4.6 Article

Changes in bark properties and hydrology following prescribed fire in Pinus taeda and Quercus montana

Journal

HYDROLOGICAL PROCESSES
Volume 37, Issue 1, Pages -

Publisher

WILEY
DOI: 10.1002/hyp.14799

Keywords

bark density; bark hygroscopicity; bark porosity; Chestnut oak; loblolly pine; prescribed fire

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Prescribed fire as a silvicultural technique is growing in popularity in the eastern United States. This study found that prescribed fire regimes alter the structure of bark, leading to changes in hydrological processes and drier conditions in the forest. Bark physical properties vary among species, with oak bark having higher density and slower drying rate compared to pine bark. However, both species showed lower density, higher porosity, greater water storage capacity, and faster drying in stands burned every 3 years.
In the eastern United States, the use of prescribed fire as a silvicultural technique to manage for desirable upland tree species is increasing in popularity. Bark physical properties such as thickness, density, and porosity have known associations with fire tolerance among species. These physical properties simultaneously influence rainfall interception and canopy storage and thus are of interest across a range of disciplines. Furthermore, while these characteristics are innate to a species, it is unknown whether repeated exposure to fire facilitates physical change in bark structure and whether these changes are consistent among species. To answer these questions, bark samples were collected from mature pine (Pinus taeda L.) and oak (Quercus montana Willd.) trees from sites across the Bankhead National Forest in Alabama, USA under three different burn regimes: 3-year cycle, 9-year cycle, and no fire. Samples were analysed in the laboratory for bulk density, porosity, water storage capacity, and hygroscopicity (the amount of atmospheric water vapour absorbed by bark during non-rainfall conditions). Drying rates of saturated samples under simulated wetting conditions were also assessed. Oak bark had higher bulk density, lower porosity, and dried slower than pine bark. Interestingly, bark from both species had lower bulk density, higher porosity, greater water storage capacity, and dried faster in stands that were burned every 3 years compared to other fire regimes (p < 0.001). In summary, this study demonstrates that prescribed fire regimes in an eastern US forest alter bark structure and thus influence individual tree control on hydrological processes. The increase in bark water storage capacity, coupled with faster bark evaporation times may lead to less water inputs to the forest floor and drier overall conditions. Further investigation of this fire-bark-water feedback loop is necessary to understand the extent of these mechanisms controlling landscape-scale conditions.

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