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Traprock Transformation into Clayey Materials in Soil Environments of the Central Siberian Plateau, Russia

Published online by Cambridge University Press:  01 January 2024

Sofia N. Lessovaia ,
Michael Plötze ,
Svyatoslav Inozemzev  and
Sergey Goryachkin
Sofia N. Lessovaia*
Affiliation:
St. Petersburg State University, Universitetskaya nab. 7/9, 199034, St. Petersburg, Russia
Michael Plötze
Affiliation:
ETH Zurich, Institute for Geotechnical Engineering, CH-8093, Zurich, Switzerland
Svyatoslav Inozemzev
Affiliation:
Dokuchaev Soil Science Society, Pyzhevsky 7, 119017, Moscow, Russia
Sergey Goryachkin
Affiliation:
Institute of Geography, Russian Academy of Science, Staromonetnyi per. 119017, Moscow, Russia
*
*E-mail address of corresponding author: [email protected]
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Abstract

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The study of hard rock conversion into fine earths and clayey materials in the pedosphere is important in understanding the relative proportions of recent soil features to features that were inherited from ancient epochs. Cold environments are widely thought to be areas of physical weathering, but the coexistence of physical and chemical processes have also been shown. To further examine mafic rock (dolerite) weathering in soil environments and the conversion into clayey materials, Entic Podzols formed in the cold continental climate were studied. The key study was located in the central part of the flood basalt complex, or traps (traprocks), of the Central Siberian Plateau (Russia). The qualitative mineralogy was studied using X-ray diffraction and the quantitative mineral composition was determined using X-ray diffraction and subsequent Rietveld analysis. The micromorphological characteristics of the soils were studied in thin sections. Dolerite fragments and fine earths were sampled from soil profiles underlain by dolerite. XRD analyses indicated that pyroxene and especially plagioclase contents in the dolerite fragments and fine earths decreased from the bottom to the top soil horizons mostly in the mature soil profiles that were affected by chemical weathering of dolerite. The dioctahedral and trioctahedral smectites in the soils were inherited from a dolerite previously subjected to chemical weathering. The smectite was conserved in the inherited aggregates and protected against dissolution even in acidic soil horizons. Recent pedogenesis processes fractured individual fragments, converted it into soil micromass, and slightly decreased the total smectite content of the <1 µm soil fraction. However, in soil samples collected from the bottom to the top horizons of a mature soil profile, trioctahedral smectite contents decreased as dioctahedral smectite contents increased. This suggests that dioctahedral smectites formed by pedogenic alteration of inherited trioctahedral smectites.

Keywords

Dolerite WeatheringEntic PodzolsPetrography StudySmectiteXRD-amorphous Phase
Type
Article
Information
Clays and Clay Minerals , Volume 64 , Issue 5 , October 2016 , pp. 668 - 676
Copyright
Copyright © Clay Minerals Society 2016

Footnotes

This paper is published as part of a special section on the subject of ‘Clays in the Critical Zone,’ arising out of presentations made during the 2015 Clay Minerals Society-Euroclay Conference held in Edinburgh, UK.

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