Dendrogeomorphology in Evaluating Erosive Processes in an Urban Conservation Unit

Q4 Social Sciences
Ricardo De Faria Nicolau, K. M. S. Faria, R. Momoli, M. P. Chagas
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引用次数: 0

Abstract

Water erosion is a worldwide problem that has been depleting soils mainly in tropical regions, due to the greater volume of precipitated water. In this sense, recent prediction methods in tropical regions such as dendrogeomorphology are necessary and important to identify and date the influence and correlation between erosion processes and vegetation. This study aimed to understand and scale the erosive processes, through the annual historical recognition of the rate of soil loss and sedimentation, applying the concepts of dendrogeomorphology in the evaluation of the stem and roots of trees of the species of Anadenanthera macrocarpa and Schefflera morototoni, in a conservation unit in the Brazilian Cerrado. Trees were selected in the following soil level conditions: (i) having root exposure, (ii) no exposure (buried), and (iii) no change in soil level (control). Cross-dating was performed using the COFECHA software program, and the information applied in dating scars and abnormal radial growth periods were observed in exposed roots and associated with the beginning of erosion processes. The results indicated that the occurrence of the erosive processes ascertained by anatomical changes in the exposed roots and a most common erosive rains date from 2006, 2008, 2009, 2010, 2012, 2013, 2016 and 2017. While changes in the trunk growth ring width start from 1992, with similar years between the two species of 2013 and 2017. The highest soil accumulation rates were 18.6 mm/year, vertical losses were 500 mm per year and horizontal losses were 665 mm. Finally, there is a positive correlation between the number of scars and an abrupt increase in the growth rings of the exposed roots with the number of erosive rains.
城市保护单元侵蚀过程评价中的树木地貌学
水土流失是一个世界性的问题,主要是在热带地区,由于沉淀水量较大,水土流失导致土壤流失。从这个意义上说,热带地区最近的预测方法,如树木地貌,对于识别和确定侵蚀过程与植被之间的影响和相关性是必要和重要的。本研究旨在通过对土壤流失和沉积速率的年度历史识别,将树木地貌学的概念应用于巴西塞拉多一个保护区的大果菊和莫罗托尼Schefflera morotoni物种的树干和树根的评估,从而了解和确定侵蚀过程的规模。在以下土壤水平条件下选择树木:(i)有根系暴露,(ii)没有暴露(掩埋),和(iii)土壤水平没有变化(对照)。使用COFCHA软件程序进行了年代测定,在暴露的根中观察到了用于年代测定疤痕和异常径向生长期的信息,这些信息与侵蚀过程的开始有关。结果表明,通过暴露根的解剖变化和最常见的侵蚀性降雨确定的侵蚀过程发生在2006年、2008年、2009年、2010年、2012年、2013年、2016年和2017年。而树干生长环宽度的变化始于1992年,2013年和2017年这两个物种的变化年份相似。土壤累积速率最高为18.6mm/年,垂直损失为500mm/年,水平损失为665mm。最后,伤痕数量和裸露根系生长环的突然增加与侵蚀性降雨的数量呈正相关。
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来源期刊
Anuario do Instituto de Geociencias
Anuario do Instituto de Geociencias Social Sciences-Geography, Planning and Development
CiteScore
0.70
自引率
0.00%
发文量
45
审稿时长
28 weeks
期刊介绍: The Anuário do Instituto de Geociências (Anuário IGEO) is an official publication of the Universidade Federal do Rio de Janeiro (UFRJ – CCMN) with the objective to publish original scientific papers of broad interest in the field of Geology, Paleontology, Geography and Meteorology.
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