Effects of forest thinning on soil-plant carbon and nitrogen dynamics

被引:54
作者
Bai, Shahla Hosseini [1 ,2 ]
Dempsey, Raymond [3 ]
Reverchon, Frederique [1 ,4 ]
Blumfield, Timothy J. [1 ]
Ryan, Sean [5 ]
Cernusak, Lucas A. [3 ]
机构
[1] Griffith Univ, Sch Environm, Environm Futures Res Inst, Brisbane, Qld, Australia
[2] Univ Sunshine Coast, Fac Sci Hlth Educ & Engn, Brisbane, Qld, Australia
[3] James Cook Univ, Coll Sci & Engn, Cairns, Qld, Australia
[4] Inst Ecol AC, Red Estudios Mol Avanzados, Apartado Postal 63, Xalapa, Veracruz, Mexico
[5] CEO Private Forestry Serv Queensland Australia, Brisbane, Qld, Australia
关键词
Stable isotopes; Inorganic nitrogen; Corymbia spp; Eucalyptus spp; Farm forestry; Water soluble total N and C; PINUS-TABULAEFORMIS PLANTATION; FOLIAR DELTA-N-15 VALUES; N-15; NATURAL-ABUNDANCE; TREE GROWTH; ISOTOPE DISCRIMINATION; RESTORATION TREATMENTS; ECTOMYCORRHIZAL COMMUNITY; NUTRIENT AVAILABILITY; WATER AVAILABILITY; BURNING TREATMENTS;
D O I
10.1007/s11104-016-3052-5
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Corymbia spp. (previously included in the genus Eucalyptus) are common species in sub/tropical Australia and produce high quality timber and round logs. Thinning of native forests helps to preserve native tree species and is more sustainable than replacing native forest stands with mono-species plantations to produce timber. This study aimed to explore the effects of native forest thinning on soil-plant carbon (C) and nitrogen (N) dynamics in two experimental sites, Esk (5 years post-thinning) and Herberton (7 years post-thinning), situated in Queensland, Australia. The two sites had different thinning regimes. The final stocking rates varied between 75 and 200 stems ha(-1) at Esk and between 250 and 400 stems ha(-1) at Herberton. The thinned plots were compared to un-thinned plots. Soil samples were collected to measure labile C and N. Leaf samples were collected from C. variegata and C. citriodora in Esk and Herberton respectively. Thinning did not change soil total C, total N, delta N-15 and inorganic N at either Esk or Herberton. However, at Esk, intensive thinning resulted in decreases in water soluble total N (WSTN). Foliar delta C-13 did not vary with respect to thinning whereas foliar delta N-15 values were more enriched in thinned areas than those of un-thinned plots. The stepwise linear regression indicated that both foliar total N and delta N-15 were explained mainly by soil TN and WSTN. Thinning did not change soil C and N most likely due to the retention of thinned materials on site and their incorporation into soil. Foliar delta C-13 was not thinning-dependent due to homeostatic maintenance of the ratio of intercellular to ambient CO2 concentrations during photosynthesis. In our study, soil N was not a limiting factor for foliar N, however, foliar N was mainly driven by WSTN which may foreshadow a possible N limitation in severely thinned plots in the long term. We conclude that forest thinning does not decrease soil C and N availability in native Corymbia forests for several years post-thinning if the thinned materials are retained on site.
引用
收藏
页码:437 / 449
页数:13
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