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沟壑演化与低地地貌对重新造林的调整。

Gully evolution and geomorphic adjustments of badlands to reforestation.

机构信息

Climatic Change and Climate Impacts, Institute for Environmental Sciences, University of Geneva, Boulevard Carl-Vogt 66, CH-1205 Geneva, Switzerland.

Department of Earth and Environmental Sciences, University of Geneva, CH-1205 Geneva, Switzerland.

出版信息

Sci Rep. 2017 Mar 22;7:45027. doi: 10.1038/srep45027.

Abstract

Badlands and gullied areas are among those geomorphic environments with the highest erosion rates worldwide. Nevertheless, records of their evolution and their relations with anthropogenic land transformation are scarcer. Here we combine historical data with aerial photographs and tree-ring records to reconstruct the evolution of a badland in a Mediterranean environment of Central Spain. Historical sources suggest an anthropogenic origin of this badland landscape, caused by intense quarrying activities during the 18 century. Aerial photographs allowed detection of dramatic geomorphic changes and the evolution of an emerging vegetation cover since the 1960s, due to widespread reforestation. Finally, tree-ring analyses of exposed roots allowed quantification of recent channel incision of the main gully, and sheet erosion processes. Our results suggest that reforestation practices have influenced the initiation of an episode of incision in the main channel in the 1980s, through the hypothesized creation of disequilibrium in water-sediment balance following decoupling of hillslopes from channel processes. These findings imply an asymmetry in the geomorphic response of badlands to erosion such that in the early evolution stages, vegetation removal results in gullying, but that reforestation alone does not necessarily stabilize the landforms and may even promote renewed incision.

摘要

荒地和沟壑地区是世界上侵蚀率最高的地貌环境之一。然而,它们的演化记录及其与人为土地转化的关系却较为少见。在这里,我们结合历史数据、航空照片和树木年轮记录,重建了西班牙中部一个地中海环境荒地的演化过程。历史资料表明,这种荒地景观是由 18 世纪剧烈采石活动引起的人为起源。航空照片检测到了自 20 世纪 60 年代以来的剧烈地貌变化和新兴植被覆盖的演化,这是由于广泛的重新造林。最后,对暴露的根系进行树木年轮分析,定量了近期主沟的深切和片蚀过程。我们的结果表明,重新造林实践可能通过假设在山坡与河道过程脱钩后,水沙平衡的失衡,影响了主河道在 20 世纪 80 年代切入阶段的开始。这些发现意味着荒地对侵蚀的地貌响应存在不对称性,即在早期演化阶段,植被移除会导致沟壑,但仅重新造林不一定能稳定地貌,甚至可能促进重新切入。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9d38/5361202/95199f17c398/srep45027-f1.jpg

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