Zobrazeno 1 - 10
of 523
pro vyhledávání: '"J.S. Price"'
Publikováno v:
Journal of Hydrology: Regional Studies, Vol 40, Iss , Pp 101031- (2022)
Study region: A channel fen in the Athabasca Oil Sands Area, Alberta, Canada Study focus: We assessed the hydrological changes to the hydrology of a moderate-rich fen after the construction of a road (perpendicular to flow) in 2003 and a pipeline (ob
Externí odkaz:
https://doaj.org/article/8ce4520f54e141f7a2987d6e46cd7807
Publikováno v:
Mires and Peat, Vol 20, Iss 05, Pp 1-15 (2017)
To harvest Sphagnum on a cyclic basis and rapidly accumulate biomass, active water management is necessary. The goal of this study is to determine the hydrological conditions that will maximise CO2 uptake in Sphagnum farming basins following the moss
Externí odkaz:
https://doaj.org/article/40c92b241896470582f13e0ba5632056
Autor:
S. Malloy, J.S. Price
Publikováno v:
Mires and Peat, Vol 19, Iss 05, Pp 1-15 (2017)
Water availability is a major concern when restoring degraded vacuum harvested peatlands. The seasonal expression of water arising from the compression of underlying organic deposits may provide a source of water. A bog near Rimouski, Québec (Canada
Externí odkaz:
https://doaj.org/article/e0e8561f3e5142a0a708e5c410d45512
Publikováno v:
Mires and Peat, Vol 16, Iss 12, Pp 1-18 (2015)
Peatlands occurring in regions with high rates of total evaporation (ET), matching or exceeding precipitation (P) during seasonal dry periods or longer-term dry spells, are dependent on sustained groundwater flows to ensure peat accumulation. The obj
Externí odkaz:
https://doaj.org/article/2717e6eb769a4c04831ce071f18d791d
Autor:
S.J. Scarlett, J.S. Price
Publikováno v:
Mires and Peat, Vol 12, Iss 04, Pp 1-12 (2013)
In the oil sands development region near Fort McMurray, Alberta, wetlands cover ~62 % of the landscape, and ~95 % of these wetlands are peatlands. A saline fen was studied as a reference site for peatland reclamation. Despite highly saline conditions
Externí odkaz:
https://doaj.org/article/0074729d72594f5aaa411c6d10e7ac55
Publikováno v:
Mires and Peat, Vol 6, Iss 07, Pp 1-10 (2010)
This article describes two spring mire complexes in the Kruger National Park (South Africa) that are fed by thermal water with a temperature of 37–42°C. The mires are small (1–20 m in diameter). The peat thickness is 1–2.5 m, of which 1–1.5
Externí odkaz:
https://doaj.org/article/c80008cdd22a4b83b84c738b07fe5c09
Publikováno v:
Mires and Peat, Vol 3, Iss 05, Pp 1-13 (2008)
In the Canadian Western Boreal Plain (WBP), wetlands (ponds and peatlands) comprise up to 50% of the landscape and represent unique habitat where summer precipitation is often outpaced by evapotranspiration and hillslope groundwater position does not
Externí odkaz:
https://doaj.org/article/1ab8f26fa88b4caa8c694986bb56c4a0
Autor:
P. Whittington, M. Strack, R. van Haarlem, S. Kaufman, P. Stoesser, J. Maltez, J.S. Price, M. Stone
Publikováno v:
Mires and Peat, Vol 2, Iss 09, Pp 1-14 (2007)
Links between local hydrology and vegetation type exist in wetlands, yet it is unclear what role peat volume change plays in these interactions. We measured peat volume change and hydraulic conductivity (Kfield) at three contrasting sites located on
Externí odkaz:
https://doaj.org/article/461b2187d46143eb8dd81278c9412bb5
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Akademický článek
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