Soil morphological characteristics in the active volcanic toposequence zone at Tangkuban Parahu volcano, Indonesia

Soil formation in volcanic terrains presents a significant challenge due to the diverse physical and chemical properties imparted by volcanic activity, which are not yet fully understood. This study investigates the unique morphological characteristics of soil profiles within crater topography seque...

Full description

Saved in:
Bibliographic Details
Main Authors: Dani Lukman Hakim, Bjoern Machalett, Riyanto Adji, Rachmi Satwhikawara, Syamsu Alam
Format: Article
Language:English
Published: Universitas Lancang Kuning 2024-07-01
Series:Jurnal Ilmiah Pertanian
Subjects:
Online Access:https://dev-journal.unilak.ac.id/index.php/jip/article/view/20956
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1825206486183182336
author Dani Lukman Hakim
Bjoern Machalett
Riyanto Adji
Rachmi Satwhikawara
Syamsu Alam
author_facet Dani Lukman Hakim
Bjoern Machalett
Riyanto Adji
Rachmi Satwhikawara
Syamsu Alam
author_sort Dani Lukman Hakim
collection DOAJ
description Soil formation in volcanic terrains presents a significant challenge due to the diverse physical and chemical properties imparted by volcanic activity, which are not yet fully understood. This study investigates the unique morphological characteristics of soil profiles within crater topography sequences at the Tangkuban Parahu Volcano, Indonesia. To address this gap, five representative sample profiles (I, II, III, IV, V) were analyzed. The Ratu Crater pathway topography was characterized by steep to very steep slopes. Detailed analysis identified three predominant soil layers, each with distinct features such as color, texture, porosity, and chemical composition, reflecting different stages of soil formation. At the highest elevation near the crater rim, Profile V was composed mainly of volcanic ash, with a loose structure, high porosity, and acidic pH, indicative of recent volcanic deposits. Profile III, at intermediate elevations, consisted of highly weathered soil with sandy loam textures and clear layer demarcations, suggesting prolonged soil development and consolidation. Profile I, at the lowest elevation, featured loamy sand with significant weathering and organic matter incorporation, indicating advanced soil development stages. The findings underscore the impact of volcanic activity on soil morphology, revealing distinct layers that correlate with various ages and developmental stages. Understanding these processes can inform agricultural practices.
format Article
id doaj-art-77cec681fecc42c8881ed217f4bb70a2
institution Kabale University
issn 1829-8346
2502-5988
language English
publishDate 2024-07-01
publisher Universitas Lancang Kuning
record_format Article
series Jurnal Ilmiah Pertanian
spelling doaj-art-77cec681fecc42c8881ed217f4bb70a22025-02-07T09:32:17ZengUniversitas Lancang KuningJurnal Ilmiah Pertanian1829-83462502-59882024-07-01212Soil morphological characteristics in the active volcanic toposequence zone at Tangkuban Parahu volcano, IndonesiaDani Lukman Hakim0Bjoern Machalett1Riyanto Adji2Rachmi Satwhikawara3Syamsu Alam4Department of Agribusiness, Faculty of Business, President University, Bekasi 17530, Indonesia Department of Landscape Architecture, Faculty of Landscape Architecture, Horticulture and Forestry, Erfurt University of Applied Sciences, Erfurt 99085, Germany Department of Agribusiness, Faculty of Business, President University, Bekasi 17530, Indonesia Department of Agribusiness, Faculty of Business, President University, Bekasi 17530, Indonesia Department of Soil Science, Faculty of Agriculture, Halu Oleo University, Kendari 93232, IndonesiaSoil formation in volcanic terrains presents a significant challenge due to the diverse physical and chemical properties imparted by volcanic activity, which are not yet fully understood. This study investigates the unique morphological characteristics of soil profiles within crater topography sequences at the Tangkuban Parahu Volcano, Indonesia. To address this gap, five representative sample profiles (I, II, III, IV, V) were analyzed. The Ratu Crater pathway topography was characterized by steep to very steep slopes. Detailed analysis identified three predominant soil layers, each with distinct features such as color, texture, porosity, and chemical composition, reflecting different stages of soil formation. At the highest elevation near the crater rim, Profile V was composed mainly of volcanic ash, with a loose structure, high porosity, and acidic pH, indicative of recent volcanic deposits. Profile III, at intermediate elevations, consisted of highly weathered soil with sandy loam textures and clear layer demarcations, suggesting prolonged soil development and consolidation. Profile I, at the lowest elevation, featured loamy sand with significant weathering and organic matter incorporation, indicating advanced soil development stages. The findings underscore the impact of volcanic activity on soil morphology, revealing distinct layers that correlate with various ages and developmental stages. Understanding these processes can inform agricultural practices. https://dev-journal.unilak.ac.id/index.php/jip/article/view/20956volcanic soil formationmorphological characteristicssoil profile analysisRatu crater topographyagricultural soil management
spellingShingle Dani Lukman Hakim
Bjoern Machalett
Riyanto Adji
Rachmi Satwhikawara
Syamsu Alam
Soil morphological characteristics in the active volcanic toposequence zone at Tangkuban Parahu volcano, Indonesia
Jurnal Ilmiah Pertanian
volcanic soil formation
morphological characteristics
soil profile analysis
Ratu crater topography
agricultural soil management
title Soil morphological characteristics in the active volcanic toposequence zone at Tangkuban Parahu volcano, Indonesia
title_full Soil morphological characteristics in the active volcanic toposequence zone at Tangkuban Parahu volcano, Indonesia
title_fullStr Soil morphological characteristics in the active volcanic toposequence zone at Tangkuban Parahu volcano, Indonesia
title_full_unstemmed Soil morphological characteristics in the active volcanic toposequence zone at Tangkuban Parahu volcano, Indonesia
title_short Soil morphological characteristics in the active volcanic toposequence zone at Tangkuban Parahu volcano, Indonesia
title_sort soil morphological characteristics in the active volcanic toposequence zone at tangkuban parahu volcano indonesia
topic volcanic soil formation
morphological characteristics
soil profile analysis
Ratu crater topography
agricultural soil management
url https://dev-journal.unilak.ac.id/index.php/jip/article/view/20956
work_keys_str_mv AT danilukmanhakim soilmorphologicalcharacteristicsintheactivevolcanictoposequencezoneattangkubanparahuvolcanoindonesia
AT bjoernmachalett soilmorphologicalcharacteristicsintheactivevolcanictoposequencezoneattangkubanparahuvolcanoindonesia
AT riyantoadji soilmorphologicalcharacteristicsintheactivevolcanictoposequencezoneattangkubanparahuvolcanoindonesia
AT rachmisatwhikawara soilmorphologicalcharacteristicsintheactivevolcanictoposequencezoneattangkubanparahuvolcanoindonesia
AT syamsualam soilmorphologicalcharacteristicsintheactivevolcanictoposequencezoneattangkubanparahuvolcanoindonesia