1 Alberta Conservation Association 2017/18 Project Summary Report Project Name: North Saskatchewan River Drainage Fish Sustainab
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Municipal Guide
Municipal Guide Planning for a Healthy and Sustainable North Saskatchewan River Watershed Cover photos: Billie Hilholland From top to bottom: Abraham Lake An agricultural field alongside Highway 598 North Saskatchewan River flowing through the City of Edmonton Book design and layout by Gwen Edge Municipal Guide: Planning for a Healthy and Sustainable North Saskatchewan River Watershed prepared for the North Saskatchewan Watershed Alliance by Giselle Beaudry Acknowledgements The North Saskatchewan Watershed Alliance would like to thank the following for their generous contributions to this Municipal Guide through grants and inkind support. ii Municipal Guide: Planning for a Healthy and Sustainable North Saskatchewan Watershed Acknowledgements The North Saskatchewan Watershed Alliance would like to thank the following individuals who dedicated many hours to the Municipal Guide project. Their voluntary contributions in the development of this guide are greatly appreciated. Municipal Guide Steering Committee Andrew Schoepf, Alberta Environment Bill Symonds, Alberta Municipal Affairs David Curran, Alberta Environment Delaney Anderson, St. Paul & Smoky Lake Counties Doug Thrussell, Alberta Environment Gabrielle Kosmider, Fisheries and Oceans Canada George Turk, Councillor, Lac Ste. Anne County Graham Beck, Leduc County and City of Edmonton Irvin Frank, Councillor, Camrose County Jolee Gillies,Town of Devon Kim Nielsen, Clearwater County Lorraine Sawdon, Fisheries and Oceans Canada Lyndsay Waddingham, Alberta Municipal Affairs Murray Klutz, Ducks -
Fisheries Barriers in Native Trout Drainages
Alberta Conservation Association 2018/19 Project Summary Report Project Name: Fisheries Barriers in Native Trout Drainages Fisheries Program Manager: Peter Aku Project Leader: Scott Seward Primary ACA Staff on Project: Jason Blackburn, David Jackson, and Scott Seward Partnerships Alberta Environment and Parks Environment and Climate Change Canada Key Findings • We compiled existing barrier location information within the Peace River, Athabasca River, North Saskatchewan River, and Red Deer River basins into a centralized database. • We catalogued fish habitat and community data for the Narraway River watershed for use in a population restoration feasibility framework. • We identified 107 potential barrier locations within the Narraway River watershed, using Google Earth ©, which will be refined using valley confinement modeling and validated with ground truthing in 2019. Introduction Invasive species pose one of the greatest threats to Alberta native trout species, through hybridization, competition, and displacement. These threats are partially mediated by the presence of natural headwater fish-passage barriers, namely waterfalls, that impede upstream 1 invasions. In Alberta, several sub-populations of native trout remain genetically pure primarily because of waterfalls. Identification and inventory of waterfalls in the Peace River, Athabasca River, North Saskatchewan River, and Red Deer River basins isolating pure populations and their habitats is critical to inform population recovery and build implementation strategies on a stream by stream basis. For example, historical stocking of non-native trout to the Narraway River watershed may be endangering native bull trout and Arctic grayling. Non-native cutthroat trout, rainbow trout, and brook trout have been stocked in the Torrens River, Stetson Creek, and Two Lakes, all of which have connectivity to the Narraway River. -
Brazeau River Gas Plant
BRAZEAU RIVER GAS PLANT Headquartered in Calgary with operations focused in Western Canada, KEYERA operates an integrated Canadian-based midstream business with extensive interconnected assets and depth of expertise in delivering midstream energy solutions. Image input specifications Our business consists of natural gas gathering and processing, Width 900 pixels natural gas liquids (NGLs) fractionation, transportation, storage and marketing, iso-octane production and sales and diluent Height 850 pixels logistic services for oil sands producers. 300dpi We are committed to conducting our business in a way that 100% JPG quality balances diverse stakeholder expectations and emphasizes the health and safety of our employees and the communities where we operate. Brazeau River Gas Plant The Brazeau River gas plant, located approximately 170 kilometres southwest of the city of Edmonton, has the capability PROJECT HISTORY and flexibility to process a wide range of sweet and sour gas streams with varying levels of NGL content. Its process includes 1968 Built after discovery of Brazeau Gas inlet compression, sour gas sweetening, dehydration, NGL Unit #1 recovery and acid gas injection. 2002 Commissioned acid gas injection system Brazeau River gas plant is located in the West Pembina area of 2004 Commissioned Brazeau northeast Alberta. gas gathering system (BNEGGS) 2007 Acquired 38 kilometre sales gas pipeline for low pressure sweet gas Purchased Spectra Energy’s interest in Plant and gathering system 2015 Connected to Twin Rivers Pipeline 2018 Connected to Keylink Pipeline PRODUCT DELIVERIES Sales gas TransCanada Pipeline System NGLs Keylink Pipeline Condensate Pembina Pipeline Main: 780-894-3601 24-hour emergency: 780-894-3601 www.keyera.com FACILITY SPECIFICATIONS Licensed Capacity 218 Mmcf/d OWNERSHIP INTEREST Keyera 93.5% Hamel Energy Inc. -
Brazeau Subwatershed
5.2 BRAZEAU SUBWATERSHED The Brazeau Subwatershed encompasses a biologically diverse area within parts of the Rocky Mountain and Foothills natural regions. The Subwatershed covers 689,198 hectares of land and includes 18,460 hectares of lakes, rivers, reservoirs and icefields. The Brazeau is in the municipal boundaries of Clearwater, Yellowhead and Brazeau Counties. The 5,000 hectare Brazeau Canyon Wildland Provincial Park, along with the 1,030 hectare Marshybank Ecological reserve, established in 1987, lie in the Brazeau Subwatershed. About 16.4% of the Brazeau Subwatershed lies within Banff and Jasper National Parks. The Subwatershed is sparsely populated, but includes the First Nation O’Chiese 203 and Sunchild 202 reserves. Recreation activities include trail riding, hiking, camping, hunting, fishing, and canoeing/kayaking. Many of the indicators described below are referenced from the “Brazeau Hydrological Overview” map locat- ed in the adjacent map pocket, or as a separate Adobe Acrobat file on the CD-ROM. 5.2.1 Land Use Changes in land use patterns reflect major trends in development. Land use changes and subsequent changes in land use practices may impact both the quantity and quality of water in the Subwatershed and in the North Saskatchewan Watershed. Five metrics are used to indicate changes in land use and land use practices: riparian health, linear development, land use, livestock density, and wetland inventory. 5.2.1.1 Riparian Health 55 The health of the riparian area around water bodies and along rivers and streams is an indicator of the overall health of a watershed and can reflect changes in land use and management practices. -
Land Use, Climate Change and Ecological Responses in the Upper
Land use, climate change and ecological responses in the Upper North 1 Saskatchewan and Red Deer River Basins: A scientific assessment Land use, climate change and ecological responses in the Upper North Saskatchewan and Red Deer River Basins: A scientific assessment Dan Farr, Colleen Mortimer, Faye Wyatt, Andrew Braid, Charlie Loewen, Craig Emmerton, Simon Slater Cover photo: Wayne Crocker This publication can be found at: open.alberta.ca/publications/9781460140697. Comments, questions, or suggestions regarding the content of this document may be directed to: Ministry of Environment and Parks, Environmental Monitoring and Science Division 10th Floor, 9888 Jasper Avenue NW, Edmonton, Alberta, T5J 5C6 Tel: 780-229-7200 Toll Free: 1-844-323-6372 Fax: 780-702-0169 Email: [email protected] Media Inquiries: [email protected] Website: environmentalmonitoring.alberta.ca Recommended citation: Farr. D., Mortimer, C., Wyatt, F., Braid, A., Loewen, C., Emmerton, C., and Slater, S. 2018. Land use, climate change and ecological responses in the Upper North Saskatchewan and Red Deer River Basins: A scientific assessment. Government of Alberta, Ministry of Environment and Parks. ISBN 978-1-4601-4069-7. Available at: open.alberta.ca/publications/9781460140697. © Her Majesty the Queen in Right of Alberta, as represented by the Minister of Alberta Environment and Parks, 2018. This publication is issued under the Open Government Licence - Alberta open.alberta.ca/licence. Published September 2018 ISBN 978-1-4601-4069-7 Land use, climate change and ecological responses in the Upper North 2 Saskatchewan and Red Deer River Basins: A scientific assessment Acknowledgements The authors are grateful to the external reviewers for providing their technical reviews and feedback, which have enhanced this work. -
South Saskatchewan River Basin Adaptation to Climate Variability Project
South Saskatchewan River Basin Adaptation to Climate Variability Project Climate Variability and Change in the Bow River Basin Final Report June 2013 This study was commissioned for discussion purposes only and does not necessarily reflect the official position of the Climate Change Emissions Management Corporation, which is funding the South Saskatchewan River Basin Adaptation to Climate Variability Project. The report is published jointly by Alberta Innovates – Energy and Environment Solutions and WaterSMART Solutions Ltd. This report is available and may be freely downloaded from the Alberta WaterPortal website at www.albertawater.com. Disclaimer Information in this report is provided solely for the user’s information and, while thought to be accurate, is provided strictly “as is” and without warranty of any kind. The Crown, its agents, employees or contractors will not be liable to you for any damages, direct or indirect, or lost profits arising out of your use of information provided in this report. Alberta Innovates – Energy and Environment Solutions (AI-EES) and Her Majesty the Queen in right of Alberta make no warranty, express or implied, nor assume any legal liability or responsibility for the accuracy, completeness, or usefulness of any information contained in this publication, nor that use thereof infringe on privately owned rights. The views and opinions of the author expressed herein do not necessarily reflect those of AI-EES or Her Majesty the Queen in right of Alberta. The directors, officers, employees, agents and consultants of AI-EES and the Government of Alberta are exempted, excluded and absolved from all liability for damage or injury, howsoever caused, to any person in connection with or arising out of the use by that person for any purpose of this publication or its contents. -
HDP 2006 05 Report 1
Report #1 1998 CWS Air Surveys In response to a general lack of knowledge on the abundance and distribution of the Harlequin Duck within Alberta, the Canadian Wildlife Service in cooperation with Alberta Environment undertook helicopter surveys of the eastern slopes of Alberta in 1998 and 1999. In 1998 the survey area encompassed streams along the eastern slopes of Alberta between the communities of Grande Cache and Nordegg. Ground truthing was provided by foot surveys on the McLeod River conducted by Bighorn Wildlife Technologies Ltd. Local area biologists helped with selection of blocks of streams to be surveyed where harlequins were most likely to occur and assisted in the helicopter surveys. Helicopter survey methods are detailed in Gregoire et al. (1999). Global Positioning Coordinates (GPS) were recorded for all sightings as well as survey start and end points. The Universal Transverse Mercator (UTM) coordinate system was used for recording sightings of Harlequin Duck and other wildlife. Survey start and end points were recorded in Latitude and Longitude. Five digit numbers hand written in the field survey reports represent the BSOD (now WHIMIS) ID number for that observation. What this document contains. - A summary of the 1998 surveys (Gregoire et al. 1999. Canadian Wildlife Service Technical Report Series No. 329), - The field results for the helicopter survey conducted between the Brazeau and North Saskatchewan Rivers - The results of a foot survey on the Blackstone River. , · Harlequin L?.uck ·surveys in the Centr~I - .Eastern Slopes o.f Albert9: . ·Spring 1998. T - • ~ Paul Gr~goire, Jeff Kneteman and Jim Allen . .-"• r, ~ ~-. Prairie and Northern Region 1999 .1;._-, - 1 ,~ .Canadian Wildlife Service '' ,· ~: ,. -
BRAZEAU RIVER Field Wherein Production May Be Commingled in the Wellbore, And
COMMINGLING Order No. MU8834 MADE at the City of Calgary, in the Province of Alberta, on 5th day of July 2018. ALBERTA ENERGY REGULATOR The Alberta Energy Regulator (AER) pursuant to the Oil and Gas Conservation Act, chapter O-6 of the Revised Statutes of Alberta, 2000, orders as follows: 1) The following table shows • the specified pools and wells in the BRAZEAU RIVER Field wherein production may be commingled in the wellbore, and • the allocation factors to prorate the commingled production to the specified pools: Wells Allocation Pools (Unique Identifier) Percentage a) BRAZEAU RIVER EDMONTON A and All None BRAZEAU RIVER BELLY RIVER XXX b) BRAZEAU RIVER EDMONTON E and All None BRAZEAU RIVER LOWER EDMONTON A c) BRAZEAU RIVER BELLY RIVER V and All None BRAZEAU RIVER BELLY RIVER W d) BRAZEAU RIVER BELLY RIVER X and 00/01-21-047-14W5/0 80 BRAZEAU RIVER BELLY RIVER FF 00/01-21-047-14W5/0 20 e) BRAZEAU RIVER BELLY RIVER X, 00/08-19-047-14W5/0 80 BRAZEAU RIVER BASAL BELLY RIVER D, 00/08-19-047-14W5/0 20 BRAZEAU RIVER BELLY RIVER X, 00/12-19-047-14W5/0 80 BRAZEAU RIVER BASAL BELLY RIVER D, 00/12-19-047-14W5/0 20 Application No. 1909250 Order No. MU8834 Page 1 of 8 BRAZEAU RIVER BELLY RIVER X, and 00/01-24-047-15W5/0 80 BRAZEAU RIVER BASAL BELLY RIVER D 00/01-24-047-15W5/0 20 f) BRAZEAU RIVER BELLY RIVER X, 00/15-20-047-14W5/0 45 BRAZEAU RIVER BASAL BELLY RIVER D, and 00/15-20-047-14W5/0 45 BRAZEAU RIVER BASAL BELLY RIVER Y 00/15-20-047-14W5/0 10 g) BRAZEAU RIVER BELLY RIVER X, 00/07-27-047-14W5/0 50 BRAZEAU RIVER BASAL BELLY RIVER M, 00/07-27-047-14W5/0 -
North Saskatchewan River Drainage, Fish Sustainability Index Data Gaps Project, 2015
North Saskatchewan River Drainage, Fish Sustainability Index Data Gaps Project, 2015 The Alberta Conservation Association is a Delegated Administrative Organization under Alberta’s Wildlife Act. North Saskatchewan River Drainage, Fish Sustainability Index Data Gaps Project, 2015 Mike Rodtka, Chad Judd and Andrew Clough Alberta Conservation Association 101 – 9 Chippewa Road Sherwood Park, Alberta, Canada T8A 6J7 Report Editors PETER AKU KELLEY KISSNER Alberta Conservation Association 50 Tuscany Meadows Cr. NW 101 – 9 Chippewa Rd. Calgary, AB T3L 2T9 Sherwood Park, AB T8A 6J7 Conservation Report Series Type Data ISBN: 978-0-9949118-3-4 Disclaimer: This document is an independent report prepared by Alberta Conservation Association. The authors are solely responsible for the interpretations of data and statements made within this report. Reproduction and Availability: This report and its contents may be reproduced in whole, or in part, provided that this title page is included with such reproduction and/or appropriate acknowledgements are provided to the authors and sponsors of this project. Suggested Citation: Rodtka, M., C. Judd, and A. Clough. 2016. North Saskatchewan River drainage, Fish Sustainability Index data gaps project, 2015. Data Report, D-2016-105, produced by Alberta Conservation Association, Sherwood Park, Alberta, Canada. 17 pp + App. Cover photo credit: David Fairless Digital copies of conservation reports can be obtained from: Alberta Conservation Association 101 – 9 Chippewa Rd. Sherwood Park, AB T8A 6J7 Toll Free: 1-877-969-9091 Tel: (780) 410-1998 Fax: (780) 464-0990 Email: [email protected] Website: www.ab-conservation.com i EXECUTIVE SUMMARY Alberta Environment and Parks Fish Sustainability Index is a standardized process of assessment that provides a landscape-level overview of fish sustainability within the province and enables broad-scale evaluation of management actions and land-use planning. -
Water Quality in the South SK River Basin
Water Quality in the South SK River Basin I AN INTRODUCTION TO THE SOUTH SASKATCHEWAN RIVER BASIN I.1 The Saskatchewan River Basin The South Saskatchewan River joins the North Saskatchewan River to form one of the largest river systems in western Canada, the Saskatchewan River System, which flows from the headwater regions along the Rocky Mountains of south-west Alberta and across the prairie provinces of Canada (Alberta, Saskatchewan, and Manitoba). The Prairie physiographic region is characterized by rich soils, thick glacial drift and extensive aquifer systems, and a consistent topography of broad rolling hills and low gradients which create isolated surface wetlands. In contrast, the headwater region of the Saskatchewan River (the Western Cordillera physiographic region) is dominated by thin mineral soils and steep topography, with highly connected surface drainage systems and intermittent groundwater contributions to surface water systems. As a result, the Saskatchewan River transforms gradually in its course across the provinces: from its oxygen-rich, fast flowing and highly turbid tributaries in Alberta to a meandering, nutrient-rich and biologically diverse prairie river in Saskatchewan. There are approximately 3 million people who live and work in the Saskatchewan River Basin and countless industries which operate in the basin as well, including pulp and paper mills, forestry, oil and gas extraction, mining (coal, potash, gravel, etc.), and agriculture. As the fourth longest river system in North America, the South Saskatchewan River Basin covers an incredibly large area, draining a surface of approximately 405 860 km² (Partners FOR the Saskatchewan River Basin, 2009). Most of the water that flows in the Saskatchewan River originates in the Rocky Mountains of the Western Cordillera, although some recharge occurs in the prairie regions of Alberta and Saskatchewan through year-round groundwater contributions, spring snow melt in March or April, and summer rainfall in May and early July (J.W. -
Northern Leopard Frog Recovery Program
Northern Leopard Frog Recovery Program Year 5 (2003) Kris Kendell In cooperation with: Northern Leopard Frog Recovery Program Year 5 (2003) This publication may be cited as: Kendell, K. 2004. Northern leopard frog recovery program: Year 5 (2003). Unpublished report, Alberta Conservation Association, Edmonton, AB. 14 pp. ii TABLE OF CONTENTS ACKNOWLEDGEMENTS....................................................................................................... iv EXECUTIVE SUMMARY ........................................................................................................ v 1.0 INTRODUCTION .................................................................................................................... 1 2.0 STUDY AREA ......................................................................................................................... 2 2.1 Egg mass collection and frog release sites........................................................................ 2 2.2 Captive rearing site ........................................................................................................... 2 3.0 METHODS ............................................................................................................................... 3 3.1 Captive rearing.................................................................................................................. 3 3.2 Marking............................................................................................................................. 3 3.3 Release (2003) ................................................................................................................. -
Supplementary Materials Hydrologic-Land Surface Modelling of a Complex System Under Precipitation Uncertainty: a Case Study of the Saskatchewan River Basin, Canada
Supplementary Materials Hydrologic-Land Surface Modelling of a Complex System under Precipitation Uncertainty: A Case Study of the Saskatchewan River Basin, Canada Fuad Yassin1, Saman Razavi1, Jefferson S. Wong1, Alain Pietroniro2, Howard Wheater1 1Global Institute for Water Security, University of Saskatchewan, National Hydrology Research Centre, 11 Innovation Boulevard, Saskatoon, SK, S7N 3H5, Canada 2National Hydrology Research Center, Environment Canada, 11 Innovation Boulevard, Saskatoon, SK, S7N 3H5, Canada 1 1.0 MESH new features In order to enable MESH to model complex and highly managed basins (e.g. SaskRB), new water management features (irrigation, reservoir operation, and diversion) have been integrated recently into the MESH framework. The irrigation algorithm is based on the soil moisture deficit approach, similar to that of Pokhrel et al. (2016). The net irrigation 5 water demand is estimated as the difference between target soil moisture content (휃푇) and the simulated actual soil moisture (휃푘). 휌 퐼푅 = 푤 ∑푛 {max[(휃 − 휃 ), 0] ∗ 퐷 } (S1) ∆푡 푘=1 푇 푘 푘 -2 -3 where IR [kg m s] is the net irrigation demand, 휌푤[kg m ] is the density of water; ∆푡 is model time step; 휃푇 is given as 훼 ∗ 3 -3 휃퐹퐶 ; 휃퐹퐶 and 휃푘 [m m ] are the field capacity and simulated actual volumetric soil moisture content, respectively; 훼 [-] is the 10 parameter that defines the upper soil moisture limit which has been used varyingly from 0.5 to 1; and 퐷푘 [m] is the thickness of 휅푡ℎ soil layer, n represents the number of soil layers considered in the calculation. In order to represent irrigation effects, the standard CLASS three soil layer configuration has been changed to four soil layers so that the bottom of the third soil layer is set to around 1m.