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Soil Organic Carbon Sequestration in Rice-Wheat System under Conservation and Conventional Agriculture in Western Chitwan, Nepal

机译:保护和常规农业下尼泊尔奇旺的稻麦系统中的土壤有机碳固存

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Soil organic carbon plays the crucial role in maintaining soil quality. The impact and rate of SOC sequestration in CA and conventional agriculture is still in investigation in this environment. A field experiment was initiated in 2011/12 and continued up to 2012/13 to compare the organic carbon buildup in the soil due to conservation and conventional agriculture. The soil organic carbon data represents the cumulative after five crop cycle. The treatments consisted conventionally tilled direct seeded rice followed by zero tilled wheat, conventionally tilled transplanted rice followed by conventionally tilled wheat, zero tilled direct seeded rice followed by zero tilled direct seeded wheat without residue retention, zero tilled direct seeded rice followed by direct seeded wheat with residue retention, permanent raised bed of rice followed by wheat without residue retention and permanent raised bed of rice followed by wheat with residue retention in randomized complete block design with three replications. About 4 t ha-1 of standing rice and wheat crop and about 70% residue of moongbean was retained for succeeding crop in retained treatments. Soil samples from each treatments were collected from two soil depths (0-20 and 20-40cm) and analyzed. Result showed that, soil organic carbon buildup was affected significantly by tillage and residue level in upper depth of 0-20 cm but not in lower depth of 20-40 cm. Higher SOC content of 19.44 g kg-1 of soil was found in zero tilled residue retained plots followed by 18.53 g kg-1 in permanently raised bed with residue retained plots. Whereas, the lowest level of SOC content of 15.86 g kg-1 of soil were found in puddled transplanted rice followed by wheat planted under conventionally tilled plots. Zero tilled residue retained plots sequestrated 0.91 g kg-1 yr-1 SOC in the year 2012/13 which was 22.63% higher over the conventionally tilled residue removed plots after five seasons of experimentation. Therefore, CA in rice-wheat system can help directly in building–up of soil organic carbon and improve the fertility status of soil.
机译:土壤有机碳在维持土壤质量方面起着至关重要的作用。在这种环境下,SOC封存对CA和常规农业的影响和速率仍在研究中。 2011/12年开始进行实地试验,并持续到2012/13年,以比较由于保护和常规农业而在土壤中积累的有机碳。土壤有机碳数据代表五个作物周期后的累积量。处理方法包括:常规耕种的直纹水稻,然后是零耕种的小麦,常规耕种的移栽水稻,然后是常规耕种的小麦,零耕种的直纹水稻,然后是零耕种的无残留直纹小麦,零耕种的直纹水稻,然后是直纹小麦具有残留物保留的水稻,永久性增高床,然后是无残留小麦的小麦,永久性增高的水稻床,然后是具有残留物保持的小麦,采用随机重复完整区组设计,重复三次。在保留的处理中,约有4 t ha-1的站立稻谷和小麦作物和约70%的月亮豆残留物被保留用于后续作物。从两种土壤深度(0-20和20-40cm)收集每种处理的土壤样品并进行分析。结果表明,耕作和残渣水平​​在0-20 cm的较高深度对土壤有机碳积累有显着影响,而在20-40 cm的较低深度则不受耕作和残留水平的影响。在零耕残渣保留地中发现较高的SOC含量,为19.44 g kg-1,随后在永久残渣保留地中的永久性升高床中发现18.53 g kg-1。而在水化水稻和随后在常规耕地中种植的小麦中,SOC的最低水平为15.86 g kg-1。零耕种残留残留地在2012/13年度的固碳残留量为0.91 g kg-1 yr-1 SOC,比经过五个季节的常规耕种残留残留地增加了22.63%。因此,稻麦系统中的CA可以直接帮助土壤有机碳的积累,并改善土壤的肥力状况。

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