Parent material, elemental composition, and pedogenic processes in ophiolitic soils in Eastern Taiwan


Citation

Cascante, Marvin Decenilla and Cho, Yin Wu and Chia, Yu Yang and Hui, Zhen Hum and Zeng, Yei Hseu (2025) Parent material, elemental composition, and pedogenic processes in ophiolitic soils in Eastern Taiwan. Pertanika Journal Tropical Agricultural Science (Malaysia), 48 (3). 991 -1017. ISSN 1511-3701

Abstract

The ophiolite complex in Chishang, Eastern Taiwan, exhibits a wide variety of soil parent materials, resulting in notable variations in elemental composition and pedological properties. This study characterized soils from four pedons along a toposequence, focusing on mineral composition, micromorphology, general properties, and elemental composition. A mass balance model quantified the mobility of clay, along with major and trace elements. The soils predominantly comprised chlorites, feldspars, quartz, micas, and calcite, with higher silica (Si) concentrations followed by Al. Some of the studied soils had elevated Ca/Mg ratios (≥ 1.0), indicating a primary derivation from sedimentary parent material, such as mudstone. However, concentrations of Cr (71.2 to 105.0 mg kg⁻¹), Ni (43.2 mg kg⁻¹), and Co (20.3 to 27.9 mg kg⁻¹) were notably lower than those reported in other global studies on ophiolite complexes. A significant and positive correlation occurred between Fe- and Al-oxides and Cr, Ni, and Co. The poor correlations between these trace metals and other soil properties (pH, organic carbon, Ca/Mg ratio, rare earth elements) suggest that these factors had limited influence on Cr, Ni, and Co concentrations. The strong (p < 0.01) correlations among trace metals indicate a genetic linkage formed during soil development rather than anthropogenic activities. Additionally, trace metal enrichment in surface soils, as evidenced by the increase of clay and Fe/Al oxides, implies that these components provide crucial adsorption sites for Cr, Ni, and Co.


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Abstract

The ophiolite complex in Chishang, Eastern Taiwan, exhibits a wide variety of soil parent materials, resulting in notable variations in elemental composition and pedological properties. This study characterized soils from four pedons along a toposequence, focusing on mineral composition, micromorphology, general properties, and elemental composition. A mass balance model quantified the mobility of clay, along with major and trace elements. The soils predominantly comprised chlorites, feldspars, quartz, micas, and calcite, with higher silica (Si) concentrations followed by Al. Some of the studied soils had elevated Ca/Mg ratios (≥ 1.0), indicating a primary derivation from sedimentary parent material, such as mudstone. However, concentrations of Cr (71.2 to 105.0 mg kg⁻¹), Ni (43.2 mg kg⁻¹), and Co (20.3 to 27.9 mg kg⁻¹) were notably lower than those reported in other global studies on ophiolite complexes. A significant and positive correlation occurred between Fe- and Al-oxides and Cr, Ni, and Co. The poor correlations between these trace metals and other soil properties (pH, organic carbon, Ca/Mg ratio, rare earth elements) suggest that these factors had limited influence on Cr, Ni, and Co concentrations. The strong (p < 0.01) correlations among trace metals indicate a genetic linkage formed during soil development rather than anthropogenic activities. Additionally, trace metal enrichment in surface soils, as evidenced by the increase of clay and Fe/Al oxides, implies that these components provide crucial adsorption sites for Cr, Ni, and Co.

Additional Metadata

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Item Type: Article
AGROVOC Term: bog soils
AGROVOC Term: soil parent materials
AGROVOC Term: minerals
AGROVOC Term: elements
AGROVOC Term: trace elements
AGROVOC Term: metals
AGROVOC Term: soil analysis
AGROVOC Term: elemental analysis
AGROVOC Term: mudstone
AGROVOC Term: clay
Geographical Term: Taiwan
Depositing User: Ms. Azariah Hashim
Date Deposited: 07 May 2026 08:30
Last Modified: 07 May 2026 08:30
URI: http://webagris.upm.edu.my/id/eprint/25294

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