Changes in soil carbon stocks from 1960 to 2000 in the main Belgian cropland areas

Inventories of soil organic carbon (SOC) stocks for 1960, 1990 and 2000 have recently become available for Belgium. From these inventories we selected three agricultural regions (Polders, Loam belt and Condroz) with 60 to 80 % of the agricultural area under cropland in order to analyse the driving...

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Main Authors: Roelandt C., Lettens S., van Wesemael B., Van Orshoven J.
Format: Article
Language:English
Published: Presses Agronomiques de Gembloux 2004-01-01
Series:Biotechnologie, Agronomie, Société et Environnement
Subjects:
Online Access:http://www.pressesagro.be/base/text/v8n2/133.pdf
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spelling doaj-ef66906ecde24420bc57200968dce8702020-11-25T00:52:43ZengPresses Agronomiques de GemblouxBiotechnologie, Agronomie, Société et Environnement1370-62331780-45072004-01-0182133139Changes in soil carbon stocks from 1960 to 2000 in the main Belgian cropland areasRoelandt C.Lettens S.van Wesemael B.Van Orshoven J.Inventories of soil organic carbon (SOC) stocks for 1960, 1990 and 2000 have recently become available for Belgium. From these inventories we selected three agricultural regions (Polders, Loam belt and Condroz) with 60 to 80 % of the agricultural area under cropland in order to analyse the driving forces of the changes in SOC stocks over time. The observed values of SOC stocks of typical soil associations for each agricultural region are compared to simulations with the RothC soil carbon model. After estimating the local parameters by fitting the model to SOC values from a long term experiment in central Belgium, the model was run from 1960 to 2000 for typical soil profiles of soil associations in the three agricultural regions. The main factors inducing changes in SOC stocks are the increase in plough depth as a result of continued mechanisation in the 1960s and the sustained input of organic amendments in the form of farm yard manure and slurry. In contrast to earlier publications on CO2 emissions from agricultural soils, the model did not predict a decrease in SOC stocks for the period 19902000. The decrease in animal manure production observed during the 1990s for those regions with a concentration of intensive livestock breeding in Flanders suggests that SOC stocks in croplands will continue to decrease. This will lead to an emission of 0.41 Mt CO2 per year for the three main cropland areas of Belgium in the near future and hence partly offset the carbon sequestration potential of improved cropland management (0.95 Mt CO2 per year).http://www.pressesagro.be/base/text/v8n2/133.pdfSoil organic carbonlong term experimentsmodellingcarbon sequestrationBelgium
collection DOAJ
language English
format Article
sources DOAJ
author Roelandt C.
Lettens S.
van Wesemael B.
Van Orshoven J.
spellingShingle Roelandt C.
Lettens S.
van Wesemael B.
Van Orshoven J.
Changes in soil carbon stocks from 1960 to 2000 in the main Belgian cropland areas
Biotechnologie, Agronomie, Société et Environnement
Soil organic carbon
long term experiments
modelling
carbon sequestration
Belgium
author_facet Roelandt C.
Lettens S.
van Wesemael B.
Van Orshoven J.
author_sort Roelandt C.
title Changes in soil carbon stocks from 1960 to 2000 in the main Belgian cropland areas
title_short Changes in soil carbon stocks from 1960 to 2000 in the main Belgian cropland areas
title_full Changes in soil carbon stocks from 1960 to 2000 in the main Belgian cropland areas
title_fullStr Changes in soil carbon stocks from 1960 to 2000 in the main Belgian cropland areas
title_full_unstemmed Changes in soil carbon stocks from 1960 to 2000 in the main Belgian cropland areas
title_sort changes in soil carbon stocks from 1960 to 2000 in the main belgian cropland areas
publisher Presses Agronomiques de Gembloux
series Biotechnologie, Agronomie, Société et Environnement
issn 1370-6233
1780-4507
publishDate 2004-01-01
description Inventories of soil organic carbon (SOC) stocks for 1960, 1990 and 2000 have recently become available for Belgium. From these inventories we selected three agricultural regions (Polders, Loam belt and Condroz) with 60 to 80 % of the agricultural area under cropland in order to analyse the driving forces of the changes in SOC stocks over time. The observed values of SOC stocks of typical soil associations for each agricultural region are compared to simulations with the RothC soil carbon model. After estimating the local parameters by fitting the model to SOC values from a long term experiment in central Belgium, the model was run from 1960 to 2000 for typical soil profiles of soil associations in the three agricultural regions. The main factors inducing changes in SOC stocks are the increase in plough depth as a result of continued mechanisation in the 1960s and the sustained input of organic amendments in the form of farm yard manure and slurry. In contrast to earlier publications on CO2 emissions from agricultural soils, the model did not predict a decrease in SOC stocks for the period 19902000. The decrease in animal manure production observed during the 1990s for those regions with a concentration of intensive livestock breeding in Flanders suggests that SOC stocks in croplands will continue to decrease. This will lead to an emission of 0.41 Mt CO2 per year for the three main cropland areas of Belgium in the near future and hence partly offset the carbon sequestration potential of improved cropland management (0.95 Mt CO2 per year).
topic Soil organic carbon
long term experiments
modelling
carbon sequestration
Belgium
url http://www.pressesagro.be/base/text/v8n2/133.pdf
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