Parent Material, Elemental Composition, and Pedogenic Processes in Ophiolitic Soils in Eastern Taiwan
Journal
Pertanika Journal of Tropical Agricultural Science
Journal Volume
48
Journal Issue
3
Start Page
991
End Page
1017
ISSN
2231-8542
Date Issued
2025-05-16
Author(s)
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.
Subjects
Mass balance
mudstone
ophiolitic soils
pedogenesis
trace metals
Publisher
Universiti Putra Malaysia
Type
journal article