocks of the local basement. 168: 1465:Evaporites: A Geological Compendium 1016:42,995 mg/L (42.995 g/L) 938:12,894 mg/L (12.894 g/L) 911:Smackover Formation, Arkansas, USA 368: 274:129,500 mg/L (129.5 g/L) 202: 16:Extracting materials from saltwater 13: 2246:Journal of Geochemical Exploration 1751:, Mineral Commodity Summary, 2016. 1631: 941:Brine at Depth, (Cane Creek well) 333:In 1997 about two-thirds of world 157:The groundwater beneath saline or 14: 2307: 2207:Zeitschrift fĂĽr Angewandte Chemie 2084:Magnesium, industry in transition 1992:10.1016/j.geothermics.2022.102518 1966:Boschetti, Tiziano (2022-11-01). 1936:10.1016/j.geothermics.2022.102385 1880:10.1016/j.geothermics.2021.102286 1854:Boschetti, Tiziano (2022-01-01). 1539:Fluids in Subsurface Environments 1358: 1275:reparations following World War I 1019:Brine at depth (Cane Creek well) 1005:35,200 mg/L (35.2 g/L) 994:56,100 mg/L (56.1 g/L) 962:Magnesium and magnesium compounds 795:Brine at depth (Cane Creek well) 711:Brine at depth (Cane Creek well) 550:Brine at depth (Cane Creek well) 453:22,500 mg/L (22.5 g/L) 442:19,400 mg/L (19.4 g/L) 414:17,700 mg/L (17.7 g/L) 328: 186:Deep brines in sedimentary basins 1208:extracting uranium from seawater 983:1,350 mg/L (1.35 g/L) 919:Deep brine in sedimentary basin 903:2,970 mg/L (2.97 g/L) 784:Deep brine in sedimentary basin 778:Morrow Sandstone, Oklahoma, USA 773:Deep brine in sedimentary basin 697:1,050 mg/L (1.05 g/L) 686:4.6 mg/L (0.0046 g/L) 633:Enough time to concentrate brine 428:5,730 mg/L (5.73 g/L) 2233: 2198: 2177: 2162: 2147: 2122: 2117:United States Mineral Resources 2109: 2096: 2076: 2063: 2046: 2035: 2023: 2014: 1959: 1902: 1847: 1833:GeoEnergy, Think (2022-07-08). 1826: 1801: 1789: 1763: 1754: 1741: 1618: 1605: 1328:10.1016/j.marpolbul.2020.111773 1156:Shallow brine beneath dry lake 927:10,000 mg/L (10 g/L) 792:596 mg/L (0.596 g/L) 708:829 mg/L (0.829 g/L) 700:Shallow brine beneath dry lake 564:Shallow brine beneath dry lake 547:142 mg/L (0.142 g/L) 519:Shallow brine beneath dry lake 464:6,200 mg/L (6.2 g/L) 445:Shallow brine beneath dry lake 431:Shallow brine beneath dry lake 212:Materials recovered from brines 136: 1770:Kaneya, Rui (April 13, 2015). 1501: 1295: 1153:56 mg/L (0.056 g/L) 1103:270 mg/L (0.27 g/L) 892:65 mg/L (0.065 g/L) 781:300 mg/L (0.30 g/L) 770:160 mg/L (0.16 g/L) 624:Igneous or geothermal activity 621:Tectonically driven subsidence 603:The shallow brine beneath the 572:170 mg/L (0.17 g/L) 561:690 mg/L (0.69 g/L) 533:220 mg/L (0.22 g/L) 516:300 mg/L (0.30 g/L) 403:380 mg/L (0.38 g/L) 174:a source of colloidal silica ( 1: 1288: 801:Brines are a major source of 655:Saskatchewan Research Council 224:, is or has been a source of 125:has been used as a source of 2266:10.1016/0375-6742(88)90051-9 1265:(the German inventor of the 1231: 1228: 1195: 1192: 1155: 1152: 1149: 1144: 1137: 1134: 1105: 1102: 1099: 1094: 1087: 1084: 1018: 1015: 1012: 1007: 1004: 1002:Dead Sea, Israel and Jordan 1001: 996: 993: 990: 985: 982: 979: 940: 937: 934: 929: 926: 924:Dead Sea, Israel and Jordan 923: 918: 913: 910: 905: 902: 899: 894: 891: 888: 794: 791: 788: 783: 780: 777: 772: 769: 766: 761: 754: 751: 710: 707: 704: 699: 696: 693: 688: 685: 682: 574: 571: 568: 563: 560: 554: 549: 546: 540: 535: 532: 523: 518: 515: 509: 504: 501: 498: 466: 463: 461:Dead Sea, Israel and Jordan 460: 455: 452: 450:Da Chaidam Salt Lake, China 449: 444: 441: 435: 430: 427: 421: 416: 413: 410: 405: 402: 399: 273: 270: 7: 1116: 694:Salar de Olaroz, Argentina 344: 117: 10: 2312: 1508:Roth, Sammy (2019-10-14). 1386:10.1016/j.jece.2020.104418 1177: 1174:, recovery is uneconomic. 870: 480: 279: 99: 1626:Basin and Range Symposium 1308:Marine Pollution Bulletin 1150:Searles Lake, California 733: 639:U.S. Department of Energy 381: 2227:10.1002/ange.19270401103 2056:T. Krukowski, "Iodine," 1463:Warren, John K. (2016). 972:Magnesium concentration 851:Anadarko Basin, Oklahoma 825: 664: 627:Lithium-rich source rock 392:Potassium concentration 2102:R. Gordon Bloomquist, 1813:Innovation News Network 1232:0.000004 mg/L (4.0 1213: 1127:Tungsten concentration 1100:Salton Sea, California 1066: 767:Kanto Gas Field, Japan 569:Salton Sea, California 255: 1747:US Geological Survey, 1613:2013 Minerals Yearbook 1188:Uranium concentration 881:Bromine concentration 859:, at locations in the 491:Lithium concentration 361:, from the remnant of 301:brine at one plant in 37:) which are naturally 23: 2240:McHugh, J.B. (1988). 1138:0.0001 mg/L (1.0 744:Iodine concentration 22: 1795:Rockstone Research ( 1259:in the early 1900s. 1242:Attempts to extract 1196:0.003 mg/L (3.0 1031:Dow Chemical Company 1013:Paradox Basin, Utah 705:Paradox Basin, Utah 675:Boron concentration 556:Salar de Olaroz mine 423:Salar de Olaroz mine 355:El Caracol, Ecatepec 2258:1988JCExp..30...85M 2219:1927AngCh..40..303H 1984:2022Geoth.10502518B 1927:2022Geoth.10102385S 1872:2022Geoth..9802286B 1650:. 17 September 2020 1320:2020MarPB.16111773P 1224:Gold concentration 1172:ion exchange resins 1088:0.01 mg/L (1.0 1077:Zinc concentration 935:Paradox Basin Utah 789:Utah Paradox Basin 755:0.06 mg/L (6.0 587:orders of magnitude 266:Salt concentration 45:. The brine may be 2291:Chinese inventions 2089:2009-01-07 at the 2082:Marvin Lieberman, 2060:, June 2011, p.74. 2058:Mining Engineering 630:Permeable aquifers 536:Geothermal waters 309:), and another in 24: 2286:Mining techniques 1515:Los Angeles Times 1249:Prescott Jernegan 1240: 1239: 1204: 1203: 1160: 1159: 1110: 1109: 1106:Geothermal brine 1023: 1022: 945: 944: 857:Pennsylvanian age 799: 798: 715: 714: 579: 578: 575:Geothermal brine 471: 470: 278: 277: 169:Geothermal brines 2303: 2296:Economic geology 2270: 2269: 2237: 2231: 2230: 2202: 2196: 2181: 2175: 2172:Bernard L. Cohen 2166: 2160: 2151: 2145: 2138: 2129: 2126: 2120: 2113: 2107: 2100: 2094: 2080: 2074: 2067: 2061: 2055: 2050: 2044: 2039: 2033: 2027: 2021: 2018: 2012: 2011: 1963: 1957: 1956: 1938: 1906: 1900: 1899: 1851: 1845: 1844: 1842: 1841: 1830: 1824: 1823: 1821: 1820: 1805: 1799: 1793: 1787: 1786: 1784: 1782: 1767: 1761: 1758: 1752: 1745: 1739: 1738: 1736: 1734: 1722: 1713: 1712: 1710: 1708: 1697: 1682: 1681: 1679: 1677: 1666: 1660: 1659: 1657: 1655: 1638: 1629: 1622: 1616: 1609: 1603: 1600: 1589: 1583: 1572: 1569: 1558: 1551: 1542: 1535: 1526: 1525: 1523: 1522: 1505: 1499: 1496: 1487: 1480: 1469: 1468: 1460: 1451: 1450: 1434: 1424: 1415: 1414:Tom (1989), 103. 1412: 1406: 1405: 1365: 1356: 1355: 1314:(Pt B): 111773. 1299: 1284: 1280: 1235: 1218: 1217: 1199: 1182: 1181: 1141: 1121: 1120: 1091: 1071: 1070: 966: 965: 947:All the world's 916: 875: 874: 866: 846: 816: 758: 738: 737: 669: 668: 594:Salar de Atacama 485: 484: 437:Salar de Atacama 386: 385: 376:colloidal silica 369:Colloidal silica 351:sodium carbonate 339:Seagraves, Texas 260: 259: 203:Industrial brine 59:in-situ leaching 2311: 2310: 2306: 2305: 2304: 2302: 2301: 2300: 2276: 2275: 2274: 2273: 2238: 2234: 2213:(11): 303–314. 2203: 2199: 2182: 2178: 2167: 2163: 2159:, 22 Aug. 2012. 2152: 2148: 2139: 2132: 2127: 2123: 2114: 2110: 2101: 2097: 2091:Wayback Machine 2081: 2077: 2068: 2064: 2053: 2051: 2047: 2040: 2036: 2028: 2024: 2019: 2015: 1964: 1960: 1907: 1903: 1852: 1848: 1839: 1837: 1831: 1827: 1818: 1816: 1807: 1806: 1802: 1794: 1790: 1780: 1778: 1768: 1764: 1759: 1755: 1746: 1742: 1732: 1730: 1723: 1716: 1706: 1704: 1703:. 19 April 2018 1699: 1698: 1685: 1675: 1673: 1668: 1667: 1663: 1653: 1651: 1647:Cornish Lithium 1640: 1639: 1632: 1623: 1619: 1610: 1606: 1601: 1592: 1586:Projects Olaroz 1584: 1575: 1570: 1561: 1552: 1545: 1536: 1529: 1520: 1518: 1506: 1502: 1497: 1490: 1481: 1472: 1461: 1454: 1447: 1425: 1418: 1413: 1409: 1366: 1359: 1300: 1296: 1291: 1282: 1278: 1233: 1216: 1197: 1180: 1169: 1139: 1119: 1089: 1069: 1039:Freeport, Texas 964: 914: 873: 864: 853: 844: 828: 814: 756: 736: 667: 647:Imperial Valley 596:dry lakebed in 483: 384: 371: 347: 331: 319:Great Salt Lake 288:sodium chloride 284: 258: 214: 205: 188: 171: 155: 141:There are many 139: 120: 111: 102: 17: 12: 11: 5: 2309: 2299: 2298: 2293: 2288: 2272: 2271: 2252:(1–3): 85–94. 2232: 2197: 2176: 2161: 2146: 2130: 2121: 2108: 2095: 2075: 2062: 2045: 2034: 2022: 2013: 1958: 1901: 1846: 1825: 1800: 1788: 1762: 1753: 1740: 1714: 1683: 1661: 1630: 1617: 1615:, August 2015. 1604: 1590: 1573: 1559: 1543: 1527: 1500: 1488: 1470: 1452: 1446:978-0313313424 1445: 1416: 1407: 1357: 1293: 1292: 1290: 1287: 1238: 1237: 1230: 1226: 1225: 1222: 1215: 1212: 1202: 1201: 1194: 1190: 1189: 1186: 1179: 1176: 1167: 1158: 1157: 1154: 1151: 1147: 1146: 1143: 1136: 1132: 1131: 1128: 1125: 1118: 1115: 1108: 1107: 1104: 1101: 1097: 1096: 1093: 1086: 1082: 1081: 1078: 1075: 1068: 1065: 1035:Michigan Basin 1021: 1020: 1017: 1014: 1010: 1009: 1006: 1003: 999: 998: 995: 992: 988: 987: 984: 981: 977: 976: 973: 970: 963: 960: 943: 942: 939: 936: 932: 931: 928: 925: 921: 920: 917: 912: 908: 907: 904: 901: 897: 896: 893: 890: 886: 885: 882: 879: 872: 869: 861:Anadarko Basin 852: 849: 827: 824: 797: 796: 793: 790: 786: 785: 782: 779: 775: 774: 771: 768: 764: 763: 760: 753: 749: 748: 745: 742: 735: 732: 713: 712: 709: 706: 702: 701: 698: 695: 691: 690: 687: 684: 680: 679: 676: 673: 666: 663: 635: 634: 631: 628: 625: 622: 619: 616: 605:Salar de Uyuni 577: 576: 573: 570: 566: 565: 562: 559: 552: 551: 548: 545: 538: 537: 534: 531: 529:United Kingdom 521: 520: 517: 514: 511:Clayton Valley 507: 506: 503: 500: 496: 495: 492: 489: 482: 479: 469: 468: 465: 462: 458: 457: 454: 451: 447: 446: 443: 440: 433: 432: 429: 426: 419: 418: 415: 412: 408: 407: 404: 401: 397: 396: 393: 390: 383: 380: 370: 367: 346: 343: 335:sodium sulfate 330: 329:Sodium sulfate 327: 325:, California. 307:Dead Sea Works 280:Main article: 276: 275: 272: 268: 267: 264: 257: 254: 250:sodium sulfate 213: 210: 204: 201: 187: 184: 170: 167: 154: 151: 138: 135: 119: 116: 110: 107: 101: 98: 15: 9: 6: 4: 3: 2: 2308: 2297: 2294: 2292: 2289: 2287: 2284: 2283: 2281: 2267: 2263: 2259: 2255: 2251: 2247: 2243: 2236: 2228: 2224: 2220: 2216: 2212: 2208: 2201: 2194: 2193:0-87480-840-5 2190: 2186: 2180: 2173: 2170: 2165: 2158: 2157:New Scientist 2155: 2150: 2143: 2137: 2135: 2125: 2118: 2112: 2105: 2099: 2092: 2088: 2085: 2079: 2072: 2066: 2059: 2049: 2043: 2038: 2031: 2026: 2017: 2009: 2005: 2001: 1997: 1993: 1989: 1985: 1981: 1977: 1973: 1969: 1962: 1954: 1950: 1946: 1942: 1937: 1932: 1928: 1924: 1920: 1916: 1912: 1905: 1897: 1893: 1889: 1885: 1881: 1877: 1873: 1869: 1865: 1861: 1857: 1850: 1836: 1829: 1814: 1810: 1804: 1798: 1792: 1777: 1773: 1766: 1757: 1750: 1744: 1728: 1721: 1719: 1702: 1696: 1694: 1692: 1690: 1688: 1671: 1665: 1649: 1648: 1643: 1637: 1635: 1627: 1621: 1614: 1608: 1599: 1597: 1595: 1587: 1582: 1580: 1578: 1568: 1566: 1564: 1556: 1550: 1548: 1540: 1534: 1532: 1517: 1516: 1511: 1504: 1495: 1493: 1485: 1479: 1477: 1475: 1466: 1459: 1457: 1448: 1442: 1438: 1433: 1432: 1423: 1421: 1411: 1403: 1399: 1395: 1391: 1387: 1383: 1380:(5): 104418. 1379: 1375: 1371: 1364: 1362: 1353: 1349: 1345: 1341: 1337: 1333: 1329: 1325: 1321: 1317: 1313: 1309: 1305: 1298: 1294: 1286: 1276: 1272: 1268: 1267:Haber process 1264: 1260: 1258: 1254: 1253:United States 1250: 1245: 1236:10 g/L) 1227: 1223: 1220: 1219: 1211: 1209: 1200:10 g/L) 1191: 1187: 1184: 1183: 1175: 1173: 1165: 1148: 1142:10 g/L) 1133: 1129: 1126: 1123: 1122: 1114: 1098: 1092:10 g/L) 1083: 1079: 1076: 1073: 1072: 1064: 1062: 1057: 1055: 1050: 1046: 1044: 1040: 1036: 1032: 1027: 1011: 1000: 989: 978: 974: 971: 968: 967: 959: 957: 956: 950: 933: 922: 909: 898: 887: 883: 880: 877: 876: 868: 862: 858: 848: 842: 838: 834: 823: 821: 812: 811:United States 808: 804: 787: 776: 765: 759:10 g/L) 750: 746: 743: 740: 739: 731: 728: 725: 723: 719: 703: 692: 681: 677: 674: 671: 670: 662: 658: 656: 650: 648: 644: 640: 632: 629: 626: 623: 620: 617: 614: 613: 612: 609: 606: 601: 599: 595: 590: 588: 584: 567: 557: 553: 543: 542:Paradox Basin 539: 530: 526: 522: 512: 508: 497: 493: 490: 487: 486: 478: 475: 459: 448: 438: 434: 424: 420: 409: 398: 394: 391: 388: 387: 379: 377: 366: 364: 360: 356: 352: 342: 340: 336: 326: 324: 320: 314: 312: 308: 304: 300: 295: 293: 289: 283: 269: 265: 262: 261: 253: 251: 247: 243: 239: 235: 231: 227: 223: 219: 209: 200: 196: 193: 192:connate water 183: 181: 177: 166: 162: 160: 150: 148: 144: 134: 132: 128: 124: 115: 106: 97: 95: 91: 87: 83: 79: 75: 71: 67: 62: 60: 56: 52: 51:surface water 48: 44: 40: 36: 32: 28: 21: 2249: 2245: 2235: 2210: 2206: 2200: 2184: 2183:Plazak, Dan 2179: 2171: 2164: 2156: 2149: 2141: 2124: 2116: 2111: 2098: 2078: 2070: 2065: 2057: 2048: 2037: 2025: 2016: 1975: 1971: 1961: 1918: 1914: 1904: 1863: 1859: 1849: 1838:. Retrieved 1828: 1817:. Retrieved 1815:. 2022-02-22 1812: 1803: 1791: 1779:. Retrieved 1775: 1765: 1756: 1743: 1731:. Retrieved 1705:. Retrieved 1674:. Retrieved 1672:. 7 May 2018 1664: 1652:. Retrieved 1645: 1625: 1620: 1612: 1607: 1554: 1538: 1519:. Retrieved 1513: 1503: 1464: 1430: 1410: 1377: 1373: 1311: 1307: 1297: 1261: 1241: 1205: 1161: 1111: 1058: 1054:Rowley, Utah 1051: 1047: 1028: 1024: 1008:Saline lake 952: 946: 930:Saline lake 867:ppm iodine. 854: 829: 800: 729: 726: 716: 659: 651: 636: 615:Arid climate 610: 602: 591: 580: 558:, Argentina 472: 467:Saline lake 456:Saline lake 425:, Argentina 372: 363:Lake Texcoco 348: 332: 323:Searles Lake 315: 296: 285: 218:Searles Lake 215: 206: 197: 189: 172: 163: 156: 143:saline lakes 140: 137:Saline lakes 121: 112: 103: 63: 27:Brine mining 26: 25: 1972:Geothermics 1915:Geothermics 1860:Geothermics 1263:Fritz Haber 837:Pleistocene 359:Mexico City 147:Lake Natron 55:groundwater 2280:Categories 1978:: 102518. 1921:: 102385. 1866:: 102286. 1840:2022-07-11 1819:2022-07-11 1776:Civil Beat 1521:2019-10-17 1289:References 643:geothermal 502:0.17 mg/L 349:Soda ash ( 294:deposits. 222:California 180:Salton Sea 2008:250395603 2000:0375-6505 1953:247240697 1945:0375-6505 1896:244036105 1888:0375-6505 1781:March 13, 1402:225309628 1394:2213-3437 1352:226224643 1336:0025-326X 1229:Seawater 1193:Seawater 1145:Seawater 1124:Location 1095:Seawater 1074:Location 1061:magnesium 986:Seawater 969:Location 895:Seawater 878:Location 762:Seawater 741:Location 722:potassium 689:Seawater 672:Location 513:, Nevada 505:Seawater 488:Location 406:Seawater 389:Location 292:evaporite 271:Seawater 242:phosphate 159:dry lakes 90:potassium 86:magnesium 39:dissolved 35:compounds 2087:Archived 1733:March 9, 1344:33128985 1164:tungsten 1117:Tungsten 833:Pliocene 809:and the 525:Cornwall 439:, Chile 345:Soda ash 299:Dead Sea 282:Sea salt 246:soda ash 176:Wairakei 127:sea salt 123:Seawater 118:Seawater 49:, other 47:seawater 31:elements 2254:Bibcode 2215:Bibcode 2093:, 2001. 1980:Bibcode 1923:Bibcode 1868:Bibcode 1749:Lithium 1654:17 July 1316:Bibcode 1271:Germany 1257:England 1221:Source 1185:Source 1178:Uranium 1130:Source 1080:Source 1043:Velasco 975:Source 949:bromine 884:Source 871:Bromine 747:Source 678:Source 583:lithium 544:, Utah 494:Source 481:Lithium 477:ocean. 395:Source 263:Source 238:lithium 234:bromine 131:bittern 100:History 94:bromine 82:lithium 74:calcium 2191:  2054:  2042:Iodine 2030:Iodine 2006:  1998:  1951:  1943:  1894:  1886:  1707:7 June 1676:7 June 1443:  1439:–256. 1400:  1392:  1350:  1342:  1334:  1283:  1279:  1135:Ocean 1085:Ocean 991:Ocean 980:Ocean 900:Ocean 889:Ocean 865:  845:  841:Honshu 820:shales 803:iodine 752:Ocean 734:Iodine 683:Ocean 499:Ocean 474:Potash 411:Ocean 400:Ocean 382:Potash 311:Jordan 303:Israel 286:Salt ( 248:, and 230:potash 78:iodine 2004:S2CID 1949:S2CID 1892:S2CID 1398:S2CID 1348:S2CID 953:see: 847:ppm. 826:Japan 807:Japan 718:Boron 665:Boron 598:Chile 357:, in 226:borax 43:brine 2189:ISBN 1996:ISSN 1941:ISSN 1884:ISSN 1783:2016 1735:2022 1709:2019 1678:2019 1656:2021 1441:ISBN 1390:ISSN 1340:PMID 1332:ISSN 1244:gold 1214:Gold 1067:Zinc 1029:The 256:Salt 70:NaCl 66:salt 2262:doi 2223:doi 1988:doi 1976:105 1931:doi 1919:101 1876:doi 1437:255 1382:doi 1324:doi 1312:161 1273:'s 835:to 72:), 41:in 33:or 2282:: 2260:. 2250:30 2248:. 2244:. 2221:. 2211:40 2209:. 2133:^ 2052:S. 2002:. 1994:. 1986:. 1974:. 1970:. 1947:. 1939:. 1929:. 1917:. 1913:. 1890:. 1882:. 1874:. 1864:98 1862:. 1858:. 1811:. 1774:. 1717:^ 1686:^ 1644:. 1633:^ 1593:^ 1576:^ 1562:^ 1546:^ 1530:^ 1512:. 1491:^ 1473:^ 1455:^ 1419:^ 1396:. 1388:. 1376:. 1372:. 1360:^ 1346:. 1338:. 1330:. 1322:. 1310:. 1306:. 1056:. 527:, 365:. 252:. 244:, 240:, 236:, 232:, 228:, 220:, 92:, 88:, 84:, 80:, 76:, 53:, 2268:. 2264:: 2256:: 2229:. 2225:: 2217:: 2010:. 1990:: 1982:: 1955:. 1933:: 1925:: 1898:. 1878:: 1870:: 1843:. 1822:. 1785:. 1737:. 1711:. 1680:. 1658:. 1524:. 1449:. 1404:. 1384:: 1378:8 1354:. 1326:: 1318:: 1234:Ă— 1198:Ă— 1168:3 1140:Ă— 1090:Ă— 815:Ă— 757:Ă— 305:( 68:(

Index


elements
compounds
dissolved
brine
seawater
surface water
groundwater
in-situ leaching
salt
NaCl
calcium
iodine
lithium
magnesium
potassium
bromine
Seawater
sea salt
bittern
saline lakes
Lake Natron
dry lakes
Wairakei
Salton Sea
connate water
Searles Lake
California
borax
potash

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