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Changes in organic carbon distribution with depth in agricultural soils in northern Belgium, 1960–2006
Author(s) -
MEERSMANS J.,
VAN WESEMAEL B.,
DE RIDDER F.,
FALLAS DOTTI M.,
DE BAETS S.,
VAN MOLLE M.
Publication year - 2009
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/j.1365-2486.2009.01855.x
Subject(s) - loam , topsoil , environmental science , soil water , soil carbon , soil science , silt , soil texture , total organic carbon , hydrology (agriculture) , agronomy , geology , environmental chemistry , chemistry , paleontology , geotechnical engineering , biology
In most studies concerning the carbon (C) exchange between soil and atmosphere only the topsoil (0–0.3 m) is taken into account. However, it has been shown that important amounts of stable soil organic carbon (SOC) are also stored at greater depth. Here, we developed a quantitative model to estimate the evolution of the distribution of SOC with depth between 1960 (database ‘Aardewerk’) and 2006 in northern Belgium. This temporal analysis was conducted under different land use, texture and drainage conditions. The results indicate that intensified land management practices seriously affect the SOC status of the soil. The increase in plough depth and a change in crop rotation result in a significant decrease of C near the surface for dry silt loam cropland soils, (i.e. 1.02 ± 0.23 kg C m −2 in the top 0.3 m between 1960 and 2006). In wet to extremely wet grasslands, topsoil SOC decreased significantly, indicating a negative influence of intensive soil drainage on SOC stock. This resulted in a decline of SOC between 1960 and 2006 in the top 1 m, ranging from 3.99 ± 2.57 kg C m −2 in extremely wet silt loam soils to 2.04 ± 2.08 kg C m −2 in wet sandy soils. A slight increase of SOC stock is observed under dry to moderately wet grasslands at greater depths corresponding to increased livestock densities in the region. The increase of SOC in the top 1 m under grassland ranges from 0.65 ± 1.39 kg C m −2 in well drained silt loam soils to 2.59 ± 6.49 kg C m −2 in moderately drained silt loam soils over entire period.