The management of rice straw, fertilisers and leaf litters in rice cropping systems in Northeast Thailand. 1. Soil carbon dynamics

Declines in soil organic mailer (SOM) have occurred in most rainfed rice cropping systems in the world. Such declines threaten the sustainability of these systems and steps need to be taken to reverse the decline. Paired soil samples collected from forest and cropped areas in Northeast Thailand reve...

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Published inPlant and soil Vol. 209; no. 1; pp. 21 - 28
Main Authors Naklang, K. (Ubon Rice Research Center, Ubon Ratchathani (Thailand).), Whitbread, A, Lefroy, R, Blair, G, Wonprasaid, S, Konboon, Y, Suriya-arunroj, D
Format Journal Article
LanguageEnglish
Published Dordrecht Kluwer Academic Publishers 1999
Springer
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Summary:Declines in soil organic mailer (SOM) have occurred in most rainfed rice cropping systems in the world. Such declines threaten the sustainability of these systems and steps need to be taken to reverse the decline. Paired soil samples collected from forest and cropped areas in Northeast Thailand revealed an approximately 70% decline in both labile carbon (CL) and total carbon (CT) in the surface 10 cm as a result of cropping. CL was found to be higher in the 20-40 cm soil layer in the cropped than the forest soil indicating C leaching or soil mixing. In a field experiment it was found that CL, and a calculated Carbon Management Index (CMI), increased with annual applications of low rates (1500 kg/ha dry matter) of leaf litter from Cajanus cajan, Phyllanthus taxodifolius, Acacia auriculiformis and Samanae saman. Five seasons of leaf litter application increased the CT pool by 24-37% and more than doubled CL and soil C lability. The retention of rice straw improved CT in the first year of the trial but led to no significant increases in subsequent years. Higher rates of fertilisers did not result in increased soil C, despite increased yields. Crop residues, leaf litters and green manures with slow breakdown rates are needed to rehabilitate soil C. CL and the CMI can be used effectively to monitor the rate of change in soil C.
Bibliography:P34
2000000509
P35
ISSN:0032-079X
1573-5036
DOI:10.1023/A:1004571015620