首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Effects of different irrigation regimes on soil compaction in a winter wheat-summer maize cropping system in the North China Plain
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Effects of different irrigation regimes on soil compaction in a winter wheat-summer maize cropping system in the North China Plain

机译:华北平原冬小麦-夏玉米种植系统不同灌溉方式对土壤紧实的影响

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An adjusted irrigation regime may help to minimize the risk of soil compaction, which is a major yield constraining factor in global crop production, constituting a serious issue in the winter wheat-summer maize double cropping system of the North China Plain. Thus this study aimed to evaluate the natural changes of soil penetration resistance (PR) and soil bulk density (BD) caused by freezing/thawing (FT) and wetting/drying (WD) cycles. This was tested under full irrigation (FI) and deficit irrigation (DI) over three double cropping seasons from 2011 to 2014, following a conventional tillage sequence of shallow, deep and shallow tillage before the first, second and third season, respectively. The results showed that in the deeper soil layer FT during winter reduced the PR by 22.9%, 34.7% and - 18.7% under FI for the three seasons, respectively. The values under DI were 4.5%, 8.0% and - 33.8% for the three seasons, respectively. However the compaction alleviating effects due to FT were only of temporary nature. Furthermore FI caused a stronger recompaction after deep tillage compared to DI, mainly attributed to increased slumping of soil. On the contrary DI reduced the BD by 8.4% in the deep soil layer by fostering intensive cycles of WD over the three double cropping seasons. Results also showed that DI resulted in a higher physical quality of subsoil, expressed by the value of S, compared to FI It was concluded that irrigation intensity should be reduced after deep tillage to minimize and slow down subsequent recompaction. (C) 2015 Elsevier B.V. All rights reserved.
机译:调整灌溉制度可能有助于最大程度地减少土壤致密化的风险,土壤致密化是全球农作物产量的主要限制因素,在华北平原冬小麦-夏季玉米双季种植系统中构成严重问题。因此,本研究旨在评估由于冻融(FT)和湿润/干燥(WD)循环引起的土壤渗透阻力(PR)和土壤容重(BD)的自然变化。在分别于第一,第二和第三季之前进行浅,深和浅耕的常规耕作顺序后,分别于2011年至2014年的三个双季作物进行了全灌(FI)和亏水(DI)灌溉。结果表明,在三个季节中,冬季深层土壤FT在FI下使PR分别降低了22.9%,34.7%和-18.7%。在三个季节中,DI下的值分别为4.5%,8.0%和-33.8%。但是,由于FT引起的压实减轻效果只是暂时的。此外,与DI相比,FI在深耕后引起更强的夯实作用,这主要归因于土壤下陷的增加。相反,DI通过在三个双季种植季节中加强WD的密集周期,使深层土壤的BD降低了8.4%。结果还表明,与FI相比,DI可以提高土壤深层的物理质量(用S值表示)。结论是深耕后应降低灌溉强度,以最大程度降低和减缓随后的压实。 (C)2015 Elsevier B.V.保留所有权利。

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