Artificial weathering of tropical woods. Part 2: Color change

被引:50
|
作者
Kishino, M
Nakano, T
机构
[1] Shimane Univ, Interdisciplinary Fac Sci & Engn, Dept Nat Resources Proc Engn, Lab Mat Recycling, Matsue, Shimane 6908504, Japan
[2] Hokkaido Forest Prod Res Inst, Asahikawa, Hokkaido, Japan
关键词
artificial weathering; CIE L* a* b*; color change; DRIFT spectra; tropical woods; UV-Vis diffuse reflectance spectra; yellowing;
D O I
10.1515/HF.2004.085
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
This paper describes the change in diffuse reflectance Fourier transform infrared (DRIFT) and ultravioletvisible (UVVis) diffuse reflectance spectra of the following eight tropical woods during artificial weathering up to 600 h in relation to their color changes, especially to yellowing: Amnurana acreana, Acacia auriculiformis, Dipterocarpus spp., Eucalyptus marginata, Eucalyptus robusta, Shorea spp. and Tabebuia spp. with relatively high and low specific gravity. For A. acreana, A. auriculiformis, Dipterocarpus spp. and both Tabebuia spp., Deltab* (yellowing) increased with exposure up to 50 h, and decreased above 50 h. For E. marginata, E. robusta and Shorea spp., on the other hand, both Deltaa* (shift to red) and Deltab* decreased with increased exposure time. For woods in which Deltab* increased, the Deltab* showed a positive dependence on the difference in relative intensity ratio of a band at 1740 cm(-1) to that at 2900 cm(-1) (DeltaD(1740)/D-2900) in DRIFT spectra of specimens before and after exposure. This result indicated that the increased band at 1740 cm(-1) played a significant role in the increased Deltab*. Then again, also for woods in which Deltab* decreased, the DeltaD(1740)/D-2900 increased, but was not related to the Deltab*. The DeltaD(1740)/D-2900 for woods in which Deltab* decreased had a positive relationship to the difference in remission function at 410 nm (DeltaF(Rinfinity)(410)) in UVVis diffuse reflectance spectra for specimens before and after exposure, while woods in which Deltab* increased were independent of the DeltaF(Rinfinity)(410). Therefore, it is suggested that woods in which Deltab* increased and decreased differ from one another in the contribution to the increase in the band at 1740 cm(-1), resulting in either an increase or decrease of Deltab*.
引用
收藏
页码:558 / 565
页数:8
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