Difference between revisions of "Machuqueira do Grou Experimental Plot"

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*[http://www.sustentabilidade.amorim.com/xms/files/INICIATIVAS/DOCUMENTACAO/2010_-_Doc__celiege_final_2011-05-17.pdf  Antunes, S., Carmo, M.R., Gouveia, F., Tavares, M. do C., Oliveira, N., Bessa, P. Ferreira, J.G. (2010): VALUATION OF ECOSYSTEM SERVICES AT THE LOCAL SCALE CASE STUDY – THE ROLE OF THE CORK OAK MONTADO AT HERDADE DA MACHOQUEIRA DO GROU(PORTUGAL)]
 
*[http://www.sustentabilidade.amorim.com/xms/files/INICIATIVAS/DOCUMENTACAO/2010_-_Doc__celiege_final_2011-05-17.pdf  Antunes, S., Carmo, M.R., Gouveia, F., Tavares, M. do C., Oliveira, N., Bessa, P. Ferreira, J.G. (2010): VALUATION OF ECOSYSTEM SERVICES AT THE LOCAL SCALE CASE STUDY – THE ROLE OF THE CORK OAK MONTADO AT HERDADE DA MACHOQUEIRA DO GROU(PORTUGAL)]
 
*[http://dspace.uevora.pt/rdpc/bitstream/10174/12231/1/PhD%20ccamiloalves%20versao%20corrigida2.pdf Camilo Alves, C. (2014): STUDIES ON CORK OAK DECLINE: AN INTEGRATED APPROACH, PHD thesis, Universidade de Évora, Portugal]
 
*[http://dspace.uevora.pt/rdpc/bitstream/10174/12231/1/PhD%20ccamiloalves%20versao%20corrigida2.pdf Camilo Alves, C. (2014): STUDIES ON CORK OAK DECLINE: AN INTEGRATED APPROACH, PHD thesis, Universidade de Évora, Portugal]
*[https://www.ufz.de/export/data/1/55798_JESIUM_2012_09_02-07_dubbert.pdf Dubbert, M., Cuntz, M., Piayda, A.,Pereira, J., Maguas, C., Werner, C.: Partitioning evapotranspiration – Testing the Craig and Gordon equation against field measurements of evaporative δ 18O]
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*Correia, A.C., Costa e Silva, F., Correia, A.V., Hussain, M.Z., Rodrigues, A.D., David, J.S., Pereira, J.S. (2014): Carbon sink strength of a Mediterranean cork oak understorey: how do semi-deciduous and evergreen shrubs face summer drought? Journal of Vegetation Science, 25(2), 411–426, DOI: 10.1111/jvs.12102.
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*[https://www.ufz.de/export/data/1/55798_JESIUM_2012_09_02-07_dubbert.pdf Dubbert, M., Cuntz, M., Piayda, A.,Pereira, J.S, Maguas, C., Werner, C.: Partitioning evapotranspiration – Testing the Craig and Gordon equation against field measurements of evaporative δ 18O]
 
*[https://epub.uni-bayreuth.de/1742/1/dubbert_diss_final_23.09.2014.pdf Dubbert, M. (2014): Water balance and productivity of a Mediterranean oak woodland Quantifying understory vegetation impacts by development of a stable oxygen isotope partitioning approach, Dissertation University of Bayreuth, Germany]
 
*[https://epub.uni-bayreuth.de/1742/1/dubbert_diss_final_23.09.2014.pdf Dubbert, M. (2014): Water balance and productivity of a Mediterranean oak woodland Quantifying understory vegetation impacts by development of a stable oxygen isotope partitioning approach, Dissertation University of Bayreuth, Germany]
 
*[http://www.isa.utl.pt/cef/ForEcoGen/Posters/Marjan_Coruche.pdf Jongen, M., Lecomte, X., Pereira, J.S.: The impact of changes in the amount and timing of precipitation on the herbaceous understorey of Mediterranean evergreen oak woodlands]
 
*[http://www.isa.utl.pt/cef/ForEcoGen/Posters/Marjan_Coruche.pdf Jongen, M., Lecomte, X., Pereira, J.S.: The impact of changes in the amount and timing of precipitation on the herbaceous understorey of Mediterranean evergreen oak woodlands]

Revision as of 13:00, 6 March 2015

Location

Located in a private property near Coruche, Portugal.

Catchment size

Climate

Climate is semi-arid, with strong seasonality in precipitation and temperatures.

Average monthly precipitation in Machuqueira do Grou

Geology

Topography

Aerial view of the corkoak stand in June 2014

Vegetation/Land use

Mixed land use. Corkoaks are used for cork extraction. Understorey is used for pasture or recreational hunting.

Context of investigation

The experimental plot was initiated by the University of Lisbon, Centre of Forest Ecology. Most of the monitoring is focused on vertical carbon exchanges. As a by-product, a lot of hydrological variables have been monitored. The University of Potsdam is now investigating the understorey evapotranspiration in this stand. The objective is to understand the different stability regimes affecting the vertical transport of latent heat in different forest densities.

Measurements/Equipment

Eddy covariance tower 2 complete bowen ratio meteorological stations (soil heat flux, 4 component radiometer, wind velocity at different heights, soil moisture, psychrometry at different heights) 2 simplified micrometeorological stations (soil heat flux, 2 component radiometer, wind velocity, soil moisture) Sapflow measurements Monthly field spectrometry of leafs, grasses and shrubs

Links to project webpages

References