Department of Biology, University of South Dakota, Vermillion, SD 57069, USA.
Environ Manage. 2012 May;49(5):990-1008. doi: 10.1007/s00267-012-9842-5. Epub 2012 Apr 4.
Construction of six large dams and reservoirs on the Missouri River over the last 50-75 years has resulted in major landscape changes and alterations in flow patterns, with implications for riparian forests dominated by plains cottonwood (Populus deltoides). We quantified changes in land cover from 1892-1950s and the 1950s-2006 and the current extent and age structure of cottonwood forests on seven segments (two reservoir and five remnant floodplain) comprising 1127 km (53 %) of the unchannelized upper two-thirds of the Missouri River. Riparian forest area declined by 49 %; grassland 61 %; shrubland 52 %; and sandbar habitat 96 %; while agricultural cropland increased six-fold and river/reservoir surface area doubled from 1892 to 2006. Net rates of erosion and accretion declined between the 1892-1950s and 1950s-2006 periods. Accretion exceeded erosion on remnant floodplain segments, resulting in declines in active channel width, particularly in 1950s-2006. Across all study segments in 2006, most cottonwood stands (67 %) were >50 years old, 22 % were 25-50 years old, and only 10 % were <25 years old. Among stands <50 years old, the higher proportion of 25-50 year old stands represents recruitment that accompanied initial post-dam channel narrowing; while declines in sandbar and shrubland area and the low proportion of stands <25 years old suggest declines in geomorphic dynamism and limited recruitment under recent river management. Future conservation and restoration efforts should focus both on limiting further loss of remnant cottonwood stands and developing approaches to restore river dynamics and cottonwood recruitment processes.
在过去的 50-75 年里,密苏里河上建造了六座大型水坝和水库,这导致了主要的景观变化和水流模式的改变,这对以平原山杨(Populus deltoides)为主的河岸森林产生了影响。我们量化了 1892-1950 年代和 1950-2006 年期间的土地覆盖变化,以及当前七个区段(两个水库和五个残留洪泛区)上山杨森林的范围和年龄结构,这些区段涵盖了密苏里河未渠化的上三分之二部分的 1127 公里(53%)。河岸林面积减少了 49%;草地增加了 61%;灌木林减少了 52%;沙洲栖息地减少了 96%;而农业耕地增加了六倍,河流/水库表面积在 1892 年至 2006 年间增加了一倍。在 1892-1950 年代和 1950-2006 年代期间,侵蚀和淤积的净速率下降。在残留洪泛区区段上,淤积超过了侵蚀,导致活跃河道宽度下降,尤其是在 1950-2006 年代期间。在 2006 年的所有研究区段中,大多数山杨林(67%)的树龄>50 年,22%的树龄为 25-50 年,只有 10%的树龄<25 年。在树龄<50 年的林分中,25-50 年生林分的比例较高,这代表了最初大坝建成后河道变窄时的新的林分形成;而沙洲和灌木林面积的减少以及树龄<25 年的林分比例较低,则表明地貌动态的下降以及在最近的河流管理下新的林分形成有限。未来的保护和恢复工作应既侧重于限制剩余山杨林的进一步损失,又要制定方法来恢复河流动力和山杨的形成过程。