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首页> 外文期刊>Soil & Tillage Research >Twenty years of conservation tillage research in subarctic Alaska: II. Impact on soil hydraulic properties
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Twenty years of conservation tillage research in subarctic Alaska: II. Impact on soil hydraulic properties

机译:北极亚拉斯加保护性耕作研究的二十年:II。对土壤水力特性的影响

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摘要

Soil management practices are needed in the subarctic that stabilize the soil against the forces of wind and water as well as conserve soil water for crop production. There is a paucity of information, however, regarding the long-term effects of conservation tillage on soil hydraulic properties in subarctic Alaska. The objective of this study was therefore to characterize infiltration, water retention, and saturated hydraulic conductivity of a soil 20 years after establishing tillage and straw management treatments in interior Alaska. The strip plot experimental design, established on a silt loam and maintained in continuous barley (Hordeum vulgare L.), included tillage as the main treatment and straw management as the secondary treatment. Tillage treatments included no tillage, autumn chisel plow, spring disk, and intensive tillage (autumn and spring disk) while straw treatments included retaining or removing stubble and loose straw from the soil surface after harvest. Soil properties were measured after sowing in spring 2004; saturated hydraulic conductivity was measured by the falling-head method, infiltration was measured using a double-ring infiltrometer, and water retention was assessed by measuring the temporal variation in in-situ soil water content. No tillage resulted in greater saturated hydraulic conductivity and generally retained more water against gravitational and matric forces than other tillage treatments. Infiltration was greater in autumn chisel plow than other tillage treatments and was presumably suppressed in no tillage by an organic layer overlying mineral soil. Infiltration was also enhanced by retaining straw on rather than removing straw from the soil surface after harvest. No tillage is not yet a sustainable management practice in this region due to lack of weed control strategies. In addition, the formation of an organic layer in no tillage has important ramifications for the soil hydrological and thermal environment. Therefore, minimum tillage (i.e., autumn chiselplow or spring disk) appears to be a viable management option for maximizing infiltration in interior Alaska.
机译:亚北极地区需要土壤管理措施,以稳定土壤抵抗风和水的作用,并节约土壤水用于作物生产。但是,关于保护性耕作对阿拉斯加亚北极土壤水力特性的长期影响的信息很少。因此,本研究的目的是表征在阿拉斯加内部进行耕作和秸秆处理后20年的土壤入渗,保水和饱和导水率。在淤泥质壤土上建立并维持在连续大麦中的带状地带实验设计包括耕作作为主要处理,秸秆管理作为辅助处理。耕作方法包括不耕作,秋季凿犁,春季盘和密集耕作(秋季和春季盘),而秸秆处理包括在收获后保留或清除土壤表面的残茬和疏松秸秆。在2004年春季播种后测量土壤性质;用落头法测量饱和导水率,用双环渗透仪测量渗透率,并通过测量原位土壤含水量的时间变化来评估保水率。与其他耕作处理相比,没有耕作产生更大的饱和水力传导率,并且通常在重力和基质力的作用下保留了更多的水。与其他耕作相比,秋季凿耕机的入渗量更大,并且据推测,在耕作过程中,覆盖层覆盖的无机层可抑制土壤入渗。收获后将秸秆保留在土壤中而不是从土壤表面清除秸秆,也增强了土壤的渗透。由于缺乏杂草控制策略,该地区尚无耕作方法尚未成为可持续的管理方法。此外,免耕有机层的形成对土壤水文和热环境有重要影响。因此,尽量减少耕种(即秋季凿犁或春季盘耕作)似乎是使阿拉斯加内部的渗透最大化的可行管理选择。

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