Investigation of vegetation history of buried chernozem soils using near-infrared spectroscopy (NIRS)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F15%3A10291123" target="_blank" >RIV/00216208:11310/15:10291123 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985912:_____/15:00432316

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.quaint.2014.07.035" target="_blank" >http://dx.doi.org/10.1016/j.quaint.2014.07.035</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.quaint.2014.07.035" target="_blank" >10.1016/j.quaint.2014.07.035</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Investigation of vegetation history of buried chernozem soils using near-infrared spectroscopy (NIRS)

Popis výsledku v původním jazyce

The environmental conditions of the evolution of chernozems in Central Europe have not been satisfactory explained. In this paper, seven buried chernozems were investigated using near-infrared spectroscopy (NIRS) in order to get information about the former vegetation cover. Near-infrared (NIR) data were collected from organic matter of recent natural grasslands and forests. The spectra from these two groups of soils were perfectly discriminated by a multivariate statistical analysis. The statistical model was applied on the buried soils. There are four types of vegetation development within the chernozems before the burial. Comparison to other paleoenvironmental proxies shows no major contradiction and confirms the potential of the NIRS as a paleopedological proxy. The identified changes of vegetation are from grassland vegetation to forest vegetation and vice versa. These changes bring new data to the discussion about the pedogenesis of chernozems. According to the radiocarbon dating

Název v anglickém jazyce

Investigation of vegetation history of buried chernozem soils using near-infrared spectroscopy (NIRS)

Popis výsledku anglicky

The environmental conditions of the evolution of chernozems in Central Europe have not been satisfactory explained. In this paper, seven buried chernozems were investigated using near-infrared spectroscopy (NIRS) in order to get information about the former vegetation cover. Near-infrared (NIR) data were collected from organic matter of recent natural grasslands and forests. The spectra from these two groups of soils were perfectly discriminated by a multivariate statistical analysis. The statistical model was applied on the buried soils. There are four types of vegetation development within the chernozems before the burial. Comparison to other paleoenvironmental proxies shows no major contradiction and confirms the potential of the NIRS as a paleopedological proxy. The identified changes of vegetation are from grassland vegetation to forest vegetation and vice versa. These changes bring new data to the discussion about the pedogenesis of chernozems. According to the radiocarbon dating

Druh

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

CEP obor

DF - Pedologie

OECD FORD obor

—

Projekt

—

Návaznosti

S - Specificky vyzkum na vysokych skolach<br>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

Quaternary International

ISSN

1040-6182

e-ISSN

—

Svazek periodika

365

Číslo periodika v rámci svazku

Apr

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

9

Strana od-do

203-211

Kód UT WoS článku

000353334700015

EID výsledku v databázi Scopus

2-s2.0-84928215975