Ecosystem processes in semiarid grasslands. II.* Litter production decomposition and nutrient dynamics

Autor: EK Christie

Publikováno v: Australian Journal of Agricultural Research. 30:29

Changes in tissue nutrient concentration and nutrient uptake of a C3 native grassland and a sown C4 buffel grassland community, growing on infertile sandy red earth soils near Charleville, were studied. The seasonal pattern of litter production of gr

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::db12a6deeb7df8039c8c064e6f8e55d2
https://doi.org/10.1071/ar9790029

Physiological responses of semiarid grasses. IV.* Photosynthetic rates of Thyridolepis mitchelliana and Cenchrus ciliaris leaves

Autor: EK Christie

Publikováno v: Australian Journal of Agricultural Research. 26:459

Photosynthesis response curves of mulga and buffel grasses to irradiance and to carbon dioxide concentration, together with studies of leaf anatomy and chloroplast structure, showed that the former was a C3 and the latter a C4 species. This is held t

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::6917e115282241b508cc45e1380a752e
https://doi.org/10.1071/ar9750459

Physiological responses of the semi-arid grasses Thyridolepsis and Astrebla compared with Cenchrus

Autor: EK Christie

Publikováno v: The Rangeland Journal. 1:208

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::c004007adb3af126c16b6b97ca50a5d4
https://doi.org/10.1071/rj9780208

Physiological responses of semiarid grasses. III.* Growth in relation to temperature and soil water deficit

Autor: EK Christie

Publikováno v: Australian Journal of Agricultural Research. 26:447

The optimum temperature for vegetative growth of mulga grass was about 25°C, and for Mitchell and buffel grasses 30°. Buffel grass had the highest yield at all temperatures, partly because of its higher growth rate which in turn can be ascribed to

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::2ffa90370ae1b718f86388b8f8a413a8
https://doi.org/10.1071/ar9750447

Biological-physical interactions are fundamental to understanding and managing coastal dynamics.

Autor: Solan M; School of Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Waterfront Campus, European Way, Southampton SO14 3ZH, UK., Spencer T; Cambridge Coastal Research Unit, Department of Geography, University of Cambridge, Downing Place, Cambridge CB2 3EN, UK., Paterson DM; Scottish Oceans Institute, School of Biology, Sediment Ecology Research Group, University of St Andrews, St Andrews, Fife KY16 8LB, UK., Unsworth CA; Marine Physics and Ocean Climate, National Oceanography Centre, Joseph Proudman Building, 6 Brownlow Street, Liverpool L3 5DA, UK., Christie EK; Cambridge Coastal Research Unit, Department of Geography, University of Cambridge, Downing Place, Cambridge CB2 3EN, UK., Blight AJ; Scottish Oceans Institute, School of Biology, Sediment Ecology Research Group, University of St Andrews, St Andrews, Fife KY16 8LB, UK., Brown J; Marine Physics and Ocean Climate, National Oceanography Centre, Joseph Proudman Building, 6 Brownlow Street, Liverpool L3 5DA, UK., Brooks H; Cambridge Coastal Research Unit, Department of Geography, University of Cambridge, Downing Place, Cambridge CB2 3EN, UK.; Environment Agency, Tyneside House, Skinnerburn Road, Newcastle Business Park, Newcastle upon Tyne NE4 7AR, UK., Lichtman ID; Marine Physics and Ocean Climate, National Oceanography Centre, Joseph Proudman Building, 6 Brownlow Street, Liverpool L3 5DA, UK., Wei X; Marine Physics and Ocean Climate, National Oceanography Centre, Joseph Proudman Building, 6 Brownlow Street, Liverpool L3 5DA, UK., Li X; Department of Geography and Planning, School of Environmental Sciences, University of Liverpool, Liverpool L69 7ZT, UK.; Energy and Environment Research Group, College of Engineering, Swansea University, Swansea SA2 8PP, UK., Thorne P; Marine Physics and Ocean Climate, National Oceanography Centre, Joseph Proudman Building, 6 Brownlow Street, Liverpool L3 5DA, UK., Leyland J; School of Geography and Environmental Science, University of Southampton, Highfield, Southampton SO17 1BJ, UK., Godbold JA; School of Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Waterfront Campus, European Way, Southampton SO14 3ZH, UK., Thompson C; School of Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Waterfront Campus, European Way, Southampton SO14 3ZH, UK.; Channel Coastal Observatory, National Oceanography Centre, University of Southampton, Waterfront Campus, European Way, Southampton SO14 3ZH, UK., Williams ME; Marine Physics and Ocean Climate, National Oceanography Centre, Joseph Proudman Building, 6 Brownlow Street, Liverpool L3 5DA, UK.; Departamento de Ingeniería Hidráulica y Ambiental, Facultad de Ingeniería, Pontificia Universidad Católica de Chile, Santiago, Chile.; Facultad de Ciencias Biológicas, Pontificia Universidad Católica de Chile, Santiago, Chile., Plater A; Department of Geography and Planning, School of Environmental Sciences, University of Liverpool, Liverpool L69 7ZT, UK., Moller I; Cambridge Coastal Research Unit, Department of Geography, University of Cambridge, Downing Place, Cambridge CB2 3EN, UK.; Department of Geography, Trinity College Dublin, Museum Building, Dublin 2, Ireland., Amoudry LO; Marine Physics and Ocean Climate, National Oceanography Centre, Joseph Proudman Building, 6 Brownlow Street, Liverpool L3 5DA, UK.

Publikováno v: Royal Society open science [R Soc Open Sci] 2023 Jul 12; Vol. 10 (7), pp. 230155. Date of Electronic Publication: 2023 Jul 12 (Print Publication: 2023).