Transpiration of Anatolian black pine and sessile oak forest stands in a sub-humid region of Turkey


Ozcelik M. S. , ŞENGÖNÜL K.

ANNALS OF FOREST RESEARCH, vol.64, no.1, pp.111-128, 2021 (Journal Indexed in SCI) identifier identifier

  • Publication Type: Article / Article
  • Volume: 64 Issue: 1
  • Publication Date: 2021
  • Doi Number: 10.15287/afr.2021.2047
  • Title of Journal : ANNALS OF FOREST RESEARCH
  • Page Numbers: pp.111-128
  • Keywords: principal component regression, sap flow, trunk heat balance, watershed management, vegetation management, SAP FLOW MEASUREMENTS, TREE WATER-USE, DECIDUOUS FOREST, CANOPY TRANSPIRATION, THERMAL DISSIPATION, QUERCUS-PETRAEA, SOIL-MOISTURE, GAS-EXCHANGE, HEAT-BALANCE, SCOTS PINE

Abstract

Transpiration is a key component of the watershed water budget. Therefore, determining the transpiration of forest stands with different characteristics have been of interest for watershed hydrology and forest management practices in a wide range of environments. The objectives of this study were to compare transpiration of Anatolian black pine (Pinus nigra Arn. subsp. pallasiana (Lamb.) Holmboe) and sessile oak (Quercus petraea (Matt.) Liebl.) tree stands and to model transpiration based on the measured climatic factors. Stand transpirations were calculated from sap flow measurements made by the trunk heat balance method. We conducted an exploratory factor analysis (PCR) to detect affecting meteorological factors of stand transpiration, and we developed linear regression equations to predict transpiration of pine and oak stands. Mean daily and yearly canopy transpiration (Ec) were 1.05 mm day(-1) and 378.3 mm year(-1) for the pine stand and 3.52 mm day(-1) and 801.7 mm year(-1) for the oak stand. There was a highly positive correlation between daily stand transpiration and wind speed, global radiation, air vapour pressure deficit and air temperature, but a negative correlation with relative humidity for both stands. Soil water potential had little effect on stand transpiration. The model equations accounted for 81% of the variations in transpiration for the pine stand and 85% for the oak stand. Therefore, the transpiration of forest stands should be considered for effective vegetation management practices, as model equations to estimate the transpiration of pine and oak stands in the region.