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Microstructural development in volcanic ash soils from South Chile
Indexado
WoS WOS:000316978100007
Scopus SCOPUS_ID:84873969163
DOI 10.1016/J.STILL.2013.01.007
Año 2013
Tipo artículo de investigación

Citas Totales

Autores Afiliación Chile

Instituciones Chile

% Participación
Internacional

Autores
Afiliación Extranjera

Instituciones
Extranjeras


Abstract



Streaming potential measurements and amplitude sweep tests were performed on a range of Andosols from South Chile to find out about aggregation strength and mechanisms, as well as thixotropy and microstructural stability. Different stages in soil development and types of land use (pasture vs. natural forest) were considered and compared. Younger, alu-andic Andosols along with Al-humus-complexes contained higher levels of volcanic glass, indicated by their low pH values (pH(H2O) < 5), and high ratios of sodium pyrophosphate extractable Al (Al-p) to acid ammonium oxalate extractable Al (Al-o) (Al-p/Al-o > 0.5). Alu-andic Andosols were also found to have (super)hydrophobicity in addition to typically high contents of amorphous iron (ferrihydrite). On the contrary, in well-developed, sil-andic Andosols (Al-p/Al-o < 0.5), allophane contents increased, accompanied by higher pH values (pH(H2O) > 5 and <7). Based on rheological data, the gel-sol-gel transformation (thixotropy) was better defined in sil-andic Andosols. Integral z, a dimensionless rheological parameter that represents quasi-elasticity was used to quantify stiffness degradation, and to identify single stages of thixotropy in allophanic Andosols. Scanning electron micrographs revealed that mineralogical components were predominated by volcanic glass (e.g. vesicular) and amorphous iron oxides in addition to fungal hyphae in younger acidic Andosols, while these characteristics were absent in well-developed Andosols. Here weathered minerals e.g. biotite, as well as halloysite, (proto)imogolite and allophanes were identified, indicating desilication and a shift from alu-andic to sil-andic Andosols. Zeta potentials derived from conducted particle charge density (PCD) measurements supported the assumptions that (i) Al-humus-complexes promoted aggregation in partially superhydrophobic topsoils of alu-andic Andosols, especially at ungrazed sites (or 1 year under pasture), and that (ii) thixotropic behaviour is related to allophanic, sil-andic Andosols, and better pronounced at sites which had been under pasture for 50 years. (C) 2013 Elsevier B.V. All rights reserved.

Revista



Revista ISSN
Soil & Tillage Research 0167-1987

Métricas Externas



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Disciplinas de Investigación



WOS
Soil Science
Scopus
Agronomy And Crop Science
Soil Science
Earth Surface Processes
SciELO
Sin Disciplinas

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Publicaciones WoS (Ediciones: ISSHP, ISTP, AHCI, SSCI, SCI), Scopus, SciELO Chile.

Colaboración Institucional



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Autores - Afiliación



Ord. Autor Género Institución - País
1 Baumgarten, W. - Univ Kiel - Alemania
Christian-Albrechts-Universität zu Kiel - Alemania
2 DORNER-FERNANDEZ, JOSE MIGUEL Hombre Universidad Austral de Chile - Chile
3 Horn, Rainer Hombre Univ Kiel - Alemania
Universidad Austral de Chile - Chile
Christian-Albrechts-Universität zu Kiel - Alemania

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Origen de Citas Identificadas



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Citas identificadas: Las citas provienen de documentos incluidos en la base de datos de DATACIENCIA

Citas Identificadas: 13.51 %
Citas No-identificadas: 86.49 %

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Citas identificadas: Las citas provienen de documentos incluidos en la base de datos de DATACIENCIA

Citas Identificadas: 13.51 %
Citas No-identificadas: 86.49 %

Financiamiento



Fuente
FONDECYT
Fondo Nacional de Desarrollo Científico y Tecnológico
German Research Foundation
Deutsche Forschungsgemeinschaft
Fondo Nacional de Desarrollo Científico, Tecnológico y de Innovación Tecnológica
Conicyt-DFG

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Agradecimientos



Agradecimiento
The authors are grateful for the SEM analysis, which was done by U. Schuldt as well as B. Pragel, Institute of Geosciences, Palaeontology and Historical Geology, CAU Kiel. A special thank is dedicated to Dr. Gordon Jock Churchman, University of Adelaide, for his scientific support. We would also like to thank V. Schroeren, S. Kneesch, and N. Stoppe for their technical support. We are indebted to the German Research Foundation (DFG Ho 911/39) for the financial support and also to the international cooperation programmes FONDECYT 7070332 and CONICYT-DFG.
The authors are grateful for the SEM analysis, which was done by U. Schuldt as well as B. Prägel, Institute of Geosciences, Palaeontology and Historical Geology, CAU Kiel. A special thank is dedicated to Dr. Gordon Jock Churchman, University of Adelaide, for his scientific support. We would also like to thank V. Schroeren, S. Kneesch, and N. Stoppe for their technical support. We are indebted to the German Research Foundation (DFG Ho 911/39 ) for the financial support and also to the international cooperation programmes FONDECYT 7070332 and CONICYT-DFG.

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