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Recalcitrant and labile carbon pools in a sub-humid tropical soil under different tillage combinations: A case study of rice-wheat system

机译:不同耕作方式下半湿润热带土壤难顽固碳库的研究-以稻麦系统为例

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摘要

In order to utilize agricultural soils as an option to offset atmospheric carbon, it is essential to ascertain the degree of stability of the accrued carbon. A two step acid hydrolysis technique was used to separate labile and recalcitrant carbon pools in soil upto 30 cm depth to analyze their responses to different tillage managements after eight years of continuous practice in a sub-humid tropical rice-wheat system of Indo-Gangetic plains. There were four tillage practices; tillage before sowing/transplantation of every crop (RCT-WCT), tillage before transplanting of rice but no tillage before sowing the succeeding wheat crop (RCT-WNT), tillage before sowing of wheat but no tillage before sowing of rice (RNT-WCT), and no tillage before sowing of rice as well as wheat (RNT-WNT). It was observed that reduction in tillage frequency enhanced the total and recalcitrant carbon contents in soil with the maximum rate of sequestration recorded under RNT-WNT (0.59 tC ha(-1) yr(-1)). The fraction of carbon translated into recalcitrant pool was constant under all the tillage combinations indicating that carbon stabilization was dependent predominantly on organic matter input in the rice-wheat system. Conventional tillage on the other hand caused loss of carbon from the soil as observed by reduction in total soil carbon content under RCT-WCT. Reduction in recalcitrant carbon content under RCT-WCT further indicated that acid hydrolysis might not represent long term carbon accumulation reliably. Concentration of phenolics in labile pool increased under RNT-WNT, RCT-WNT and RNT-WCT practices which also had higher total and recalcitrant carbon pools. This indicated towards contribution of phenolics in carbon stabilization in the soil. Results of the present study further suggested that adoption of no till agriculture in the region offers significant carbon sequestration opportunity under proper agricultural management
机译:为了利用农业土壤来抵消大气中的碳,必须确定积碳的稳定性。在印度-恒河平原半湿润的热带稻麦系统中连续练习八年后,采用两步酸水解技术分离了深度不超过30 cm的土壤中不稳定和顽固的碳库,以分析它们对不同耕作方式的响应。有四种耕作方式;每种作物的播种/移植前的耕作(RCT-WCT),水稻移栽前的耕作,但随后的小麦作物的播种前的耕作(RCT-WNT),小麦的播种前的耕作但水稻的播种前的耕作(RNT-WCT) ),并且在播种水稻和小麦(RNT-WNT)之前不要耕种。观察到,耕作频率的降低提高了土壤的总碳含量和顽固碳含量,在RNT-WNT模式下记录的最大固存速率为(0.59 tC ha(-1)yr(-1))。在所有耕作组合下,转化为顽calc库的碳含量均保持不变,这表明碳稳定主要取决于稻麦系统中输入的有机物。另一方面,常规耕作会导致土壤中碳的流失,这是通过RCT-WCT下土壤总碳含量的减少而观察到的。在RCT-WCT下降低顽固性碳含量进一步表明,酸水解可能无法可靠地代表长期碳积累。在RNT-WNT,RCT-WNT和RNT-WCT的操作下,不稳定库中的酚类浓度增加,而总库和顽固碳库也更高。这表明酚醛对土壤碳稳定的贡献。本研究结果进一步表明,在适当的农业管理下,该地区采用免耕农业将提供大量的固碳机会。

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