Woodall C W, Russell M B, Walters B F, D'Amato A W, Fraver S, Domke G M
Forest Service, Northern Research Station, US Department of Agriculture, 1992 Folwell Avenue, St Paul, MN, 55108, US.
Department of Forest Resources, University of Minnesota, Saint Paul, Minnesota, US.
Oecologia. 2015 Mar;177(3):861-874. doi: 10.1007/s00442-014-3171-8. Epub 2014 Nov 28.
Downed dead wood (DDW) in forest ecosystems is a C pool whose net flux is governed by a complex of natural and anthropogenic processes and is critical to the management of the entire forest C pool. As empirical examination of DDW C net flux has rarely been conducted across large scales, the goal of this study was to use a remeasured inventory of DDW C and ancillary forest attributes to assess C net flux across forests of the Eastern US. Stocks associated with large fine woody debris (diameter 2.6-7.6 cm) decreased over time (-0.11 Mg ha(-1) year(-1)), while stocks of larger-sized coarse DDW increased (0.02 Mg ha(-1) year(-1)). Stocks of total DDW C decreased (-0.14 Mg ha(-1) year(-1)), while standing dead and live tree stocks both increased, 0.01 and 0.44 Mg ha(-1) year(-1), respectively. The spatial distribution of DDW C stock change was highly heterogeneous with random forests model results indicating that management history, live tree stocking, natural disturbance, and growing degree days only partially explain stock change. Natural disturbances drove substantial C transfers from the live tree pool (≈-4 Mg ha(-1) year(-1)) to the standing dead tree pool (≈3 Mg ha(-1) year(-1)) with only a minimal increase in DDW C stocks (≈1 Mg ha(-1) year(-1)) in lower decay classes, suggesting a delayed transfer of C to the DDW pool. The assessment and management of DDW C flux is complicated by the diversity of natural and anthropogenic forces that drive their dynamics with the scale and timing of flux among forest C pools remaining a large knowledge gap.
森林生态系统中的倒伏枯木(DDW)是一个碳库,其净通量受自然和人为过程的复杂组合支配,对整个森林碳库的管理至关重要。由于很少在大尺度上对DDW碳净通量进行实证研究,本研究的目标是利用重新测量的DDW碳清单和辅助森林属性来评估美国东部森林的碳净通量。与大型细木残体(直径2.6 - 7.6厘米)相关的储量随时间减少(-0.11 Mg ha⁻¹ 年⁻¹),而较大尺寸的粗DDW储量增加(0.02 Mg ha⁻¹ 年⁻¹)。总DDW碳储量减少(-0.14 Mg ha⁻¹ 年⁻¹),而立木和活树储量均增加,分别为0.01和0.44 Mg ha⁻¹ 年⁻¹。DDW碳储量变化的空间分布高度异质,随机森林模型结果表明,管理历史、活树蓄积量、自然干扰和生长度日只能部分解释储量变化。自然干扰导致大量碳从活树库(≈ -4 Mg ha⁻¹ 年⁻¹)转移到立木库(≈ 3 Mg ha⁻¹ 年⁻¹),而较低腐烂等级的DDW碳储量仅略有增加(≈ 1 Mg ha⁻¹ 年⁻¹),这表明碳向DDW库的转移存在延迟。驱动DDW动态的自然和人为力量的多样性使DDW碳通量的评估和管理变得复杂,森林碳库之间通量的规模和时间仍然存在很大的知识空白。