首页> 外文期刊>Agriculture, Ecosystems & Environment: An International Journal for Scientific Research on the Relationship of Agriculture and Food Production to the Biosphere >Short-term conservation agriculture and biomass-C input impacts on soil C dynamics in a savanna ecosystem in Cambodia
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Short-term conservation agriculture and biomass-C input impacts on soil C dynamics in a savanna ecosystem in Cambodia

机译:短期保护性农业和生物量碳输入对柬埔寨稀树草原生态系统中土壤碳动态的影响

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摘要

Conservation agriculture (CA) is an effective tool that is used to increase soil C sequestration and enhance soil quality and agronomic productivity. However, rigorous empirical evidence from Southeast Asia, particularly in the Cambodian agro-ecosystem, is still scarce. We hypothesized that high and diversified biomass-C inputs in CA might be the first step toward to increase SOC in the topsoil by creating the C flow to support C storage overtime. Thus, the aim of this study was to quantify the short-term (i.e., five year) impacts of soil management and cropping systems on soil organic C (SOC), soil total N (STN), particulate organic C (POC) and mineral-associated organic C (MAOC). There were three distinct experiments comprised of a combination of cover and main crops including rice-, soybean- and cassava-based cropping systems, hereafter designated as RcCS, SbCS and CsCS, respectively. The experimental plots were laid out in a randomized complete block design with three replicates. Soil management treatments included conventional tillage (CT) and no-till (NT) and a selected adjacent area of reference vegetation (RV). Soil sampling was conducted in 2011 and 2013 at seven depths (0-5, 5-10, 10-20, 20-40, 40-60, 6080 and 80-100 cm). Soil management and crop sequences significantly affected SOC and STN stocks in all three cropping systems. On average, NT SOC stocks at 0-5 cm depth was greater than those of CT by 10%, 20% and 18% and STN stocks by 8%, 25% and 16% for RcCS, SbCS and CsCS, respectively. SOC levels followed the order RV > NT > CT. SOC stocks in the subsoil layers were consistently lower in NT than in CT in all three cropping systems. POC stocks at 0-5 cm depth in NT were on average 22%, 20% and 78% greater than those in CT in RcCS, SbCS and CsCS, respectively. However, significant differences were detected only in RcCS and CsCS. The major POC stocks were found at 0-20 cm depth. NT treatments in SbCS stored 9% greater MAOC stocks at 0-5 cm depth than those in CT, and an increasing trend of NT was observed in RcCS and CsCS. In all three cropping systems, NT systems with diversified crop species significantly increased SOC stocks ranging by 6 to 28% and POC stocks by 56-127% in the surface soils and tended to restore SOC and POC in the subsoil layers after five years. The results leads to accept the hypothesis that short-term CA associated with high biomass-C inputs (particularly bi-annual rotations) promotes SOC recovery in the topsoil layer and creates a potential to increase SOC in the subsoil layers when deeprooting cover crops are included in crop rotations. (C) 2015 Elsevier B.V. All rights reserved.
机译:保护性农业(CA)是一种有效的工具,可用于增加土壤碳固存并提高土壤质量和农艺生产力。但是,仍然缺乏来自东南亚的严格的经验证据,尤其是在柬埔寨的农业生态系统中。我们假设,CA中大量和多样化的生物质C输入可能是通过创建C流以支持C超时存储来增加表土SOC的第一步。因此,本研究的目的是量化土壤管理和耕作制度对土壤有机碳(SOC),土壤总氮(STN),颗粒有机碳(POC)和矿物的短期(即五年)影响-相关的有机碳(MAOC)。有三个不同的实验,包括覆盖作物和主要农作物的组合,包括水稻,大豆和木薯为基础的种植系统,以下分别称为RcCS,SbCS和CsCS。实验地块以随机重复的完整图块设计进行布局,一式三份。土壤管理处理措施包括常规耕作(CT)和免耕(NT)以及参考植被的选定相邻区域(RV)。在2011年和2013年在七个深度(0-5、5-10、10-20、20-40、40-60、6080和80-100厘米)进行了土壤采样。土壤管理和作物种植顺序显着影响了所有三个种植系统中的SOC和STN储量。平均而言,RcCS,SbCS和CsCS在0-5 cm深度处的NT SOC储量分别比CT分别大10%,20%和18%和STN储量分别为8%,25%和16%。 SOC含量遵循RV> NT> CT的顺序。在所有三种耕作系统中,地下土壤的SOC储量在北领地均始终低于CT。在NT中,0-5 cm深度的POC存量分别比RcCS,SbCS和CsCS的CT分别高22%,20%和78%。但是,仅在RcCS和CsCS中检测到显着差异。发现了主要的POC库存,深度为0-20厘米。 SbCS中的NT处理在0-5 cm深度处比CT中存储的MAOC储量多9%,并且在RcCS和CsCS中观察到NT的增加趋势。在所有三种耕作系统中,具有多种作物种类的NT系统显着增加了表层土壤的SOC量,范围为6%至28%,POC量的范围为56-127%,并且倾向于在五年后恢复地下土壤层中的SOC和POC。结果导致接受这样的假说,即与高生物量碳输入(特别是一年两次的轮换)相关的短期CA促进表土层的SOC恢复,并且当包括深层覆盖作物在内时,有可能增加地下土壤的SOC。在轮作中。 (C)2015 Elsevier B.V.保留所有权利。

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