Applicability of Thermal Dissipation Method in Sap Flow Measurement of Karst Shrub Community

Author:

Qin Jiashuang12,Ni Longkang12,Gu Daxing12,Yang Kaijun12ORCID,Huang Qibo3,Tan Yu12,Liao Suhui12

Affiliation:

1. Guangxi Key Laboratory of Plant Conservation and Restoration Ecology in Karst Terrain, Guangxi Institute of Botany, Chinese Academy of Sciences, Guilin 541006, China

2. Guangxi Guilin Urban Ecosystem National Observation and Research Station, National Forestry and Grassland Administration, Guilin 541006, China

3. International Research Centre on Karst under the Auspices of UNESCO, National Center for International Research on Karst Dynamic System and Global Change, Guilin 541004, China

Abstract

Although the thermal dissipation probe (TDP) method is prominent in forest transpiration studies, the accurate estimation of sap flow density in particular trees with different wood structures remains highly variable. To verify the applicability of the TDP method in the measurement of the transpirational water consumption of shrub communities in degraded karst areas in southern China, Granier’s original formula was validated and corrected using the isolated stem segment method with Celtis sinensis, Xylosma congesta, Triadica sebifera, Paliurus ramosissimus, Pyracantha fortuneana, Sageretia thea, and Phanera championii. Finally, the correction coefficients were analyzed in relation to wood structural parameters. Our study reveals that the sap flow density estimated using Granier’s original formula exhibited varying degrees of overestimation or underestimation compared to the measured sap flow density. The differences ranged from −78.9% to 114.2%, highlighting the need for formula correction. Consequently, we adjusted the coefficients α and β of the original formula (n = 3–5), resulting in a revised range of 0.0047–0.0509 g cm−2 s−1 and 0.5882–1.9821 (R2 = 0.81–0.97), respectively. The conduit diameter was significantly correlated with the correction coefficient α. It is currently unknown whether the results obtained for a particular species can be applied to different growth environments and more prominent individuals of the same species. In conclusion, it is necessary to verify the applicability of Granier’s original formula when estimating water consumption through transpiration in trees.

Funder

National Nature Science Foundation of China

Fund of Guangxi Key Laboratory of Plant Conservation and Restoration Ecology in Karst Terrain

Guangxi Academy of Sciences Gui Scientist Launch Project

Guangxi Scientific and Technological Project

Publisher

MDPI AG

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