Abstract

Sap flow is the movement of fluid within plants, whereas reference evapotranspiration (ETo) occurs external to plants as the transfer of water vapor from a hypothetical grass crop. Yet, on daily time scales, and when soil moisture is non-limiting, sap flow has a positive linear relationship with ETo. Furthermore, the E2.88 model hypothesises that sap flow (Q) is equal to ETo when parameters are normalized by leaf area (AL) via the following relationship: Q/AL = ETo/2.88. The value of 2.88 is the supposed leaf area index of the hypothetical grass in the ETo model. Therefore, the E2.88 model potentially provides a null or expected value of sap flow based on independent ETo parameters and leaf area. A test of the E2.88 model was conducted via three sap flow methods (dual method approach [DMA], heat ratio [HRM], and Tmax method) on the measurement of three woody species: Pyrus communis L. (var. Beurre Bosc Pear), Syzygium floribundum F. Muell. (Weeping Lilly Pilly), and Syzygium paniculatum Gaertn. (Lilly Pilly). A data compilation of the literature expanded the sample size to include additional species. The measured trees and data compilation found a strong, positive correlation between sap flow and ETo normalized by leaf area. However, the interpretation of the results was dependent on the sap flow method. The DMA had an average accuracy of 1.6%, whereas the HRM and Tmax significantly underestimated and overestimated sap flow, respectively. This study suggested that sap flow can be reliably estimated from accurate leaf area and ETo measurements and when other variables, such as soil moisture, are non-limiting.

Highlights

  • Total plant volumetric sap flow (Q) is the movement of fluid within xylem and is functionally correlated with transpiration, stem refilling and transport of solutes

  • The three sap flow methods used in this study showed differences in the diel pattern of sap flow

  • For P. communis, there was a significant positive linear correlation between daily ETo and Q (L d−1 ) when sap flow was estimated via the dual method approach (DMA) (r2 = 0.824, p < 0.001, n = 35), heat ratio method (HRM) (r2 = 0.811, p < 0.001, n = 35) and Tmax (r2 = 0.177, p = 0.012, n = 35)

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Summary

Introduction

Total plant volumetric sap flow (Q) is the movement of fluid within xylem and is functionally correlated with transpiration, stem refilling and transport of solutes. The E2.88 model has the form of Q/AL = ETo /2.88 where AL is total plant leaf area (m2 ). The 2.88 constant is derived from leaf area index (LAI) of the hypothetical reference grass crop of height 0.12 m [1,7]. The assumptions of the E2.88 model include non-limiting soil moisture and transpiration is conditioned by leaf area [7]. If the generality of the E2.88 model is demonstrated it will prove valuable for plant–water relations, physiological comparisons, irrigation and water resource management because sap flow may be estimated, under non-limiting soil moisture, without the need for site specific calibrations

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