Magnetic and chemical parameters of andic soils and their relation to selected pedogenesis factors

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F16%3A00452452" target="_blank" >RIV/67985530:_____/16:00452452 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.catena.2015.12.005" target="_blank" >http://dx.doi.org/10.1016/j.catena.2015.12.005</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.catena.2015.12.005" target="_blank" >10.1016/j.catena.2015.12.005</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Magnetic and chemical parameters of andic soils and their relation to selected pedogenesis factors

Popis výsledku v původním jazyce

In the case of andic soils - developed on volcanic rocks - permanently humid conditions are essential for andosolisation processes. Although volcanic rocks are usually rich in highly magnetic iron oxides, knowledge about these minerals in andic soils with respect to the soil development is missing. The aim of this contribution is to investigate the relationship between magnetic and basic chemical properties of soils developed on volcanic basement and parameters related to the pedogenesis factors. The studied sites are located on basaltic lava flows in the eastern part of the French Massif Central. Investigated pedons with alu-andic, sil-andic, and vitric properties were pedologically described and analysed by a set of magnetic and soil-chemical methods. Magnetic parameters include low-field volume-specific and mass-specific magnetic susceptibility, frequency-dependent magnetic susceptibility, remanent properties (including S-ratio) and coercivities.

Název v anglickém jazyce

Magnetic and chemical parameters of andic soils and their relation to selected pedogenesis factors

Popis výsledku anglicky

In the case of andic soils - developed on volcanic rocks - permanently humid conditions are essential for andosolisation processes. Although volcanic rocks are usually rich in highly magnetic iron oxides, knowledge about these minerals in andic soils with respect to the soil development is missing. The aim of this contribution is to investigate the relationship between magnetic and basic chemical properties of soils developed on volcanic basement and parameters related to the pedogenesis factors. The studied sites are located on basaltic lava flows in the eastern part of the French Massif Central. Investigated pedons with alu-andic, sil-andic, and vitric properties were pedologically described and analysed by a set of magnetic and soil-chemical methods. Magnetic parameters include low-field volume-specific and mass-specific magnetic susceptibility, frequency-dependent magnetic susceptibility, remanent properties (including S-ratio) and coercivities.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DF - Pedologie

OECD FORD obor

—

Projekt

<a href="/cs/project/GA13-10775S" target="_blank" >GA13-10775S: Kvantifikace vlivu vulkanické mateční horniny na magnetické vlastnosti půd</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2016

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

CATENA

ISSN

0341-8162

e-ISSN

—

Svazek periodika

139

Číslo periodika v rámci svazku

April

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

12

Strana od-do

179-190

Kód UT WoS článku

000371189200018

EID výsledku v databázi Scopus

2-s2.0-84953896632