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首页> 外文期刊>Fresenius environmental bulletin >IMPACT OF DIFFERENT TILLAGE PRACTICES ON DISTRIBUTION OF SOIL ORGANIC CARBON AND TOTAL NITROGEN IN CLAY LOAM SOIL
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IMPACT OF DIFFERENT TILLAGE PRACTICES ON DISTRIBUTION OF SOIL ORGANIC CARBON AND TOTAL NITROGEN IN CLAY LOAM SOIL

机译:不同耕作实践对粘土壤土土壤有机碳和总氮分布的影响

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Reduced tillage is one of strategies for mitigat-ing climate change in agriculture. Enhancement of soil organic matter content by reduced or no-tillage practice and Ca-amendment application has been recognized as important strategies to combat soil degradation. Possibilities to reduce tillage clayey soil have not been sufficiently investigated in Lithu-ania before. Research was carried out during 2016-2018 at the Joniskelis Experimental Station of the Lithuanian Research Centre for Agriculture and For-estry on a clay loam(siltic, drainic), Endocalcary-Endohypogleyic Cambisol(CMgn-w-can) in the ex-periment, established in 2006. The studied treat-ments included: deep ploughing (DP)at 21-23 cm depth(control),ploughless tillage at 10-12 cm depth (PT), as well as ploughless tillage and aftereffect of lime sludge last incorporated in 2014(PT+aLS)and no-till in the autumn with a cover crop for winter mulch (NT+WM). Soil samples were collected an-nually after the main crop harvest from three soil depth 0-10,10-20, and 20-30 cm.?Reduced tillage systems significantly increased soil organic carbon (SOC) content in the upper(0-10 cm) soillayerby order PT+aLS>NT+WM>PT>DP and shows SOC stratification in reduced tillage systems. Water extractable organic carbon (WEOC)content was higher under PT and NT+WM treat-ments at 0-10 and 10-20 cm layers, however under PT+aLS the WEOC content was lower compared to DP. Cations from lime sludge stabilized mobile and labile forms of SOC,reducing WEOC content. Total nitrogen(TN)in soil was less affected by applied re-duced tillage systems, amount of TN in the upper(0-10 cm) soil layer increased significantly only under NT+WM.High correlation coefficients were ob-served for the relationship of SOCvs TN, indicating a close relation between SOC and TN accumulation in soil;lower correlation coefficients were observed for the relations of SOC vs WEOC, and TN vs WEOC.
机译:减少耕作是农业促进气候变化的策略之一。通过减少或无耕作实践和CA-MENUMENTMENT申请改善土壤有机质含量并已被认为是对抗土壤退化的重要策略。降低耕作粘土土壤的可能性之前在岩石益腹之前没有得到充分调查。 2016 - 2018年在粘土壤土(硅,排水),内炽渣 - 内孔珠酚(CMGN-W-CAN)中的玉米米科斯研究中心Joniskelis实验站的2016 - 2018年在2016 - 2018年在魔法壤土(硅,排水),内炎 - 内核珠酚(CMGN-W-WAL)中的实验站进行了研究,成立于2006年。所研究的治疗方法包括:深耕(DP)在21-23厘米的深度(控制),止血耕作在10-12厘米深度(PT),以及LIME污泥的吹气耕作和后果的损坏于2014年(Pt + Als)并入秋季,冬季覆盖覆盖作物(NT + WM)。在三种土壤深度0-10,10-20和20-30厘米的主要作物收获后收集土壤样品。较高的耕作系统,较高的土壤有机碳(SoC)含量显着增加(0-10 CM)Soillayerby Order Pt + Als> NT + WM> Pt> DP并在减小的耕作系统中显示SOC分层。在0-10和10-20cm的Pt + WM处理下,水可提取的有机碳(WEOC)含量较高,但在Pt + Als下,与DP相比,WEOC含量较低。来自石灰污泥的阳离子稳定移动和不稳定形式的SoC,减少韦约内容。土壤中的总氮(TN)受施加的重新耕作系统的影响较小,上部(0-10cm)土壤中的TN的量仅在NT + WM下显着增加。具有对关系的影响性系数SOCVS TN,表明土壤中SOC和TN积累之间的密切关系; SOC VS WEOC的关系观察到较低的相关系数,以及TN VS WEOC。

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