4.5 Article

Branch transpiration of pine and spruce scaled to tree and canopy using needle biomass distributions

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TREES-STRUCTURE AND FUNCTION
卷 14, 期 7, 页码 384-397

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SPRINGER HEIDELBERG
DOI: 10.1007/PL00009774

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boreal forest; Norway spruce; Scots pine; sap-flow; allometric relationships

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Branch water exchange and total tree water uptake were measured in a mixed Norway spruce and Scots pine stand in central Sweden during the 1995 and 1996 growing seasons. Branch transpiration was scaled to canopy level on the basis of a branch conductance model, using vertical needle-area distributions obtained by destructive sampling. Comparison with total tree water uptake scaled to canopy level showed agreement within 10%, for periods when the canopy was not affected by climatically induced stress. Comparison of scaled fluxes on individual trees showed that measurements of transpiration at branch level provide information on the direct response of transpiration to variations in weather, and furthermore that the time-lag between transpiration and tree water uptake was as much as 3 h. The vertical needle-area distribution of Scots pine was similar to that found by other authors. Needle-area distribution on Norway spruce, which has not been described before, showed that it has its largest needle area at the top of the crown. Specific needle area varied considerably both within trees and between trees. For spruce, mean specific needle area (+/-SD) varied from 2.4+/-0.5 mm(2) mg(-1) at the top of the crown to 7.1+/-1.9 mm(2) mg(-1) at the base. Corresponding figures for Scots pine were 3.4+/-2.0 and 9.1+/-2.1.

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