Ice Mitigation Measures Used During the Construction of the Keeyask Generating Station After the Failure of the Ice Boom
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Sea Ice Engineering
Sea Ice Engineering theory and application Claude Daley Sea Ice Engineering 2017 –Notes ii © Claude G. Daley 2017 With components developed by D.B.Colbourne and B.W.T. Quinton All rights reserved. No reproduction, copy or transmission of this publication may be made without written permission. This draft is solely for the use of students registered in EN8074 and EN9096, in Winter 2016. All enquiries to: C.G. Daley Faculty of Engineering and Applied Science Memorial University of Newfoundland St. John’s Newfoundland and Labrador Canada A1B 3X5 Email: [email protected] Note: images, sketches and photo's are © C. Daley unless otherwise noted Cover image by C. Daley from GEM Simulation Program Sea Ice Engineering 2017 –Notes iii …………………………………… Contents Acknowledgments ........................................................................................................................... vi 1 Introducing Arctic Offshore Engineering ................................................................................ 1 1.1 Overview ......................................................................................................................... 1 1.2 Basics .............................................................................................................................. 1 1.3 Current Arctic Engineering Activities ............................................................................ 3 1.4 Transportation ................................................................................................................. 4 1.4.1 -
Rapid Access Ice Drill: a New Tool for Exploration of the Deep Antarctic Ice Sheets and Subglacial Geology
Journal of Glaciology (2016), Page 1 of 16 doi: 10.1017/jog.2016.97 © The Author(s) 2016. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons. org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. Rapid Access Ice Drill: a new tool for exploration of the deep Antarctic ice sheets and subglacial geology JOHN W. GOODGE,1 JEFFREY P. SEVERINGHAUS2 1Department of Earth and Environmental Sciences, University of Minnesota, Duluth, MN 55812, USA 2Scripps Institution of Oceanography, UC San Diego, La Jolla, CA 92093, USA Correspondence: John W. Goodge <[email protected]> ABSTRACT. A new Rapid Access Ice Drill (RAID) will penetrate the Antarctic ice sheets in order to create borehole observatories and take cores in deep ice, the glacial bed and bedrock below. RAID is a mobile drilling system to make multiple long, narrow boreholes in a single field season in Antarctica. RAID is based on a mineral exploration-type rotary rock-coring system using threaded drill pipe to cut through ice using reverse circulation of a non-freezing fluid for pressure-compensation, maintenance of temperature and removal of ice cuttings. Near the bottom of the ice sheet, a wireline latching assem- bly will enable rapid coring of ice, the glacial bed and bedrock below. Once complete, boreholes will be kept open with fluid, capped and available for future down-hole measurement of temperature gradient, heat flow, ice chronology and ice deformation. RAID is designed to penetrate up to 3300 m of ice and take cores in <200 hours, allowing completion of a borehole and coring in ∼10 d at each site. -
Ice Core Science
PAGES International Project Offi ce Sulgeneckstrasse 38 3007 Bern Switzerland Tel: +41 31 312 31 33 Fax: +41 31 312 31 68 [email protected] Text Editing: Leah Christen News Layout: Christoph Kull Hubertus Fischer, Christoph Kull and Circulation: 4000 Thorsten Kiefer, Editors VOL.14, N°1 – APRIL 2006 Ice Core Science Ice cores provide unique high-resolution records of past climate and atmospheric composition. Naturally, the study area of ice core science is biased towards the polar regions but ice cores can also be retrieved from high .pages-igbp.org altitude glaciers. On the satellite picture are those ice cores covered in this issue of PAGES News (Modifi ed image of “The Blue Marble” (http://earthobservatory.nasa.gov) provided by kk+w - digital cartography, Kiel, Germany; Photos by PNRA/EPICA, H. Oerter, V. Lipenkov, J. Freitag, Y. Fujii, P. Ginot) www Contents 2 Announcements - Editorial: The future of ice core research - Dating of ice cores - Inside PAGES - Coastal ice cores - Antarctica - New on the bookshelf - WAIS Divide ice core - Antarctica - Tales from the fi eld - ITASE project - Antarctica - In memory of Nick Shackleton - New Dome Fuji ice core - Antarctica - Vostok ice drilling project - Antarctica 6 Program News - EPICA ice cores - Antarctica - The IPICS Initiative - 425-year precipitation history from Italy - New sea-fl oor drilling equipment - Sea-level changes: Black and Caspian Seas - Relaunch of the PAGES Databoard - Quaternary climate change in Arabia 12 National Page 40 Workshop Reports - Chile - 2nd Southern Deserts Conference - Chile - Climate change and tree rings - Russia 13 Science Highlights - Global climate during MIS 11 - Greece - NGT and PARCA ice cores - Greenland - NorthGRIP ice core - Greenland 44 Last Page - Reconstructions from Alpine ice cores - Calendar - Tropical ice cores from the Andes - PAGES Guest Scientist Program ISSN 1563–0803 The PAGES International Project Offi ce and its publications are supported by the Swiss and US National Science Foundations and NOAA. -
Lakes in Winter
NORTH AMERICAN LAKE NONPROFIT ORG. MANAGEMENT SOCIETY US POSTAGE 1315 E. Tenth Street PAID Bloomington, IN 47405-1701 Bloomington, IN Permit No. 171 Lakes in Winter in Lakes L L INE Volume 34, No. 4 • Winter 2014 Winter • 4 No. 34, Volume AKE A publication of the North American Lake Management Society Society Management Lake American North the of publication A AKE INE Contents L L Published quarterly by the North American Lake Management Society (NALMS) as a medium for exchange and communication among all those Volume 34, No. 4 / Winter 2014 interested in lake management. Points of view expressed and products advertised herein do not necessarily reflect the views or policies of NALMS or its Affiliates. Mention of trade names and commercial products shall not constitute 4 From the Editor an endorsement of their use. All rights reserved. Standard postage is paid at Bloomington, IN and From the President additional mailing offices. 5 NALMS Officers 6 NALMS 2014 Symposium Highlights President 11 2014 NALMS Awards Reed Green Immediate Past-President 15 2014 NALMS Photo Contest Winners Terry McNabb President-Elect 16 2014 NALMS Election Results Julie Chambers Secretary Sara Peel Lakes in Winter Treasurer Michael Perry 18 Lake Ice: Winter, Beauty, Value, Changes, and a Threatened NALMS Regional Directors Future Region 1 Wendy Gendron 28 Fish in Winter – Changes in Latitudes, Changes in Attitudes Region 2 Chris Mikolajczyk Region 3 Imad Hannoun Region 4 Jason Yarbrough 32 A Winter’s Tale: Aquatic Plants Under Ice Region 5 Melissa Clark Region 6 Julie Chambers 38 A Winter Wonderland . of Algae Region 7 George Antoniou Region 8 Craig Wolf 44 Water Monitoring Region 9 Todd Tietjen Region 10 Frank Wilhelm 48 Winter Time Fishery at Lake Pyhäjärvi Region 11 Anna DeSellas Region 12 Ron Zurawell At-Large Nicki Bellezza Student At-Large Ted Harris 51 Literature Search LakeLine Staff Editor: William W. -
Mountain Springs (1890-1948)
Mountain Springs (1890-1948) The Early Years Bowmans Creek for the Lehigh Valley Railroad. Apparently, Splash Dam No. 1 was used as a splash dam at least through 1895, but it was not suc- The ice industry at Mountain Springs may not have been intentionally cessful. The fall in the creek was too steep and the twisting creek bed designed. Harveys Lake would have been the natural site for a major ice caused the released water to rush ahead of the logs, and too often the industry, but the Wright and Barnum patents to the lake discouraged its logs became stranded along the shore instead of being carried down- development. Indeed, Splash Dam No. 1 at Bean Run was developed by stream to the mill. Albert Lewis, not for the ice industry, but as an extension of his lumber With the completion and sale by Lewis to the Lehigh Valley of the rail- industry at Stull downstream on Bowmans Creek. road along the creek in 1893, a splash dam was not critical to carry the In October 1890, the Albert Lewis Lumber and Manufacturing logs to mill. His company ran log railroad lines into the forest lands to Company began construction of a log and timber dam on Bowmans haul timber to the Lehigh Valley line and then down to Stull. Lewis then Creek, near Bean Run, a small stream which runs into the creek. The ini- converted Splash Dam No. 1 to icecutting in the mid-1890s, an industry tial dam site was a failure; the creek bed was too soft to support a dam. -
Ice Cutting at Bantam Lake N
Ice House Ruins Tour Map Follow the Lake Trail (L = yellow blaze) Round trip ~ 1 mile Ice Cutting at Bantam Lake Berkshire Ice Company 1908-1927 Museum and Parking Lot Southern New England Ice Company 1927-1929 Lake Trail 8 6 7 5 4 3 2 1 Before the advent of the refrigerator, people kept food from spoiling by placing it in an icebox—a wooden cabinet with shelves for perishables and a large compartment for a block N of ice to keep everything cold. Where did this ice come Bantam Lake from? It was cut from lakes and ponds in the winter in re- gions where the temperatures were below freezing for ex- tended periods of time. Ice blocks were cut by farmers for Photos are courtesy of the Morris Historical Society and the family use and by crews employed by large commercial Bantam Historical Society with special thanks to Lee Swift and concerns. Both occurred at Bantam Lake. The commercial Betsy Antonucci. operation was centered on the north shore and involved White Memorial Foundation one of the largest ice block storage facilities in southern 71 Whitehall Road, P.O. Box 368 New England. The company even had railroad service Litchfield, CT 06763 making the distribution of ice to distant cities possible. (860) 567-0857 www.whitememorialcc.org 2014 West side of ice house showing box car and men shoveling snow from the tracks 8. The railroad line – This spur (now the beginning of the Butter- nut Brook Trail) led out to the main line of the Shepaug Railroad near the Lake Station. -
Student Journal Pages
♦ Caring ♦ Community ♦ Diversity ♦ Honesty ♦ Inclusiveness ♦ Respect ♦ Responsibility ♦ Stewardship ♦ Caring ♦ C ommunity Inclusiveness ♦ ♦ Diversity Honesty ♦ ♦ Honesty Honesty versity MY FROST Di ♦ ♦ VALLEY YMCA Inclusiveness Community ♦ ♦ JOURNAL Respect Caring ♦ ♦ Name: ______________________________ Responsibility Stewardship ♦ School: _____________________________ ♦ Stewardship Dates: ______________________________ Responsibility ♦ ♦ Caring Respect Respect ♦ ♦ Community Inclusiveness ♦ ♦ Diversity Honesty Honesty ♦ ♦ Honesty Diversity ♦ ♦ Inclusiveness Community Community ♦ Caring ♦ Community ♦ Diversity ♦ Honesty ♦ Inclusiveness ♦ Respect ♦ Responsibility ♦ Stewardship ♦ Caring ♦ ♦ Caring ♦ Community ♦ Diversity ♦ Honesty ♦ Inclusiveness ♦ Respect ♦ Responsibility ♦ Stewardship ♦ Caring ♦ Community FROST VALLEY YMCA Inclusiveness ♦ ♦ School Journal Diversity Honesty ♦ ♦ WORD FIND PUZZLE Honesty Diversity ♦ ♦ S S M N R I C S Y A L N C T L O P Y Y U T R S B U R U E U A T A S T D E S S E R T T I M E T I E Inclusiveness O U C F S Y T I T Y O T C J O I I S E S G S O O S L Y S H T C N P E V F S G N L B R Y C L S R T E S R R Y R E O N I S T R U I S R E T L M E T I Community ♦ I D F N A T P T M T E A M B U I L D I N G R S T ♦ M V C A E O S N B P M M I S O L L K S T E I D T Respect O Y E I M E E E T I O S Y T A O S O R T O M V N Caring D L P T A D R C N C N S Y V I T I O E R O C T C ♦ G B J U L I U S F O R S T M A N N E V A N E N I ♦ U R V E R W T N P D H S I C C U E S I S A T E E Responsibility A S N V P R N S E I O S Y L M A R O D C V -
Keeyask Generation Project Environmental Effects Summary Document
Keeyask Generation Project Environmental Effects Summary Document November 2012 Prepared for: Canadian Environmental Assessment Agency CEAR 11-03-64144 Table of Contents INTRODUCTION PART A - KEEYASK GENERATION PROJECT ENVIRONMENTAL IMPACT STATEMENT EXECUTIVE SUMMARY PART B - KEEYASK TRANSMISSION PROJECT ENVIRONMENTAL ASSESSMENT REPORT EXECUTIVE SUMMARY Introduction The Canadian Environmental Assessment Agency (the Agency) invites the public to comment on the potential environmental effects of the Keeyask Generation Project and the proposed measures to prevent or mitigate those effects as described in this document. Keeyask Hydropower Limited Partnership proposes the construction, operation and decommissioning of the Project, a 695 megawatt hydroelectric generating station to be located at Gull Rapids on the lower Nelson River, approximately 180 kilometres northeast of Thompson, Manitoba. The Keeyask Generation Project includes a powerhouse complex, spillway, dams, dykes, reservoir and supporting infrastructure (the Project). The federal environmental assessment also considers a proposal by Manitoba Hydro for a 22 kilometre transmission line to provide construction power to the Keeyask Generation Project and three 35 kilometre long transmission lines within a single corridor to transmit electricity from the Keeyask Generation Project to the existing Radisson Converter Station near Gillam, Manitoba as part of the Project. This document is based on the Environmental Impact Statement for the Keeyask Generation Project submitted by the Keeyask Hydropower Limited Partnership in July 2012 and the Environmental Assessment Report submitted by Manitoba Hydro in November 2012. The environmental impact analyses are presented in two parts within this document. Part A includes the Executive Summary of the Keeyask Generation Project Environmental Impact Statement. Part B includes Executive Summary of the Keeyask Transmission Project Environmental Assessment Report. -
Regelation: Why Does Ice Melt Under Pressure?
Regelation: why does ice melt under pressure? Phase-boundary reversible dispersivity and hydrogen-bond extraordinary recoverability Chang Q Sun [email protected] Nanyang Technological University, Singapore Unlike other unusual materials whose bonds contract under compression, the O:H nonbond undergoes contraction and the H-O bond elongation towards O:H and H-O length symmetry in water and ice. The energy drop of the H-O bond dictates the melting point Tm depression of ice. Once the pressure is relieved, the O:H-O bond fully recovers its initial state, resulting in Regelation. Ref: [1] Anomaly 2: Floating ice, http://arxiv.org/abs/1501.04171 [2] Anomaly 1: Mpemba effect, http://arxiv.org/abs/1501.00765 [3] Hydrogen-bond relaxation dynamics: resolving mysteries of water ice. Coord. Chem. Rev., 2015. 285: 109-165. 1 Anomaly: Ice Regelation Observations in Figure 1 revealed the following: 1) Ice melts under pressure and freezes again when the pressure is relieved [1-4]Error! Bookmark not defined.. An ice block remains a solid after a weighted wire cutting it through [5]. 2) Ice melts at a limit temperature of -22C under 210 MPa pressure but a -95 MPa pressure (tension) raises the melting point up to +6.5C [6, 7]. a b 280 270 (K) Quasi-solid Liquid m T 260 V pdvH TP() V C 110 TPCH()00 E 250 -100 -50 0 50 100 150 200 P(MPa) Figure 1 Regelation of ice. (a) A weighted wire cuts a block of ice through without severing it [5]. (b) Theoretical formulation [8] of the pressure dependence of the ice melting temperature Tm(P) or the phase boundary between the liquid and quasi-solid [6, 7] indicates that the H-O bond energy relaxation dictates the Tm(P). -
Lake Sturgeon (Acipenser Fulvescens) in Canada
Information in Support of the 2017 COSEWIC Assessment and Status Report on the Lake Sturgeon (Acipenser fulvescens) in Canada Cameron C. Barth, Duncan Burnett, Craig A. McDougall, and Patrick A. Nelson North/South Consultants Inc. 83 Scurfield Boulevard Winnipeg, Manitoba R3Y 1G4 2018 Canadian Manuscript Report of Fisheries and Aquatic Sciences 3166 Canadian Manuscript Report of Fisheries and Aquatic Sciences Manuscript reports contain scientific and technical information that contributes to existing knowledge but which deals with national or regional problems. Distribution is restricted to institutions or individuals located in particular regions of Canada. However, no restriction is placed on subject matter, and the series reflects the broad interests and policies of Fisheries and Oceans Canada, namely, fisheries and aquatic sciences. Manuscript reports may be cited as full publications. The correct citation appears above the abstract of each report. Each report is abstracted in the data base Aquatic Sciences and Fisheries Abstracts. Manuscript reports are produced regionally but are numbered nationally. Requests for individual reports will be filled by the issuing establishment listed on the front cover and title page. Numbers 1-900 in this series were issued as Manuscript Reports (Biological Series) of the Biological Board of Canada, and subsequent to 1937 when the name of the Board was changed by Act of Parliament, as Manuscript Reports (Biological Series) of the Fisheries Research Board of Canada. Numbers 1426 - 1550 were issued as Department of Fisheries and Environment, Fisheries and Marine Service Manuscript Reports. The current series name was changed with report number 1551. Rapport manuscrit canadien des sciences halieutiques et aquatiques Les rapports manuscrits contiennent des renseignements scientifiques et techniques qui constituent une contribution aux connaissances actuelles, mais qui traitent de problèmes nationaux ou régionaux. -
Water Quality Monitoring Areas 0 10 20 Miles Filelocation: G:\EIS\Keeyask\Publish Mxds\AEMP\AEMP WQ Monitoringareas 20120920.Mxd
Port Nelson Weir River Deer Gillam Island Island ER IV R N O S L E N Weir River Goose C re e k ÚÕ Potential Conawapa G.S. L Swift imestone Riv er KEEYASK GENERATING STATION Creek TO KETTLE GENERATING STATION PR 280 ÚÕ STEPHENS ¾À Limestone DOWNSTREAM OF KETTLE GENERATING STATION G.S. Angling Lake Kettle G.S. ÚÕ LAKE ÚÕ Longspruce ÚÕ G.S. Proposed Clark Gull Lake Keeyask G.S. Lake CLARK LAKE OUTLET TO Assean Lake KEEYASK GENERATING STATION SPLIT LAKE Aiken River Kelsey G.S. ÚÕ SPLIT LAKE AREA Fox River Legend Area Boundary NELSON RIVER 0 25 50 KilometresOkaw Creek Projection: UTM Zone 15, NAD 83 Data Source: NTS base 1:500 000 Water Quality Monitoring Areas 0 10 20 Miles FileLocation: G:\EIS\Keeyask\Publish_MXDs\AEMP\AEMP_WQ_MonitoringAreas_20120920.mxd Map 4 KEEYASK GENERATION PROJECT DRAFT - October 2012 capture the extent of effects. Sampling locations along the gradient should represent different exposure levels (e.g., within the mixing zone vs. fully mixed river condition). The hybrid design allows for statistical testing for effects in the area immediately downstream of construction activities and also provides an estimate of the spatial extent of effects. Effects will be evaluated through statistical comparisons of key parameters between reference and exposure locations during each sampling event and to pre-Project baseline data. Water quality data will also be compared to MWQSOGs and CCME guidelines for the protection of aquatic life (PAL), Health Canada guidelines for drinking water, and any regulatory requirements specified in environmental approvals for the Project. As previously noted, water quality data collected under CAMP at locations in the region will be considered to provide context for observed changes. -
Movement and Habitat Use of Juvenile Lake Sturgeon (Acipenser Fulvescens , Rafinesque, 1817) in a Large Hydroelectric Reservoir (Nelson River, Canada)
Received: 2 October 2016 | Accepted: 15 January 2017 DOI: 10.1111/jai.13378 ORIGINAL ARTICLE Movement and habitat use of juvenile Lake Sturgeon (Acipenser fulvescens , Rafinesque, 1817) in a large hydroelectric reservoir (Nelson River, Canada) C. L. Hrenchuk | C. A. McDougall | P. A. Nelson | C. C. Barth North/South Consultants Inc. , Winnipeg , MB , Canada Summary Movement and habitat utilization of juvenile Lake Sturgeon (Acipenser fulvescens) were Correspondence Claire L. Hrenchuk, North/South Consultants examined in Stephens Lake, a large hydroelectric reservoir on the Nelson River, Inc., Winnipeg, MB, Canada. Manitoba, Canada, between 21 June 2011, and 15 October 2012. Stephens Lake is Email: [email protected] defined by a sharp hydraulic gradient at the upstream end (Gull Rapids) and a pro- Funding information nounced reservoir transition zone (RTZ ), characterized by a change in substrate com- Keeyask Hydropower Limited Partnership ; Manitoba Hydro’ s Lake Sturgeon Stewardship position from coarse to fine. Twenty juvenile Lake Sturgeon <600 mm fork length and Enhancement Program were captured in the RTZ , implanted with acoustic transmitters, and tracked using stationary receivers. Our primary hypothesis considered that, if foraging behaviour was contingent on sand substrate, these fish would spend the majority of the open- water season foraging in the relatively small area where hydraulic gradients dictate sand deposition. Data indicated that tracked individuals were highly bottom oriented, and utilized deeper thalweg habitats exclusively during the first open-water season. On average, juveniles spent only 22% of their open-water time in the RTZ (river kilo- meter [rkm] 4.5–7.0). Most fish spent more time upstream as opposed to downstream, but a few individuals did utilize backwatered thalweg areas, suggesting that silt-overlay habitats may be suitable for foraging.