Elemental composition and mineralogical characteristics of volcanic ash and soil affected by the eruption of Mount Semeru, East Java

Q3 Social Sciences
Tri Candra Setiawati, M. Nurcholis, Basuki Basuki, S. A. Budiman, D. Yudiantoro
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Abstract

The eruption of Mount Semeru at the end of 2021 was responsible for emitting volcanic ash with specific characteristics. These unique mineralogy and chemical properties have both positive and negative effects on soil fertility, as excessive heavy metals adversely affect soil, plants, and the environment. Therefore, this study aimed to determine the distribution of volcanic ash cover from the eruption of Mount Semeru and investigate elemental composition as well as mineral characteristics of volcanic ash and soil covered by volcanic ash. The investigation was carried out in Supiturang village, Pronojiwo District, Lumajang, East Java, Indonesia. Sampling was carried out following the toposequence method, covering agricultural land within approximately ± 15 km from Mount Semeru. Pure volcanic ash was collected at sites not contaminated with soil. At the site location, it was found that the depth of volcanic ash cover ranged from “thin” (<2 cm) to “very thick” (>10 cm). The results of SEM and XRD analyses showed that of the pure volcanic ash contained quartz (50%), rock fragments (15%), plagioclase (12%), hornblende (10%), opaque (8%), and pyroxene (5%) minerals. The results of XRF analysis showed that the dominant elements in volcanic ash and soil were silica (Si), aluminum (Al), calcium (Ca), iron (Fe), and potassium (K). Several non-essential heavy metal elements found were Pb, Sn, and As, while rare minerals discovered were Y, Nb, Eu, and Yb at relatively low concentrations. The SEM analysis showed the structure of volcanic ash dominated by prismatic and blocky.
受东爪哇塞梅鲁火山喷发影响的火山灰和土壤的元素组成和矿物学特征
2021 年底塞梅鲁火山的喷发造成了具有特殊性质的火山灰的喷发。这些独特的矿物学和化学特性对土壤肥力既有积极影响,也有消极影响,因为过量的重金属会对土壤、植物和环境造成不利影响。因此,本研究旨在确定塞梅鲁火山喷发后火山灰覆盖层的分布情况,并调查火山灰和火山灰覆盖土壤的元素组成和矿物特性。调查在印度尼西亚东爪哇省卢马让市普罗诺吉沃区苏皮图朗村进行。采样按照地形序列法进行,覆盖了距离塞梅鲁火山约 ± 15 公里范围内的农田。在未受土壤污染的地点采集了纯火山灰。在取样地点发现,火山灰覆盖的深度从 "薄"(10 厘米)到 "厚 "不等。扫描电镜和 XRD 分析结果显示,纯火山灰含有石英(50%)、岩石碎片(15%)、斜长石(12%)、角闪石(10%)、不透明(8%)和辉石(5%)等矿物。XRF 分析结果显示,火山灰和土壤中的主要元素是硅(Si)、铝(Al)、钙(Ca)、铁(Fe)和钾(K)。发现的几种非基本重金属元素为铅、锡和砷,而稀有矿物质为钇、铌、铕和镱,含量相对较低。扫描电镜分析表明,火山灰的结构以棱柱形和块状为主。
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来源期刊
Journal of Degraded and Mining Lands Management
Journal of Degraded and Mining Lands Management Environmental Science-Nature and Landscape Conservation
CiteScore
1.50
自引率
0.00%
发文量
81
审稿时长
4 weeks
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