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...
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Universitas Lancang Kuning
2024-07-01
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Series: | Jurnal Ilmiah Pertanian |
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Online Access: | https://dev-journal.unilak.ac.id/index.php/jip/article/view/20956 |
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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.
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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 |
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