13C Labelling of soil n-hentriacontane (C31) by maize cultivation

Éric Lichtfouse

doi:10.1016/0040-4039(94)02305-U

¹³C Labelling of soil n-hentriacontane (C₃₁) by maize cultivation

Éric Lichtfouse

Sorbonne Université

科研成果: 期刊稿件 › 文章 › 同行评审

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摘要

The fate of plant carbon into molecular organic substances from soils can be followed by stable carbon analysis. Soil organic matter has thus been progressively labelled with ¹³C at natural abundance by cultivation of Zea mays, a C₄ plant, on a soil which was previously under isotopically distinct C₃ vegetation. The molar carbon percentage of maize n-hentriacontane within soil n-hentriacontane has been calculated by isotopic means and amounts to around 50% after 23 years of maize cultivation.

源语言	英语
页（从-至）	529-530
页数	2
期刊	Tetrahedron Letters
卷	36
期	4
DOI	https://doi.org/10.1016/0040-4039(94)02305-U
出版状态	已出版 - 23 1月 1995
已对外发布	是

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title = "13C Labelling of soil n-hentriacontane (C31) by maize cultivation",

abstract = "The fate of plant carbon into molecular organic substances from soils can be followed by stable carbon analysis. Soil organic matter has thus been progressively labelled with 13C at natural abundance by cultivation of Zea mays, a C4 plant, on a soil which was previously under isotopically distinct C3 vegetation. The molar carbon percentage of maize n-hentriacontane within soil n-hentriacontane has been calculated by isotopic means and amounts to around 50\% after 23 years of maize cultivation.",

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N2 - The fate of plant carbon into molecular organic substances from soils can be followed by stable carbon analysis. Soil organic matter has thus been progressively labelled with 13C at natural abundance by cultivation of Zea mays, a C4 plant, on a soil which was previously under isotopically distinct C3 vegetation. The molar carbon percentage of maize n-hentriacontane within soil n-hentriacontane has been calculated by isotopic means and amounts to around 50% after 23 years of maize cultivation.

AB - The fate of plant carbon into molecular organic substances from soils can be followed by stable carbon analysis. Soil organic matter has thus been progressively labelled with 13C at natural abundance by cultivation of Zea mays, a C4 plant, on a soil which was previously under isotopically distinct C3 vegetation. The molar carbon percentage of maize n-hentriacontane within soil n-hentriacontane has been calculated by isotopic means and amounts to around 50% after 23 years of maize cultivation.

UR - https://www.scopus.com/pages/publications/0028871132

U2 - 10.1016/0040-4039(94)02305-U

DO - 10.1016/0040-4039(94)02305-U

M3 - 文章

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SN - 0040-4039

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SP - 529

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JO - Tetrahedron Letters

JF - Tetrahedron Letters

IS - 4

ER -

13C Labelling of soil n-hentriacontane (C31) by maize cultivation

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¹³C Labelling of soil n-hentriacontane (C₃₁) by maize cultivation