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Conservation Tillage Impacts on Soil Aggregation and Carbon Pools in a Sandy Clay Loam Soil of the Indian Himalayas

机译:保护性耕作对印度喜马拉雅山沙质壤质壤土土壤团聚和碳库的影响

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摘要

Soil conservation and C sequestration are critical issues in rainfed farming of the Indian Himalayas. This study, conducted from 2003 through 2009 on a sandy clay loam soil (Typic Haplaquept) near Almora, India, evaluated the effect of seasonal tillage alterations (year-round conventional tillage [CT-CT], year-round no tillage [NT-NT], CT in the Rabi [winter] season and NT in the Kharif [summer/rainy] season (CT-NT) and the reverse [NT-CT] of the latter treatment) on soil organic carbon (SOC) retention, soil aggregation, aggregate-associated C concentrations and particulate organic matter-carbon (POM-C) in the 0- to 15-cm soil layer. Results indicate that the plots under NT-NT, NT-CT, and CT-NT had nearly 16, 12, and 10% higher total SOC content compared with CT-CT (similar to 12 g kg(-1) soil) in the 0- to 5-cm soil layer. However, tillage had no impact on total SOC content in the subsurface (5- to 15-cm) soil layer. Although the labile pools of SOC were positively affected by conservation tillage practices (CT-NT, NT-NT, and NT-CT), the less labile pool was only influenced by the continuous NT and NT-CT in the 0- to 5-cm depth. Plots under NT-NT and NT-CT had about 27 and 19% higher labile SOC pool than CT-CT plots (5.65 g C kg(-1) soil), and NT-NT and NT-CT plots had about 14 and 11% higher less labile SOC pool than CT-CT plots (2.61 g C kg(-1) soil) in that soil layer. Plots under NT-NT and one seasonal tillage (NT-CT and CT-NT) also had higher macroaggregates and macroaggregate-associated SOC after 6 yr of study than CT-CT plots. Greater proportion of microaggregates within macroaggregates in the plots under NT-NT compared with CT-CT was also observed in the surface layer only. The NT-CT plots had similar effects on all studied soil properties to CT-NT plots, apart from the mean weight diameter (MWD) and labile SOC pool in the 0- to 5-cm soil layer were higher under former plots than the latter. Plots under NT-NT had about 10% higher coarse (250-2000 mu m) intra-aggregate particulate organic matter-C (iPOM-C) within >2000 mu m sand free aggregates in the 0- to 5-cm soil layer compared with CT-CT plots. The fine (53-250 mu m) iPOM-C within the 250- to 2000-mu m aggregates was also higher in the continuous NT plots compared with CT within both >2000 and 250 to 2000 mu m sand free aggregate size classes in that soil layer. Thus, the adoption of continuous NT is the best management option for improvement of soil C under a rainfed lentil [Lens esculentus (L.)]-finger millet [Eleusine coracona (L.) Gaertn.] cropping system of the Indian Himalayas, as the management practice has the potential to improve productivity and soil aggregation with greater accumulation of POM-C, and SOC stabilization apart from other known benefits like weed control, less cultivation cost, and higher profits.
机译:土壤保护和固碳是印度喜马拉雅山雨养农业中的关键问题。该研究于2003年至2009年在印度阿尔莫拉附近的砂质壤土(典型的Haplaquept)上进行,评估了季节性耕作变更(全年常规耕作[CT-CT],全年无耕作[NT- NT],Rabi [冬季]的CT和Kharif [夏季/雨季]的NT(CT-NT)和后一种处理的反向[NT-CT])对土壤有机碳(SOC)保留,土壤的影响0至15厘米土壤层中的团聚体,团聚体相关的C浓度和颗粒有机碳(POM-C)。结果表明,与CT-CT(类似于12 g kg(-1)土壤)相比,NT-NT,NT-CT和CT-NT下的土壤总SOC含量高出近16、12和10%。 0至5厘米土壤层。但是,耕作对地下(5至15厘米)土壤层中的总SOC含量没有影响。尽管SOC的不稳定库受到保护性耕作实践(CT-NT,NT-NT和NT-CT)的积极影响,但不稳定的库仅受0至5-连续的NT和NT-CT影响厘米深。 NT-NT和NT-CT下的土壤不稳定SOC池比CT-CT(5.65 g C kg(-1)土壤)高27%和19%,而NT-NT和NT-CT地块的不稳定SOC池高约14和11在该土壤层中,不稳定的SOC池比CT-CT图(2.61 g C kg(-1)土壤)少%。在研究了6年后,NT-NT和一个季节性耕作(NT-CT和CT-NT)下的田间土壤中的大颗粒和与大颗粒相关的SOC也比CT-CT样高。在NT-NT下,与CT-CT相比,在NT-NT下的大块体中的微聚集体比例也更大,仅在表层。 NT-CT地块对所有研究的土壤特性的影响均与CT-NT地块相似,除了0-5 cm土层中的平均重径(MWD)和不稳定的SOC库在前者下高于后者。 。在NT-NT下,0至5厘米土壤层中> 2000微米无砂骨料中的粗粒(250-2000微米)骨料内部颗粒有机碳(iPOM-C)高约10%与CT-CT图。在连续NT田块中,在250到2000微米的骨料中,细粒(53-250微米)iPOM-C也比在大于2000和250到2000微米的无砂骨料尺寸类别中的CT高。土壤层。因此,在印度喜马拉雅山的旱作扁豆[Lens esculentus(L。)]-小米[Eleusine coracona(L.)Gaertn。]种植系统下,采用连续NT是改善土壤C的最佳管理选择。除杂草控制,更少的种植成本和更高的利润外,该管理实践还可能通过增加POM-C的积累和提高SOC稳定性来提高生产力和土壤聚集。

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