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RESEARCH ARTICLE

Influence of parent rock on soil clay mineralogy and physicochemical properties: a case study from the O’Higgins region, central Chile

Eduardo Navarro-Hasse A , Ursula Kelm B , Oscar Jerez B , Carolina Yáñez C and Alexander Neaman https://orcid.org/0000-0002-1819-0872 D *
+ Author Affiliations
- Author Affiliations

A Magíster en Ciencias del Suelo, Escuela de Graduados, Facultad de Ciencias Agrarias y Alimentarias, Universidad Austral de Chile, Valdivia, Chile.

B Instituto de Geología Económica Aplicada, Universidad de Concepción, Concepción, Chile.

C Instituto de Biología, Pontificia Universidad Católica de Valparaíso, Valparaíso, Chile.

D Departamento de Recursos Ambientales, Facultad de Ciencias Agronómicas, Universidad de Tarapacá, Arica, Chile.

* Correspondence to: alexander.neaman@gmail.com

Handling Editor: Claudio Bini

Soil Research 62, SR24011 https://doi.org/10.1071/SR24011
Submitted: 12 January 2024  Accepted: 7 October 2024  Published: 24 October 2024

© 2024 The Author(s) (or their employer(s)). Published by CSIRO Publishing

Abstract

Context

Lithology plays a crucial role in soil formation processes, and its interaction with soil properties is closely tied to climatic factors, making regional-scale investigations essential.

Aims

This study aimed to investigate the impact of lithology on both clay mineralogy and the physicochemical properties of soils in the O’Higgins region of central Chile.

Methods

We examined soils derived from seven distinct rock types: (1) lithic tuff (volcanoclastic, felsic); (2) andesite (volcanic, intermediate); (3) ash tuff (volcanoclastic, felsic); (4) breccia flow (volcanoclastic, intermediate; (5) granite (plutonic, felsic); (6) quartz schist (metamorphic); and (7) muscovite schist (metamorphic). A total of 21 topsoil samples (0–10 cm) and seven rock samples were collected for analysis.

Key results

Kaolinite and illite were ubiquitous in all soil samples, whereas smectite and vermiculite were restricted to soils derived from volcanic and volcanoclastic parent materials. Notably, the physicochemical characteristics of the soils converged toward a sandy loam texture with high base saturation levels (>90%).

Conclusions

The parent material exerts a significant influence on the clay mineral composition of soils in the study area. Conversely, the underlying lithology appears to have a negligible impact on the physicochemical properties of the soils in the region.

Implications

The findings of this study highlight the need for a more extensive and diverse sampling strategy to elucidate the complex relationships between lithology, soil clay mineralogy, and soil physicochemical properties. A more comprehensive understanding of these interactions can only be achieved through the inclusion of a larger and more representative sample set.

Keywords: Alfisols, central Chile, clay minerals, Inceptisols, lithology, lithosequence, O’Higgins region, phyllosilicates.

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