Radially transmitted changes in hydraulic and osmotic pressures help explain reversible and irreversible patterns of tree stem expansion
Sebastian Pfautsch1,2, John E. Drake2,3, Michael J. Aspinwall2,4, Victor Resco de Dios5,6,7, Craig V.M. Barton2, Patrick Meir8,9, Mark G. Tjoelker2, David T. Tissue2, and Maurizio Mencuccini10,11
1Urban Studies, School of Social Science, Western Sydney University, Locked Bag 1797, Penrith, NSW 2751, Australia
2Hawkesbury Institute for the Environment, Western Sydney University, Locked Bag 1797, Penrith, NSW 2751, Australia
3Sustainable Resources Management, State University of New York College of Environmental Science and Forestry, 1 Forestry Drive, Syracuse, NY 13210, United States
4School of Forestry and Wildlife Services, Auburn University, 602 Duncan Drive, Auburn, AL 36849, United States
5School of Life Science and Engineering, Southwest University of Science and Technology, Mianyang, Sichuan 621010, P.R. China
6Departament of Crop and Forest Sciences, University of Lleida, Lleida 25198, Spain
7Joint Research Unit CTFC-AGROTECNIO-CERCA Centre, Lleida 25198, Spain
8School of Geosciences, University of Edinburgh, United Kingdom
9Research School of Biology, Australian National University, Canberra, ACT 2601, Australia
10ICREA, Barcelona 08010, Spain
11CREAF, Cerdanyola del Vallès, Barcelona 08193, Spain
Corresponding Author         Sebastian Pfautsch
Phone                                   +61 2 9685 9081
Email                                    s.pfautsch@westernsydney.edu.au