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:不同耕作方式对粘壤土土壤有机碳和全氮分布的影响

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摘要

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:减少耕作是减缓农业气候变化的策略之一。通过减少或免耕以及施用钙改良剂来提高土壤有机质含量已被公认为防治土壤退化的重要策略。以前在立陶宛没有充分研究过减少耕作粘土的可能性。2016-2018年,立陶宛农业研究中心Joniskelis实验站对粘壤土(粉硅质,排水性)进行了研究,该研究于2006年建立。研究的处理方法包括:21-23 cm深度深耕(DP)(对照)、10-12 cm深度(PT)的免耕、2014年最后一次掺入的石灰污泥的免耕和后效(PT+aLS)和秋季免耕,冬季覆盖作物覆盖(NT+WM)。主要作物收获后,每年从0-10、10-20和20-30 cm三个土壤深度采集土壤样品。少耕系统显著提高了上层(0-10 cm)土层土壤有机碳(SOC)含量,顺序为PT+aLS>NT+WM>PT>DP,并表现出少耕系统土壤有机碳分层。在PT和NT+WM处理下,0-10和10-20 cm层的水可萃取有机碳(WEOC)含量较高,而在PT+aLS处理下,WEOC含量低于DP。石灰污泥阳离子稳定了SOC的流动和不稳定形式,降低了WEOC含量。土壤全氮(TN)受减耕制度的影响较小,上层(0-10 cm)土层TN含量仅在NT+WM下显著增加。土壤中SOC与TN的关系具有较高的相关系数,表明土壤中SOC与TN积累量关系密切;SOC与WEOC以及TN与WEOC的关系相关系数较低。

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