Land Management Search Results
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Eleven plantations of each of jack pine ( Pinus banksiana Lamb.) and black spruce ( Picea mariana [Mill.] B.S.P.) were established with bareroot stock during a 3-year period beginning in 1980 on sites...
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In most years, evaporation exceeds summer rainfall. Using natural aspen stands as a comparison, it is expected that water use from the soil cover will continue to increase as the ecosystem ages.
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Nature-based Solutions leverage nature and the power of healthy ecosystems to protect people, optimise infrastructure and safeguard a stable and biodiverse future. Explore topics related to Nature...
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Authors
Wetland Knowledge Exchange
Resource Date:
November
2023
Cassandra Chabot-Madlung, County of Grande Prairie presents - Wetland Replacement Program: How it Started & Who Can Participate This is a Municipal viewpoint of Alberta Environment and Protected Areas...
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Authors
Richard Johnson
P. Bork
E.A.D. Allen
W.H. James
L. Koverny
The experiments detailed in this report show that it was possible to increase the solids content of sludge to 50% solids by adding three parts sand (tailings sand) to one part sludge.
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Authors
Paul Moore
Benjamin Didemus
Alexander Furukawa
James Waddington
Resource Date:
March
2021
A critical ‘threshold’ peat depth specific for different hydrogeological and hydroclimatic regions can be used to assess what peatlands are especially vulnerable to climate change mediated drought.
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Authors
Camille Defrenne
Jessica Moore
Colin Tucker
Louis Lamit
Evan Kane
Randall Kolka
Rodney Chimner
Jason Keller
Erik Lilleskov
Drainage-induced encroachment by trees may have major effects on the carbon balance of northern peatlands, and responses of microbial communities are likely to play a central mechanistic role. We...
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Authors
Lorna Harris
David Olefeldt
Nicolas Pelletier
Christian Blodau
Klaus-Holger Knorr
Julie Talbot
Liam Heffernan
Merritt Turetsky
Resource Date:
August
2023
Rapid, ongoing permafrost thaw of peatlands in the discontinuous permafrost zone is exposing a globally significant store of soil carbon (C) to microbial processes. Mineralization and release of this...
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Authors
Stephen Moran
Mark Trudell
Terry Macyk
Daphne Cheel
The first phase of the study, which was completed in 1984, included characterization and instrumentation of two study areas: the Battle River study area, which included Diplomat, Vesta and Paintearth...
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Authors
Sheel Bansal
Irena Creed
Brian Tangen
Scott Bridgham
Ankur Desai
Ken Krauss
Scott Neubauer
Gregory Noe
Donald Rosenberry
Carl Trettin
Kimberly Wickland
Scott Allen
Ariane Arias‑Ortiz
Anna Armitage
Dennis Baldocchi
Kakoli Banerjee
David Bastviken
Peter Berg
Matthew Bogard
Alex Chow
William Conner
Christopher Craft
Courtney Creamer
Tonya DelSontro
Jamie Duberstein
Meagan Eagle
Siobhan Fennessy
Sarah Finkelstein
Mathias Göckede
Sabine Grunwald
Meghan Halabisky
Ellen Herbert
Mohammad Jahangir
Olivia Johnson
Miriam Jones
Jefrey Kelleway
Sara Knox
Kevin Kroeger
Kevin Kuehn
David Lobb
Amanda Loder
Shizhou Ma
Damien Maher
Gavin McNicol
Jacob Meier
Beth Middleton
Christopher Mills
Purbasha Mistry
Abhijit Mitra
Courtney Mobilian
Charles Schutte
Changchun Song
Camille Stagg
Jessica Turner
Rodrigo Vargas
Mark Waldrop
Marcus Wallin
Zhaohui Aleck Wang
Eric Ward
Debra Willard
Stephanie Yarwood
Xiaoyan Zhu
Wetlands cover a small portion of the world, but have disproportionate influence on global carbon (C) sequestration, carbon dioxide and methane emissions, and aquatic C fluxes. However, the underlying...
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Authors
Amy Wotherspoon
Nelson Thiffault
Robert Bradley
Scarification is a mechanical site preparation technique designed to create microsites that will favor the growth of planted tree seedlings after clearcutting. However, the positive growth response of...
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Authors
Kimberley Murray
Melanie Bird
Maria Strack
Michael Cody
Bin Xu
Resource Date:
April
2021
This article outlines the results of monitoring two restored oil sands exploration sites, and discusses the effectiveness of treatments on tree recovery and greenhouse gas emissions.
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Authors
Anthony Stewart
Meghan Halabisky
Chad Babcock
David Butman
David D’Amore
Monika Moskal
Inland wetlands are critical carbon reservoirs storing 30% of global soil organic carbon (SOC) within 6% of the land surface. However, forested regions contain SOC-rich wetlands that are not included...
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Authors
Doug Maynard
K. E. Hogg
Ed Wass
M.P. Curran
Soil disturbance from forest harvesting has been shown to compromise site productivity. We established satellite trials in five of the Long-Term Soil Productivity (LTSP) sites in southeast British...
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Authors
Anne Naeth
Donna White
David Chanasyk
Terry Macyk
Chris Powter
Don Thacker
To provide coordinated direction for reclamation research in Alberta, the need to review the current understanding and the role of soil physical properties in soil disturbance related activities was...
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Authors
Pedocan Land Evaluation Ltd.
Part 1 of this manual is a background and explanatory section that describes the terminology used in soil surveys and presents the assumptions and conventions upon which the interpretations are based
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Authors
Pedocan Land Evaluation Ltd.
Part 2 presents typical data and interpretations for each soil series in Alberta. The interpretations were made by applying the guidelines in Part 1, and checking the results against experience
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Authors
Nia Perron
Jennifer Baltzer
Oliver Sonnentag
Transpiration is a globally important component of evapotranspiration. Careful upscaling of transpiration from point measurements is thus crucial for quantifying water and energy fluxes. In spatially...
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Authors
Teemu Juselius-Rajamäki
Minna Väliranta
Atte Korhola
Resource Date:
October
2023
Peatlands are the most dense terrestrial carbon stock and since the last glacial epoch northern peatlands have accumulated between 400 and 1000 Gt of carbon. Although the horizontal development...
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Authors
Dale Vitt
Melissa House
Lilyan Glaeser
Minerogenous peatlands that accumulate deep deposits of organic matter (fens) were an important part of the pre-disturbance landscape across Alberta’s oil sands mining area. Bryophytes occupy 80–100%...