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
| 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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