Zobrazeno 1 - 7
of 7
pro vyhledávání: '"C. G. Barker"'
Publikováno v:
Global Change Biology. 18:2824-2837
Increases in the emissions and associated atmospheric deposition of nitrogen (N) have the potential to cause significant changes to the structure and function of N-limited ecosystems. Here, we present the results of a long-term (13 year) experiment a
Publikováno v:
Global Change Biology. 12:1241-1252
Atmospheric deposition of nitrogen is responsible for widespread changes in the structure and function of sensitive seminatural ecosystems. The proposed reduction in emissions of nitrogenous pollutants in Europe under the Gothenburg Protocol raises t
Autor:
Jacqueline A. Carroll, Andrew C. Terry, C. G. Barker, Gerrit W. Heil, Mike A. Ashmore, N. Cresswell, Sally A. Power, Simon J.M. Caporn, Michael G. Pilkington, Deirdre B. Wilson, Emma R. Green
Publikováno v:
Water, Air, & Soil Pollution: Focus. 4:259-267
The results from three long-term field manipulation studies of the impacts of increased nitrogen deposition (0–120 kg N ha−1 yr−1) on lowland and upland heathlands in the UK were compared, to test if common responses are observed. Consistent in
Publikováno v:
Biological Conservation. 120:41-52
A field experiment was carried out to investigate the impact of four different management treatments on the response of Calluna-dominated heathland to nitrogen additions of 0 or 30 kg ha−1 yr−1 at a lowland heath in Surrey, England. Post-manageme
Publikováno v:
The Scientific World Journal
The Scientific World Journal, Vol 1, Pp 714-721 (2001)
Scopus-Elsevier
The Scientific World Journal, Vol 1, Pp 714-721 (2001)
Scopus-Elsevier
Atmospheric nitrogen deposition has been shown to affect both the structure and the function of heathland ecosystems. Heathlands are semi-natural habitats and, as such, undergo regular management by mowing or burning. Different forms of management re
Autor:
C. G. Barker
Publikováno v:
Journal of the Institution of Electrical Engineers. 84:18-20
Autor:
C. G. Barker
Publikováno v:
Nature. 205:1001-1002
IT has been known since the late nineteenth century that rocks and minerals evolve gas when heated. Early workers1,2 were hampered by the lack of adequate methods for analysing small quantities of gas. They attempted to offset this by using large sam