Morphology of Soils in the Impact Zone of Kuchiger Hot Springs, the Barguzin Depression

N. B. Khitrov; V. L. Ubugunov; V. I. Ubugunova; Yu. A. Rupyshev; T. A. Ayushina; A. D. Zhambalova; E. G. Tsyrempilov; A. E. Paramonova; Ts. N. Nasatueva

doi:10.1134/S106422931912007X

Morphology of Soils in the Impact Zone of Kuchiger Hot Springs, the Barguzin Depression

Authors: Khitrov N.B.¹, Ubugunov V.L.², Ubugunova V.I.², Rupyshev Y.A.², Ayushina T.A.², Zhambalova A.D.², Tsyrempilov E.G.², Paramonova A.E.², Nasatueva T.N.²
Affiliations:
1. Dokuchaev Soil Science Institute
2. Institute of General and Experimental Biology, Siberian Branch of the Russian Academy of Sciences
Issue: Vol 52, No 12 (2019)
Pages: 1477-1498
Section: Genesis and Geography of Soils
URL: https://journals.rcsi.science/1064-2293/article/view/225304
DOI: https://doi.org/10.1134/S106422931912007X
ID: 225304

Cite item

Full Text

Open Access
Restricted Access

Access granted
Restricted Access

Subscription Access

Abstract
About the authors
References
Statistics

Abstract

First data on the specific morphology and physicochemical properties of soils forming in the zone of active discharge of ascending solutions of deep thermal water of Kuchiger hot springs of the fluoride hydrosulfuric bicarbonate–sulfate–sodium type are presented. The soil cover was studied along the transect crossing the mire with active gas hydrothermal griffons, an island within the mire, and the adjacent margin of alluvial plain in the northwestern part of the Barguzin Depression near the village of Kuchiger, Kurumkan district of the Buryat Republic. The features of peat–mucky gley soils (Eutric Rheic Sapric Histosols (Fluvic, Sodic)) predominating within the mire are described. The profiles of weakly developed and alluvial soils (Eutric Sodic Gleyic Fluvisols (Epiloamic, Endoarenic, Humic)) forming under the impact of ascending gas hydrothermal fluids bear the features of turbation and impregnation with condensed organic matter in their mineral and organic horizons. These features are not included in the international and Russian soil classification systems. It is suggested that they should be diagnosed and indicated by symbols imp (various degrees of impregnation), int (intruded material), and IMP (black sandy–silty horizon strongly impregnated with condensed organic matter). The inclusion of these features into the list of diagnostic properties allows us to specify impregnated and hydrothermally turbated soil subtypes in the new Russian soil classification system. Hypotheses of the genesis of soils along the entire transect and the appearance of islands within the mire massif are suggested.

Keywords

Baikal rift zone, gas-hydrothermal fluids, soil morphology, impregnation with organic matter, soil classification, hydrogen sulfide, pyrite, soil salinization

Username
Password
Remember me

Forgot password?	Register

Username
Password
Remember me

Forgot password?	Register

Morphology of Soils in the Impact Zone of Kuchiger Hot Springs, the Barguzin Depression

Full Text

Abstract

Keywords

About the authors

This website uses cookies