Cage Farm on the Benthic Environment and Nvertebrate Falina of Lake3]5, Experimental Lakes Area

Total Page:16

File Type:pdf, Size:1020Kb

Cage Farm on the Benthic Environment and Nvertebrate Falina of Lake3]5, Experimental Lakes Area THE INF'LUENCE OF A R-A.NBOW TROIJT (ONCORHYNCHUS MYKTSS) CAGE FARM ON THE BENTHIC ENVIRONMENT AND NVERTEBRATE FALINA OF LAKE3]5, EXPERIMENTAL LAKES AREA. By Rebecca Rooney A Thesis Submitted to the Faculty of Graduate Studies University of Manitoba In Partial Fulfillment of the Requirement for the Degree of Masters of Science, Department of Entomology Copyright @ 2006 by Rebecca Rooney THE UNIVERSITY OF MANITOBA FACULTY OF GRADUATE STUDIES COPYRIGHT PERMISSION The Influence of a Rainbow Trout (Oncorhyncltus mykiss) Cage Farm on the Benthic Environment and Invertebrate Fauna of Lake 375, Experimental Lakes Area by Rebecca Rooney A ThesisÆracticum submitted to the Faculty of Graduate Studies of The University of Manitoba in partial fulfillment of the requirement of the degree of Master of Science Rebecca Rooney O 2006 , Permission has been granted to the Library of the University of Manitoba to lend or sell copies of 'l this thesis/practicum, to the National Library of Canada to microfilm this thesis and to lend or sell ' copies of the film, and to University Microfilms Inc. to publish an abstract of this thesis/practicum. This reproduction or copy of this thesis has been made available by authority of the copyright owner solely for the purpose of private study and research, and may only be reproduced and copied I Ls permitted by copyright laws or with express written authorization from the copyright owner. ,i Acknowledgements I would never have completed this thesis without the inspiration, support, and guidance of my advisor Dr. Cheryl Podemski. Every time I strayed from the path and became lost, I could trust her like a compass. I would also like to thank my committee members Dr. Terry Galloway and Dr. Brenda Hann for their encouragement tempered by reality checks. Kelsey Fetterly, Natalie Nikkel, and Shannon McPhee provided field assistance and kept singing despite the hour or the odour. Dr. Cindy Gilmore and her team provided invaluable advice on working with sulfide. I would also like to thank Steven Page for answering my chemistry questions and Susan Kasian for indefatigable enthusiasm and statistical expertise. puuiu Azevedo and Mike Meeker also shared their knowledge with me. The graduate students at the Freshwater Institute proved it could be done and helped me keep faith. I particularly appreciate the inspiration and emotional support of Ginger Gill, Mark Lowden, Dianne Orihel, and Lisa Loseto. Of course, none of this would have been possible without the love and support of my family, particularly Marie-Lynn Hamilton. Thank you for complaining minimally about my absence. I promise to be home more often, unlessItryaPhD... Abstract I examined the development of effects from an experimental rainbow trout farm on sediment nutrients; metals; pore-water ammonia; sulfide; and zoobenthic density, richness, and biomass across the spatial gradient in organic loading created with distance from the farm. Pore-water total ammonia was the first variable to respond. Beneath the farm it reached 481.6 times the concentration in reference sediment (77 mgl-') by September 2004. At this time sediment organic carbon, nitrogen, and phosphonts were 3.2,4.5, and 18.6 times the reference sediment concentration, respectively. Invertebrate density was significantly reduced under the cage, reaching 442 individuals m-2 in October 2003 vs. 11089 individuals m-2 atreference stations. Thereafter, density remained below 600 individuals m-' . Taxarichness was also depressed, but biomass was variable. Variables with the most potential for incorporation into monitoring schemes included total ammonia and invertebrate density. The effects of farming were localized, extending only 5 m beyond the cage edge. lll Table of Contents Acknowledgements ii Abstract iii Table of Contents iv List of Tables vii List of Figures viii Chapter I: Aquaculture and the Receiving Environment 1 Context of the Industry I The State of Capture Fisheries i Aquaculture: an Alternative 1 History of Aquaculture 2 Three Forms of Freshwater Aquaculture J Pond Førming J Land-based Farming J Cage Farming 4 Aquaculture in Canada 6 History 6 Canadian Freshwater Aquaculture Markets 6 Environmental Impacts of Cage Aquaculture 8 Soluble llaste 8 Solid Waste 9 Effects on Sediment Chemistry T2 Sediment Nutrients t2 Eutrophication 13 Heavy Metals T7 Effects on Water Column and Pore-Water Chemistry t9 The Importance of Pore-Water I9 Dissolved Oxygen 20 Pore-Water Ammonia 23 Sulfide 25 Effects on the Zoobenthos 26 Evidencefor Pearson and Rosenberg Predictions: Marine Case Studies 29 Evidencefor Pearson and Rosenberg Predictions: Fresltwater Case Studies 3i Conclusion 36 Summary of observed fficts J/ Problems with the Literature 39 iv Chapter II: Description of the Study 43 Knowledge Gaps in the Literature 40 Tables and Figures 42 Study Objectives 43 Site Description 45 Chapter III: Farm Effects on the Benthic Environment 49 Farm Operation 46 Tables and Figures 47 Introduction 49 Methods 53 Study Design 53 Pore-water Chemistry 54 Sediment Chemistry 55 Faeces, Feed, and Net Pen Materiøl 56 Statistical Analyses s6 Results 58 Principal Components Analysis 58 Pore-water Chemistry 58 Sediment Chemistry 59 Faeces, Feed, and Net Pen Material 60 Discussion 60 Princip al Comp onents Analysis 60 Pore-water Chemistry 61 Sediment Chemistry 6s Conclusions ll Tables and Figures 73 Chapter IV: Farm Effects on the Zoobenthos 81 lntroduction 81 Methods 85 Study Design 8s Core Samples 85 Invertebrate Metrics 86 Statistical Analyses 88 Results 89 Principal Components Analysis 89 Changes with Distance 90 Discussion 93 Community Changes: PCA 93 Changes in Density 96 Changes in Taxa Richness 100 Changes in Biomass 101 Chapter V: General Conclusions - lnterrelation of Chemistry and Biology rt2 Recommendations t04 Conclusion 105 Summary of Findings T12 Chemistry TT2 Biology 113 Interrelation of Chemical and Biological Metrics 115 Whole Lake Implications t20 Eutrophication t20 Trophic Effects T22 Recommendations for Future Studies r22 Recommendations for Monitoring r27 Monitoring Study Design t21 Chemistry r27 Biology 130 Propos ed Monitoring Scheme r33 Conclusion r33 Tables and Figures 135 References 137 Appendix I: Taxa Recovered fromL375 t70 vi List of Tables Table2.I: Summary of farming operation information: stocking and harvest dates, number of fish, and mean fish weight. 47 Table 3.1: Federal and provincial sediment quality guidelines for selected variables, with values reported it pg g-t dry-weight (CCME 1995; Jaagumagi and Persaud 1999). IJ Table 3.2: Two-tailed t-test results, comparing sediment TOC, TN, and TP in October 2003 with concentrations obtained in September 2004. 74 Table 3.3: Mean concentration of metals and nutrients in reference sediment (45 m from farm edge), sediment beneath the cage, feed, farm rvaste, and the net pen material. Concentrations in mg g-l dry-weight. NA: not analysed. 75 Table 4.1: Coefficients used in length-mass conversion for Chironomidae larvae. Values were obtained from Benke et al. (1999). r07 Table 4.2: Station scores on the three significant principal components analysis axes obtained from analysis of invertebrate density along the transect sampled in June 2003. The first, second, and third axes explai ned 39 .2o/o, 3 4.Io/o, and Il .4o/o of the variation in the dataset, respectively. Taxawith eigenvectors > 0.25 included : Harp acticoida (0. 290), Tanytarsin i (-0'259), | | Orthoc ladii ni (-0 .4228), and Nemato da (-0 .7 3 3) . 108 Table 5.1: Results of first sampling transect to show a significant difference between station means in one-way ANOVAs on 1o g-transformed chemical and biolo gical metrics. 135 Table 5.2: Lethal concentration, producing 50o/o mortality after exposure to unionized ammonia for the specified duration, excepting sphaeriids and gastropods. Values for Sphaeriidae and Gastropoda are EC5es where the response for Sphaeriidae is burial and for Gastropoda is retreat into shell. NR indicates not reported. t36 vii List of Figures Figure 1.1: Predicted relationship between benthic invertebrate diversity (-), density (...), and biomass C I along a gradient in organic enrichment, as predicted by Pearson and Rosenberg (1e78). 42 Figure 2.1: Bathymetric map of L375 (Kaisian, S. unpublished data), showing the location of the 10 m by 10 m farm (tan square) and the location of sampling sites (red and blue squares) along the 15 m isobath. Sample label C is beneath the cage centre, E is beneath the cage edge, and numbers represent the distance from the cage edge in metres. Sampling sites in red were sampled on all sampling dates, but those in blue were added to the transect only for July, August, and September 2004. 48 Figure 3.1 : Mean scores on the first PCA axis for sediment collected from along the transect with distance from the farm's edge on September 2004. The axis explained 89.8% of the variation in the dataset. Variables with eigenvectors > 10.251 included total pore-water ammonia (-0.549), phosphorus (-0.279), calcium (- 0.249), aluminum (0.280), and iron (0.286). Spread on y-axis is only to disperse points for legibility. The y-axis does not represent a variable. 76 Figure 3.2: Mean total ammonia (mg L-t¡ in sediment pore-water obtained from the transect stations sampled on July 2003 (a), October 2003 (b), }l4ay 2004 (c), and September 2004 (d). Error bars indicate one standard error of the mean. Circles reflect Tukey's groupings. In September 2004, the 1 m station was excluded from statistical analyses to meet ANOVA assumptions; it is therefore not part of a Tukey's group' 77 Figure 3.3 Mean sediment pH at stations along the distance transect. Error bars represent one standard error of the mean. Circles indicate Tukey's groupings. 78 viii Figure 3.4: Mean sediment total organic carbon (TOC), total nitrogen (TN), and total phosphorus (TP) concentration (mg g-1) at different distances from the L375 farm.
Recommended publications
  • Lake Constance)
    Characteristics and implications of surface gravity waves in the littoral zone of a large lake (Lake Constance) Dissertation Zur Erlangung des akademischen Grades des Doktors der Naturwissenschaften (Dr. rer. nat.) an der Universität Konstanz Mathematisch-Naturwissenschaftliche Sektion Fachbereich Biologie vorgelegt von Hilmar Hofmann Konstanz, 2007 Tag der mündlichen Prüfung: 23.06.2008 Referent: Prof. Dr. Frank Peeters Referent: Dr. habil. Klaus Jöhnk Referent: Prof. Dr. habil. Karl-Otto Rothhaupt Bibliografische Information der Deutschen Nationalbibliothek Die Deutsche Nationalbibliothek verzeichnet diese Publikation in der Deutschen Nationalbibliografie; detaillierte bibliografische Daten sind im Internet über http://dnb.ddb.de abrufbar. 1. Aufl. - Göttingen : Cuvillier, 2008 Zugl.: Konstanz, Univ., Diss., 2007 978-3-86727-714-3 © CUVILLIER VERLAG, Göttingen 2008 Nonnenstieg 8, 37075 Göttingen Telefon: 0551-54724-0 Telefax: 0551-54724-21 www.cuvillier.de Alle Rechte vorbehalten. Ohne ausdrückliche Genehmigung des Verlages ist es nicht gestattet, das Buch oder Teile daraus auf fotomechanischem Weg (Fotokopie, Mikrokopie) zu vervielfältigen. 1. Auflage, 2008 Gedruckt auf säurefreiem Papier 978-3-86727-714-3 Table of contents Summary 1 Zusammenfassung 3 General introduction 7 Chapter 1: Temporal scales of water level fluctuations in lakes and 17 their ecological implications Introduction 18 Materials and methods 19 Results 20 Discussion 25 Conclusions 32 Chapter 2: The relative importance of wind and ship waves in the 35 littoral zone
    [Show full text]
  • Global Lake Responses to Climate Change
    REVIEWS Global lake responses to climate change R. Iestyn Woolway 1,2 ✉ , Benjamin M. Kraemer 3,11, John D. Lenters4,5,6,11, Christopher J. Merchant 7,8,11, Catherine M. O’Reilly 9,11 and Sapna Sharma10,11 Abstract | Climate change is one of the most severe threats to global lake ecosystems. Lake surface conditions, such as ice cover, surface temperature, evaporation and water level, respond dramatically to this threat, as observed in recent decades. In this Review, we discuss physical lake variables and their responses to climate change. Decreases in winter ice cover and increases in lake surface temperature modify lake mixing regimes and accelerate lake evaporation. Where not balanced by increased mean precipitation or inflow, higher evaporation rates will favour a decrease in lake level and surface water extent. Together with increases in extreme- precipitation events, these lake responses will impact lake ecosystems, changing water quantity and quality, food provisioning, recreational opportunities and transportation. Future research opportunities, including enhanced observation of lake variables from space (particularly for small water bodies), improved in situ lake monitoring and the development of advanced modelling techniques to predict lake processes, will improve our global understanding of lake responses to a changing climate. Lakes are critical natural resources that are sensitive to For example, changes in ice cover and water temperature changes in climate. There are more than 100 million modify (and are influenced by) evaporation rates9, which lakes globally1, holding 87% of Earth’s liquid sur­ can subsequently alter lake levels and surface water face freshwater2. Lakes support a global heritage of extent12.
    [Show full text]
  • Diurnal and Seasonal Variations of Thermal Stratification and Vertical
    Journal of Meteorological Research 1 Yang, Y. C., Y. W. Wang, Z. Zhang, et al., 2018: Diurnal and seasonal variations of 2 thermal stratification and vertical mixing in a shallow fresh water lake. J. Meteor. 3 Res., 32(x), XXX-XXX, doi: 10.1007/s13351-018-7099-5.(in press) 4 5 Diurnal and Seasonal Variations of Thermal 6 Stratification and Vertical Mixing in a Shallow 7 Fresh Water Lake 8 9 Yichen YANG 1, 2, Yongwei WANG 1, 3*, Zhen ZHANG 1, 4, Wei WANG 1, 4, Xia REN 1, 3, 10 Yaqi GAO 1, 3, Shoudong LIU 1, 4, and Xuhui LEE 1, 5 11 1 Yale-NUIST Center on Atmospheric Environment, Nanjing University of Information, 12 Science and Technology, Nanjing 210044, China 13 2 School of Environmental Science and Engineering, Nanjing University of Information, 14 Science and Technology, Nanjing 210044, China 15 3 School of Atmospheric Physics, Nanjing University of Information, Science and Technology, 16 Nanjing 210044, China 17 4 School of Applied Meteorology, Nanjing University of Information, Science and 18 Technology, Nanjing 210044, China 19 5 School of Forestry and Environmental Studies, Yale University, New Haven, CT 06511, 20 USA 21 (Received June 21, 2017; in final form November 18, 2017) 22 23 Supported by the National Natural Science Foundation of China (41275024, 41575147, Journal of Meteorological Research 24 41505005, and 41475141), the Natural Science Foundation of Jiangsu Province, China 25 (BK20150900), the Startup Foundation for Introducing Talent of Nanjing University of 26 Information Science and Technology (2014r046), the Ministry of Education of China under 27 grant PCSIRT and the Priority Academic Program Development of Jiangsu Higher Education 28 Institutions.
    [Show full text]
  • Long-Term Influence of Climate and Experimental Eutrophication Regimes on Phytoplankton 4 Blooms 5 6 7 Kateri R
    bioRxiv preprint doi: https://doi.org/10.1101/658799; this version posted June 3, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Article type: Letter 2 3 Long-term influence of climate and experimental eutrophication regimes on phytoplankton 4 blooms 5 6 7 Kateri R. Salk1, Jason J. Venkiteswaran2, Raoul-Marie Couture3, Scott N. Higgins4, Michael J. 8 Paterson4, and Sherry L. Schiff5 9 10 1Nicholas School of the Environment, Duke University, Durham, North Carolina, USA 11 2Department of Geography and Environmental Studies, Wilfrid Laurier University, Ontario, 12 Canada 13 3Department of Chemistry, Université Laval, Quebec, Canada 14 4IISD Experimental Lakes Area Inc., Manitoba, Canada 15 5Department of Earth and Environmental Sciences, University of Waterloo, Ontario, Canada 16 17 18 Corresponding author: 19 Kateri Salk 20 [email protected] 21 Nicholas School of the Environment 22 Duke University 23 Durham, NC 27708 24 USA 25 26 Author Contribution Statement 27 KRS conducted modeling and analysis efforts. RMC provided expertise on model application 28 and validation. SLS and JJV provided guidance on the research questions. KRS, RMC, JJV, and 29 SLS analyzed model fit, guided scenario analysis, and provided interpretations of results. SNH 30 and MJP provided guidance on historical data analyses, model input data, and postprocessing 31 analyses. KRS wrote the manuscript, and all coauthors contributed edits to the manuscript. 32 1 bioRxiv preprint doi: https://doi.org/10.1101/658799; this version posted June 3, 2019.
    [Show full text]
  • David W. Schindler (1940–2021): Trailblazing Scientist and Advocate for the Environment RETROSPECTIVE Karen A
    RETROSPECTIVE David W. Schindler (1940–2021): Trailblazing scientist and advocate for the environment RETROSPECTIVE Karen A. Kidda,1, William F. Donahueb, Erin N. Kellyc, Peter R. Leavittd, and Heidi Swansonc On March 4th, 2021, the global aquatic sciences com- munity lost one of its most influential scientists, David W. Schindler. Dave’s landmark research that led to bet- ter protection of fresh waters around the world, his un- canny ability to identify, raise the profile of, and address key crises in aquatic sciences, and his tireless education of the public and decision makers on environmental issues have left an unmatched legacy. Throughout his monumental career, Dave’s research shone a light on the ecological crises unfolding in fresh- water ecosystems. His trailblazing approach included listening to those who were closest to the environment or a problem he was working on, particularly the wisdom of Indigenous knowledge holders, applying science in a way that was respectful of Indigenous ways of know- ing, and using research findings and his own reputa- tion to amplify their voices and effect more holistic stewardship. Much to the chagrin of some politicians and industries, Dave’s remarkable scientific acumen was matched by his tireless commitment and formida- ble ability to raise public awareness of environmental issues. For him, fresh waters had to be protected, and to do so, science had to be communicated: it was this moral conscience and modus operandi that under- pinned Dave’s decades of effecting real-world change. For many years, he was the most quoted Canadian ac- ademic in the media, a measure of his unwavering com- mitment to putting science in the public eye and one that was recognized with the Royal Canadian Institute’s David W.
    [Show full text]
  • Nutrients, Eutrophication and Harmful Algal Blooms Along the Freshwater to Marine Continuum
    Received: 18 April 2019 Revised: 22 June 2019 Accepted: 2 July 2019 DOI: 10.1002/wat2.1373 OVERVIEW Nutrients, eutrophication and harmful algal blooms along the freshwater to marine continuum Wayne A. Wurtsbaugh1 | Hans W. Paerl2 | Walter K. Dodds3 1Watershed Sciences Department, Utah State University, Logan, Utah Abstract 2Institute of Marine Sciences, University of Agricultural, urban and industrial activities have dramatically increased aquatic North Carolina at Chapel Hill, Morehead nitrogen and phosphorus pollution (eutrophication), threatening water quality and City, North Carolina biotic integrity from headwater streams to coastal areas world-wide. Eutrophication 3Division of Biology, Kansas State creates multiple problems, including hypoxic “dead zones” that reduce fish and University, Manhattan, Kansas shellfish production; harmful algal blooms that create taste and odor problems and Correspondence threaten the safety of drinking water and aquatic food supplies; stimulation of Wayne A. Wurtsbaugh, Watershed Sciences Department, Utah State University, Logan, greenhouse gas releases; and degradation of cultural and social values of these Utah 94322-5210. waters. Conservative estimates of annual costs of eutrophication have indicated $1 Email: [email protected] billion losses for European coastal waters and $2.4 billion for lakes and streams in Funding information the United States. Scientists have debated whether phosphorus, nitrogen, or both NSF Konza LTER, Grant/Award Numbers: need to be reduced to control eutrophication along the freshwater to marine contin- NSF OIA-1656006, NSF DEB 1065255; uum, but many management agencies worldwide are increasingly opting for dual Dimensions of Biodiversity, Grant/Award Numbers: 1831096, 1240851; US National control. The unidirectional flow of water and nutrients through streams, rivers, Science Foundation, Grant/Award Numbers: lakes, estuaries and ultimately coastal oceans adds additional complexity, as each CBET 1230543, 1840715, OCE 9905723, of these ecosystems may be limited by different factors.
    [Show full text]
  • Long-Term Changes in Cyanobacteria Populations in Lake Kinneret (Sea of Galilee), Israel: an Eco-Physiological Outlook
    Life 2015, 5, 418-431; doi:10.3390/life5010418 OPEN ACCESS life ISSN 2075-1729 www.mdpi.com/journal/life Review Long-Term Changes in Cyanobacteria Populations in Lake Kinneret (Sea of Galilee), Israel: An Eco-Physiological Outlook Ora Hadas 1,†,*, Aaron Kaplan 2,† and Assaf Sukenik 3,† 1 The Yigal Allon Kinneret Limnological Laboratory, Israel Oceanographic and Limnological Research, Migdal, Israel 2 Department of Plant and Environmental Sciences, The Hebrew University of Jerusalem, Jerusalem, Israel; E-Mail: [email protected] 3 The Yigal Allon Kinneret Limnological Laboratory, Israel Oceanographic and Limnological Research, Migdal, Israel; E-Mail: [email protected] † These authors contributed equally to this work. * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +972-4-6721444 (ext. 204). Academic Editors: John C. Meeks and Robert Haselkorn Received: 19 November 2014 / Accepted: 29 January 2015 / Published: 5 February 2015 Abstract: The long-term record of cyanobacteria abundance in Lake Kinneret (Sea of Galilee), Israel, demonstrates changes in cyanobacteria abundance and composition in the last five decades. New invasive species of the order Nostocales (Aphanizomenon ovalisporum and Cylindrospermopsis raciborskii) became part of the annual phytoplankton assemblage during summer-autumn. Concomitantly, bloom events of Microcystis sp. (Chroococcales) during winter-spring intensified. These changes in cyanobacteria pattern may be partly attributed to the management policy in Lake Kinneret’s vicinity and watershed aimed to reduce effluent discharge to the lake and partly to climate changes in the region; i.e., increased water column temperature, less wind and reduced precipitation. The gradual decrease in the concentration of total and dissolved phosphorus and total and dissolved nitrogen and an increase in alkalinity, pH and salinity, combined with the physiological features of cyanobacteria, probably contributed to the success of cyanobacteria.
    [Show full text]
  • LEE HRENCHUK BIOLOGIST, IISD Experimental Lakes Area
    LEE HRENCHUK BIOLOGIST, IISD Experimental Lakes Area Lee is part of the fish crew at IISD-ELA. Her research focuses on monitoring and assessing the effects of a variety of environmental perturbations (including mercury deposition, cage aquaculture, endocrine disrupting chemicals, eutrophication and climate change) on fish ecology and behaviour in small, oligotrophic lakes in the boreal shield. Lee conducted aquatic field research in both the Canadian Arctic and in Antarctica before settling more permanently at IISD-ELA. Post-graduate studies included examining the accumulation of mercury in yellow perch as part of the whole-lake Mercury Experiment to Assess Atmospheric Loading In Canada and the United States (METAALICUS) at ELA. Lee is an advocate for communicating science to a broader audience and has volunteered with Fort Whyte Alive, the Manitoba Museum and Fisheries and Oceans Canada to talk about scientific ideas and environmental issues with the public. Employment Biologist (IISD Experimental Lakes Area Inc.) Supervisors: Dr. Michael Paterson, Dr. Vince Palace April 2014 to present When IISD Experimental Lakes Area (IISD-ELA) took over operation of ELA from Fisheries and Oceans Canada, I chose to leave my position with DFO and continue my research program with IISD-ELA. My experience and responsibilities at IISD-ELA are much the same as they were with DFO, conducting scientific research to assess the impacts of whole-ecosystem experiments on fish ecology and behaviour at IISD-ELA. My research has focused on monitoring the effects of a variety of environmental perturbations (including mercury deposition, cage aquaculture, endocrine disrupting chemicals, eutrophication, and climate change) on fish in small, oligotrophic lakes in the boreal shield.
    [Show full text]
  • The Atmosphere Submodel for the Assessment of Canada's Nuclear
    } * AECL CA9400058 ~ AECL Research EACL Recherche AECL-9889, COG-91-199 The Atmosphere Submodel for the Assessment of Canada's Nuclear Fuel Waste Management Concept Le sous-modele d'atmosphere pour revaluation du concept du Programme canadien de gestion des dechets de combustible nucleaire B.D. Amiro September 1992 septembre AECL RESEARCH THE ATMOSPHERE SUBMODEL FOR THE ASSESSMENT OF CANADA'S NUCLEAR FUEL WASTE HANAGEMEKT CONCEPT by 8.D. Aniro Whiteshell Laboratories Pinawa, Manitoba ROE 1L0 1992 AECL-9889 COG-91-199 LE SOUS-MODÈLE D'ATMOSPHÈRE POUR L'ÉVALUATION DU CONCEPT DU PROGRAMME CANADIEN DE GESTION DES DÉCHETS DE COMBUSTIBLE NUCLÉAIRE par B.D. Amlro RÉSUMÉ Dans le cadre du Programme canadien de gestion des déchets de combustible nucléaire, on fait de la recherche sur un concept de stockage permanent des déchets de combustible nucléaire immobilisés dans une enceinte creusée à grande profondeur dans la roche plutonlque stable. Quand les barrières de protection auront fini par se rompre dans un avenir lointain, des nucléides radioactifs et chimiquement toxiques, entraînés par les eaux souterraines, pourraient migrer de l'enceinte à la biosphère. Ils pourraient parcourir un cycle dans les eaux superficielles, le sol, l'atmosphère et la chaîne alimentaire. Entre autres, le programme vise à évaluer le mouvement des nucléides par des techniques de modélisation pour calculer la dose radio- logique aux êtres humains et la concentration de contaminants dans 1'environnement. Afin d'atteindre ces objectifs, on a réalisé un modèle de biosphère com- portant quatre sous-modèles. On décrit dans ce rapport le sous-modèle d'atmosphère et les voies par lesquelles les nucléides pourraient traverser l'atmosphère.
    [Show full text]
  • Yukon and Kuskokwim Whitefish Strategic Plan
    U.S. Fish & Wildlife Service Whitefish Biology, Distribution, and Fisheries in the Yukon and Kuskokwim River Drainages in Alaska: a Synthesis of Available Information Alaska Fisheries Data Series Number 2012-4 Fairbanks Fish and Wildlife Field Office Fairbanks, Alaska May 2012 The Alaska Region Fisheries Program of the U.S. Fish and Wildlife Service conducts fisheries monitoring and population assessment studies throughout many areas of Alaska. Dedicated professional staff located in Anchorage, Fairbanks, and Kenai Fish and Wildlife Offices and the Anchorage Conservation Genetics Laboratory serve as the core of the Program’s fisheries management study efforts. Administrative and technical support is provided by staff in the Anchorage Regional Office. Our program works closely with the Alaska Department of Fish and Game and other partners to conserve and restore Alaska’s fish populations and aquatic habitats. Our fisheries studies occur throughout the 16 National Wildlife Refuges in Alaska as well as off- Refuges to address issues of interjurisdictional fisheries and aquatic habitat conservation. Additional information about the Fisheries Program and work conducted by our field offices can be obtained at: http://alaska.fws.gov/fisheries/index.htm The Alaska Region Fisheries Program reports its study findings through the Alaska Fisheries Data Series (AFDS) or in recognized peer-reviewed journals. The AFDS was established to provide timely dissemination of data to fishery managers and other technically oriented professionals, for inclusion in agency databases, and to archive detailed study designs and results for the benefit of future investigations. Publication in the AFDS does not preclude further reporting of study results through recognized peer-reviewed journals.
    [Show full text]
  • Lake Aeration System for Canyon Lake, California
    LAKE AERATION SYSTEM FOR CANYON LAKE, CALIFORNIA Prepared for: Lake Elsinore & San Jacinto Watersheds Authority (LASJWA) Santa Ana Watershed Project Authority (SAWPA) 11615 Sterling Ave. Riverside, California 92503-4979 Prepared by: Arlo W. Fast Limnological Associates <www.arlofast.com> May 2002 EXECUTIVE SUMMARY Canyon Lake is a monomictic, eutrophic lake that typically stratifies from about late-February/early-March through late-November/early-December each year. The water column is divided into three depth zones, with the deep-water hypolimnion starting at about the 20 to 25 foot depths by mid- summer, with oxygen depletions at or near zero at 16 to 18 feet. The hypolimnion becomes anaerobic and devoid of dissolved oxygen by early summer each year. This anaerobiosis results in releases of dissolved iron, manganese, ammonia, hydrogen sulfide, phosphorus (P) and other substances that degrade potable water quality. Phosphorus release from sediments under anaerobic conditions may increase eutrophication through internal P loading. Artificial destratification by a combination of air injection and axial-flow water pumps should maintain aerobic conditions throughout the water column in the main body of Canyon Lake all year. A well-mixed condition and aerobic conditions in Canyon Lake should achieve expected improvements in water quality including reduced iron, manganese, ammonia, hydrogen sulfide, and phosphorus, with probable reductions in algal densities. This hybrid destratification system includes two axial-flow water pumps (3-HP each) and 400-SCFM of air injection from two air-line diffusers. Total capital and annual operating costs are estimated at $325,000 and $35,000/yr respectively. 2 TABLE OF CONTENTS EXECUTIVE SUMMARY……………………………………… 2 I.
    [Show full text]
  • IISD Experimental Lakes Area the World’S Freshwater Laboratory
    IISD Experimental Lakes Area The World’s Freshwater Laboratory “IISD-ELA is the place for high-impact science. It is unlike any other facility for its ability to answer the big and pressing questions.” —Dr. Karen Kidd, Canada Research Chair, Canadian Rivers Institute and University of New Brunswick In a time of growing populations and a rapidly changing climate, the world is struggling to respond to challenges to their fresh water. These challenges include the impacts of climate change, agricultural runoff, water management, contaminants such as mercury and organic pollutants, and a growing list of new chemical substances. ENTER IISD-ELA: an exceptional natural laboratory comprised of 58 small lakes and their watersheds set aside for scientific research. Located in a remote region of northwestern Ontario, Canada, it is one of the only places in the world where it is possible to conduct experiments on whole ecosystems. By manipulating these small lakes, scientists are able to examine how all aspects of the ecosystem—from the atmosphere to fish populations—respond. Findings of real-world experiments are often much more accurate than those from research conducted at smaller scales, such as in laboratories. For the last 50 years, our unique research approach has influenced billion-dollar decisions of governments and industries. It has generated more cost-effective environmental policies, regulations and management—all in the name of keeping our water clean. Algal Blooms Blanketing our Lakes Changing Climate, Algal blooms occur when too many nutrients enter a body of water, and Changing Lakes algae feed on them. Groundbreaking discoveries at IISD-ELA regarding Our scientists are mimicking which nutrients cause algal blooms led to policy changes around the conditions that could be world that restrict phosphorus entering lakes and rivers.
    [Show full text]