Ice-Templating, Freeze Casting: Beyond Materials Processing S
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3D Convection, Phase Change, and Solute Transport in Mushy Sea Ice
3D convection, phase change, and solute transport in mushy sea ice Dan Martin, James Parkinson, Andrew Wells, Richard Katz Lawrence Berkeley National Laboratory (USA), Oxford University (UK). Summary: ● Simulated brine drainage via 3-D convection in porous mushy sea ice ● Shallow region near ice-ocean interface is desalinated by many small brine channels ● Full-depth “mega-channels” allow drainage from saline layer near top of ice. What is a mushy layer? Dense brine drains convectively from porous mushy sea ice into the ocean. - What is spatial structure of this flow in 3 dimensions? Upper fig.: Sea ice is a porous mixture of solid ice crystals (white) and liquid brine (dark). H. Eicken et al. Cold Regions Science and Technology 31.3 (2000), pp. 207–225 Lower fig.: Trajectory (→) of a solidifying salt water parcel through the phase diagram. As the temperature T decreases, the ice fraction increases and the residual brine salinity SI increases making the fluid denser, which can drive convection. Using a linear approximation for the liquidus curve, the freezing point is - Problem setup Numerically solve mushy-layer equations for porous ice-water Cold upper boundary O matrix g T=-10 C, no normal salt flux, no vertical flow (see appendix). 2m Initial conditions z S=30g/kg O T=Tfreezing (S=30g/kg) + 0.2 C U = 0 Horizontally periodic O y Plus small random O(0.01 C) temperature perturbation x 4m 4m Open bottom boundary Inflow/outflow, with constant pressure O Inflow: S=30g/kg, T=Tfreezing (S=30g/kg) + 0.2 C Movie Contours of: Ice permeability -function of ice porosity; (red lower, green higher ~ice-ocean interface) Velocity (blue lower, purple higher). -
Internal Frost Damage in Concrete - Experimental Studies of Destruction Mechanisms
Internal frost damage in concrete - experimental studies of destruction mechanisms Fridh, Katja 2005 Link to publication Citation for published version (APA): Fridh, K. (2005). Internal frost damage in concrete - experimental studies of destruction mechanisms. Division of Building Materials, LTH, Lund University. Total number of authors: 1 General rights Unless other specific re-use rights are stated the following general rights apply: Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the public portal Read more about Creative commons licenses: https://creativecommons.org/licenses/ Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. LUND UNIVERSITY PO Box 117 221 00 Lund +46 46-222 00 00 Download date: 09. Oct. 2021 LUND INSTITUTE OF TECHNOLOGY LUND UNIVERSITY Division of Building Materials INTERNAL FROST DAMAGE IN CONCRETE Experimental studies of destruction mechanisms Katja Fridh Report TVBM-1023 Doctoral thesis Lund 2005 ISRN LUTVDG/TVBM--05/1023--SE(1-276) ISSN 0348-7911 TVBM ISBN 91-628-6558-7 Lund Institute of Technology Telephone: 46-46-2227415 Division of Building Materials Telefax: 46-46-2224427 Box 118 www.byggnadsmaterial.lth.se SE-221 00 Lund, Sweden Preface The work presented here was carried out at the Division of Building Materials at the Lund Institute of Technology. -
Steven D. Vance –
Steven D. Vance Research Focus My research focuses on using geophysical and geochemical methods to understand ocean worlds: how oceans couple to the thermal evolution and composition, and what this might mean for life. I am also interested in the global geochemical fluxes in ocean worlds, by analogy to biogeochemical fluxes in the Earth system. My experimental research involves collecting thermodynamic equations of state for fluids and ices. I have applied these equations of state to evaluating oceanic heat transport and double diffusive convection in Europa, and to the geophysical constraints imposed by ocean composition on the radial structures of Europa, Ganymede, Callisto, Enceladus, and Titan. In recent years I have used these models to explore the parameter space of possible geophysical signals—seismic, magnetic, and gravitational—in the interest of improving the fidelity of returned science from investigations of ocean composition and habitability. Education 2001–2007 Ph.D., University of Washington, Seattle, Geophysics and Astrobiology. 1996–2000 B.S., University of California, Santa Cruz, Physics (with honors). Ph.D. Thesis title Thesis title: High Pressure and Low Temperature Equations of State for Aqueous Sulfate Solutions: Applications to the Search for Life in Extraterrestrial Oceans, with Particular Reference to Europa advisor Prof. J. Michael Brown Bachelor Thesis title The Role of Methanol Frost in Particle Sticking and the Formation of Planets in the Early Solar Nebula advisor Prof. Frank G. Bridges Current Appointments Research -
An Experimental Study of Ice-Bed Separation During Glacial Sliding Benjamin Brett Etp Ersen Iowa State University
Iowa State University Capstones, Theses and Graduate Theses and Dissertations Dissertations 2012 An experimental study of ice-bed separation during glacial sliding Benjamin Brett etP ersen Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/etd Part of the Geology Commons, and the Geophysics and Seismology Commons Recommended Citation Petersen, Benjamin Brett, "An experimental study of ice-bed separation during glacial sliding" (2012). Graduate Theses and Dissertations. 12701. https://lib.dr.iastate.edu/etd/12701 This Thesis is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Graduate Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. An experimental study of ice-bed separation during glacial sliding by Benjamin Brett Petersen A thesis submitted to the graduate faculty in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Major: Geology Program of Study Committee: Neal R. Iverson, Major Professor Igor Beresnev Carl E. Jacobson Iowa State University Ames, Iowa 2012 Copyright © Benjamin Brett Petersen, 2012. All rights reserved. ii TABLE OF CONTENTS ACKNOWLEDGMENTS iii ABSTRACT iv CHAPTER 1. INTRODUCTION 1 1.1 Ice-bed separation 1 1.2 Sliding models 2 1.3 Hydrology models 5 1.4 Quarrying 8 1.5 Experimental studies of cavitation 9 1.6 Motivation and objectives 10 CHAPTER 2. METHODS 12 2.1 The ring-shear device 12 2.2 Procedure 19 2.3 Data processing 25 CHAPTER 3. -
Reconstructing the Confluence Zone Between Laurentide and Cordilleran Ice Sheets Along the Rocky Mountain Foothills, Southwest Alberta
This is a repository copy of Reconstructing the confluence zone between Laurentide and Cordilleran ice sheets along the Rocky Mountain Foothills, southwest Alberta. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/105138/ Version: Accepted Version Article: Utting, D., Atkinson, N., Pawley, S. et al. (1 more author) (2016) Reconstructing the confluence zone between Laurentide and Cordilleran ice sheets along the Rocky Mountain Foothills, southwest Alberta. Journal of Quaternary Science, 31 (7). pp. 769-787. ISSN 0267-8179 https://doi.org/10.1002/jqs.2903 Reuse Unless indicated otherwise, fulltext items are protected by copyright with all rights reserved. The copyright exception in section 29 of the Copyright, Designs and Patents Act 1988 allows the making of a single copy solely for the purpose of non-commercial research or private study within the limits of fair dealing. The publisher or other rights-holder may allow further reproduction and re-use of this version - refer to the White Rose Research Online record for this item. Where records identify the publisher as the copyright holder, users can verify any specific terms of use on the publisher’s website. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ Reconstructing the confluence zone between Laurentide and Cordilleran ice sheets along the Rocky Mountain Foothills, south-west Alberta Daniel J. Utting1, Nigel Atkinson1, Steven Pawley1, Stephen J. -
Ice Crystal Growth Through Nonbasal Plane Adsorption of Antifreeze Proteins
Blocking rapid ice crystal growth through nonbasal plane adsorption of antifreeze proteins Luuk L. C. Olijvea,b, Konrad Meisterc, Arthur L. DeVriesd, John G. Dumane, Shuaiqi Guof,g, Huib J. Bakkerc, and Ilja K. Voetsa,b,h,1 aInstitute for Complex Molecular Systems, Eindhoven University of Technology, 5600 MB Eindhoven, The Netherlands; bLaboratory of Macromolecular and Organic Chemistry, Department of Chemical Engineering and Chemistry, Eindhoven University of Technology, 5600 MB Eindhoven, The Netherlands; cInstitute for Atomic and Molecular Physics, Foundation for Fundamental Research on Matter, 1098 XG Amsterdam, The Netherlands; dDepartment of Animal Biology, University of Illinois at Urbana–Champaign, Urbana, IL 61801; eDepartment of Biological Sciences, University of Notre Dame, Notre Dame, IN 46556; fProtein Function Discovery Group, Queen’s University, Kingston, ON, Canada K7l 3N6; gDepartment of Biomedical and Molecular Sciences, Queen’s University, Kingston, ON, Canada K7l 3N6; and hLaboratory of Physical Chemistry, Department of Chemical Engineering and Chemistry, Eindhoven University of Technology, 5600 MB Eindhoven, The Netherlands Edited by Pablo G. Debenedetti, Princeton University, Princeton, NJ, and approved January 26, 2016 (received for review December 14, 2015) Antifreeze proteins (AFPs) are a unique class of proteins that bind AFPs also target different—sometimes multiple—ice crystal planes, to growing ice crystal surfaces and arrest further ice growth. AFPs including prism, pyramidal, and basal faces (Fig. 1) (13). Recent have gained a large interest for their use in antifreeze formula- Monte Carlo and molecular dynamics simulations confirm this tions for water-based materials, such as foods, waterborne paints, specificity (14–16). and organ transplants. Instead of commonly used colligative AFPs exhibit two forms of activities. -
CAT — Creative Authors' Treasury
SCIO WRITERS CLUB December 2016 Volume 5, Issue 2 Elementary CAT — Creative Authors’ Treasury Winter Edition— Inside this issue: Winter Snow Winter Snow 1 Winter is Coming Winter Snow Winter Oh, so much snow Thank You 2 Who would ever know how I Like People No, no, no too much snow, why? Our river is going to over flow from snow So much depends The Winter Sorrow 3 It’s too much for our shovels to handle The Cabin We can have snow, not too much Winter Snow is falling down fast Acrostic Poems 4 It is vast Sled 6 By Noah Little Pigs 9 Ginger Bread Guys Winter is Coming Brrr feel that cold wind Snowathysis 10 That means winter is coming Snow 12 With its great Christmas cheer The Winter Race So get out your coats Puzzle Page 13 Because winter is on the way. The Snowman 14 By Lillian Cline Page 2 CAT — Creative Authors’ Treasury Winter Winter is here Winter is the coldest time of year Winter is like ice Winter is the best time of year Snow is cold Winter is cold all around I Like By Kiara Grover I like my family I like my brothers I like my life I like my friend Thank You I like the snow Thank you! I like Christmas Thank You, for being there for me Thank You, for loving me Thank You, for taking care of me By Cameron Halsey And most of all, thank You for keeping a smile on my face By Alivia Thomason People People There’s people just like you and me Short people, tall people, skinny people, fat people, bald people, hairy people, short hair people, Long haired people, fashion people, old people, young people, rich people, poor people, people with hats, people with no hats, smart people, people with a job, cool people, not cool people, mean people, nice people and so many more people like me don’t judge anyone no matter what By Emma Eck Page 3 So much depends upon The Cabin So much depends upon A Christmas present In the woods To cherish, and keep, Where it was snowing Until the end of time A cabin was lit up The best present ever With Christmas lights Oh thank you, Dad. -
Antarctic Peninsula the Extended Expedition to the White Continent 1 to 16 January 2013
ANTA RCTIC PENINSULA T HE E XTENDED EXP EDITION TO THE WHITE C ONTINENT C HEESEMANS’ E C OLOGY S AFARIS E XPEDITION L OG 2013 CHEESEMANS’ ECOLOGY SAFARIS EXPEDITION LOG Antarctic Peninsula The Extended Expedition to the White Continent 1 to 16 January 2013 Markus Eichenberger Willian Draisma Willian Draisma Designed by Debbie Thompson and Kate Spencer Dailies coordinated by Joe Kaplan and written by Tom Fleischner, Jessica Joganic, Rosemary Joganic, Joe Kaplan, Samantha Oester, Christina Prahl, Clemens Vanderwerf, and Shirley West; with contributions from other participants Images by passengers and sta as credited Cover Photo Almirante Brown By Kathy Richardson Back Cover Photo Grandidier Channel By Dustin Richards This Page Photo Almirante Brown By Willian Draisma COPYRIGHT NOTICE Copyright ©2013 Cheesemans’ Ecology Safaris Photographers hold the copyright to their work. ii TABLE OF CONTENTS INTRODUCTION Introduction 1 For over twenty years, Cheesemans’ Ecology Safaris has op- The Expedition 2 erated the longest, most in-depth expeditions to the Ant- arctic region, a destination of supreme splendor and seren- Ushuaia and Embarkation 1 January 4 ity that deserves no less. We are honored that each of you At Sea to The Peninsula 2 January 6 chose to travel with us on this lifetime journey. Much time Half Moon Island 3 January 8 and e ort was invested, most of it “behind the scenes,” to ensure that you had the same life altering experience that Cierva Cove and Danco Island 4 January 10 so many of our previous expedition participants a rm. Cuverville Island and Port Lockroy 5 January 12 On 31 December we celebrated New Year’s Eve in Ushuaia, Antarctic Circle and Detaille Island 6 January 16 Argentina, and then boarded our ship the Ortelius the fol- Hugh Rose David Meeks Petermann and Booth Islands 7 January 18 lowing morning, sailing 2,337 miles over the next 16 days, with 97 passengers, 13 Paradise Bay and Almirante Brown 8 January 22 expedition sta , and the hardworking ship’s crew. -
A Simple Guide to Roofing
a simple guide to roofing 21 Pages of tips to avoid costly mistakes Notes How to choose the Right Contractor? for your project It’s important to recognize that your projects success is not simply how many shingles, and how much labour, and the price you paid. It’s in the preparation process before and after. You are trusting this to the contractor, and before you spend your hard earned money we strongly recommended that you read this guide book before beginning your contractor selection process. Remember! You are trusting your most expensive asset to a contractor who is TEARING the roof off of your home! Most common BBB complaints: of the time 33% 7% contractor cannot even be found of the time the contractor or contacted to does not respond to complaint. request a response! Some important questions to ask: Are they using employees or subcontractors? Insurance is very important. Subcontractors are not insured by the company. They may provide an estimate that SAYS they will only use fully insured sub-contractors, and even show a copy of the agree- ment their make their subcontractors sign. However, neither of these is a confirmation that the contrac- tor is actually presently insured! This goes for manufacturer certifications as well! Ask for proof! Do not feel uneasy asking for this, as it is not unreasonable for you to be concerned. The professional contractor will be ready to have this information available. The true professional will appreciate that you are an educated customer that values the extra measures they have taken to protect YOU - the home owner. -
The Arctic Game
University of Denver Digital Commons @ DU Electronic Theses and Dissertations Graduate Studies 1-1-2012 The Arctic Game Sarah E. Nuernberger University of Denver Follow this and additional works at: https://digitalcommons.du.edu/etd Part of the Climate Commons, and the International Relations Commons Recommended Citation Nuernberger, Sarah E., "The Arctic Game" (2012). Electronic Theses and Dissertations. 894. https://digitalcommons.du.edu/etd/894 This Thesis is brought to you for free and open access by the Graduate Studies at Digital Commons @ DU. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of Digital Commons @ DU. For more information, please contact [email protected],[email protected]. THE ARCTIC GAME __________ A Thesis Presented to the Faculty of the Josef Korbel School of International Studies University of Denver __________ In Partial Fulfillment of the Requirements for the Degree Master of Arts __________ by Sarah E. Nuernberger June 2012 Advisor: Dr. Dale Rothman ©Copyright by Sarah E. Nuernberger 2012 All Rights Reserved Author: Sarah E. Nuernberger Title: THE ARCTIC GAME Advisor: Dr. Dale Rothman Degree Date: June 2012 Abstract Since outsiders first visited the Arctic, they have believed in man’s ability to conquer the region. Today’s Arctic conquest is not one of heroic exploration, but rather one of ownership and exploitation. This paper illustrates contestation in the Arctic through the metaphor of a game, with attendant prizes, players, and rules. It focuses on how to prevent the future destruction of the Arctic given the interactions of the Arctic’s landscape, prizes, players, and current management frameworks. -
I ABSTRACT a CONCEPTUAL MODEL of ICE SHELF
i ABSTRACT A CONCEPTUAL MODEL OF ICE SHELF SEDIMENTATION Matthew Mayerle, M.S. Department of Geology and Environmental Geosciences Northern Illinois University 2014 Ross Powell, Director Sedimentation studies of polar glacimarine systems remain few relative to temperate glacimarine systems due to the problem of accessibility below ice shelves. This thesis presents a conceptual model of ice shelf sedimentation at the scale of a continental shelf, which is an update of Howat and Domack’s (2003) model. This update adds scale, a third dimension, a decade of research on new geologic/glaciological processes, depositional bias', and greater specificity to their model. The shelf-scale model groups facies into deformation till, glacigenic debris flows, shelfstone mud, and diatomaceous mud. Furthermore, the model is tested and shown to be capable of replicating the facies distribution and major landforms found in two distinctly different Antarctic paleo-ice stream troughs within time constraints dictated by radiometric dating. It is hoped that ideas and techniques presented by this conceptual model will serve as a launching pad for more advanced computational models in the future, which are badly needed in order to help constrain future behavior of ice sheets in a warming world. i NORTHERN ILLINOIS UNIVERSITY DE KALB, ILLINOIS DECEMBER 2014 A CONCEPTUAL MODEL OF ICE SHELF SEDIMENTATION BY MATTHEW WILLIAM MAYERLE ©2014 Matthew Mayerle A THESIS SUBMITTED TO THE GRADUATE SCHOOL IN PARTIAL FULLFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE DEPARTMENT OF GEOLOGY AND ENVIRONMENTAL GEOSCIENCES Thesis Director: Ross D. Powell ii DEDICATION With love to my parents William and Margaret Mayerle, whose long hours of work provided me with the gift of education. -
High Arctic Sovereignty Revisited
ARCTIC VOL. 56, NO. 1 (MARCH 2003) P. 101–109 InfoNorth The Muskox Patrol: High Arctic Sovereignty Revisited by Peter Schledermann HE ROLE OF THE ROYAL CANADIAN MOUNTED POLICE Under Sverdrup’s hugely successful leadership, mem- (RCMP) in the Canadian government’s quest to bers of the Norwegian expedition spent four years map- T secure international recognition of its claims to ping and surveying large, often unknown portions of the sovereignty over the High Arctic islands is a chapter of High Arctic islands. The only people they encountered Canadian history rarely visited. Yet the sovereignty battle were North Greenlandic Inughuit who had crossed Smith over a group of Arctic islands few can even name was the Sound to assist the American explorer Robert Peary in his stuff of high-stakes political poker: bluff indifference mixed quest to reach the North Pole. When the expedition re- with sudden bursts of national interest, courage, hardships, turned to Norway in 1902, Sverdrup began what would and dedication of a high order. Canadian government become a lifelong, personal struggle to press his govern- activities in the High Arctic between 1900 and 1933 were ment into pursuing the claim he had set in motion. While carried out almost exclusively in response to the real or the Norwegian government expressed little official inter- perceived intentions of other nations to challenge Canada’s est in the matter, the Dominion of Canada government sovereignty claims. This story is currently being presented took the claim far more seriously. For centuries, American as a proposal for a documentary film, “The Muskox Pa- and European whalers and explorers had frequented Arctic trol,” by Ole Gjerstad and Peter Schledermann.