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首页> 外文期刊>Soil and Water Research >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:长期种植不同耕作制度和施肥的卢维索尔的土壤结构

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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 Dolná 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 (MWD WSA ), 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 Ca 2+ , Mg 2+ 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 Ca 2+ , Mg 2+ 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起着重要作用。在1994年至2011年之间,我们通过在DolnáMalanta地区(斯洛伐克)进行的长期重复田间试验,研究了土壤耕作和施肥方式对肥沃的Haplic Luvisol土壤结构稳定性的影响。从暴露于以下处理条件的土地上反复收集土壤样品:常规耕作(CT)和最小耕作(MT)结合常规(NPK)和增强作物残茬的施肥(CR + NPK)。 MT导致土壤关键有机质含量(St)与CT相比增加了7%。与仅NPK处理相比,添加作物残留物和NPK肥料显着提高了St值(增加了7%)。土壤耕作和施肥对土壤结构的其他参数没有任何显着影响,例如干筛平均重径(MWD),水稳性团聚体的平均重径(MWD WSA ),脆弱性系数( Kv),水稳定骨料的稳定性指数(Sw),结皮指数(Ic),水稳定大骨料(WSA ma )和微骨料(WSA mi < / sub>)。在所有处理组合中,IC与有机物含量相关。令人惊讶的是,腐殖质的质量与土壤管理实践没有相互作用,不会影响土壤结构参数。较高的碱性阳离子,CEC和碱性饱和度(Bs)之和与较高的Sw值相关,但是较高的水解酸度(Ha)导致CT处理中的骨料稳定性较低。 K + 的较高含量是导致CT中MWD WSA 和MWD值较高的原因。在MT中,Ca 2+ ,Mg 2+ 和Na + 的含量与WSA mi 和WSA ma 。 Na + 的含量较高,对St值具有负面影响,并且在Ca 2+ ,Mg 2+ 和Na + < / sup>和Ic处理NPK。

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