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Long-term patterns of Douglas-fir and western hemlock mortality in the western Cascade Mountains of Washington and Oregon.

机译:华盛顿和俄勒冈州喀斯喀特山脉西部的道格拉斯冷杉和西铁杉死亡率的长期分布。

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Change in temporal patterns of mortality rates, tree population structure (size and density), biomass accumulation, input of coarse woody debris, and causes of mortality of Douglas-fir (Pseudotsuga menziesii (Mirb.) Franco) and western hemlock (Tsuga heterophylla (Raf) Sargent) were investigated in nine stands spanning the young (45–80 yr), mature (81–200 yr), and old-growth (>200 yr) stages of forest development using long-term records (12 to 84 yr) in permanent plots in the Cascade Mountains of western Washington and Oregon. High average annual mortality rates for Douglas-fir (1.1–2.9%) occurred in young stands which was driven by the mortality of small, suppressed trees (25 cm DBH). In old growth, mortality rates were substantially lower (0.5–0.7%) and causes were from density-independent agents notably root and stem decay. In young and mature stands, the high rates of mortality of small Douglas-fir had little negative effect on the accumulation of biomass which increased steadily (∼4.8 Mg ha−1 yr−1). However, in old growth, due to minimal recruitment, slow growth, and continued mortality, Douglas-fir biomass accumulation rates were mostly negative and standing stocks decreased. Average annual input of Douglas-fir woody debris was similar among all stand ages (∼2.1 Mg ha −1 yr−1). Western hemlock average annual mortality rates were low in young (0.0%) and mature (0.1%) stands, but, in old growth, rates were greater (0.3–0.5%) due to a combination of suppression, snow loading and physical damage from falling trees. Western hemlock contribution to biomass was minimal as the majority of individuals were small. Mortality was also composed mostly of small trees and input to woody debris was light (0.2–0.8 Mg ha−1 yr −1). Many of the patterns that emerge from these records support previous assumptions about mortality, although these are among the first data to confirm these trends. The larger perspective provided by these data sets allow for some new inferences about relationships of tree mortality to forest stand development and ecosystem processes.
机译:死亡率,树木种群结构(大小和密度),生物量的积累,粗木屑的输入以及道格拉斯冷杉( Pseudotsuga menziesii (Mirb。)Franco)的死亡原因随时间的变化和西部铁杉((Raf)Sargent)在9个林分中进行了调查,这些林分年轻(45-80岁),成熟(81-200岁)和陈年(> 200岁)在华盛顿西部和俄勒冈州的喀斯喀特山脉永久性地块中使用长期记录(12至84年)记录森林发展的各个阶段。幼小林分道格拉斯冷杉的年平均死亡率很高(1.1%至2.9%),这是由小型,受压抑的树木(<25 cm DBH)的死亡率所驱动。在旧的增长中,死亡率大大降低(0.5-0.7%),其原因是与密度无关的物质,尤其是根和茎的腐烂。在幼小和成熟的林分中,小道格拉斯冷杉的高死亡率对稳定地增加(〜4.8 Mg ha -1 yr -1 )。然而,在旧的增长中,由于最少的募集,缓慢的增长和持续的死亡率,花旗松生物量积累速率大多为负,而常备种群减少。花旗松木屑的年平均输入量在所有林分年龄之间均相似(〜2.1 Mg ha -1 yr -1 )。西部铁杉幼年(0.0%)和成熟(0.1%)林的年平均死亡率低,但在老龄林中,由于压抑,积雪和物理损害造成的死亡率更高(0.3-0.5%)倒下的树木。西方铁杉对生物量的贡献很小,因为大多数个体很小。死亡率也主要由小树组成,木质碎片的输入量很小(0.2–0.8 Mg ha -1 yr -1 )。从这些记录中得出的许多模式都支持先前关于死亡率的假设,尽管这些是确认这些趋势的首批数据之一。这些数据集提供的更大视角允许对树木死亡率与林分发育和生态系统过程之间关系的一些新推论。

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