Soil Layers Properties of a Profile Developed on the Past Depositional Series on Merbabu Volcano Central Java Indonesia

M. Nurcholis, Susila Herlambang, Sri Aminah Suwartikaningsih, D. Fiantis, D. Yudiantoro
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引用次数: 1

Abstract

A wide and deep soil profile (around 1200 cm) was observed at Ketep Park West Slope of Merbabu volcano Central Java, Indonesia to identify the soil morphology, physical and, chemical and mineralogical properties.  Results showed that several soil development processes occurred in each volcanic deposits with different characteristics.  Most soil layers met some of andic soil properties criteria such bulk density <0.9 g.cm-3, P retention of >85%, and (Alo + ½ Feo) >2.0%.  A thin melanic material showing black color layer was found at the lower part of the soil profile, i.e. in depth from 726 to 798 cm.  The dominant material in most soil layers is an allophane.  Minerals in the sand fraction were dominated by labradorite and augite, with some layers were hypersthene and green hornblende.
印尼中爪哇Merbabu火山过去沉积系列剖面的土层性质
在印度尼西亚中爪哇Merbabu火山的Ketep公园西坡观测了一个宽而深的土壤剖面(约1200厘米),以确定土壤形态、物理、化学和矿物学性质。结果表明,各火山沉积均经历了不同特征的土壤发育过程。大部分土层的容重达到85%,(Alo + 1 / 2 Feo) >2.0%。在土壤剖面下部,即深度726 ~ 798 cm处,发现了一层黑色的薄黑色物质。在大多数土层中占主导地位的物质是铁矾。砂段矿物以拉布拉长石和辉长岩为主,部分层为超长石和绿角闪石。
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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