Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Paul Birdsey"'
Publikováno v:
Environmental Management. 54:465-478
Tamarisk removal is a widespread restoration practice on rivers in the southwestern USA, but impacts of removal on fish habitat have rarely been investigated. We examined whether tamarisk removal, in combination with a large spring flood, had the pot
Autor:
James W. Brantingham, Morne du Plessis, Paul Birdsey, Bernhard Zipfel, Tammy Kay Cassa, Gregory F. Parkin-Smith
Publikováno v:
The Foot. 21:71-78
Hallux abducto valgus (HAV) is a frequent cause of great toe pain and disability, yet common treatments are only supported by mixed or equivocal research findings. Surgery often only provides modest improvement and post-surgery complications may sign
Autor:
Clay Perschon, Gary E. Belovsky, David Naftz, Robert Baskin, John Luft, Chad Larson, Chad Mellison, Heidi Mahon, James Van Leeuwen, Paul Birdsey, Don Paul, Ryan Mosley
Publikováno v:
Ecosphere. 5:art37
Autor:
Heidi K. Mahon, Ryan Mosley, Robert L. Baskin, Chad Larson, James Van Leeuwen, Doyle W. Stephens, Clay Perschon, David L. Naftz, Gary E. Belovsky, Paul Birdsey, John Luft, David V. Allen, Don S. Paul, Chad Mellison
Publikováno v:
Ecosphere. 2:art33
Great Salt Lake (Utah, USA) is one of the world's largest hypersaline lakes, supporting many of the western U.S.'s migratory waterbirds. This unique ecosystem is threatened, but it and other large hypersaline lakes are not well understood. The ecosys
Autor:
Craig Thomas, Vincent A. Lamarra, Victor Kollock, Rex C. Herron, V. Dean Adams, Paul Birdsey, Mary E. Pitts
Publikováno v:
Lake and Reservoir Management. 1:213-218
In the 1975 National Eutrophication Survey Bear Lake had the best overall water quality of all Utah lakes sampled. However, this oligotrophic state would not be retained because of a mesotrophic level of loading. Because of the unique characteristics
Publikováno v:
Lake and Reservoir Management. 1:229-233
Bear Lake is a hardwater lake located in a limestone basin on the border of Utah and Idaho with a surface area of 282 km2, maximum depth of 63 m, and a mean depth of 10 m. The lake was formed by tectonic activity approximately 28,000 years B.P. with