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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Carbon pools in stream-riparian corridors: legacy of disturbance along mountain streams of south-eastern Wyoming
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Carbon pools in stream-riparian corridors: legacy of disturbance along mountain streams of south-eastern Wyoming

机译:河岸走廊的碳库:怀俄明州东南部山区河流沿岸扰动的遗留物

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Streams and their accompanying riparian environments are intrinsic components of terrestrial carbon cycling. However, they have been understudied in terms of the magnitude of their storage components and the role of disturbance in determining carbon storage capacity. This study presents partial carbon budgets for stream-riparian corridors along six study reaches in mountain headwater streams of southeast Wyoming to evaluate the impact of tie-driving, a historic disturbance legacy, on contemporary carbon storage. Detailed measurements of biomass were collected for in-stream components of carbon including fine and coarse particulate organic matter and in-stream large wood. Biomass was also estimated for riparian components including standing trees (live and dead), regenerating conifers, shrubs and herbaceous vegetation, downed wood, litter, and duff (partially decayed litter). Biomass was converted to carbon for all components and differences in storage were compared between tie-driven and non-driven reaches. Carbon content in riparian soils (to approximately 20 cm) was also measured. Twice the amount of carbon was stored in the riparian areas relative to the streams; most carbon was stored in standing trees (live and dead). While overall carbon storage within the riparian areas and streams were similar between disturbance conditions, the amount of carbon stored in large in-stream wood and downed wood on the floodplain was significantly higher in systems that were not tie-driven. The results of this study indicate that legacies of tie-driving influence carbon storage within the region, while also capturing baseline estimates of carbon storage in the wake of recent bark beetle infestations. Copyright (c) 2015 John Wiley & Sons, Ltd.
机译:河流及其伴随的河岸环境是陆地碳循环的内在组成部分。但是,就其存储成分的大小以及扰动在确定碳存储容量方面的作用而言,尚未对它们进行研究。这项研究提出了怀俄明州东南部山区源头河流沿六个研究河段的河岸走廊的部分碳预算,以评估领带驾驶(一种历史性的干扰遗产)对当代碳储存的影响。收集了包括细小颗粒有机物和粗大颗粒木炭在内的碳的上游成分的生物量详细测量值。还估计了生物量的河岸成分,包括站立的树木(活的和死的),再生的针叶树,灌木和草本植物,倒下的木材,垃圾和达芙(部分腐烂的垃圾)。将生物质转化为所有成分的碳,并比较领带驱动和非驱动触及范围之间的存储差异。还测量了河岸土壤(约20厘米)中的碳含量。相对于溪流,在河岸地区储存了两倍的碳。大部分碳储存在站立的树木中(活着的和死去的)。尽管扰动条件之间,河岸区域和河流中的总碳存储量相似,但在非领带驱动的系统中,洪泛平原上大型流木和倒下木中的碳存储量明显更高。这项研究的结果表明,领带驾驶的遗留影响了该地区的碳储量,同时还捕获了最近的树皮甲虫侵扰后碳储量的基线估计值。版权所有(c)2015 John Wiley&Sons,Ltd.

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