Evaluation of Methods for Recovering Potash from Carnallite Ore
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Brine Evolution in Qaidam Basin, Northern Tibetan Plateau, and the Formation of Playas As Mars Analogue Site
45th Lunar and Planetary Science Conference (2014) 1228.pdf BRINE EVOLUTION IN QAIDAM BASIN, NORTHERN TIBETAN PLATEAU, AND THE FORMATION OF PLAYAS AS MARS ANALOGUE SITE. W. G. Kong1 M. P. Zheng1 and F. J. Kong1, 1 MLR Key Laboratory of Saline Lake Resources and Environments, Institute of Mineral Resources, CAGS, Beijing 100037, China. ([email protected]) Introduction: Terrestrial analogue studies have part of the basin (Kunteyi depression). The Pliocene is served much critical information for understanding the first major salt forming period for Qaidam Basin, Mars [1]. Playa sediments in Qaidam Basin have a and the salt bearing sediments formed at the southwest complete set of salt minerals, i.e. carbonates, sulfates, part are dominated by sulfates, and those formed at the and chlorides,which have been identified on Mars northwest part of basin are partially sulfates dominate [e.g. 2-4]. The geographical conditions and high eleva- and partially chlorides dominate. After Pliocene, the tion of these playas induces Mars-like environmental deposition center started to move towards southeast conditions, such as low precipitation, low relative hu- until reaching the east part of the basin at Pleistocene, midity, low temperature, large seasonal and diurnal T reaching the second major salt forming stage, and the variation, high UV radiation, etc. [5,6]. Thus the salt bearing sediments formed at this stage are mainly playas in the Qaidam Basin servers a good terrestrial chlorides dominate. The distinct change in salt mineral reference for studying the depositional and secondary assemblages among deposition centers indicates the processes of martian salts. migration and geochemical differentiation of brines From 2008, a set of analogue studies have been inside the basin. -
Potash Case Study
Mining, Minerals and Sustainable Development February 2002 No. 65 Potash Case Study Information supplied by the International Fertilizer Industry Association This report was commissioned by the MMSD project of IIED. It remains the sole Copyright © 2002 IIED and WBCSD. All rights reserved responsibility of the author(s) and does not necessarily reflect the views of the Mining, Minerals and MMSD project, Assurance Group or Sponsors Group, or those of IIED or WBCSD. Sustainable Development is a project of the International Institute for Environment and Development (IIED). The project was made possible by the support of the World Business Council for Sustainable Development (WBCSD). IIED is a company limited by guarantee and incorporated in England. Reg No. 2188452. VAT Reg. No. GB 440 4948 50. Registered Charity No. 800066 1 Introduction 2 2 Global Resources and Potash Production 3 3 The use of potassium in fertilizer 4 3.1 Potassium Fertilizer Consumption 4 3.2 Potassium fertilization issues 6 Appendix A 8 1 Introduction Potash and Potassium Potassium (K) is essential for plant and animal life wherein it has many vital nutritional roles. In plants, potassium and nitrogen are the two elements required in greatest amounts, while in animals and humans potassium is the third most abundant element, after calcium and phosphorus. Without sufficient plant and animal intake of potassium, life as we know it would cease. Human and other animals atop the food chain depend upon plants for much of their nutritional needs. Many soils lack sufficient quantities of available potassium for satisfactory yield and quality of crops. For this reason available soil potassium levels are commonly supplemented by potash fertilization to improve the potassium nutrition of plants, particularly for sustaining production of high yielding crop species and varieties in modern agricultural systems. -
Mining Methods for Potash
Potash—A Vital Agricultural Nutrient Sourced from Geologic Deposits Open File Report 2016–1167 U.S. Department of the Interior U.S. Geological Survey Cover. Photos of underground mining operations, Carlsbad, New Mexico, Intrepid Potash Company, Carlsbad West Mine. Potash—A Vital Agricultural Nutrient Sourced from Geologic Deposits By Douglas B. Yager Open File Report 2016–1167 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Director U.S. Geological Survey, Reston, Virginia: 2016 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://store.usgs.gov/. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Yager, D.B., 2016, Potash—A vital agricultural nutrient sourced from geologic deposits: U.S. Geological Survey Open- File Report 2016–1167, 28 p., https://doi.org/10.3133/ofr20161167. ISSN 0196-1497 (print) ISSN 2331-1258 (online) ISBN 978-1-4113-4101-2 iii Acknowledgments The author wishes to thank Joseph Havasi of Compass Minerals for a surface tour of their Great Salt Lake operations. -
Fertilizer Production Expertise HPD® Evaporation and Crystallization
Fertilizer Production Expertise HPD® Evaporation and Crystallization WATER TECHNOLOGIES Fertilizer Expertise Case Study: Veolia NPK Fertilizers HPD® Evaporation and Crystallization systems from Veolia Research & Development NPK Process Capabilities Water Technologies provide innovative process solutions for large-scale fertilizer production facilities worldwide. IC Potash Corp. (ICP) - Sulfate of Potash (SOP) These systems allow production of a wide range of high-quality fertilizer products from natural sources (mined or solution mined deposits) or by-product streams from other processes that include: Chlorine / • Ammonium sulfate • Mono potassium phosphate Raw Materials Natural Gas Sulfur Phosphate Rock Hydrogen Gas Potash Source • Ammonium nitrate (MKP) • Potassium chloride (MOP) • Sodium nitrate • Potassium sulfate (SOP) • Phosphoric acid merchant/ technical/food/electrical • Monoammonium phosphate (MAP) grade ICP's Ochoa Mine project (New Mexico, USA) is • Diammonium phosphate • Potassium carbonate (DAP) • Potassium nitrate projected to produce approximately 714,000 TPY Ammonia Plant Sulfuric Acid Rock Grinding Hydrochloric Acid of Sulfate of Potash (SOP-K SO ) from Polyhalite • Epsom salt: Magnesium • Calcium phosphate 2 4 Plant Plant Plant ore (K SO .MgSO .2CaSO .2H O) for more than 50 sulfate heptahydrate • Calcium sulfate 2 4 4 4 2 years. • Magnesium sulfate • Calcium chloride monohydrate Veolia was selected to refine, confirm, and validate the overall ICP process utilizing HPD® Evaporation and Crystallization technologies through a series of bench and pilot-scale testing programs performed in Veolia’s in-house testing facility. The scope of the testing extended lants from the ore P leaching to the SOP crystallization process including Nitric Acid Plant Phosphoric Acid PlantPotassium Chloride Plant crystallization/redissolution of leonite (K2SO4. -
S40645-019-0306-X.Pdf
Isaji et al. Progress in Earth and Planetary Science (2019) 6:60 Progress in Earth and https://doi.org/10.1186/s40645-019-0306-x Planetary Science RESEARCH ARTICLE Open Access Biomarker records and mineral compositions of the Messinian halite and K–Mg salts from Sicily Yuta Isaji1* , Toshihiro Yoshimura1, Junichiro Kuroda2, Yusuke Tamenori3, Francisco J. Jiménez-Espejo1,4, Stefano Lugli5, Vinicio Manzi6, Marco Roveri6, Hodaka Kawahata2 and Naohiko Ohkouchi1 Abstract The evaporites of the Realmonte salt mine (Sicily, Italy) are important archives recording the most extreme conditions of the Messinian Salinity Crisis (MSC). However, geochemical approach on these evaporitic sequences is scarce and little is known on the response of the biological community to drastically elevating salinity. In the present work, we investigated the depositional environments and the biological community of the shale–anhydrite–halite triplets and the K–Mg salt layer deposited during the peak of the MSC. Both hopanes and steranes are detected in the shale–anhydrite–halite triplets, suggesting the presence of eukaryotes and bacteria throughout their deposition. The K–Mg salt layer is composed of primary halites, diagenetic leonite, and primary and/or secondary kainite, which are interpreted to have precipitated from density-stratified water column with the halite-precipitating brine at the surface and the brine- precipitating K–Mg salts at the bottom. The presence of hopanes and a trace amount of steranes implicates that eukaryotes and bacteria were able to survive in the surface halite-precipitating brine even during the most extreme condition of the MSC. Keywords: Messinian Salinity Crisis, Evaporites, Kainite, μ-XRF, Biomarker Introduction hypersaline condition between 5.60 and 5.55 Ma (Manzi The Messinian Salinity Crisis (MSC) is one of the most et al. -
1469 Vol 43#5 Art 03.Indd
1469 The Canadian Mineralogist Vol. 43, pp. 1469-1487 (2005) BORATE MINERALS OF THE PENOBSQUIS AND MILLSTREAM DEPOSITS, SOUTHERN NEW BRUNSWICK, CANADA JOEL D. GRICE§, ROBERT A. GAULT AND JERRY VAN VELTHUIZEN† Research Division, Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario K1P 6P4, Canada ABSTRACT The borate minerals found in two potash deposits, at Penobsquis and Millstream, Kings County, New Brunswick, are described in detail. These deposits are located in the Moncton Subbasin, which forms the eastern portion of the extensive Maritimes Basin. These marine evaporites consist of an early carbonate unit, followed by a sulfate, and fi nally, a salt unit. The borate assemblages occur in specifi c beds of halite and sylvite that were the last units to form in the evaporite sequence. Species identifi ed from drill-core sections include: boracite, brianroulstonite, chambersite, colemanite, congolite, danburite, hilgardite, howlite, hydroboracite, kurgantaite, penobsquisite, pringleite, ruitenbergite, strontioginorite, szaibélyite, trembathite, veatchite, volkovskite and walkerite. In addition, 41 non-borate species have been identifi ed, including magnesite, monohydrocalcite, sellaite, kieserite and fl uorite. The borate assemblages in the two deposits differ, and in each deposit, they vary stratigraphically. At Millstream, boracite is the most common borate in the sylvite + carnallite beds, with hilgardite in the lower halite strata. At Penobsquis, there is an upper unit of hilgardite + volkovskite + trembathite in halite and a lower unit of hydroboracite + volkov- skite + trembathite–congolite in halite–sylvite. At both deposits, values of the ratio of B isotopes [␦11B] range from 21.5 to 37.8‰ [21 analyses] and are consistent with a seawater source, without any need for a more exotic interpretation. -
United States Patent (11) 3,615,174
United States Patent (11) 3,615,174 72 Inventor William J. Lewis 3,342,548 9/1967 Macey....... A. 2319 X South Ogden, Utah 3,432,031 3/1969 Ferris........................... 209/166 X 21 Appl. No. 740,886 FOREIGN PATENTS 22, Filed June 28, 1968 45 Patented Oct. 26, 1971 1,075,166 4f1954 France ......................... 209/66 (73) Assignee NL Industries, Inc. OTHER REFERENCES New York, N.Y. Chem. Abst., Vol. 53, 1959, 9587e I & EC, Vol. 56, 7, Jy '64, 61 & 62. Primary Examiner-Frank W. Lutter 54 PROCESSFOR THE SELECTIVE RECOVERY OF Assistant Examiner-Robert Halper POTASSUMAND MAGNESUMWALUES FROM Attorney-Ward, McElhannon, Brooks & Fitzpatrick AQUEOUSSALT SOLUTIONS CONTAINING THE SAME 11 Claims, 4 Drawing Figs. ABSTRACT: Kainite immersed in brine in equilibrium con 52) U.S. Cl........................................................ 23138, verted to carnalite by cooling to about 10 C. or under. Car 209/11, 209/166,23191, 22/121 nallite so obtained purified by cold flotation. Purified carnal (5) Int. Cl......................................................... B03b 1100, lite water leached to yield magnesium chloride brine and B03d 1102, C01f 5126 potassium chloride salt. Latter optionally converted to potas 50 Field of Search............................................ 209/166,3, sium sulfate by reaction with kainite, or by reacting the carnal 10, 11; 23.19, 38, 121 lite with kainite. Naturally occurring brine concentrated to precipitate principally sodium chloride, mother liquor warm 56 References Cited concentrated to precipitate kainite, cooled under mother UNITED STATES PATENTS liquor for conversion to carnallite. A crude kainite fraction 2,479,001 8/1949 Burke........................... 23.191 purified by warm flotation and a crude carnallite fraction pu 2,689,649 9, 1954 Atwood.... -
OCCURRENCE of BROMINE in CARNALLITE and SYLVITE from UTAH and NEW MEXICO* Manrr Loursp Lrnosonc
OCCURRENCE OF BROMINE IN CARNALLITE AND SYLVITE FROM UTAH AND NEW MEXICO* Manrr Loursp LrNosonc ABSTRACT Both carnallite and sylvite from Eddy County, New Mexico, contain 0.1 per cent of bromine. The bromine content of these minerals from Grand county, utah, is three times as great. No bromine was detected in halite, polyhalite, l5ngbeinite, or anhydrite from New Mexico. Iodine was not detected in any of these minerals. on the basis of the bromine content of the sylvite from New Mexico, it is calculated that 7,000 tons of bromine were present in potash salts mined from the permian basin during the period 1931 to 1945. INrnooucrroN The Geological Survey has previously made tests for bromine and iodine in core samples of potash salts from New Mexico.r Bromine was found to be present in very small amounts. No systematic quantitative determinations were made, nor was the presenceof bromine specificalry correlated with quantitative mineral composition. Sections of potash core from four recently drilled wells and selected pure saline minerals from Eddy County, New Mexico, together with two cores from Grand County, Utah, were therefore analyzed for their bromine and iodine content. The percentage mineral composition was then correlated with the bromine content. rt was found that bromine was restricted to carnall- ite and sylvite. fodine was not detected in any of the samples analyzed. If present, its quantity must be less than .00570. Brine and sea water are the present commercial sourcesof bromine in the United States, though both Germany and U.S.S.R. have utilized potash salts as a source of bromine. -
Anomalously High Cretaceous Paleobrine Temperatures: Hothouse, Hydrothermal Or Solar Heating?
minerals Article Anomalously High Cretaceous Paleobrine Temperatures: Hothouse, Hydrothermal or Solar Heating? Jiuyi Wang 1,2 ID and Tim K. Lowenstein 2,* 1 MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China; [email protected] 2 Department of Geological Sciences and Environmental Studies, State University of New York, Binghamton, NY 13902, USA * Correspondence: [email protected]; Tel.: +1-607-777-4254 Received: 1 November 2017; Accepted: 9 December 2017; Published: 13 December 2017 Abstract: Elevated surface paleobrine temperatures (average 85.6 ◦C) are reported here from Cretaceous marine halites in the Maha Sarakham Formation, Khorat Plateau, Thailand. Fluid inclusions in primary subaqueous “chevron” and “cumulate” halites associated with potash salts contain daughter crystals of sylvite (KCl) and carnallite (MgCl2·KCl·6H2O). Petrographic textures demonstrate that these fluid inclusions were trapped from the warm brines in which the halite crystallized. Later cooling produced supersaturated conditions leading to the precipitation of sylvite and carnallite daughter crystals within fluid inclusions. Dissolution temperatures of daughter crystals in fluid inclusions from the same halite bed vary over a large range (57.9 ◦C to 117.2 ◦C), suggesting that halite grew at different temperatures within and at the bottom of the water column. Consistency of daughter crystal dissolution temperatures within fluid inclusion bands and the absence of vapor bubbles at room temperature demonstrate that fluid inclusions have not stretched or leaked. Daughter crystal dissolution temperatures are reproducible to within 0.1 ◦C to 10.2 ◦C (average of 1.8 ◦C), and thus faithfully document paleobrine conditions. -
Potash Deposits in the Devonian Prairie Evaporite, Southwestern Manitoba Lo Eo Gic G a a L B S O U
Potash deposits in the Devonian Prairie Evaporite, southwestern Manitoba lo eo gic g a a l b s o u t r i v n e a MGS y m M.P.B. Nicolas 1928 Manitoba Geological Survey, Winnipeg, Manitoba, Canada Potash Geology 3. Esterhazy Member The Esterhazy Member is the most economic Potash Exploration potash beds. It consists of euhedral to subhedal halite 2. Regional and Local Geology crystals with large anhedral sylvite crystals and minor 1. Introduction interstitial carnolite and clays (Figure 7 and 8). In Manitoba, the Paleozoic-, Mesozoic- and Cenozoic-age strata form a basinward-thickening, southwesterly- 6. Potash Resource 7. Exploration History The Prairie Evaporite is a thick Denonian-aged evaporitic sloping wedge, with the strata reaching a total thickness of 2.3 km in the extreme southestern corner of Manitoba The Esterhazy Member is intermittently present in R29W1 R28 R27 R26 R25 R24 R23 sequence dominantly consisting of halite and anhydrite. It Legend (Figure 4). The potash-bearing Devonian-age Prairie Evaporite was deposited within the Elk Point Basin (Figure Formal mineral resource estimates have been prepared for The discovery of potash in Manitoba was in an oil well T30 a narrow, elongate strip in southwestern Manitoba, includes four potash-bearing members, from oldest to youngest N 5). The Prairie Evaporite consists mainly of thick halite beds, with minor anhydrite and four localized potash beds. the Russell deposit, most recently in 2009. A historical resource drilled in 1951 at 15-18-10-27W1. This discovery led to salt distribution WA T29 from Township 5 to 21, Ranges 27 to 29 W1 (Figure E A H B C Within the basin, the formation can exceed 210 m in thickness, and lies at depths of 200 to 2,700 m below surface. -
Assessment of the Molecular Structure of the Borate Mineral Boracite
Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy 96 (2012) 946–951 Contents lists available at SciVerse ScienceDirect Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy journal homepage: www.elsevier.com/locate/saa Assessment of the molecular structure of the borate mineral boracite Mg3B7O13Cl using vibrational spectroscopy ⇑ Ray L. Frost a, , Yunfei Xi a, Ricardo Scholz b a School of Chemistry, Physics and Mechanical Engineering, Science and Engineering Faculty, Queensland University of Technology, G.P.O. Box 2434, Brisbane, Queensland 4001, Australia b Geology Department, School of Mines, Federal University of Ouro Preto, Campus Morro do Cruzeiro, Ouro Preto, MG 35400-00, Brazil highlights graphical abstract " Boracite is a magnesium borate mineral with formula: Mg3B7O13Cl. " The crystals belong to the orthorhombic – pyramidal crystal system. " The molecular structure of the mineral has been assessed. " Raman spectrum shows that some Cl anions have been replaced with OH units. article info abstract Article history: Boracite is a magnesium borate mineral with formula: Mg3B7O13Cl and occurs as blue green, colorless, Received 23 May 2012 gray, yellow to white crystals in the orthorhombic – pyramidal crystal system. An intense Raman band Received in revised form 2 July 2012 À1 at 1009 cm was assigned to the BO stretching vibration of the B7O13 units. Raman bands at 1121, Accepted 9 July 2012 1136, 1143 cmÀ1 are attributed to the in-plane bending vibrations of trigonal boron. Four sharp Raman Available online 13 August 2012 bands observed at 415, 494, 621 and 671 cmÀ1 are simply defined as trigonal and tetrahedral borate bending modes. The Raman spectrum clearly shows intense Raman bands at 3405 and 3494 cmÀ1, thus Keywords: indicating that some Cl anions have been replaced with OH units. -
Minerals Found in Michigan Listed by County
Michigan Minerals Listed by Mineral Name Based on MI DEQ GSD Bulletin 6 “Mineralogy of Michigan” Actinolite, Dickinson, Gogebic, Gratiot, and Anthonyite, Houghton County Marquette counties Anthophyllite, Dickinson, and Marquette counties Aegirinaugite, Marquette County Antigorite, Dickinson, and Marquette counties Aegirine, Marquette County Apatite, Baraga, Dickinson, Houghton, Iron, Albite, Dickinson, Gratiot, Houghton, Keweenaw, Kalkaska, Keweenaw, Marquette, and Monroe and Marquette counties counties Algodonite, Baraga, Houghton, Keweenaw, and Aphrosiderite, Gogebic, Iron, and Marquette Ontonagon counties counties Allanite, Gogebic, Iron, and Marquette counties Apophyllite, Houghton, and Keweenaw counties Almandite, Dickinson, Keweenaw, and Marquette Aragonite, Gogebic, Iron, Jackson, Marquette, and counties Monroe counties Alunite, Iron County Arsenopyrite, Marquette, and Menominee counties Analcite, Houghton, Keweenaw, and Ontonagon counties Atacamite, Houghton, Keweenaw, and Ontonagon counties Anatase, Gratiot, Houghton, Keweenaw, Marquette, and Ontonagon counties Augite, Dickinson, Genesee, Gratiot, Houghton, Iron, Keweenaw, Marquette, and Ontonagon counties Andalusite, Iron, and Marquette counties Awarurite, Marquette County Andesine, Keweenaw County Axinite, Gogebic, and Marquette counties Andradite, Dickinson County Azurite, Dickinson, Keweenaw, Marquette, and Anglesite, Marquette County Ontonagon counties Anhydrite, Bay, Berrien, Gratiot, Houghton, Babingtonite, Keweenaw County Isabella, Kalamazoo, Kent, Keweenaw, Macomb, Manistee,