印度尼西亚ungaran山下斜坡地成过程的人为干扰研究

IF 0.5 Q4 GEOGRAPHY, PHYSICAL Revista Brasileira de Geomorfologia Pub Date : 2022-07-01 DOI:10.20502/rbg.v23i3.2142
J. Juhadi, ‪Elok Surya Pratiwi, E. Trihatmoko, Aprillia Findayani, J. Sartohadi, Nur Hamid
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引用次数: 0

摘要

火山岩开采活动无疑会使植被消失,引起自然环境的变化。作为土地恢复计划的一部分,植被恢复工作经常遇到许多障碍,因为它大多是在没有充分了解采矿后地区的详细形态和土壤特征的情况下进行的。本文研究了印度尼西亚中爪哇省Ungaran山北坡安山岩开采引起的地表形态、近期地貌过程和土壤性质等地质成因变化。首先利用无人机获取的小幅面航拍图像生成数字地形模型,识别采矿引起的地表形态变化;对受影响矿区和未受影响矿区的土壤样品进行了现场观测和室内试验,分析了土壤理化性质的变化。研究表明,采矿活动已将单一的凸丘转变为由斜坡带、盆地和平坦区组成的复杂地表形态。人为干扰对矿区成土过程的影响主要表现为母质的蚀变使矿区回到土壤发育的早期阶段,表层土的减少改变了矿区的成因层位。此外,采矿结束后地表形态的变化和植被覆盖的缺失也分别在斜坡和盆地上以切口和沉积的形式触发了新的地貌过程。较细的沉积层在盆地带形成新的母物质。土壤实验室数据表明,受影响的土壤往往具有较高的碱饱和度,但较低的有机碳和全氮水平,这导致支持植被生长的不利环境。精确的地表形态设计、额外的土壤表面保护和有机质增加可以为土地管理者提供明智的建议,以控制安山岩开采后地区的土壤切口和支持植被生长。
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THE STUDY OF ANTHROPOGENIC DISTURBANCE ON GEOPEDOGENETIC PROCESS AT THE LOWER SLOPE OF MT. UNGARAN, INDONESIA
Volcanic rocks mining activity will undoubtedly remove vegetation cover and cause the physical environment changes. Revegetation effort as part of land rehabilitation program then often found many obstacles because it was mostly conducted without adequate knowledge of detailed morphology and soil characteristics at the post-mining area. This study investigates the geopedogenetic changes, including land surface morphology, recent geomorphic processes, and soil properties caused by andesite rocks exploitation at the northern flank of Mt. Ungaran, Central Java Province of Indonesia. A digital terrain model was firstly generated from small format aerial photography acquired by an unmanned aerial vehicle (UAV) to identify the surface morphology changes due to the mining. Soil observation on field and laboratory test were conducted from samples at the affected and unaffected mining areas in order to analyse the changes on pysiochemical properties. This research exhibits that the mining activities have altered a single convex hill into a complex land surface morphology consisting of sloping zone, basins and flat area. Human disturbance on pedogenetic process at the mining area are in the form of parent material alteration that make them return to the early stage of soil development and top soil reduction that modify its genetic horizons. In addition, the changes on surface morphology and the absence of vegetation cover right after the mining ends also triggered new geomorphic processes in the form of incision and deposition on slopes and basin respectively. The finer deposit layers then become a new parent material at the basin zone. Soil laboratory data demonstrate that the affected soils tend to have a high level of base saturation, but lower C-organic and N-total levels, which result in a less favourable environment for supporting vegetation growth. A precise surface morphology design, extra soil surface protection and organic matter enhancement could be wise recommendations for land managers to control soil incision and support vegetation growth at the andesite post-mining area.
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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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