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STATUS AND TREND OF COTTONWOOD FORESTS ALONG THE MISSOURI RIVER

机译:密苏里河沿岸棉花森林的现状和趋势

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摘要

From 2007-2009, we studied the current (2006) and historic (1892, mid-1950s) extent, current age distribution, and plant species composition of plains cottonwood (Populus deltoides) and non-cottonwood riparian stands along eight study segments of the Missouri River between Fort Benton, Montana and Kansas City Missouri, covering 930 river miles (1500 km) or over 1/3 of the river\u27s length. These segments included all of the unchannelized and unimpounded segments below Fort Benton, as well as portions of two impounded and one channelized segment. Based on GIS analyses of historic maps and aerial photography, the combined area of forests, woodlands, and shrublands in the historic floodplain declined 47% across all study segments from 1892 to 2006, with losses linked to clearing for human land uses (primarily agricultural cropland) or inundation by reservoirs. Most forest loss occurred between 1892 and the 1950s, while most shrubland loss has occurred from the 1950s to 2006. As of 2006, we estimate that a total of 75,600 hectares (186,900 acres) of shrubland, woodland, and forest occurred within the mapped area of the eight study segments, with 66,800 hectares (165,000 acres) or 88% of the total, composed of patch types which contain cottonwood as a significant component. Most (62%) of the cottonwood area is composed of stands \u3e50 years old, and only 14% is from stands that have recruited in the last 25 years. These patterns, along with significant historic declines in shrubland and sandbar area on most segments, indicate that the fluvial geomorphic dynamics that drive cottonwood recruitment have been reduced, and cottonwood regeneration compromised, under the river management practices of at least the last 25-30 years. A significant proportion (24%) of forest in the 25-50 year age class, however, suggested that a temporary pulse in recruitment accompanied geomorphic adjustments in the channel during the first 2-3 decades after dam closure on some segments. We sampled plant species composition and vegetation structure across an age gradient of cottonwood and non-cottonwood riparian stands in each study segment, with a total of 332 stands sampled, of which 216 were relatively intact natural cottonwood stands. Indices of plant species richness, wetland affinity, and floristic quality differed among stands and study segments, providing possible metrics for evaluating stand- and segment-level differences in biotic integrity. Segments 4 (below Garrison Dam) and 10 (below Gavins Point Dam) had the highest stand-level species richness (~35 species per stand) and highest floristic quality (Coefficient of Conservatism values) of all segments, while segment 6 (below Oahe Dam) had the lowest of each. Stressors that may influence segment-level vegetation and landscape patterns include land management (e.g., grazing, vegetation management); forest clearing for agricultural cropland and urban or exurban expansion; channel incision and cessation of overbank flooding below dams; disruption of sediment supply and transport, with resultant declines in formation of alluvial surfaces needed for cottonwood recruitment; and aggradation with resultant water table rise adjacent to river-reservoir delta areas. In the report that follows, we provide summaries of current and historic land cover, cottonwood age distribution, and vegetation patterns for each of the eight study segments, as well as an overview across all segments.
机译:从2007年至2009年,我们研究了沿该区的八个研究分部的平原杨木(杨木)和非棉花木河岸林分的当前(2006年)和历史(1892年,1950年代中期)范围,当前年龄分布以及植物种类组成。密苏里州本顿堡,蒙大拿州和堪萨斯城密苏里州之间的密苏里河,覆盖930公里(1500公里),超过河流的1/3。这些路段包括本顿堡以下所有未通道化和未扣留的路段,以及两个已扣押和一个通道化路段的一部分。根据GIS对历史地图和航空摄影的分析,从1892年到2006年,历史洪泛区中的森林,林地和灌木地的总面积在所有研究领域中下降了47%,其损失与清理人类土地用途(主要是农田)有关)或被水库淹没。大部分森林流失发生在1892年至1950年代之间,而大多数灌木丛流失发生在1950年代至2006年之间。截至2006年,我们估计在该地图区域内共有75,600公顷(186,900英亩)的灌木丛,林地和森林在八个研究区中,有66,800公顷(165,000英亩),占总研究区的88%,是由以杨木为重要成分的斑块类型组成的。三叶草地区的大部分地区(62%)由50年以上的林分组成,而只有14%来自最近25年内招募的林分。这些模式,以及大部分地区灌木丛和沙洲地区的历史性大幅度下降,表明在至少过去25-30年的河流管理实践中,驱动杨木募集的河流地貌动力学已经减少,杨木再生受到损害。 。然而,在25至50岁年龄段的森林中,有很大比例的森林(24%)表明,在某些路段关闭大坝后的最初2-3年中,临时性的脉动伴随着河道的地貌调整。在每个研究阶段,我们对杨木和非棉木河岸林分年龄梯度的植物物种组成和植被结构进行了采样,总共采样了332个林分,其中216个是相对完整的天然杨木林。林分和研究部分之间植物物种丰富度,湿地亲和力和植物质量的指标各不相同,为评估林分和部分水平生物完整性的差异提供了可能的指标。第4节(驻军大坝以下)和第10节(在Gavins Point大坝以下)在所有节段中具有最高的林分物种丰富度(每个林分约35种)和最高的植物区系(保守系数),而第6节(在Oahe以下)大坝)的价格最低。可能影响段级植被和景观格局的压力源包括土地管理(例如放牧,植被管理);为农业耕地开垦森林和城市或郊区扩张;大坝下的河道切开和停止泛滥洪水;沉积物的供应和运输中断,从而导致三角叶杨招募所需的冲积层形成减少;河流水库三角洲地区附近的水位逐渐上升。在下面的报告中,我们提供了八个研究部分中每一个的当前和历史土地覆盖,杨木年龄分布和植被模式的摘要,以及所有部分的概述。

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