Garbiles, Mary Jean D. Bsae-4M Materials of Engineering
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Evaluation of the Energy Performance of Glazing Systems and Fenestration Retrofit Solutions
The Pennsylvania State University The Graduate School College of Engineering EVALUATION OF THE ENERGY PERFORMANCE OF GLAZING SYSTEMS AND FENESTRATION RETROFIT SOLUTIONS A Thesis in Architectural Engineering by Timothy M. Ariosto ©2013 Timothy M. Ariosto Submittal in Partial Fulfillment of the Requirements for the Degree of Master of Science December 2013 The thesis of Timothy M. Ariosto was reviewed and approved* by the following: Ali M. Memari Professor of Architectural Engineering and Civil and Environmental Engineering Thesis Advisor M. Kevin Parfitt Associate Professor of Architectural Engineering Stephen Treado Associate Professor of Architectural Engineering Chimay Anumba Professor of Architectural Engineering Head of the Department of Architectural Engineering *Signatures are on file in the Graduate School ii ABSTRACT The 2011 Building Energy Databook (DOE, 2011) reported that buildings use approximately 40% of the nation’s total energy use. Residential buildings use 54% of this energy while commercial buildings use 46%. By improving the performance of building envelope components, building owners can substantially reduce their energy use. Since fenestration systems are thermally the weakest link in the building envelope, they are a logical place to seek improvements. Building owners, therefore, have two primary methods of reducing energy use. The first is by replacing inefficient single glazed window units with their newer, energy efficient counterparts. The second is to utilize window retrofit solutions, such as blinds, shutters, and curtains, in order to improve the performance of their existing systems. This thesis describes two studies conducted with the goal of aiding residential and small- scale-commercial building owners select appropriate glazing systems and window retrofit solutions. -
Origin and Character of Loesslike Silt in the Southern Qinghai-Xizang (Tibet) Plateau, China
Origin and Character of Loesslike Silt in the Southern Qinghai-Xizang (Tibet) Plateau, China U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1549 Cover. View south-southeast across Lhasa He (Lhasa River) flood plain from roof of Potala Pal ace, Lhasa, Xizang Autonomous Region, China. The Potala (see frontispiece), characteristic sym bol of Tibet, nses 308 m above the valley floor on a bedrock hill and provides an excellent view of Mt. Guokalariju, 5,603 m elevation, and adjacent mountains 15 km to the southeast These mountains of flysch-like Triassic clastic and volcanic rocks and some Mesozoic granite character ize the southernmost part of Northern Xizang Structural Region (Gangdese-Nyainqentanglha Tec tonic Zone), which lies just north of the Yarlung Zangbo east-west tectonic suture 50 km to the south (see figs. 2, 3). Mountains are part of the Gangdese Island Arc at south margin of Lhasa continental block. Light-tan areas on flanks of mountains adjacent to almost vegetation-free flood plain are modern and ancient climbing sand dunes that exhibit evidence of strong winds. From flood plain of Lhasa He, and from flood plain of much larger Yarlung Zangbo to the south (see figs. 2, 3, 13), large dust storms and sand storms originate today and are common in capitol city of Lhasa. Blowing silt from larger braided flood plains in Pleistocene time was source of much loesslike silt described in this report. Photograph PK 23,763 by Troy L. P6w6, June 4, 1980. ORIGIN AND CHARACTER OF LOESSLIKE SILT IN THE SOUTHERN QINGHAI-XIZANG (TIBET) PLATEAU, CHINA Frontispiece. -
Ultradeep Fused Silica Glass Etching with an HF- Resistant Photosensitive Resist for Optical Imaging Applications
Ultradeep fused silica glass etching with an HF- resistant photosensitive resist for optical imaging applications John M Nagarah and Daniel A Wagenaar Broad Fellows Program and Division of Biology California Institute of Technology 1200 E. California Blvd. MC 216-76 Pasadena, CA 91125 [email protected] [email protected] Abstract Microfluidic and optical sensing platforms are commonly fabricated in glass and fused silica (quartz) because of their optical transparency and chemical inertness. Hydrofluoric acid (HF) solutions are the etching media of choice for deep etching into silicon dioxide substrates, but processing schemes become complicated and expensive for etching times greater than 1 hour due to the aggressiveness of HF migration through most masking materials. We present here etching into fused silica more than 600 μm deep while keeping the substrate free of pits and maintaining a polished etched surface suitable for biological imaging. We utilize an HF-resistant photosensitive resist (HFPR) which is not attacked in 49% HF solution. Etching characteristics are compared for substrates masked with the HFPR alone and the HFPR patterned on top of Cr/Au and polysilicon masks. We used this etching process to fabricate suspended fused silica membranes, 8–16 μm thick, and show that imaging through the membranes does not negatively affect image quality of fluorescence microscopy of biological tissue. Finally, we realize small through-pore arrays in the suspended membranes. Such devices will have applications in planar electrophysiology platforms, especially where optical imaging is required. 1. Introduction Glass and fused silica are appealing materials for constructing microelectromechanical systems (MEMS), lab-on-a-chip, and microfluidic platforms due to their chemical inertness, biocompatibility, optical transparency, mechanical rigidity, high melting point, electrical insulation, gas impermeability, and ability to bond to silicon, glass, and polydimethylsiloxane (PDMS) [1-3]. -
RTU Course "Chemistry and Technology of Glass"
Rīgas Tehniskā universitāte 25.09.2021 13:41 RTU Course "Chemistry and Technology of Glass" 14113 Department of Silicate, High Temperature and Inorganic Nanomaterials Technology General data Code ĶST554 Course title Chemistry and Technology of Glass Course status in the programme Compulsory/Courses of Limited Choice; Courses of Free Choice Responsible instructor Gundars Mežinskis Volume of the course: parts and credits points 1 part, 3.0 Credit Points, 4.5 ECTS credits Language of instruction LV, EN Annotation Theoretical principles of the melting and crystallization of glasses.The melting of glasses in conditions of industry. Principles and the equipment of the main technologies of glasses. The treatment and decoration of glassy materials. The characterisation of newest tendencies in the technology of glass and glassy materials. Goals and objectives of the course in terms of Understand the structural characteristics of the glass. To be competent in in glass compositions for competences and skills different application areas, glass characteristics and production technologies. Able to determine the most important glass properties. Structure and tasks of independent studies Using the compendium of lectures and literature data, the student prepares for its own laboratory work, after the execution of works presents laboratory reports, draw conclusions. Recommended literature 1.R.Švinka, V. Švinka. Silikātu materiālu ķīmija un tehnoloģija. Rīga, 1997. 192 lpp. 2.J.E.Shelby. Introduction to Glass Science and Technology. 2nd ed. The Royal Society of Chemistry, 2005. 291 p. 3.High-Performance Glasses. Ed. M.Cable and J.M.Parker . Blackie, Glasgow and London, 1992. 346 p. 4.В.С.Горшков, В.Г.Савельев, Н.Ф.Федоров. -
Addendum #2 Fire Station #10 Renovation (F0sr)
IFB #073-2021 ADDENDUM #2 CITY OF SPRINGFIELD, MISSOURI, DIVISION OF PURCHASES INVITATION FOR BID (IFB) #073-2021 FIRE STATION #10 RENOVATION (F0SR) Margaret Juarez, Buyer Buyer’s Email: [email protected] Division of Purchases Telephone Number: 417-864-1621 218 E. Central, Springfield, MO 65802 REVISED DUE DATE: FEBRUARY 25, 2021 3:00PM The original Invitation for Bid #073-2021 for FIRE STATION #10 RENOVATION (F0SR) documents shall remain in effect except as revised by the following changes, which shall take precedence over anything to the contrary in the specifications. Please Note: The format of this addendum document will detail questions asked, answers provided, clarifications and statements made and will be denoted as follows: Q=Question, A=Answer, C= Clarification, and S= Statement S: The bid schedule has been revised as follows: • ADDITIONAL SITE VISIT: Tuesday, February 16, 2021 at 10:30am. Please sign up for this site visit by emailing Margaret Juarez at [email protected]. • FINAL QUESTIONS DUE: Wednesday, February 17, 2021 by 5:00pm. • FINAL ADDENDUM: Friday, February 19, 2021 by 5:00pm. • BIDS DUE: February 25, 2021 by 3:00pm CST. All documents must be uploaded into DemandStar by this time/date. Start your uploads early. If you need help with DemandStar, please call their Customer Service at 866-273-1863. • BID OPENING: February 25, 2021 at 3:00pm CST via Zoom. To participate, email the Buyer, Margaret Juarez at [email protected] for the Zoom link. S: Section 8.0 (Subcontractor List) in the IFB Document is hereby replaced with the following REVISED Subcontractor List (Page 3-4 of this Addendum). -
Analogues for Radioactive Waste For~1S •
PNL-2776 UC-70 3 3679 00049 3611 ,. NATURALLY OCCURRING GLASSES: ANALOGUES FOR RADIOACTIVE WASTE FOR~1S • Rodney C. Ewing Richard F. Haaker Department of Geology University of New Mexico Albuquerque, ~ew Mexico 87131 April 1979 Prepared for the U.S. Department of Energy under Contract EY-76-C-06-1830 Pacifi c i'lorthwest Laboratory Richland, Washington 99352 TABLE OF CONTENTS List of Tables. i i List of Figures iii Acknowledgements. Introduction. 3 Natural Glasses 5 Volcanic Glasses 9 Physical Properties 10 Compos i ti on . 10 Age Distributions 10 Alteration. 27 Devitrification 29 Hydration 32 Tekti tes. 37 Physical Properties 38 Composition . 38 Age Distributions . 38 Alteration, Hydration 44 and Devitrification Lunar Glasses 44 Summary . 49 Applications to Radioactive Waste Disposal. 51 Recommenda ti ons 59 References 61 Glossary 65 i LIST OF TABLES 1. Petrographic Properties of Natural Glasses 6 2. Average Densities of Natural Glasses 11 3. Density of Crystalline Rock and Corresponding Glass 11 4. Glass and Glassy Rocks: Compressibility 12 5. Glass and Glassy Rocks: Elastic Constants 13 6. Glass: Effect of Temperature on Elastic Constants 13 7. Strength of Hollow Cylinders of Glass Under External 14 Hydrostatic Pressure 8. Shearing Strength Under High Confining Pressure 14 9. Conductivity of Glass 15 10. Viscosity of Miscellaneous Glasses 16 11. Typical Compositions for Volcanic Glasses 18 12. Selected Physical Properties of Tektites 39 13. Elastic Constants 40 14. Average Composition of Tektites 41 15. K-Ar and Fission-Track Ages of Tektite Strewn Fields 42 16. Microprobe Analyses of Various Apollo 11 Glasses 46 17. -
Specialty Glass Technical Capabilities
SpecialtySpecialty GlassGlass TechnicalTechnical CapabilitiesCapabilities 07/1307/13 Web: www.abrisatechnologies.com - E–mail: [email protected] - Tel: (877) 622-7472 Page 1 Specialty Glass Products Technical Reference Document 07/13 It all starts with the basic element, the glass. Each substrate has unique and specific qualities which are matched to the application and specifications that your unique project requires. Abrisa Technologies offers: High Ion-Exchange (HIE) Thin Glass High Ion-Exchange (HIE) Aluminosilicate Thin Glass - (Page 3) Asahi Dragontrail™ - (Pages 4 & 5) Corning® Gorilla® Glass - (Pages 6 & 7) SCHOTT Xensation™ Cover Glass - (Page 8) Soda-Lime Soda-Lime (Clear & Tinted) - (Page 9) Soda-Lime (Low Iron) - (Page 10) Soda-Lime (Anti-Glare Reducing Etched Glass) - (Page 11) Patterned Glass for Light Control - (Page 12 & 13) Soda-Lime Low Emissivity (Low-E) Glass - (Page 14) Soda-Lime (Heat Absorbing Float Glass) - (Page 15) Borosilicate SCHOTT BOROFLOAT® 33 Multi-functional Float Glass - (Pages 16 & 17) SCHOTT BOROFLOAT Infrared (IRR) - (Page 18) SCHOTT SUPREMAX® Rolled Borosilicate - (Pages 19 & 20) SCHOTT D263 Colorless Thin Glass - (Pages 21 & 22) SCHOTT Duran® Lab Glass - (Pages 24 & 25) Ceramic/Glass SCHOTT Robax® Transparent Ceramic Glass - (Page 26) SCHOTT Pyran® Fire Rated Glass Ceramic - (Page 27) Quartz/Fused Silica Corning® 7980 Fused Silica - (Page 28) GE 124 Fused Quartz - (Page 309 Specialty Glass Corning® Eagle XG LCD Glass Free of Heavy Metals - (Page 30 & 31) Laminated Glass - Safety Glass - (Page 32) SCHOTT Superwhite B270® Flat Glass - (Page 33) Weld Shield - (Page 354 White Flashed Opal - (Page 35) X-Ray Glass (Radiation Shielding Glass) - (Page 376 Web: www.abrisatechnologies.com - E–mail: [email protected] - Tel: (877) 622-7472 Page 2 Specialty Glass Products Technical Reference Document 07/13 High Ion-Exchange (HIE) High Ion-Exchange (HIE) Chemically Strengthened Aluminosilicate Thin Glass High Ion-Exchange (HIE) thin glass is strong, lightweight and flexible. -
Josephine County, Oregon, Historical Society Document Oregonłs
Finding fossils in Oregon is not so much a question of Places to see fossils: where to look for them as where not to look. Fossils are rare John Day Fossil Beds National Monument in the High Lava Plains and High Cascades, but even there, , _ Contains a 40-million year record of plant and animal life . ·� � .11�'!]�:-.: some of the lakes are famous for their fossils. Many of the ill the John Day Basill ill central Oregon near the towns of .• .� . ' · sedimentary rocks in eastern Oregon contain fossil leaves or · ,,����<:l. · . ' · •· Dayville' Fossil, and Mitchell. The Cant Ranch Visitor ; ' " ' ' j ' .- � bones. Leaffossils are especially abundant in the - Center at Sheep Rock on Highway 19 includes museum : ,· .,, 1 • , .. rocks at the far side of the athletic · exhibits of fossils. Open every day 8:30-5. For general l· · . ., ;: . · : field at Wheeler High School ,...,..;� information, contact John Day Fossil Beds National . -- - ' '· in the town of Fossil. Monument, 420 West Main St., John Day, OR 97845, ' l-, Although it is rare to phone (503) 575-0721. find a complete Oregon Museum of Science and Industry animal fossil, a 1945 SE Water Ave., Portland, OR 97214. Open Thurs. & search of river Fri. 9:30-9; Sat. through Wed. 9:30-7(sumrner hours); beds may turn . l 9:30-5(rest of year), phone (503) 797-4000 up c h1ps or Condon Museum, University of Oregon even teeth. In Pacific Hall, Eugene, OR 97403. Open only by western appointment, phone (503) 346-4577. Oregon, the ' . ; Douglas County Museum of History and sedimentary ' r Natural History rocks that are 1 primarily off1-5 at exit 123 at Roseburg (PO Box 1550, Roseburg, marine in OR 97470). -
Opto-Fluidic Manipulation of Microparticles and Related Applications
University of South Florida Scholar Commons Graduate Theses and Dissertations Graduate School 11-10-2020 Opto-Fluidic Manipulation of Microparticles and Related Applications Hao Wang University of South Florida Follow this and additional works at: https://scholarcommons.usf.edu/etd Part of the Biomedical Engineering and Bioengineering Commons Scholar Commons Citation Wang, Hao, "Opto-Fluidic Manipulation of Microparticles and Related Applications" (2020). Graduate Theses and Dissertations. https://scholarcommons.usf.edu/etd/8601 This Dissertation is brought to you for free and open access by the Graduate School at Scholar Commons. It has been accepted for inclusion in Graduate Theses and Dissertations by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. Opto-Fluidic Manipulation of Microparticles and Related Applications by Hao Wang A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Biomedical Engineering Department of Medical Engineering College of Engineering University of South Florida Major Professor: Anna Pyayt, Ph.D. Robert Frisina, Ph.D. Steven Saddow, Ph.D. Sandy Westerheide, Ph.D. Piyush Koria, Ph.D. Date of Approval: October 30, 2020 Key words: Thermal-plasmonic, Convection, Microfluid, Aggregation, Isolation Copyright © 2020, Hao Wang Dedication This dissertation is dedicated to the people who have supported me throughout my education. Great appreciation to my academic adviser Dr. Anna Pyayt who kept me on track. Special thanks to my wife Qun, who supports me for years since the beginning of our marriage. Thanks for making me see this adventure though to the end. Acknowledgments On the very outset of this dissertation, I would like to express my deepest appreciation towards all the people who have helped me in this endeavor. -
Volcanic Glass Textures, Shape Characteristics
Cent. Eur. J. Geosci. • 2(3) • 2010 • 399-419 DOI: 10.2478/v10085-010-0015-6 Central European Journal of Geosciences Volcanic glass textures, shape characteristics and compositions of phreatomagmatic rock units from the Western Hungarian monogenetic volcanic fields and their implications for magma fragmentation Research Article Károly Németh∗ Volcanic Risk Solutions CS-INR, Massey University, Palmerston North, New Zealand Received 2 April 2010; accepted 17 May 2010 Abstract: The majority of the Mio-Pleistocene monogenetic volcanoes in Western Hungary had, at least in their initial eruptive phase, phreatomagmatic eruptions that produced pyroclastic deposits rich in volcanic glass shards. Electron microprobe studies on fresh samples of volcanic glass from the pyroclastic deposits revealed a primarily tephritic composition. A shape analysis of the volcanic glass shards indicated that the fine-ash fractions of the phreatomagmatic material fragmented in a brittle fashion. In general, the glass shards are blocky in shape, low in vesicularity, and have a low-to-moderate microlite content. The glass-shape analysis was supplemented by fractal dimension calculations of the glassy pyroclasts. The fractal dimensions of the glass shards range from 1.06802 to 1.50088, with an average value of 1.237072876, based on fractal dimension tests of 157 individual glass shards. The average and mean fractal-dimension values are similar to the theoretical Koch- flake (snowflake) value of 1.262, suggesting that the majority of the glass shards are bulky with complex boundaries. Light-microscopy and backscattered-electron-microscopy images confirm that the glass shards are typically bulky with fractured and complex particle outlines and low vesicularity; features that are observed in glass shards generated in either a laboratory setting or naturally through the interaction of hot melt and external water. -
Volcanic Glass As a Paleoenvironmental Proxy: Comparing Preparation Methods on Ashes from the Lee of the Cascade Range in Oregon, USA
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses Spring 7-6-2018 Volcanic Glass as a Paleoenvironmental Proxy: Comparing Preparation Methods on Ashes from the Lee of the Cascade Range in Oregon, USA Tessa Boe Carlson Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Geochemistry Commons, and the Volcanology Commons Let us know how access to this document benefits ou.y Recommended Citation Carlson, Tessa Boe, "Volcanic Glass as a Paleoenvironmental Proxy: Comparing Preparation Methods on Ashes from the Lee of the Cascade Range in Oregon, USA" (2018). Dissertations and Theses. Paper 4472. https://doi.org/10.15760/etd.6356 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. Volcanic Glass as a Paleoenvironmental Proxy: Comparing Preparation Methods on Ashes from the Lee of the Cascade Range in Oregon, USA by Tessa Boe Carlson A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology Thesis Committee: John Bershaw, Chair Ashley Streig Martin Streck Portland State University 2018 Abstract Deuterium ratios (δD) of hydrated volcanic glass have been used to reconstruct paleoenvironments, although the reliability and proper sample preparation protocol have been debated. In this study, hydrated volcanic ash samples from the lee of the Cascades were prepared using two separate methods. Method 1 involves sonicating and rinsing samples with hydrochloric acid (HCl) followed by hand-selection of glass shards (125 –212µm). -
Volcanic Glass on the Water Chemistry in a Tuflaceoiis Aquifer, Rainier Mesa, Nevada
Volcanic Glass on the Water Chemistry in a Tuflaceoiis Aquifer, Rainier Mesa, Nevada GEOLOGICAL SURVEY WATER-SUPPLY PAPER The Effect of Dissolution of Volcanic Glass on the Water Chemistry in a Tuffaceous Aquifer, Rainier Mesa, Nevada By ART F. WHITE, HANS C. CLAASSEN, and LARRY V. BENSOI 7 GEOCHEMISTRY OF WATER GEOLOGICAL SURVEY WATER-.SUPPLY PAPER 1535-Q, UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1980 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menaid, Director Library of Congress Cataloging in Publication Data White Art F. The effect of dissolution of volcanic glass on the water chemistry in a tuffaceous aquifer, Rainier Mesa, Nevada. (Geochemistry of water) (U.S. Geological Survey Water-Supply Paper 1535-Q) Bibliography: p. 33 I. Water, Underground Nevada Rainier Mesa. 2. Volcanic ash, tuff, etc. Nevada- Rainier Mesa. 3. Aquifers Nevada-Rainier Mesa. I. Claassen, Hans C., joint author. II. Benson, Larry V., joint author. III. Title. IV. Series. V. Series: United States Geological Survey Water-Supply Paper 1535-Q. TC801.U2 no. 1535-Q [GB1025.N4] 553.7'0973s [551.49] 80-6O7124 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract.......................................................... Ql Introduction....................................................... 1 Setting of Rainier Mesa .......................................... 2 Previous studies ................................................ 2 Acknowledgments..............................................