Rock and Mineral Identification for Engineers
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10-1 CHAPTER 10 DEFORMATION 10.1 Stress-Strain Diagrams And
EN380 Naval Materials Science and Engineering Course Notes, U.S. Naval Academy CHAPTER 10 DEFORMATION 10.1 Stress-Strain Diagrams and Material Behavior 10.2 Material Characteristics 10.3 Elastic-Plastic Response of Metals 10.4 True stress and strain measures 10.5 Yielding of a Ductile Metal under a General Stress State - Mises Yield Condition. 10.6 Maximum shear stress condition 10.7 Creep Consider the bar in figure 1 subjected to a simple tension loading F. Figure 1: Bar in Tension Engineering Stress () is the quotient of load (F) and area (A). The units of stress are normally pounds per square inch (psi). = F A where: is the stress (psi) F is the force that is loading the object (lb) A is the cross sectional area of the object (in2) When stress is applied to a material, the material will deform. Elongation is defined as the difference between loaded and unloaded length ∆푙 = L - Lo where: ∆푙 is the elongation (ft) L is the loaded length of the cable (ft) Lo is the unloaded (original) length of the cable (ft) 10-1 EN380 Naval Materials Science and Engineering Course Notes, U.S. Naval Academy Strain is the concept used to compare the elongation of a material to its original, undeformed length. Strain () is the quotient of elongation (e) and original length (L0). Engineering Strain has no units but is often given the units of in/in or ft/ft. ∆푙 휀 = 퐿 where: is the strain in the cable (ft/ft) ∆푙 is the elongation (ft) Lo is the unloaded (original) length of the cable (ft) Example Find the strain in a 75 foot cable experiencing an elongation of one inch. -
17. Clay Mineralogy of Deep-Sea Sediments in the Northwestern Pacific, Dsdp, Leg 20
17. CLAY MINERALOGY OF DEEP-SEA SEDIMENTS IN THE NORTHWESTERN PACIFIC, DSDP, LEG 20 Hakuyu Okada and Katsutoshi Tomita, Department of Geology, Kagoshima University, Kagoshima 890, Japan INTRODUCTION intensity of montmorillonite can be obtained by sub- tracting the (001) reflection intensity of chlorite from the Clay mineral study of samples collected during Leg 20 of preheating or pretreating reflection intensity at 15 Å. the Deep Sea Drilling Project in the western north Pacific In a specimen with coexisting kaolinite and chlorite, was carried out mainly by means of X-ray diffraction their overlapping reflections make it difficult to determine analyses. Emphasis was placed on determining vertical quantitatively these mineral compositions. For such speci- changes in mineral composition of sediments at each site. mens Wada's method (Wada, 1961) and heat treatment Results of the semiquantitative and quantitative deter- were adopted. minations of mineral compositions of analyzed samples are The following shows examples of the determination of shown in Tables 1, 2, 3, 5, and 7. The mineral suites some intensity ratios of reflections of clay minerals. presented here show some unusual characters as discussed below. The influence of burial diagenesis is also evidenced Case 1 in the vertical distribution of some authigenic minerals. Montmorillonite (two layers of water molecules between These results may contribute to a better understanding silicate layers)—kaolinite mixture. of deep-sea sedimentation on the northwestern Pacific This is the situation in which samples contain both plate. montmorillonite and kaolinite. The first-order basal reflec- tions of these minerals do not overlap. When the (002) ANALYTICAL PROCEDURES reflection of montmorillonite, which appears at about 7 Å, Each sample was dried in air, and X-ray diffraction is absent or negligible, the intensity ratio is easily obtained. -
Lord Lyon King of Arms
VI. E FEUDAE BOBETH TH F O LS BABONAG F SCOTLANDO E . BY THOMAS INNES OP LEABNEY AND KINNAIRDY, F.S.A.ScoT., LORD LYON KIN ARMSF GO . Read October 27, 1945. The Baronage is an Order derived partly from the allodial system of territorial tribalis whicn mi patriarce hth h hel s countrydhi "under God", d partlan y froe latemth r feudal system—whic e shale wasw hse n li , Western Europe at any rate, itself a developed form of tribalism—in which the territory came to be held "of and under" the King (i.e. "head of the kindred") in an organised parental realm. The robes and insignia of the Baronage will be found to trace back to both these forms of tenure, which first require some examination from angle t usuallno s y co-ordinatedf i , the later insignia (not to add, the writer thinks, some of even the earlier understoode symbolsb o t e )ar . Feudalism has aptly been described as "the development, the extension organisatione th y sa y e Family",o familyth fma e oe th f on n r i upon,2o d an Scotlandrelationn i Land;e d th , an to fundamentall o s , tribaa y l country, wher e predominanth e t influences have consistently been Tribality and Inheritance,3 the feudal system was immensely popular, took root as a means of consolidating and preserving the earlier clannish institutions,4 e clan-systeth d an m itself was s modera , n historian recognisew no s t no , only closely intermingled with feudalism, but that clan-system was "feudal in the strictly historical sense".5 1 Stavanger Museums Aarshefle, 1016. -
Transportation Vehicle Light-Weighting with Polymeric Glazing and Mouldings
GCEP Final Report for Advanced Transportation Transportation Vehicle Light-Weighting with Polymeric Glazing and Mouldings Investigators Reinhold H. Dauskardt, Professor; Yichuan Ding, Graduate Researcher; Siming Dong, Graduate Researcher; Dongjing He, Summer student; Material Science and Engineering, Stanford University. Abstract Polymeric glazing and mouldings are an extremely high “want” from the transportation community, enabling more creative designs as well as improved part consolidation。 However, plastic windows and mouldings must have high-performance and low-cost protective coating systems with lifetimes in excess of 10 years. Current polymeric glazings do not meet durability/performance requirements for near-term implementation. Our project targets new coating system manufacturing to address durability and cost issues necessary to meet or exceed transportation engineering requirements. Atmospheric plasma deposition (APD) is an emerging technique that enables plasma deposition of coatings on large and/or complex geometry substrates in ambient air without the need for expensive vacuum or inert manufacturing platforms. It is an environmentally friendly and solvent-free technique, minimizing chemical waste throughout the process as well as greenhouse gas emissions when compared to current wet chemistry aqueous sol-gel manufacturing techniques. Low deposition temperatures (<50°C) allows the deposition on plastic and organic substrates. Using our state-of-the-art APD coating capabilities, we have demonstrated the ability to deposit highly transparent bilayer organosilicate coatings with superior combinations of elastic modulus and adhesion compared to commercial sol-gel coatings. The bilayer is deposited on large substrates by atmospheric plasma, in ambient air, at room temperature, in a one-step process, using a single inexpensive precursor. The significantly improved elastic modulus translates into improved durability and resistance to scratching and environmental degradation. -
Download PDF About Minerals Sorted by Mineral Name
MINERALS SORTED BY NAME Here is an alphabetical list of minerals discussed on this site. More information on and photographs of these minerals in Kentucky is available in the book “Rocks and Minerals of Kentucky” (Anderson, 1994). APATITE Crystal system: hexagonal. Fracture: conchoidal. Color: red, brown, white. Hardness: 5.0. Luster: opaque or semitransparent. Specific gravity: 3.1. Apatite, also called cellophane, occurs in peridotites in eastern and western Kentucky. A microcrystalline variety of collophane found in northern Woodford County is dark reddish brown, porous, and occurs in phosphatic beds, lenses, and nodules in the Tanglewood Member of the Lexington Limestone. Some fossils in the Tanglewood Member are coated with phosphate. Beds are generally very thin, but occasionally several feet thick. The Woodford County phosphate beds were mined during the early 1900s near Wallace, Ky. BARITE Crystal system: orthorhombic. Cleavage: often in groups of platy or tabular crystals. Color: usually white, but may be light shades of blue, brown, yellow, or red. Hardness: 3.0 to 3.5. Streak: white. Luster: vitreous to pearly. Specific gravity: 4.5. Tenacity: brittle. Uses: in heavy muds in oil-well drilling, to increase brilliance in the glass-making industry, as filler for paper, cosmetics, textiles, linoleum, rubber goods, paints. Barite generally occurs in a white massive variety (often appearing earthy when weathered), although some clear to bluish, bladed barite crystals have been observed in several vein deposits in central Kentucky, and commonly occurs as a solid solution series with celestite where barium and strontium can substitute for each other. Various nodular zones have been observed in Silurian–Devonian rocks in east-central Kentucky. -
(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. -
Correlation of Hardness Values to Tensile Strength
Correlation of Hardness Values to Tensile Strength Semih Genculu, P.E. Various procedures and approaches are utilized to determine if a given material is suitable for a certain application. The material may be tested for its ability to deform satisfactorily during a forming operation, or perhaps for its ability to operate under a certain stress level at high temperatures. For technological purposes, economy and ease of testing are important factors. Hardness tests: In many cases it is possible to substitute for the relatively time consuming and costly tensile test with a more convenient test of the plastic deformation behavior of metals, a hardness test. Hardness is defined as resistance of a material to penetration of its surface, and the majority of commercial hardness testers force a small penetrator (indenter) into the metal by means of an applied load. A definite value is obtained as the hardness of the metal, and this number can be related to the tensile strength of the metal. In the Rockwell test, hardness is measured by the depth to which the penetrator moves under a fixed load. The elastic component of the deformation is subtracted from the total movement. In the Brinell and Vickers/Knoop scales, on the other hand, the hardness is measured by dividing the load by the area of an indentation formed by pressing the corresponding indenters into the metal. Therefore while the Rockwell number is read directly from a gage, which is part of the tester, the Brinell and Vickers/Knoop require optical measurements of the diameters or diagonals, respectively. While all indentation hardness tests may be thought to serve the same purpose, each one has definite advantages with some being more applicable to certain types of materials and size and shape parts than the others. -
Mineralogy, Fluid Inclusion, and Stable Isotope Studies of the Hog Heaven Mining District, Flathead County, Montana
Montana Tech Library Digital Commons @ Montana Tech Graduate Theses & Non-Theses Student Scholarship Spring 2020 MINERALOGY, FLUID INCLUSION, AND STABLE ISOTOPE STUDIES OF THE HOG HEAVEN MINING DISTRICT, FLATHEAD COUNTY, MONTANA Ian Kallio Follow this and additional works at: https://digitalcommons.mtech.edu/grad_rsch Part of the Geological Engineering Commons MINERALOGY, FLUID INCLUSION, AND STABLE ISOTOPE STUDIES OF THE HOG HEAVEN MINING DISTRICT, FLATHEAD COUNTY, MONTANA by Ian Kallio A thesis submitted in partial fulfillment of the requirements for the degree of Masters of Science in Geoscience Geology Option Montana Tech 2020 ii Abstract The Hog Heaven mining district in northwestern Montana is unique in that it is a high- sulfidation epithermal system containing high Ag-Pb-Zn relative to Au-Cu, with a very high Ag to Au ratio (2,330:1). The deposits are hosted within the Cenozoic Hog Heaven volcanic field (HHVF), a 30 to 36 Ma suite that consists predominantly of rhyodacite flow-dome complexes and pyroclastic rocks. The HHVF is underlain by shallow-dipping siliclastic sediments of the Mesoproterozoic Belt Supergroup. These sediments are known to host important SEDEX (e.g., Sullivan) and red-bed copper (e.g., Spar Lake, Rock Creek, Montanore) deposits rich in Ag-Pb- Zn-Cu-Ba. The HHVF erupted through and deposited on the Belt strata during a period of Oligocene extension. Outcrops and drill core samples from Hog Heaven show alteration patterns characteristic of volcanic-hosted, high-sulfidation epithermal deposits. Vuggy quartz transitions laterally into quartz-alunite alteration where large sanidine phenocrysts (up to 4 cm) have been replaced by fine-grained, pink alunite, and/or argillic alteration that is marked by an abundance of white kaolinite-dickite clay. -
Geologic Map of the Simcoe Mountains Volcanic Field, Main Central Segment, Yakama Nation, Washington by Wes Hildreth and Judy Fierstein
Prepared in Cooperation with the Water Resources Program of the Yakama Nation Geologic Map of the Simcoe Mountains Volcanic Field, Main Central Segment, Yakama Nation, Washington By Wes Hildreth and Judy Fierstein Pamphlet to accompany Scientific Investigations Map 3315 Photograph showing Mount Adams andesitic stratovolcano and Signal Peak mafic shield volcano viewed westward from near Mill Creek Guard Station. Low-relief rocky meadows and modest forested ridges marked by scattered cinder cones and shields are common landforms in Simcoe Mountains volcanic field. Mount Adams (elevation: 12,276 ft; 3,742 m) is centered 50 km west and 2.8 km higher than foreground meadow (elevation: 2,950 ft.; 900 m); its eruptions began ~520 ka, its upper cone was built in late Pleistocene, and several eruptions have taken place in the Holocene. Signal Peak (elevation: 5,100 ft; 1,555 m), 20 km west of camera, is one of largest and highest eruptive centers in Simcoe Mountains volcanic field; short-lived shield, built around 3.7 Ma, is seven times older than Mount Adams. 2015 U.S. Department of the Interior U.S. Geological Survey Contents Introductory Overview for Non-Geologists ...............................................................................................1 Introduction.....................................................................................................................................................2 Physiography, Environment, Boundary Surveys, and Access ......................................................6 Previous Geologic -
The Oxidation Ratio of Iron in Coexisting Biotite And
1423 The Canadian Mineralo gist Vol.37. pp. 1423-1429(1999\ THE OXIDATIONRATIO OF IRON IN COEXISTINGBIOTITE AND HORNBLENDEFROM GRANITICAND METAMORPHICROCKS: THE ROLE OF P, T AND f(O2) NADINES. BORODINA, GERMAN B. FERSHTATER$erro SERGEI L. VOTYAKOV Institute of Geology and Geochemistry, RussianAcademy of Sciences,Pochtoty per., 7, Eknterinburg, 620151, Russia Assrnecr Previously published and new data on the composition of coexisting biotite and homblende from granitic and metamorphic rocks show that the degree of iron oxidation, R [= Fe3*/(Fe2*+ Fe3*)], is different in these two minerals; the R of hornblende is greater. Granulite-facies minerals have the greatest difference in R, whereas in granitic rocks, those minerals show the least difference The oxidation of biotite and hornblende under high-level conditions is accompaniedby the crystallization of magnet- ite, and newly formed oxidized mafic minerals have a lower Fe/(Fe + Mg) and R than the original ones. Under mesozonal and catazonalconditions, the increasein pressureprevents the formation of magnetite, and oxidation is accompaniedby a significant increase in R; these changes in the chemical composition of hornblende are supplementedby an increase in Al. Since the Al content of homblende is known to be an indicator of pressure, such a correlation of R and Fer+ content with aluminum content points to an increaseof theseparameters with a rise of pressure Keywords:biotite, hornblende,oxidation ratio, granitic rocks, metamorphic rocks, epizonal plutons, mesozonalplutons , cat^7'onal plutons. Sorravarnr, Les donn6esnouvelles et celles tirde de la litt6rature portant sur 1acomposition de la biotite et celle de la hornblendecoexistante des roches granitiques et m6tamorphiquesmontrent qui le degrd d'oxydation du fer, R [= Fe3*/(Fe2*+ Fe3+)],est diffdrent dans ces deux mindraux. -
(2000), Voluminous Lava-Like Precursor to a Major Ash-Flow
Journal of Volcanology and Geothermal Research 98 (2000) 153–171 www.elsevier.nl/locate/jvolgeores Voluminous lava-like precursor to a major ash-flow tuff: low-column pyroclastic eruption of the Pagosa Peak Dacite, San Juan volcanic field, Colorado O. Bachmanna,*, M.A. Dungana, P.W. Lipmanb aSection des Sciences de la Terre de l’Universite´ de Gene`ve, 13, Rue des Maraıˆchers, 1211 Geneva 4, Switzerland bUS Geological Survey, 345 Middlefield Rd, Menlo Park, CA, USA Received 26 May 1999; received in revised form 8 November 1999; accepted 8 November 1999 Abstract The Pagosa Peak Dacite is an unusual pyroclastic deposit that immediately predated eruption of the enormous Fish Canyon Tuff (ϳ5000 km3) from the La Garita caldera at 28 Ma. The Pagosa Peak Dacite is thick (to 1 km), voluminous (Ͼ200 km3), and has a high aspect ratio (1:50) similar to those of silicic lava flows. It contains a high proportion (40–60%) of juvenile clasts (to 3–4 m) emplaced as viscous magma that was less vesiculated than typical pumice. Accidental lithic fragments are absent above the basal 5–10% of the unit. Thick densely welded proximal deposits flowed rheomorphically due to gravitational spreading, despite the very high viscosity of the crystal-rich magma, resulting in a macroscopic appearance similar to flow- layered silicic lava. Although it is a separate depositional unit, the Pagosa Peak Dacite is indistinguishable from the overlying Fish Canyon Tuff in bulk-rock chemistry, phenocryst compositions, and 40Ar/39Ar age. The unusual characteristics of this deposit are interpreted as consequences of eruption by low-column pyroclastic fountaining and lateral transport as dense, poorly inflated pyroclastic flows. -
Lts Ficez 5Coz7'a1ra
ltS FicEz 5coZ7'a1ra he most valuable gem- Gem-quality red beryl on quality red beryl comes white devitri- from thc Wah Wah fied rhyolite Mountains of south- matrix. This western Utah (Fig. 1). sample mea- Red beryl occurs as a secondary sures 9 x 26 mm (O.35 x 1 mineral in topaz rhyolite. Market- in.l. (Photo by able crystals from the Wah Wah Sky Hall.) Mountains have been produced from the Violet Mine, operated on a limited scale since 1976 under the ownership of the Harris family of Delta, UT. From 1989 to 1995. oroduction from the mine amounted to more than $3 million with an inventory of several million dollars of unsold gems (Harris, 1995). In 7994, Kennecott Exploration leased the mine and surrounding claims to de- termine reserves and feasibility of gem recovery. Mining and explora- E.H. Christiansen and tion activity are continuing. J.D. Keith are proles- Previous work on red beryl has s0rs arld T.J. dealt mainly with crystallographic, Thompson is a student, chemical and optical properties of the crystals (Shigley and Foord, Ieparlment of Geohgy, 1984) with only general descriptions Brigham Yrung Univer- of the geology (Ream, 1979). How- sitt Brx 251 I l, Prlvn, ever. the conditions needed for for- mation of red beryl have not been UT 84fi[2 well constrained. It is generally pro- posed that beryl originates by pre- cipitation in fractures and vugs from high-temperature silica rhyolite and andesitic lava flows. gases as they are released from slowly cooled rhyolite Beginning about 23 Ma, the style and composition of lava.