Mineralogy and Chemical Composition of Cryosols and Andosols in Antarctica
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43210%2F18%3A43911835" target="_blank" >RIV/62156489:43210/18:43911835 - isvavai.cz</a>
Result on the web
<a href="http://dx.doi.org/10.17221/231/2016-SWR" target="_blank" >http://dx.doi.org/10.17221/231/2016-SWR</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.17221/231/2016-SWR" target="_blank" >10.17221/231/2016-SWR</a>
Alternative languages
Result language
angličtina
Original language name
Mineralogy and Chemical Composition of Cryosols and Andosols in Antarctica
Original language description
The detail mineralogical analysis of soil samples from the islands near the north-eastern extremity of the Antarctic Peninsula was applied to evaluate the presence of chemical along with physical weathering. We assumed the highest degree of chemical weathering to occur at surface horizons (higher temperature and presence of liquid water). The increased amount of potential weathering products, phyllosilicates (mainly montmorillonite and chlorite), microcrystalline polymorphous silica, Fe-oxyhydroxides, and the decreased number of initial parent phases (feldspars, volcanic glass, quartz, olivine) in fraction < 2 mm and in the upper soil horizons confirmed the process of chemical weathering. The dominant amount of montmorillonite in the clay fraction was used to determine the crystal thickness using the BWA technique. Mean thickness of crystal in soil profiles rising towards the surface suggests the effect of chemical weathering. The isotopic evaluation of montmorillonite could provide further proof of chemical weathering in future research. The origin of zeolite mineral - clinoptilolite, in the studied samples present mostly at ca. 10 wt %, has remained undisclosed. Clinoptilolite could be a product of hydrothermal alteration, chemical weathering or both. The question of its origin is also a subject for future research.The distribution of macro elements of the studied soil samples confirms more chemical weathered material in the soil profiles of James Ross Island. It also indicates more intensive or longer weathering on James Ross and King George Islands than on Deception Island.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10505 - Geology
Result continuities
Project
<a href="/en/project/QJ1210263" target="_blank" >QJ1210263: Agronomic measures to a reduction of water erosion on arable land with utilization of organic matter plough down</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2018
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Soil and Water Research
ISSN
1801-5395
e-ISSN
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Volume of the periodical
13
Issue of the periodical within the volume
2
Country of publishing house
CZ - CZECH REPUBLIC
Number of pages
13
Pages from-to
61-73
UT code for WoS article
000430186300001
EID of the result in the Scopus database
2-s2.0-85045432554