Carbon Isotope Study of Soil Amendment with Maize

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F17%3A00096275" target="_blank" >RIV/00216224:14310/17:00096275 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.9734/IJPSS/2017/30299" target="_blank" >http://dx.doi.org/10.9734/IJPSS/2017/30299</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.9734/IJPSS/2017/30299" target="_blank" >10.9734/IJPSS/2017/30299</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Carbon Isotope Study of Soil Amendment with Maize

Popis výsledku v původním jazyce

Maize digestate was applied to follow its sequestration in arable soil profiles with accent on changes in soil organic carbon (SOC) content and the production of dissolved organic matter (DOM). Two control sites with cultivated Cambisols (rye-grass, kohlrabi) were amended by the addition of digestate from maize silage fermentation. Liquid digestate was applied once in the spring in the quantity of 18 g C/ m2. The process of amendment was checked after 4 and 12 months by the use of natural labelling of the amendment by the difference in the carbon isotope composition of the SOC (C3 vegetation) and applied digestate (C4 maize). The amendment was evaluated from the SOC content, dissolved organic carbon (DOC) and their d13C isotope composition by sampling across the soil profiles (0–90 cm). An increase of the carbon content by the amendment was measurable in the upper soil layers (0–20 cm) only. The deep soil layers are poor in carbon content (less than 0.2% of SOC) but rich in clay micro particles, which efficiently adsorbed incoming DOC with infiltrated precipitation. Change of the d13C of soil carbon was measurable down to -80 cm. Applied digestate increased the carbon content of top soil layer only. We did not observe significant migration of C4 amendment from top soil to the deeper soil layers. Digestate addition increased DOC production at both sites for the upper soil layers only. DOC released from the deep soil layers originates from the upper parts of the soil profile and not from the native carbon in the layer.

Název v anglickém jazyce

Carbon Isotope Study of Soil Amendment with Maize

Popis výsledku anglicky

Maize digestate was applied to follow its sequestration in arable soil profiles with accent on changes in soil organic carbon (SOC) content and the production of dissolved organic matter (DOM). Two control sites with cultivated Cambisols (rye-grass, kohlrabi) were amended by the addition of digestate from maize silage fermentation. Liquid digestate was applied once in the spring in the quantity of 18 g C/ m2. The process of amendment was checked after 4 and 12 months by the use of natural labelling of the amendment by the difference in the carbon isotope composition of the SOC (C3 vegetation) and applied digestate (C4 maize). The amendment was evaluated from the SOC content, dissolved organic carbon (DOC) and their d13C isotope composition by sampling across the soil profiles (0–90 cm). An increase of the carbon content by the amendment was measurable in the upper soil layers (0–20 cm) only. The deep soil layers are poor in carbon content (less than 0.2% of SOC) but rich in clay micro particles, which efficiently adsorbed incoming DOC with infiltrated precipitation. Change of the d13C of soil carbon was measurable down to -80 cm. Applied digestate increased the carbon content of top soil layer only. We did not observe significant migration of C4 amendment from top soil to the deeper soil layers. Digestate addition increased DOC production at both sites for the upper soil layers only. DOC released from the deep soil layers originates from the upper parts of the soil profile and not from the native carbon in the layer.

Druh

J_ost - Ostatní články v recenzovaných periodicích

CEP obor

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OECD FORD obor

40104 - Soil science

Projekt

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Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2017

Kód důvěrnosti údajů

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

Název periodika

International Journal of Plant & Soil Science

ISSN

2320-7035

e-ISSN

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Svazek periodika

14

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

11

Strana od-do

1-11

Kód UT WoS článku

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EID výsledku v databázi Scopus

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