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首页> 外文期刊>Ecosystems >A Decade of Streamwater Nitrogen and Forest Dynamics after a Mountain Pine Beetle Outbreak at the Fraser Experimental Forest, Colorado
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A Decade of Streamwater Nitrogen and Forest Dynamics after a Mountain Pine Beetle Outbreak at the Fraser Experimental Forest, Colorado

机译:在科罗拉多州弗雷泽实验森林爆发后的山地松树甲虫爆发后的十年流动氮气和森林动力学

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Forests of western North America are currently experiencing extensive tree mortality from a variety of bark beetle species, and insect outbreaks are projected to increase under warmer, drier climates. Unlike the abrupt biogeochemical changes typical after wildfire and timber harvesting, the outcomes of insect outbreaks are poorly understood. The mountain pine bark beetle (Dendroctonus ponderosae) began to attack lodgepole pine (Pinus contorta) at the Fraser Experimental Forest in 2002 and spread throughout the research area by 2007. We compared streamwater nitrogen (N) from 2003 through 2012 with data from the previous two decades in four watersheds with distinct forest management histories, stand structures, and responses to the beetle outbreak. Watersheds dominated by old-growth had larger trees and lost 85% of overstory pine and 44% of total basal area to bark beetles. In contrast, managed watersheds containing a mixture of second-growth (30-60 year old) and old-growth (250- to 350-year old) had higher density of subcanopy trees, smaller mean tree diameter, and lower bark beetle-induced mortality (similar to 26% of total basal area). Streamwater nitrate concentrations were significantly higher in old-growth watersheds during the outbreak than pre-outbreak levels during snowmelt and base flow seasons. In mixed-age stands, streamwater nitrate concentrations were unaffected by the outbreak. Beetle outbreak elevated inorganic N export 43 and 74% in two old-growth watersheds though the amounts of N released in streamwater were low (0.04 and 0.15 kg N ha(-1)) relative to atmospheric inputs ( 2% of annual N deposition). Increased height, diameter, and foliar N of measured in residual live trees augmented demand for N, far in excess of the change in N export during the outbreak. Reallocation of soil resources released after pine mortality to overstory and understory vegetation helps explain high nutrient retention in watersheds affected by bark beetle outbreaks.
机译:西北美洲森林目前正在从各种树皮甲虫物种中经历广泛的树脂,并且预计昆虫爆发会在加热器下增加,干燥的气候。与野火和木材收割后典型的突然生物地球化学变化不同,昆虫爆发的结果很差。山地松树甲壳虫(Dendroctonus ponderosae)于2002年开始在弗雷泽实验森林中攻击小屋松树(Pinus Contorta),到2007年的研究区蔓延。我们将Streamwater氮(n)与来自之前的数据进行了比较了2003年至2012年四十年来四个流域,具有不同的森林管理历史,立场结构和对甲虫爆发的反应。由旧成长为主的流域具有较大的树木,损失了85%的夸张松树,占巴克甲虫的总基础区域的44%。相比之下,含有二生长(30-60岁)和旧增长(250至350岁)的混合物的管理流域具有较高的细胞植物,较小的平均树径和较低的树皮甲虫引起的死亡率(类似于总基础区域的26%)。在爆发期间,旧生流域液体硝酸盐浓度明显高于冰殖期间的爆发前水平和基础流动季节。在混合年龄的展台中,流水硝酸盐浓度不受爆发的影响。甲虫爆发在两个旧生流域中升高的无机N导出43和74%,尽管流水中的n释放的n次较低(0.04和0.15kg n(-1))相对于大气输入(&1%的每年N.沉积)。在剩余活树上测量的高度,直径和叶面N增加,在爆发期间不超过N导出的不超过N导出的需求。松原死亡率释放的土壤资源重新分配给夸大和林植植被有助于解释受树皮甲虫爆发的流域的高营养保留。

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