Abstract

Research Highlights: The radial gradient of sap flux density (Js) and the effects of climatic factors on sap flow of Aleppo pine were assessed at different time scales in an eastern Mediterranean ecosystem to improve our understanding of the species water balance. Background and Objectives: Aleppo pine’s sap flow radial profile and responses to environmental parameters in the eastern Mediterranean were, to our best knowledge, originating to date from more arid planted forests. Information from natural forests in this region was lacking. Our objectives were to (a) determine the species’ radial variability in Js on a diurnal and seasonal basis and under different climatic conditions, (b) scale up to tree sap flow taking into account the radial profile of Js and (c) determine the responses of Aleppo pine’s sap flow over the year to climatic variability. Materials and Methods: Js was monitored in Aleppo pine in a natural forest in northern Greece with Granier’s method using sensors at three sapwood depths (21, 51, and 81 mm) during two periods differing in climatic conditions, particularly in soil water availability. Results: Js was the highest at 21 mm sapwood depth, and it declined with increasing depth. A steeper gradient of Js in deep sapwood was observed under drier conditions. The same patterns of radial variability in Js were maintained throughout the year, but the contribution of inner sapwood to sap flow was the highest in autumn when the lower seasonal Js was recorded in both study periods. Not taking into account the radial gradient of Js in the studied Aleppo pine would result in a c. 20.2–27.7 % overestimation of total sap flow on a sapwood basis (Qs), irrespective of climatic conditions. On a diurnal and seasonal basis, VPD was the strongest determinant of sap flux density, while at a larger temporal scale, the effect of soil water content was evident. At SWC > 20% sap flow responded positively to increasing solar radiation and VPD, indicating the decisive role of water availability in the studied region. Moreover, in drier days with VPD > 0.7 KPa, SWC controlled the variation of sap flow. Conclusions: There is a considerable radial variability in Js of the studied Aleppo pine and a considerable fluctuation of sap flow with environmental dynamics that should be taken into account when addressing the species water balance.

Highlights

  • Sap flux density and sap flow measurements are widely used in ecophysiological studies to investigate aspects of plant–water interactions such as canopy conductance [1,2,3,4,5], whole-plant hydraulic conductance [3,6], and leaf stomatal conductance [3,6,7,8,9]

  • We determined the radial variability in sap flux density of mature Aleppo pines with high diameter at breast height (DBH) in a natural forest in northern Greece during two periods with different water availability

  • We estimated that not taking into account the radial variability of sap flux density when aiming at upscaling to sap flow on a tree level, would lead to an overestimation of c. 20.2–27.7%, under varying soil water availability

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Summary

Introduction

Sap flux density and sap flow measurements are widely used in ecophysiological studies to investigate aspects of plant–water interactions such as canopy conductance [1,2,3,4,5], whole-plant hydraulic conductance [3,6], and leaf stomatal conductance [3,6,7,8,9] To estimate these variables from sap flow monitoring, sap flux density (Js) measurements need to be upscaled to the tree level. Taking into consideration radial variability is highly important when upscaling sap flux density measurements to accurately estimate tree and stand level water balance, for tracheid-bearing conifers that tend to have deep functional sapwood [18,32]

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