What Are Minerals
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(WHO) Report on Microplastics in Drinking Water
Microplastics in drinking-water Microplastics in drinking-water ISBN 978-92-4-151619-8 © World Health Organization 2019 Some rights reserved. This work is available under the Creative Commons Attribution-NonCommercial-ShareAlike 3.0 IGO licence (CC BY-NC-SA 3.0 IGO; https://creativecommons.org/licenses/by-nc-sa/3.0/igo). Under the terms of this licence, you may copy, redistribute and adapt the work for non-commercial purposes, provided the work is appropriately cited, as indicated below. In any use of this work, there should be no suggestion that WHO endorses any specific organization, products or services. The use of the WHO logo is not permitted. If you adapt the work, then you must license your work under the same or equivalent Creative Commons licence. If you create a translation of this work, you should add the following disclaimer along with the suggested citation: “This translation was not created by the World Health Organization (WHO). WHO is not responsible for the content or accuracy of this translation. The original English edition shall be the binding and authentic edition”. Any mediation relating to disputes arising under the licence shall be conducted in accordance with the mediation rules of the World Intellectual Property Organization. Suggested citation. Microplastics in drinking-water. Geneva: World Health Organization; 2019. Licence: CC BY-NC-SA 3.0 IGO. Cataloguing-in-Publication (CIP) data. CIP data are available at http://apps.who.int/iris. Sales, rights and licensing. To purchase WHO publications, see http://apps.who.int/bookorders. To submit requests for commercial use and queries on rights and licensing, see http://www.who.int/about/licensing. -
Minerals in Your Home Activity Book Minerals in Your Home Activity Book
Minerals In Your Home Activity Book Minerals in Your Home Activity Book Written by Ann-Thérèse Brace, Sheila Stenzel, and Andreea Suceveanu Illustrated by Heather Brown Minerals in Your Home is produced by MineralsEd. © 2017 MineralsEd (Mineral Resources Education Program of BC) 900-808 West Hastings St., Vancouver, BC V6C 2X4 Canada Tel. (604) 682-5477 | Fax (604) 681-5305 | Website: www.MineralsEd.ca Introduction As you look around your home, it is important to think of the many things that you have and what are they made from. It’s simple - everything is made from Earth’s natural resources: rocks, soil, plants, animals, and water. They can be used in their natural state, or processed, refined and manufactured by people into other useable things. The resources that grow and can be replaced when they die or are harvested, like plants and animals, are called renewable resources. Those that cannot be regrown and replaced, like rocks, soil and water, are called non-renewable resources. All natural resources are valuable and we must use them conservatively. Mineral resources are natural Earth materials that must be mined from the ground. We use them every day, and they are non- renewable. Some are changed very little before they are used, like the rock granite for example, that is commonly used to make kitchen countertops or tombstones. Other mineral resources, like those that contain useful metals, must be processed to extract the metal ingredient. The metal is then manufactured into different parts of a product, like a toaster or a smartphone. Whether you are practicing violin in your room, eating a meal in the kitchen, watching TV in the living room or brushing your teeth in the bathroom, your daily activities use things that come from mineral resources. -
40 Common Minerals and Their Uses
40 Common Minerals and Their Uses Aluminum Beryllium The most abundant metal element in Earth’s Used in the nuclear industry and to crust. Aluminum originates as an oxide called make light, very strong alloys used in the alumina. Bauxite ore is the main source aircraft industry. Beryllium salts are used of aluminum and must be imported from in fluorescent lamps, in X-ray tubes and as Jamaica, Guinea, Brazil, Guyana, etc. Used a deoxidizer in bronze metallurgy. Beryl is in transportation (automobiles), packaging, the gem stones emerald and aquamarine. It building/construction, electrical, machinery is used in computers, telecommunication and other uses. The U.S. was 100 percent products, aerospace and defense import reliant for its aluminum in 2012. applications, appliances and automotive and consumer electronics. Also used in medical Antimony equipment. The U.S. was 10 percent import A native element; antimony metal is reliant in 2012. extracted from stibnite ore and other minerals. Used as a hardening alloy for Chromite lead, especially storage batteries and cable The U.S. consumes about 6 percent of world sheaths; also used in bearing metal, type chromite ore production in various forms metal, solder, collapsible tubes and foil, sheet of imported materials, such as chromite ore, and pipes and semiconductor technology. chromite chemicals, chromium ferroalloys, Antimony is used as a flame retardant, in chromium metal and stainless steel. Used fireworks, and in antimony salts are used in as an alloy and in stainless and heat resisting the rubber, chemical and textile industries, steel products. Used in chemical and as well as medicine and glassmaking. -
The Rutile Deposits of the Eastern United States
THE RUTILE DEPOSITS OF THE EASTERN UNITED STATES. By THOMAS L. WATSON. INTRODUCTION. The titanium-bearing minerals comprise more than 60 distinct species, grouped under a variety of mineral and chemical forms, chiefly as oxides, titanates, titano-silicates, silicates, columbates, and iantalates. These minerals are widely distributed in a variety of associations and in such quantity as to make titanium a relatively abundant element. Clarke* estimates the. amount of titanium in the solid crust of the earth to be 0.44 per cent, equivalent in oxide to 0.73 per cent, the element thus standing in the ninth place in the scale of abundance, next to potassium. Most of the titanium-bearing minerals, however, are rare and are only of scientific interest. The largest concentrations of the element are as oxide (rutile), as iron titanate (ilmenite), and in iron ferrate (magnetite) as intergrown ilmenite. Of these three forms the prin cipal source of the element at present is rutile. The known workable deposits of rutile, however, are extremely few and widely sepa rated, and as the demand for titanium has greatly increased in the last few years it has been necessary for some uses to turn to ilmenite or highly titaniferous magnetites. This paper briefly summarizes present knowledge of the geology of the rutile deposits in the eastern United States and for the sake of comparison discusses several foreign deposits, each of which has produced some rutile. Of the known deposits in the United, States only those in Virginia are of commercial importance. These have been made the subject of a special report 2 by the Virginia Geological Survey, which was preceded by a preliminary paper on the rutile deposits of Amherst and Nelson counties.3 1 Clarke, F. -
Mineral Collecting Sites in North Carolina by W
.'.' .., Mineral Collecting Sites in North Carolina By W. F. Wilson and B. J. McKenzie RUTILE GUMMITE IN GARNET RUBY CORUNDUM GOLD TORBERNITE GARNET IN MICA ANATASE RUTILE AJTUNITE AND TORBERNITE THULITE AND PYRITE MONAZITE EMERALD CUPRITE SMOKY QUARTZ ZIRCON TORBERNITE ~/ UBRAR'l USE ONLV ,~O NOT REMOVE. fROM LIBRARY N. C. GEOLOGICAL SUHVEY Information Circular 24 Mineral Collecting Sites in North Carolina By W. F. Wilson and B. J. McKenzie Raleigh 1978 Second Printing 1980. Additional copies of this publication may be obtained from: North CarOlina Department of Natural Resources and Community Development Geological Survey Section P. O. Box 27687 ~ Raleigh. N. C. 27611 1823 --~- GEOLOGICAL SURVEY SECTION The Geological Survey Section shall, by law"...make such exami nation, survey, and mapping of the geology, mineralogy, and topo graphy of the state, including their industrial and economic utilization as it may consider necessary." In carrying out its duties under this law, the section promotes the wise conservation and use of mineral resources by industry, commerce, agriculture, and other governmental agencies for the general welfare of the citizens of North Carolina. The Section conducts a number of basic and applied research projects in environmental resource planning, mineral resource explora tion, mineral statistics, and systematic geologic mapping. Services constitute a major portion ofthe Sections's activities and include identi fying rock and mineral samples submitted by the citizens of the state and providing consulting services and specially prepared reports to other agencies that require geological information. The Geological Survey Section publishes results of research in a series of Bulletins, Economic Papers, Information Circulars, Educa tional Series, Geologic Maps, and Special Publications. -
Chapter 2 the Solid Materials of the Earth's Surface
CHAPTER 2 THE SOLID MATERIALS OF THE EARTH’S SURFACE 1. INTRODUCTION 1.1 To a great extent in this course, we will be dealing with processes that act on the solid materials at and near the Earth’s surface. This chapter might better be called “the ground beneath your feet”. This is the place to deal with the nature of the Earth’s surface materials, which in later sections of the chapter I will be calling regolith, sediment, and soil. 1.2 I purposely did not specify any previous knowledge of geology as a prerequisite for this course, so it is important, here in the first part of this chapter, for me to provide you with some background on Earth materials. 1.3 We will be dealing almost exclusively with the Earth’s continental surfaces. There are profound geological differences between the continents and the ocean basins, in terms of origin, age, history, and composition. Here I’ll present, very briefly, some basic things about geology. (For more depth on such matters you would need to take a course like “The Earth: What It Is, How It Works”, given in the Harvard Extension program in the fall semester of 2005– 2006 and likely to be offered again in the not-too-distant future.) 1.4 In a gross sense, the Earth is a layered body (Figure 2-1). To a first approximation, it consists of concentric shells: the core, the mantle, and the crust. Figure 2-1: Schematic cross section through the Earth. 73 The core: The core consists mostly of iron, alloyed with a small percentage of certain other chemical elements. -
Minerals for Livestock
Station BulIetn 503 October 1951 Minerals for Livestock J. R. Haag Agrkultural Experiment Station Oregon State College Corvallis Foreword Oregon livestock producers are aware of the need for additional information on the use of mineral sup- plements.These materials frequently are purchased when not needed with the particular rations that are being used.The intelligent use of minerals pays divi- dends.Over-use may be harmful. This bulletin has been revised to give livestock pro- ducers and feed dealers the latest available information that will assist them in selecting and feeding only such materials as may be needed to supplement the natural supply already available in their feedstuffs. Although noteworthy progress is being made we believe that research must be intensified in Oregon to provide more complete information on the adequacy of minerals in feed produced in the various areas of the State.Evidence being accumulated by our research staff indicates that deficiencies peculiar to certain areas are causing serious losses among livestock. Dean and Director Minerals for Livestock By J. R. HAAG, Chemist (Animal Nutrition) Oregon State College animals require an abundance of palatable feedstuffs as a FARMsource of energy, fats, proteins, minerals, and vitamins.These feedstuffs must be suitable for the kind of livestock maintained and, in addition, must be available at a cost that will permit profitable livestock production. The mineral salts constitute only one of the groups of nutrients that play important parts in animal nutrition.Some mineral ele- ments, like calcium and phosphorus, are needed in large amounts, while others, like iodine, are required only invery minute traces. -
13. Nutrient Minerals in Drinking Water: Implications for the Nutrition
13. NUTRIENT MINERALS IN DRINKING WATER: IMPLICATIONS FOR THE NUTRITION OF INFANTS AND YOUNG CHILDREN Erika Sievers Institute of Public Health North Rhine Westphalia Munster, Germany ______________________________________________________________________________ I. INTRODUCTION The WHO Global Strategy on Infant and Young Child Feeding emphasizes the importance of infant feeding and promotes exclusive breastfeeding in the first six months of life. In infants who cannot be breast-fed or should not receive breast milk, substitutes are required. These should be a formula that complies with the appropriate Codex Alimentarius Standards or, alternatively, a home-prepared formula with micronutrient supplements (1). Drinking water is indispensable for the reconstitution of powdered infant formulae and needed for the preparation of other breast-milk substitutes. As a result of the long-term intake of a considerable volume in relation to body weight, the concentrations of nutrient minerals in drinking water may contribute significantly to the total trace element and mineral intake of infants and young children. This is especially applicable to formula-fed infants during the first months of life, who may be the most vulnerable group affected by excessive concentrations of nutrients or contaminants in drinking water. Defining essential requirements of the composition of infant formulae, the importance of the quality of the water used for their reconstitution has been acknowledged by the Scientific Committee on Food, SCF, of the European Commission (2). Although it was noted that the mineral content of water may vary widely depending upon its source, the optimal composition remained undefined. Recommendations for the composition of infant formulae refer to total nutrient content as prepared ready for consumption according to manufacturer’s instructions. -
The Seven Crystal Systems
Learning Series: Basic Rockhound Knowledge The Seven Crystal Systems The seven crystal systems are a method of classifying crystals according to their atomic lattice or structure. The atomic lattice is a three dimensional network of atoms that are arranged in a symmetrical pattern. The shape of the lattice determines not only which crystal system the stone belongs to, but all of its physical properties and appearance. In some crystal healing practices the axial symmetry of a crystal is believed to directly influence its metaphysical properties. For example crystals in the Cubic System are believed to be grounding, because the cube is a symbol of the element Earth. There are seven crystal systems or groups, each of which has a distinct atomic lattice. Here we have outlined the basic atomic structure of the seven systems, along with some common examples of each system. Cubic System Also known as the isometric system. All three axes are of equal length and intersect at right angles. Based on a square inner structure. Crystal shapes include: Cube (diamond, fluorite, pyrite) Octahedron (diamond, fluorite, magnetite) Rhombic dodecahedron (garnet, lapis lazuli rarely crystallises) Icosi-tetrahedron (pyrite, sphalerite) Hexacisochedron (pyrite) Common Cubic Crystals: Diamond Fluorite Garnet Spinel Gold Pyrite Silver Tetragonal System Two axes are of equal length and are in the same plane, the main axis is either longer or shorter, and all three intersect at right angles. Based on a rectangular inner structure. Crystal shapes include: Four-sided prisms and pyramids Trapezohedrons Eight-sided and double pyramids Icosi-tetrahedron (pyrite, sphalerite) Hexacisochedron (pyrite) Common Tetragonal Crystals: Anatase Apophyllite Chalcopyrite Rutile Scapolite Scheelite Wulfenite Zircon Hexagonal System Three out of the four axes are in one plane, of the same length, and intersect each other at angles of 60 degrees. -
Scandium Mineralization Associated with Hydrothermal Lazulite-Quartz Veins in the Lower Austroalpine Grobgneis Complex, Eastern Alps, Austria
Bernhard, F. (2001): Scandium mineralization associated with hydrothermal lazulite-quartz veins in the Lower Austroalpine Grobgneis complex, Eastern Alps, Austria. In: Piestrzynski A. et al. (eds.): Mineral Deposits at the Beginning of the 21st Century. Proceedings of the joint sixth biennial SGA-SEG meeting. Kraków, Poland. A.A.Balkema Publishers, 935-938. Scandium mineralization associated with hydrothermal lazulite-quartz veins in the Lower Austroalpine Grobgneis complex, Eastern Alps, Austria F. Bernhard Institut für Technische Geologie und Angewandte Mineralogie, Technische Universität Graz, Rechbauerstraße 12, A-8010 Graz, Austria ABSTRACT: Lazulite (MgAl2(PO4)2(OH)2)-quartz veins within the Lower Austroalpine Grobgneis complex, Austria, have Sc-contents up to 200 ppm. The predominant Sc-carrier is pretulite, ScPO4, and this phase oc- curs as a wide-spread accessory mineral. Vein formation took place at temperatures of 300-500° C and low pressure during Permo-Triassic extensional tectonics and fluid flow. Mg-enriched alteration zones suggest that vein material was not derived from the immediate host rocks. Eo-Alpine metamorphism and deformation overprinted the veins to varying degrees. Despite the low tonnage of the Sc-rich veins, this new type of Sc- mineralization may point to larger Sc-accumulations in similar phosphate-rich hydrothermal environments. 1 INTRODUCTION The long-known lazulite (MgAl2(PO4)2(OH)2)- quartz veins in northeastern Styria and southern Scandium is a moderately abundant transition ele- Lower Austria contain significant Sc-enrichments in ment with an average content ca. 7 ppm in the upper the form of pretulite, ScPO4 (Bernhard et al. 1998b). and ca. 25 ppm in the lower continental crust (We- This contribution gives data on the geology, miner- depohl 1995). -
Compositional Asymmetry in Replacement Tourmaline – an Example from the Tauern Window, Eastern Alps
Geological Volume 4 Number 2 Mater ials August 12, 2002 Researc h Compositional asymmetry in replacement tourmaline – An example from the Tauern Window, Eastern Alps Darrell J. Henry1, Barbara L. Dutrow2 and Jane Selverstone3 1, 2Department of Geology and Geophysics, Louisiana State University, Baton Rouge, Louisiana 70808, USA 1<[email protected]>, 2<[email protected]>, 3Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA 3<[email protected] > Abstract Tourmaline, partially replacing pre-existing tourmaline from a tectonically-dismembered tourmalinite vein, has developed distinctive compositional asymmetry that reflects influx of reac- tive fluids. The tourmalinite clast, enclosed in a quartzite from the Tauern Window, Eastern Alps, experienced a clockwise P-T-t path with maximal burial depths of 35-40 km (10-11 kbar), peak temperatures of ~550°C and major deformation preceding peak thermal conditions. The primary tourmaline of the tourmalinite clast, generation-1, is texturally and compositionally heterogeneous, ranging from schorl to dravite [Mg / (Mg + Fe) = 0.27 - 0.61] with highly-variable Al consistent X X with combinations of the Al(NaR)-1 and AlO(R(OH))-1 exchange vectors, where represents X-site vacancy and R is Fe2+ + Mn + Mg. Generation-2 tourmaline is manifest as distinctive compo- sitionally-asymmetric bands of colorless foitite (zone 1) and blue schorl (zone 2) replacing genera- tion-1 tourmaline. Replacement takes place along a scalloped margin and advances preferentially towards the analogous pole (-c) of generation-1 tourmaline. The two zones of generation-2 range from foitite to schorl with a restricted ratio of Mg / (Mg + Fe) of 0.32 - 0.41, but with variable X, X Al, Na and R predominantly reflecting Al(NaR)-1. -
Mineral Materials from BLM-Administered Federal Lands
How to Obtain Mineral Materials From BLM-Administered Federal Lands Including Stone, Sand and Gravel, Clay, and Other Materials Introduction The Department of the Interior‘s Bureau of Land Man- agement (BLM) is a multiple-use land management agency responsible for administering 262 million acres of public land located primarily in the western United States, including Alaska. The BLM manages many resource programs, such as minerals, forestry, wilderness, recreation, fisheries and wildlife, wild horses and burros, archaeology, and range- land. This brochure con- tains information about the mineral materials program. Mineral materi- als include common vari- eties of sand, stone, gravel, pumice, pumicite, clay, rock, and petrified Concrete and asphalt aggregate (crushed stone) used for airport wood. The major Federal runways, highways, bridges, and high-rise buildings. law governing mineral materials is the Materials Act of 1947 (July 31, 1947), as amended (30 U.S. Code 601 et seq.). This law authorizes the BLM to sell mineral materials at fair market value and to grant free-use permits for mineral materials to Government agencies. It also allows the BLM to issue free-use permits for a limited amount of material to nonprofit organizations. How Are Mineral Materials Important to Our Society? Mineral materials are among our most basic natural resources. These materials are in everyday construction, agriculture, and decorative applications (Table 1). The United States uses about 2 billion tons of crushed stone, dimension stone, and sand and gravel every year. Our highways, bridges, power plants, dams, high-rise buildings, railroad beds, and airport runways, along with their foundations and sidewalks, all use mineral materials of one type or another.