首页> 外文期刊>River Research and Applications >LARGE WOOD DEBRIS RECRUITMENT ON DIFFERING RIPARIAN LANDFORMS ALONG A GULF COASTAL PLAIN (USA) STREAM: A COMPARISON OF LARGE FLOODS AND AVERAGE FLOWS
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LARGE WOOD DEBRIS RECRUITMENT ON DIFFERING RIPARIAN LANDFORMS ALONG A GULF COASTAL PLAIN (USA) STREAM: A COMPARISON OF LARGE FLOODS AND AVERAGE FLOWS

机译:沿沿海平原(美国)流向的不同日地地形的大型木材碎片招募:大型洪水和平均流量的比较

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In southeastern Coastal Plain streams, wood debris can be very abundant and is recruited from extensive forested floodplains. Despite importance of wood debris, there have been few opportunities to examine recruitment and redistribution of wood in an undisturbed setting, particularly in the southeastern Coastal Plain. Following extensive flooding in 1994, measurements of individual downed trees (species, dbh, orientation, distance from base-flow channel and condition) were made across replicated riparian landforms in a Gulf Coastal Plain 5th-order stream. Annually, the fate of these trees was determined and newly recruited trees were noted. More than 300 downed trees have been recorded. Recruitment varied across landforms with more constrained reaches having greatest mortality. Total tree mortality varied substantially across years. Generally, tree recruitment was greatest in years with substantial floods (1994 and 1998). For each riparian landform type, tree mortality was correlated with the maximum daily flow during the period preceding annual debris surveys. This relationship was particularly strong for sand ridges (r~2 = 0.942) and low terraces (r~2 = 0.915), but was significant for floodplains (r~2 = 0.413). Greatest rates of debris recruitment per maximum daily flow were observed for sand ridges followed by low terraces. Flood characteristics also influenced debris recruitment. The 1994 flood was caused by a tropical storm and resulted in a rapid rise in streamflow. Much of the debris recruited during this flood was from toppled trees and was oriented parallel to the stream channel. In contrast, the 1998 flood was preceded by a wetter than average winter with more gradually rising flows and there was no relationship between riparian landform and debris characteristics. These results indicate that wood recruitment dynamics in Coastal Plain streams are complex. Wood recruitment rates are controlled by cyclical variations in climate interacting with riparian geomorphology. Infrequent high flows appear critical in the maintenance of the instream debris pool.
机译:在东南沿海平原溪流中,木屑可能非常丰富,并从森林茂密的洪泛区中收集。尽管木屑很重要,但在不受干扰的环境中,尤其是在东南沿海平原,几乎没有机会检查木材的募集和重新分配。在1994年发生大洪水之后,在墨西哥湾沿岸平原五阶河流中复制的河岸地貌中对单个倒下的树木(物种,dbh,方向,距基流通道的距离和状况)进行了测量。每年,确定这些树木的命运并记录新近采伐的树木。记录下来的树木超过300棵。不同地貌的招聘情况各不相同,到达率受到限制的地区死亡率最高。树木的总死亡率多年来变化很大。通常,在发生大量洪灾的年份(1994年和1998年),树木采伐量最大。对于每种河岸地貌类型,树木死亡率与年度碎片调查之前的最大日流量相关。对于沙脊(r〜2 = 0.942)和低阶阶地(r〜2 = 0.915),这种关系特别强烈,但对于洪泛区(r〜2 = 0.413)尤其重要。观察到沙脊和低阶阶地每最大日流量的碎片收集率最高。洪水特征也影响了残骸的收集。 1994年的洪水是由热带风暴引起的,导致流量急剧上升。洪水泛滥时收集的大部分碎片来自倒塌的树木,并与水流通道平行。相比之下,1998年的洪水发生之前,冬季比平常更湿,流量逐渐增加,河岸地貌与碎片特征之间没有关系。这些结果表明沿海平原溪流的木材采伐动态是复杂的。木材的补充率受气候变化和河岸地貌相互作用的周期性变化的控制。频繁出现的高流量对于维持河内垃圾池至关重要。

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