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Content archived on 2024-05-27

Isotopic (13c) fractionation during decomposition of lignin in the soil environment

Objective

Quantify the isotopic fractionation during lignin decomposition in the soil environment , because the use of 13^C in soil organic matter studies demands the knowledge of the 13^C enrichment of the end products of long term plant residue decomposition and lignin is the plant component slowest to decompose and thus affecting soil 13^C signatures directly due to its contribution to soil samples

Fields of science (EuroSciVoc)

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Topic(s)

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Call for proposal

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Funding Scheme

RGI - Research grants (individual fellowships)

Coordinator

CONSEJO SUPERIOR DE INVESTIGACIONES CIENTIFICAS
EU contribution
No data
Address
122,Av de las Ciencias, s/n apdo. 122
15780 SANTIAGO DE COMPOSTELA
Spain
Total cost
No data