Zobrazeno 1 - 7
of 7
pro vyhledávání: '"F. E Moyano"'
Publikováno v:
Biogeosciences, Vol 15, Pp 5031-5045 (2018)
CO2 production in soils responds strongly to changes in temperature and moisture, but the magnitude of such responses at different timescales remains difficult to predict. Knowledge of the mechanisms leading to the often observed interactions in t
Externí odkaz:
https://doaj.org/article/57bc9e62871145d1aad50828482493a8
Publikováno v:
Geoscientific Model Development, Vol 9, Iss 2, Pp 841-855 (2016)
Priming of soil carbon decomposition encompasses different processes through which the decomposition of native (already present) soil organic matter is amplified through the addition of new organic matter, with new inputs typically being more labile
Externí odkaz:
https://doaj.org/article/f42776f55b6542b0ad794e1c2aa632d1
Publikováno v:
Geoscientific Model Development, Vol 6, Iss 6, Pp 2153-2163 (2013)
A widespread decrease of the topsoil carbon content was observed over England and Wales during the period 1978–2003 in the National Soil Inventory (NSI), amounting to a carbon loss of 4.44 Tg yr−1 over 141 550 km2. Subsequent modelling studies ha
Externí odkaz:
https://doaj.org/article/48510be65b834fa5ba888e32e7da8b9c
Autor:
F. E. Moyano, N. Vasilyeva, L. Bouckaert, F. Cook, J. Craine, J. Curiel Yuste, A. Don, D. Epron, P. Formanek, A. Franzluebbers, U. Ilstedt, T. Kätterer, V. Orchard, M. Reichstein, A. Rey, L. Ruamps, J.-A. Subke, I. K. Thomsen, C. Chenu
Publikováno v:
Biogeosciences, Vol 9, Iss 3, Pp 1173-1182 (2012)
Soil moisture is of primary importance for predicting the evolution of soil carbon stocks and fluxes, both because it strongly controls organic matter decomposition and because it is predicted to change at global scales in the following decades. Howe
Externí odkaz:
https://doaj.org/article/7259c88598674429b46ea1612e228630
A widespread decrease of the top soil carbon content was observed over England and Wales during the period 1978–2003 in the National Soil Inventory (NSI), amounting to a carbon loss of 4.44 Tg yr-1 over 141 550 km2. Subsequent modelling studies hav
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fc6936fe0311ddcac74a5c7eb2962777
http://dspace.lib.cranfield.ac.uk/handle/1826/8196
http://dspace.lib.cranfield.ac.uk/handle/1826/8196
Autor:
Patricia H. Bellamy, Bertrand Guenet, P. Ciais, Nicolas Vuichard, Guy J. D. Kirk, Sönke Zaehle, F. E. Moyano
Publikováno v:
Geoscientific Model Development
Geoscientific Model Development, 2013, 6 (6), pp.2153-2163. ⟨10.5194/gmd-6-2153-2013⟩
Geoscientific Model Development, Vol 6, Iss 6, Pp 2153-2163 (2013)
Geoscientific Model Development, European Geosciences Union, 2013, 6 (6), pp.2153-2163. ⟨10.5194/gmd-6-2153-2013⟩
Geoscientific Model Development, 2013, 6 (6), pp.2153-2163. ⟨10.5194/gmd-6-2153-2013⟩
Geoscientific Model Development, Vol 6, Iss 6, Pp 2153-2163 (2013)
Geoscientific Model Development, European Geosciences Union, 2013, 6 (6), pp.2153-2163. ⟨10.5194/gmd-6-2153-2013⟩
A widespread decrease of the topsoil carbon content was observed over England and Wales during the period 1978–2003 in the National Soil Inventory (NSI), amounting to a carbon loss of 4.44 Tg yr−1 over 141 550 km2. Subsequent modelling studies ha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::38079c7610be82399038f91626adcf92
https://hal.science/hal-02929650
https://hal.science/hal-02929650
Autor:
F. E. Moyano, N. Vasilyeva, L. Bouckaert, F. Cook, J. Craine, J. Curiel Yuste, A. Don, D. Epron, P. Formanek, A. Franzluebbers, U. Ilstedt, T. Kätterer, V. Orchard, M. Reichstein, A. Rey, L. Ruamps, J.-A. Subke, I. K. Thomsen, C. Chenu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9114bfb36f290b95bfb864feed372d44
https://doi.org/10.5194/bgd-8-11577-2011-supplement
https://doi.org/10.5194/bgd-8-11577-2011-supplement