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Geochemical evidence of illuvial processes in clay-rich soils on limestones in a humid temperate climate
ID
Turniški, Rok
(
Author
),
ID
Zupančič, Nina
(
Author
),
ID
Grčman, Helena
(
Author
)
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https://www.sciencedirect.com/science/article/pii/S0016706122005730
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Abstract
In environments with high precipitation, eluvial–illuvial processes play a key role in pedogenesis. Vertical translocation of clay leads to the formation of an argic horizon. Such soils are of global importance and formed on different rock substrates under different climatic conditions. However, the pedogenesis of clay-rich soils developed on limestone in humid temperate climates has not been sufficiently investigated. Therefore, this study aimed to evaluate the geochemical and mineral compositions and properties of Luvisols (10 profiles) from the Dinaric karst region and identify the geochemical indicators of eluvial–illuvial processes. The geochemical and mineral differences between the A, E, and Bt horizons could be explained by the pedogenic processes of biorecycling, migration, isomorphic substitution in minerals, surface adsorption to clay or Al/Fe oxide minerals, and precipitation from the soil solution. Illuviation is evident in the downward increase in Al2O3, Fe2O3, MgO, K2O, Ba, Co, Cr, Ga, Ni, Sc, Th, U, V, Y, and REE. Despite differences in the geochemical characteristics of the 10 studied profiles, eluvial–illuvial processes outweighed the heterogeneity of the soils from different sites and the probable contribution of allochthonous material to the soil. We established new textural and geochemical indicators that could explain the differences among horizons and profiles in light of the polygenetic origin of soil material and pedological processes.
Language:
English
Keywords:
luvisols
,
eluvial-illuvial processes
,
argic horizon
,
weathering index
,
allochthonous materials
,
dinaric karst
Work type:
Article
Typology:
1.01 - Original Scientific Article
Organization:
BF - Biotechnical Faculty
Publication status:
Published
Publication version:
Version of Record
Year:
2023
Number of pages:
15 str.
Numbering:
Vol. 429, Art. 116266
PID:
20.500.12556/RUL-142890
UDC:
55
ISSN on article:
0016-7061
DOI:
10.1016/j.geoderma.2022.116266
COBISS.SI-ID:
131422467
Publication date in RUL:
30.11.2022
Views:
646
Downloads:
139
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Record is a part of a journal
Title:
Geoderma
Shortened title:
Geoderma
Publisher:
Elsevier
ISSN:
0016-7061
COBISS.SI-ID:
4619786
Licences
License:
CC BY-NC-ND 4.0, Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International
Link:
http://creativecommons.org/licenses/by-nc-nd/4.0/
Description:
The most restrictive Creative Commons license. This only allows people to download and share the work for no commercial gain and for no other purposes.
Secondary language
Language:
Slovenian
Keywords:
pedologija
,
pedološki procesi
,
pedogeneza
,
tla
,
indeks preperevanja
,
dinarski kras
Projects
Funder:
ARRS - Slovenian Research Agency
Project number:
P4-0085
Name:
Agroekosistemi
Funder:
ARRS - Slovenian Research Agency
Project number:
P1-0008
Name:
Paleontologija in sedimentarna geologija
Funder:
ARRS - Slovenian Research Agency
Project number:
I0-0022
Name:
Mreža raziskovalnih infrastrukturnih centrov Univerze v Ljubljani (MRIC UL)
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