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首页> 外文期刊>Journal of land use science >Soil Structure after 18 Years of Long-term Different Tillage Systems and Fertilisation in Haplic Luvisol
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Soil Structure after 18 Years of Long-term Different Tillage Systems and Fertilisation in Haplic Luvisol

机译:18年后的土壤结构在长期不同耕作系统和施肥中的铺酚

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摘要

Soil structure is a key determinant of many soil environmental processes and is essential for supporting terrestrial ecosystem productivity. Management of arable soils plays a significant role in forming and maintaining their structure. Between 1994 and 2011, we studied the influence of soil tillage and fertilisation regimes on the stability of soil structure of loamy Haplic Luvisol in a replicated long-term field experiment in the Dolna Malanta locality (Slovakia). Soil samples were repeatedly collected from plots exposed to the following treatments: conventional tillage (CT) and minimum tillage (MT) combined with conventional (NPK) and crop residue-enhanced fertilisation (CR+NPK). MT resulted in an increase of critical soil organic matter content (St) by 7% in comparison with CT. Addition of crop residues and NPK fertilisers significantly increased St values (by 7%) in comparison with NPK-only treatments. Soil tillage and fertilisation did not have any significant impact on other parameters of soil structure such as dry sieving mean weight diameters (MWD), mean weight diameter of water-stable aggregates (MWDWSA), vulnerability coefficient (Kv), stability index of water-stable aggregates (Sw), index of crusting (Ic), contents of water-stable macro- (WSA(ma)) and micro-aggregates (WSA(mi)). Ic was correlated with organic matter content in all combinations of treatments. Surprisingly, humus quality did not interact with soil management practices to affect soil structure parameters. Higher sums of base cations, CEC and base saturation (Bs) were linked to higher Sw values, however higher values of hydrolytic acidity (Ha) resulted in lower aggregate stability in CT treatments. Higher content of K+ was responsible for higher values of MWD(wsA)and MWD in CT. In MT, contents of Ca2+, Mg2+ and Na+ were significantly correlated with contents of WSA(mi)and WSA(ma). Higher contents of Na+ negatively affected St values and positive correlations were detected between Ca2+, Mg2+ and Na+ and Ic in NPK treatments.
机译:土壤结构是许多土壤环境过程的关键决定因素,对于支持陆地生态系统生产力至关重要。耕地的管理在形成和维持其结构方面发挥着重要作用。在1994年至2011年期间,我们研究了土壤耕作和施肥制度对Dolna Malanta位置(斯洛伐克)复制的长期田间实验中壤土实验中壤土结构稳定性的影响。从暴露于以下治疗的地块中重复收集土壤样品:常规耕作(CT)和最小耕作(MT)与常规(NPK)和作物残留增强施肥(Cr + NPK)组合。与CT相比,MT导致临界土壤有机物质含量(ST)增加7%。与仅NPK的治疗相比,添加作物残留物和NPK肥料显着增加了ST值(达7%)。土壤耕作和施肥对土壤结构的其他参数(如干筛分的平均重量直径(MWD),平均水稳定骨料(MWDWSA),漏洞系数(KV),水的稳定性指数(MWD),水 - 稳定的聚集体(SW),壳体指数(IC),水稳定的宏观(WSA(MA))和微聚集体(WSA(MI))的含量。 IC与各种治疗组合中的有机质含量相关。令人惊讶的是,腐殖质的质量没有与土壤管理实践相互作用以影响土壤结构参数。基础阳离子,CEC和基础饱和度(BS)的高度与较高的SW值连接,但是较高的水解酸度(HA)值导致CT处理中的骨料稳定性较低。 k +含量较高负责CT中MWD(WSA)和MWD的较高值。在Mt中,Ca2 +,Mg2 +和Na +的含量与WSA(MI)和WSA(MA)的含量显着相关。在NPK处理中的Ca2 +,Mg2 +和Na +和IC之间检测到较高的Na +负影响的ST值和正相关性。

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