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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Forest age, wood and nutrient dynamics in headwater streams of the Hubbard Brook Experimental Forest, NH
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Forest age, wood and nutrient dynamics in headwater streams of the Hubbard Brook Experimental Forest, NH

机译:新罕布什尔州哈伯德布鲁克试验林的源头溪流中的森林年龄,木材和养分动态

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Instream processing may substantially alter nutrient export from forested watersheds. This study tested how instream uptake of N and P were affected by successional differences in the accumulation of large wood and debris dams in a 66-year chronosequence formed by five watersheds within the Hubbard Brook Experimental Forest (HBEF), NH. Nutrient enrichment releases in summer 1998 were used to measure the uptake velocities of phosphate, nitrate and ammonium for five streams within HBEF, and results indicated that uptake of PO43- was closely associated with forest age. In 2004, we quantified volume and abundance of large wood in each stream to test whether large wood abundance could be linked to nitrate uptake as well as phosphate. The volume of instream wood increased with forest age, at an apparent rate of 0.03 m(3) (100 m)(-1) per year for these early to mid-successional forests (r(2)=0.95); however, debris dam frequency did not. Instead, debris dam frequency, when controlled for stream size, followed a U-shaped distribution, with high dam frequency in very young forests, low frequency in forests around 20-30 years of age and increasing dam frequency again as forests matured. Phosphate uptake velocity increased strongly with both forest age and large wood volume (r(2)=0.99; P<0.001 in both cases); however, nitrate and ammonium uptake were not related to either factor. We attribute the positive relationship between phosphate uptake velocity and forest age/large wood volume to increased abiotic adsorption of phosphate by the inorganic sediments retained by wood. Nitrogen uptake in these streams is primarily biologically driven and did not vary predictably with these structural features of channels. We expect wood abundance to increase in HBEF streams as the forest matures, with a subsequent increase in stream phosphate uptake capacity. Copyright (c) 2007 John Wiley & Sons, Ltd.
机译:溪流加工可能会大大改变森林流域的养分出口。这项研究测试了新罕布什尔州布鲁克实验森林(HBEF)内的五个流域形成的66年时间序列中,大型木材和碎屑坝积累的连续差异如何影响氮和磷的吸收。 1998年夏季的营养富集释放量用于测量HBEF中五种水流的磷酸盐,硝酸盐和铵的吸收速度,结果表明PO43-的吸收与森林年龄密切相关。在2004年,我们量化了每条河流中大木材的体积和丰度,以测试大木材丰度是否与硝酸盐和磷酸盐的吸收有关。这些早期到中期的高级森林的入流木材量随森林年龄的增加而增加,表观速率为每年0.03 m(3)(100 m)(-1)(r(2)= 0.95);但是,泥石坝频率没有。相反,当控制河流的大小时,泥石坝频率呈U形分布,在非常年轻的森林中,泥石坝频率较高,在20-30岁左右的森林中,泥石坝频率较低,随着森林的成熟,泥石坝频率再次增加。磷的吸收速度随森林年龄和大木材体积而显着增加(r(2)= 0.99;两种情况下P <0.001);但是,硝酸盐和铵的吸收与这两个因素都不相关。我们将磷酸盐吸收速度与森林年龄/大木材量之间的正相关性归因于木材保留的无机沉积物对磷酸盐的非生物吸附增加。这些流中的氮吸收主要是由生物驱动的,并且不会随通道的这些结构特征发生变化。我们预计随着森林的成熟,HBEF溪流中木材的丰度将增加,溪流中磷的吸收能力也会随之增加。版权所有(c)2007 John Wiley&Sons,Ltd.

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