Soil organic carbon density and storage in podzols - a case study from Ralsko region (Czech republic)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F14%3A10272425" target="_blank" >RIV/00216208:11310/14:10272425 - isvavai.cz</a>

Výsledek na webu

<a href="http://web.natur.cuni.cz/gis/aucg/index.php?option=com_phocadownload&view=category&id=26:issue-22014&Itemid=100" target="_blank" >http://web.natur.cuni.cz/gis/aucg/index.php?option=com_phocadownload&view=category&id=26:issue-22014&Itemid=100</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.14712/23361980.2014.16" target="_blank" >10.14712/23361980.2014.16</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Soil organic carbon density and storage in podzols - a case study from Ralsko region (Czech republic)

Popis výsledku v původním jazyce

The aim of this paper is the characterization of Carbic Podzols in Ralsko region (Czech Republic) and their role in soil carbon balance. The emphasis was put on soil carbon density and storage in the subsurface mineral horizons. Soil organic carbon density calculated for studied podzol in the Ralsko region was 49,97 t.ha-1. More than 53 % of this carbon is located in the subsurface horizons, below the depth of 30 cm. The soil organic carbon density was visualised for all soil horizons. The reasons for spatial variability in soil carbon densities were sketched. Carbon density, besides other things, depends on soil horizons thickness which is very variable in case of Carbic Podzols. Therefore, the horizon thickness and its course were visualised as well.

Název v anglickém jazyce

Soil organic carbon density and storage in podzols - a case study from Ralsko region (Czech republic)

Popis výsledku anglicky

The aim of this paper is the characterization of Carbic Podzols in Ralsko region (Czech Republic) and their role in soil carbon balance. The emphasis was put on soil carbon density and storage in the subsurface mineral horizons. Soil organic carbon density calculated for studied podzol in the Ralsko region was 49,97 t.ha-1. More than 53 % of this carbon is located in the subsurface horizons, below the depth of 30 cm. The soil organic carbon density was visualised for all soil horizons. The reasons for spatial variability in soil carbon densities were sketched. Carbon density, besides other things, depends on soil horizons thickness which is very variable in case of Carbic Podzols. Therefore, the horizon thickness and its course were visualised as well.

Druh

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

CEP obor

DF - Pedologie

OECD FORD obor

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Projekt

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Návaznosti

S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2014

Kód důvěrnosti údajů

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

Název periodika

Acta Universitatis Carolinae, Geographica

ISSN

0300-5402

e-ISSN

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Svazek periodika

49

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

8

Strana od-do

65-72

Kód UT WoS článku

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EID výsledku v databázi Scopus

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