Tree stem diameter variations and transpiration in Scots pine: an analysis using a dynamic sap flow model

• Published in: Tree physiology Vol. 21; no. 12-13; pp. 889 - 897
• Main Authors: Perämäki, M, Nikinmaa, E, Sevanto, S, Ilvesniemi, H, Siivola, E, Hari, P, Vesala, T
• Format: Journal Article
• Language: English
• Published: Canada 01-08-2001
• Subjects: Models, Biological; Pinus - anatomy & histology; Pinus - physiology; Plant Stems - anatomy & histology; Plant Stems - physiology; Plant Transpiration - physiology; Trees - anatomy & histology; Trees - physiology; Water - physiology
• ISSN: 0829-318X
• DOI: 10.1093/treephys/21.12-13.889

A dynamic model for simulating water flow in a Scots pine (Pinus sylvestris L.) tree was developed. The model is based on the cohesion theory and the assumption that fluctuating water tension driven by transpiration, together with the elasticity of wood tissue, causes variations in the diameter of a tree stem and branches. The change in xylem diameter can be linked to water tension in accordance with Hookeâ s law. The model was tested against field measurements of the diurnal xylem diameter change at different heights in a 37-year-old Scots pine at Hyytiälä, southern Finland (61 degrees 51' N, 24 degrees 17' E, 181 m a.s.l.). Shoot transpiration and soil water potential were input data for the model. The biomechanical and hydraulic properties of wood and fine root hydraulic conductance were estimated from simulated and measured stem diameter changes during the course of 1 day. The estimated parameters attained values similar to literature values. The ratios of estimated parameters to literature values ranged from 0.5 to 0.9. The model predictions (stem diameters at several heights) were in close agreement with the measurements for a period of 6 days. The time lag between changes in transpiration rate and in sap flow rate at the base of the tree was about half an hour. The analysis showed that 40% of the resistance between the soil and the top of the tree was located in the rhizosphere. Modeling the water tension gradient and consequent woody diameter changes offer a convenient means of studying the link between wood hydraulic conductivity and control of transpiration.