Magnetic and geochemical characteri zation of Andosols developed on basalts in the Mass if Central, France

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F15%3A00443574" target="_blank" >RIV/67985530:_____/15:00443574 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1002/2015GC005716" target="_blank" >http://dx.doi.org/10.1002/2015GC005716</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1002/2015GC005716" target="_blank" >10.1002/2015GC005716</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Magnetic and geochemical characteri zation of Andosols developed on basalts in the Mass if Central, France

Popis výsledku v původním jazyce

Identification of Andosols is primarily based upon the content of their colloidal constituentsclay and metal-humus complexesand on the determining of andic properties. This needs time and cost-consuming geochemical analyses. Our primary aim of this studyis to describe the magnetic and geochemical properties of soils rich in iron oxides derived from strongly magnetic volcanic basement (in this case Andosols). Secondary aim is to explore links between magnetic and chemical parameters of andic soils withrespect to genesis factors: parent material age, precipitation, and thickness of the soil profile. Six pedons of andic properties, developed on basaltic lavas, were analyzed down to parent rock by a set of magnetic and geochemical methods. Magnetic dataof soil and rock samples reflect the type, concentration, and particle-size distribution of ferrimagnetic minerals. Geochemical data include soil reaction (pH in H2O), cation exchange capacity, organic carbon, and different forms of extra

Název v anglickém jazyce

Magnetic and geochemical characteri zation of Andosols developed on basalts in the Mass if Central, France

Popis výsledku anglicky

Identification of Andosols is primarily based upon the content of their colloidal constituentsclay and metal-humus complexesand on the determining of andic properties. This needs time and cost-consuming geochemical analyses. Our primary aim of this studyis to describe the magnetic and geochemical properties of soils rich in iron oxides derived from strongly magnetic volcanic basement (in this case Andosols). Secondary aim is to explore links between magnetic and chemical parameters of andic soils withrespect to genesis factors: parent material age, precipitation, and thickness of the soil profile. Six pedons of andic properties, developed on basaltic lavas, were analyzed down to parent rock by a set of magnetic and geochemical methods. Magnetic dataof soil and rock samples reflect the type, concentration, and particle-size distribution of ferrimagnetic minerals. Geochemical data include soil reaction (pH in H2O), cation exchange capacity, organic carbon, and different forms of extra

Druh

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

CEP obor

DF - Pedologie

OECD FORD obor

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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

2015

Kód důvěrnosti údajů

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

Název periodika

Geochemistry, Geophysics, Geosystems

ISSN

1525-2027

e-ISSN

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Svazek periodika

16

Číslo periodika v rámci svazku

5

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

16

Strana od-do

1348-1363

Kód UT WoS článku

000356710000007

EID výsledku v databázi Scopus

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