草地基质中桉树种植与Sesmaria河流域沟渠侵蚀恢复:源头河谷不稳定循环

IF 0.5 Q4 GEOGRAPHY, PHYSICAL
Ana Carolina Facadio, Anderson Mululo Sato, Ana Luiza Coelho Netto
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引用次数: 0

摘要

在21世纪,桉树种植园在巴西西南部Paraíba do Sul河的中部山谷扩大,取代了退化的牧场。一些研究将这些人工林与地下水位的降低联系起来,但是实地观察表明,与永久和临时地下水流有关的侵蚀活动更为重要。本研究的重点是在牧区引入桉树后,侵蚀过程的重新激活导致沟壑的退行性生长。引入桉树后,进行了入渗试验、土壤吸力监测、井水水位和沟蚀监测。结果表明:桉树覆盖有利于雨水入渗,为临时含水层和悬浮含水层提供养分。这些水流,加上永久的含水层,由于对沟壑边缘、底部和斜坡的过度压力,造成了侵蚀。引进桉树后,侵蚀率逐年下降。沟壑区树木植被开始恢复,呈现稳定趋势。随着土地利用的变化,排水和侵蚀系统正在经历一个内部调整期,以寻求新的平衡和稳定。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Eucalyptus Planting in Pasture Matrix and Erosive Reactivation of Gullies in the Sesmaria River Basin (SP/RJ): a cycle of instability in headwater valleys
In the 21st century, eucalyptus plantations have expanded in the middle valley of the Paraíba do Sul River, in the southwestern region of Brazil, replacing degraded pastures. Some studies associate these plantations with the reduction of groundwater levels, but field observations have indicated that erosive activity related to permanent and temporary underground water flows is more significant. This study focuses on the reactivation of erosive processes leading to the regressive growth of gullies after the introduction of eucalyptus in pasture areas. Infiltration experiments, soil suction monitoring, well water levels, and gully erosion were conducted after the introduction of eucalyptus. The results indicated that eucalyptus cover facilitated rainwater infiltration, feeding temporary and suspended aquifers. These flows, combined with the permanent aquifer, caused erosion due to excessive pressure on gully margins, bottoms, and slopes. Erosion rates decreased over the years after the introduction of eucalyptus. Tree vegetation began to recover in the gullies, indicating a trend towards stabilization. In response to changes in land use, the drainage and erosion system are undergoing an internal adjustment period in search of a new balance and stability.
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来源期刊
CiteScore
1.30
自引率
40.00%
发文量
56
审稿时长
16 weeks
期刊介绍: The Revista Brasileira de Geomorfologia are focused on research, analysis and application of knowledge for the development of models of large sets of relief; fluvial dynamics; the processes of aspects, such as erosion and mass movements and their impact; survey, assessment and recovery of degraded areas; surveys and assessments of natural resources; thematic mapping and integrated relief; environmental zoning; among other relevant aspects of the land relief on any scale. From a technical and instrumental basis for the development of these studies, studies that use instruments to the survey, the interpretation and generalization of data on various aspects of the Earth''s surface, including the forms of occupation and use (s) company (s) human (s). As well as the use and integration of methods and techniques that enable geo technical and instrumental character important in scientific production and the definition of public policies.
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