Perspective of soil carbon sequestration in Chilean volcanic soils

We analysed a large dataset consisting of 457 soil profiles of Andisols and Ultisols of volcanic origin compared to 60 non-volcanic soils. We hypothesised that soil pH has a greater impact on the development of Al-organomineral complexes in volcanic soils compared to non-volcanic soils, in the latter, the silt and clay fractions play a crucial role. Soil pH >4.5 strongly influenced the formation of Al-organomineral complexes in volcanic soils, while an increase in allophane content led to a decrease in SOC. Ultisols with more crystalline clays, such as halloysite and disordered kaolinite, the pH had a weaker impact and there was no effect on non-volcanic soils. Instead, a positive correlation (R2 = 0.63, p < 0.01) was found between silt and clay and SOC in non-volcanic soils, supporting our second hypothesis. Soil pH played a significant role in the interplay between Al-organomineral complexes and allophane formation, while crystalline mineralogy has a direct effect on SOC levels in non-volcanic soils.

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Publication Details

Journal
npj Materials Sustainability
Published
2024-09-13
DOI
https://doi.org/10.1038/s44296-024-00038-4
Citations
8
Primary Topic
Soil Carbon and Nitrogen Dynamics
Type
article
Field-Weighted Citation Impact
2.67

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article

Perspective of soil carbon sequestration in Chilean volcanic soils

Denisse Zamorano, Susana Valle, Efraín Duarte, Óscar Seguel et al.
8 citations
npj Materials Sustainability
Soil Carbon and Nitrogen Dynamics
2.67
article

Perspective of soil carbon sequestration in Chilean volcanic soils

Denisse Zamorano, Susana Valle, Efraín Duarte, Óscar Seguel, Francisco Nájera, José Dörner, Francisco Matus, Marco Pfeiffer, Osvaldo Salazar, Felipe Aburto, Sergio Radic‐Schilling, Radmila Jovanović, Luis Reyes-Rojas, Ciro Guerra
article en
8 citations

Abstract

We analysed a large dataset consisting of 457 soil profiles of Andisols and Ultisols of volcanic origin compared to 60 non-volcanic soils. We hypothesised that soil pH has a greater impact on the development of Al-organomineral complexes in volcanic soils compared to non-volcanic soils, in the latter, the silt and clay fractions play a crucial role. Soil pH >4.5 strongly influenced the formation of Al-organomineral complexes in volcanic soils, while an increase in allophane content led to a decrease in SOC. Ultisols with more crystalline clays, such as halloysite and disordered kaolinite, the pH had a weaker impact and there was no effect on non-volcanic soils. Instead, a positive correlation (R2 = 0.63, p < 0.01) was found between silt and clay and SOC in non-volcanic soils, supporting our second hypothesis. Soil pH played a significant role in the interplay between Al-organomineral complexes and allophane formation, while crystalline mineralogy has a direct effect on SOC levels in non-volcanic soils.

npj Materials SustainabilityVol. 2(1)
Universidad de La Frontera (CL), Pontificia Universidad Católica de Chile (CL), Austral University of Chile (CL), University of Concepción (CL), Institute of Agricultural Economics Belgrade (RS), Universidad de Magallanes (CL), University of Chile (CL), Washington State University (US), Universidad de Málaga (ES), Texas A&M University (US)
U.S. Department of Agriculture, Max-Planck-Gesellschaft, Agencia Nacional de Investigación y Desarrollo, National Institute of Food and Agriculture, Comisión Nacional de Investigación Científica y Tecnológica
Climate action
Openalex Percentile: Top 10%
Soil Carbon and Nitrogen Dynamics
2.67
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