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首页> 外文期刊>Soil & Tillage Research >Twenty years of tillage research in subarctic Alaska: I. Impact on soil strength, aggregation, roughness, and residue cover
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Twenty years of tillage research in subarctic Alaska: I. Impact on soil strength, aggregation, roughness, and residue cover

机译:北极阿拉斯加耕作研究的二十年:I.对土壤强度,聚集,粗糙度和残留物覆盖的影响

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摘要

Soil properties and surface characteristics affecting wind erosion can be manipulated through tillage and crop residue management. Little information exists, however, that describes the impact of long term tillage and residue management on soil properties in the subarctic region of the United States. This study examines the impact of 20 years of tillage and residue management on a broad range of physical properties that govern wind erosion processes on a silt loam in interior Alaska. A strip plot experimental design was established in 1983 and included intensive tillage (autumn and spring disk), spring disk, autumn chisel plow, and no tillage with straw either retained on or removed from the soil surface. Soil and residue properties measured after sowing barley (Hordeum vulgare L.) in May 2004 included penetration resistance, soil water content, shear stress, bulk density, random roughness, aggregate size distribution, and residue cover and biomass. No tillage was characterized by larger aggregates, greater soil strength (penetration resistance and shear stress), wetter soil, and greater residue cover compared to all other tillage treatments. Despite crop failures the previous 2 years, crop residue management influenced residue biomass and cover,but not soil properties. Autumn chisel and spring disk appeared to be viable minimum tillage options to intensive tillage in controlling erosion. Autumn chisel and spring disk promoted greater roughness, aggregation, and residue cover as compared with intensive tillage. Although no tillage appeared to be the most effective management strategy for mitigating wind erosion, no tillage was not a sustainable practice due to lack of weed control. No tillage also resulted in the formation of an organic layer on the soil surface over the past 20 years, which has important ramifications for long term crop production in the subarctic where the mean annual temperature is 0 [degree sign]C.
机译:可以通过耕作和作物残留管理来控制影响风蚀的土壤特性和表面特性。但是,几乎没有信息可以描述长期耕作和残留物管理对美国亚北极地区土壤性质的影响。这项研究考察了20年耕作和残茬管理对控制阿拉斯加内部淤泥质壤土上风蚀过程的广泛物理特性的影响。 1983年建立了带状样地试验设计,包括密集耕作(秋季和春季盘),春季盘,秋季凿犁,并且没有在土壤表面保留或从土壤中除去秸秆的耕作方式。在2004年5月播种大麦(Hordeum vulgare L.)后测得的土壤和残留物特性包括抗渗透性,土壤水分,剪切应力,堆积密度,随机粗糙度,骨料粒度分布以及残留物覆盖率和生物量。与所有其他耕作处理相比,没有耕作的特征是具有更大的集料,更大的土壤强度(抗穿透性和剪切应力),湿润的土壤以及更大的残茬覆盖率。尽管前两年农作物歉收,但农作物残茬管理影响了残茬生物量和覆盖度,但不影响土壤特性。在控制侵蚀方面,秋季凿和春季盘似乎是可行的最小耕作方式,而对于密集耕作而言。与密集耕作相比,秋季凿子和弹簧盘促进了更大的粗糙度,聚集和残渣覆盖。尽管没有耕作似乎是减轻风蚀的最有效管理策略,但是由于缺乏杂草控制,没有耕作不是可持续的做法。在过去的20年中,没有耕作也未在土壤表面形成有机层,这对年平均温度<0 [°C]的亚北极长期作物生产具有重要影响。

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