Changes of Soil Chemistry Characteristics of Tephra Mount Anak Krakatau-Indonesia, Through Leaching Experiment

Astriana Rahmi Setiawati, J. Lumbanraja, Ananda Ika Kurnia, Manarul Hidayat, S. N. Aini, D. Prasetyo
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Abstract

Studying the weathering process in pristine volcanic materials is crucial as this process will determine further soil characteristics. Mount Anak Krakatau is reported as one of the fastest-growing volcanoes. This volcano erupted powerfully in December 2018, ejecting tons of volcanic materials. These materials are considered pristine and unweathered tephra. Hence, a leaching experiment can be one of the crucial methods to predict further soil characteristics formed as climatic factors. Tephra sampling was conducted on 13 Augustus 2019 or eight months after the massive eruption of Mount Anak Krakatau in December 2018. Tephra samples were leached by deionized water (H2O), oxalic acid (H2C2O4) 0.02 M, and citric acid (C6H8O7) 0.02 M (solvents) for 90 days. pH of tephra increased approximately from  (3.95– 4.99 ) to (5.12–8.11). Organic-C rose about 0.2 to 1 point higher than organic-C of tephra before the leaching experiment. The increasing value of organic-C was predicted to increase CEC (Cation Exchange Capacity) (2.13–5.36 cmolc kg-1). After the leaching experiment, the tephra’s surface was weathered clearly as an impact of solvents and the growing of algae.
通过浸出试验研究印尼喀拉喀托山Tephra Mount土壤化学特征的变化
研究原始火山物质的风化过程至关重要,因为这一过程将决定进一步的土壤特征。据报道,喀拉喀托火山是增长最快的火山之一。这座火山于2018年12月猛烈喷发,喷出了大量火山物质。这些材料被认为是原始的、未风化的材料。因此,淋滤试验可以作为预测气候因素形成的进一步土壤特征的关键方法之一。Tephra采样是在2019年8月13日进行的,也就是2018年12月喀拉喀托火山大规模喷发后的8个月。去离子水(H2O)、草酸(H2C2O4) 0.02 M、柠檬酸(C6H8O7) 0.02 M(溶剂)浸出样品90 d。麻黄的pH值从(3.95 ~ 4.99)增加到(5.12 ~ 8.11)。有机碳含量比浸出试验前的麻黄有机碳含量高0.2 ~ 1点。随着有机碳的增加,CEC(阳离子交换容量)增加(2.13 ~ 5.36 cmolc kg-1)。浸出实验结束后,由于溶剂的影响和藻类的生长,样品表面风化明显。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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