Effects of 24 Years of Conservation Tillage Systems on Soil Organic Carbon and Soil Productivity

The 24-year study was conducted in southern Illinois (USA) on land similar to that being removed from Conservation Reserve Program (CRP) to evaluate the effects of conservation tillage systems on: (1) amount and rates of soil organic carbon (SOC) storage and retention, (2) the long-term corn and soy...

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Main Authors: Kenneth R. Olson, Stephen A. Ebelhar, James M. Lang
Format: Article
Language:English
Published: Hindawi Limited 2013-01-01
Series:Applied and Environmental Soil Science
Online Access:http://dx.doi.org/10.1155/2013/617504
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spelling doaj-1554c67343bb41bf9e37293fedac9ce52020-11-24T20:59:04ZengHindawi LimitedApplied and Environmental Soil Science1687-76671687-76752013-01-01201310.1155/2013/617504617504Effects of 24 Years of Conservation Tillage Systems on Soil Organic Carbon and Soil ProductivityKenneth R. Olson0Stephen A. Ebelhar1James M. Lang2Department of Natural Resources and Environmental Sciences, University of Illinois, S-224 Turner Hall, 1102 S. Goodwin Avenue Urbana, IL 61801, USADixon Springs Agricultural Center, Department of Crop Sciences, Simpson, IL 62959, USADepartment of NRES, University of Illinois, N-405 Turner Hall, 1102 S. Goodwin Avenue, Urbana, IL 61801, USAThe 24-year study was conducted in southern Illinois (USA) on land similar to that being removed from Conservation Reserve Program (CRP) to evaluate the effects of conservation tillage systems on: (1) amount and rates of soil organic carbon (SOC) storage and retention, (2) the long-term corn and soybean yields, and (3) maintenance and restoration of soil productivity of previously eroded soils. The no-till (NT) plots did store and retain 7.8 Mg C ha−1 more and chisel plow (CP) −1.6 Mg C ha−1 less SOC in the soil than moldboard plow (MP) during the 24 years. However, no SOC sequestration occurred in the sloping and eroding NT, CP, and MP plots since the SOC level of the plot area was greater at the start of the experiment than at the end. The NT plots actually lost a total of −1.2 Mg C ha−1, the CP lost −9.9 Mg C ha−1, and the MP lost −8.2 Mg C ha−1 during the 24-year study. The long-term productivity of NT compared favorably with that of MP and CP systems.http://dx.doi.org/10.1155/2013/617504
collection DOAJ
language English
format Article
sources DOAJ
author Kenneth R. Olson
Stephen A. Ebelhar
James M. Lang
spellingShingle Kenneth R. Olson
Stephen A. Ebelhar
James M. Lang
Effects of 24 Years of Conservation Tillage Systems on Soil Organic Carbon and Soil Productivity
Applied and Environmental Soil Science
author_facet Kenneth R. Olson
Stephen A. Ebelhar
James M. Lang
author_sort Kenneth R. Olson
title Effects of 24 Years of Conservation Tillage Systems on Soil Organic Carbon and Soil Productivity
title_short Effects of 24 Years of Conservation Tillage Systems on Soil Organic Carbon and Soil Productivity
title_full Effects of 24 Years of Conservation Tillage Systems on Soil Organic Carbon and Soil Productivity
title_fullStr Effects of 24 Years of Conservation Tillage Systems on Soil Organic Carbon and Soil Productivity
title_full_unstemmed Effects of 24 Years of Conservation Tillage Systems on Soil Organic Carbon and Soil Productivity
title_sort effects of 24 years of conservation tillage systems on soil organic carbon and soil productivity
publisher Hindawi Limited
series Applied and Environmental Soil Science
issn 1687-7667
1687-7675
publishDate 2013-01-01
description The 24-year study was conducted in southern Illinois (USA) on land similar to that being removed from Conservation Reserve Program (CRP) to evaluate the effects of conservation tillage systems on: (1) amount and rates of soil organic carbon (SOC) storage and retention, (2) the long-term corn and soybean yields, and (3) maintenance and restoration of soil productivity of previously eroded soils. The no-till (NT) plots did store and retain 7.8 Mg C ha−1 more and chisel plow (CP) −1.6 Mg C ha−1 less SOC in the soil than moldboard plow (MP) during the 24 years. However, no SOC sequestration occurred in the sloping and eroding NT, CP, and MP plots since the SOC level of the plot area was greater at the start of the experiment than at the end. The NT plots actually lost a total of −1.2 Mg C ha−1, the CP lost −9.9 Mg C ha−1, and the MP lost −8.2 Mg C ha−1 during the 24-year study. The long-term productivity of NT compared favorably with that of MP and CP systems.
url http://dx.doi.org/10.1155/2013/617504
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