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The effects of stubble burning and tillage on soil carbon sequestration and crop productivity in southeastern Australia
Author(s) -
Chan K.Y.,
Heenan D.P.
Publication year - 2005
Publication title -
soil use and management
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.709
H-Index - 81
eISSN - 1475-2743
pISSN - 0266-0032
DOI - 10.1079/sum2005357
Subject(s) - carbon sequestration , tillage , environmental science , productivity , soil carbon , agroforestry , agronomy , crop productivity , no till farming , crop , soil water , soil fertility , soil science , ecology , carbon dioxide , biology , economics , macroeconomics
. In Australia, stubble burning and tillage are two of the major processes responsible for the decline of soil organic carbon concentration in cropped soils, and the resulting soil degradation. However, the relative importance of these two practices in influencing the soil organic carbon concentration and the long‐term impact on soil quality and productivity are not clear. The effects of stubble burning as practised by farmers in southeastern Australia were evaluated in two field trials, one of 19 years duration, the other of 5 years. Conventional tillage (three tillage passes) led to greater loss of soil organic carbon than stubble burning. Loss of total soil organic carbon attributed to stubble burning in the 0–10 cm layer was estimated to be 1.75 t C ha −1 over the period of the 19‐year trial, equivalent to 29% of that lost due to tillage. In the 5‐year trial, no change in soil organic carbon due to stubble burning was detectable. Changes in soil quality associated with stubble burning detected in the longer trial included a reduction in macro‐aggregate stability, and increases in pH and exchangeable K + . Only the latter two were detected in the shorter trial. A higher mean wheat yield (average 0.15 t ha −1 ) following stubble burning was observed in the 19‐year trial but not in the 5‐year trial. Research to monitor the longer term effects of stubble burning is needed, and to identify conditions where loss of soil organic carbon is minimized.