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Soil Disturbance-Residue Management Effect on Winter Wheat Growth and Yield

机译:土壤干扰 - 残留管理对冬小麦生长发育及产量的影响

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摘要

The need to reduce soil erosion, maximize soil water conservation, and optimize grain production in dryland cropping systems in the Central Great Plains has culminated in development of nontilled fallow systems. These systems have greatly reduced the degree of soil disturbance, and the amount and degree of residue incorporation. The objectives of this study were to evaluate the influence of soil disturbance and residue management on soil temperature, soil water, and winter wheat (Triticum aestivum L.) growth. Two field studies were established in 1981 and 1982 on an Alliance silt loam (Fine-silty, mixed, mesic Aridic Argiustoll) with treatments consisting of various degrees of soil disturbance (moldboard plow, tandem disk, and no tillage), residue incorporation (on the soil surface or incorporated), and amount of residue applied (0.0, 0.5, and 1.0 of that produced by the previous crop). Decreased soil disturbance (tillage) and increased residue application decreased maximum, and increased minimum, soil temperatures. In all tillage treatments, soil water content showed a significant positive linear relationship to residue application rate. Grain yield was similar for all treatment factors, except tillage within the 1983- 1984 season when tilled (3.48 Mg ha-1) treatments produced more grain than the nontilled (3.20 Mg ha-1) treatment. Early development and growth of winter wheat was slowed by the presence of residues (surface or incorporated) or the absence of tillage. However, by completion of heading, phenology and yield were similar for all treatments. Cooler soil temperatures slowed development and growth during those stages when the meristem temperature was influenced most by soil temperature. However, after jointing, when air temperature and photo-period were controlling development and growth, differences among treatments disappeared. Interaction of wheat development with soil temperature, air temperature, and daylength may contribute to the crop\u27s inability to consistently capitalize, in terms of grain yield, on the greater amount of water stored in nontilled and mulched systems.
机译:在中部大平原的旱地种植系统中,减少土壤侵蚀,最大程度地节水和优化谷物生产的需求最终导致了非倾斜休耕系统的发展。这些系统极大地减少了土壤扰动的程度,并减少了残留物的掺入数量和程度。这项研究的目的是评估土壤扰动和残留管理对土壤温度,土壤水和冬小麦(Triticum aestivum L.)生长的影响。 1981年和1982年对Alliance淤泥壤土(细粉质,混合性,中性的Argiustoll泥土)进行了两次田间研究,处理方法包括不同程度的土壤扰动(mol刨犁,纵排圆盘和免耕),残渣掺入(上土壤表面或掺入的土壤),以及施用的残留量(上一茬作物的残留量的0.0、0.5和1.0)。减少的土壤干扰(耕作)和增加的残留物施用减少了土壤温度,最大降低了土壤温度。在所有耕作处理中,土壤含水量与残留物施用量均呈显着正线性关系。除1983-1984年的耕作(耕种(3.48 Mg ha-1)处理比未耕种(3.20 Mg ha-1)处理产生更多的谷物)外,所有处理因素的谷物产量均相似。残留(表面或掺入)或没有耕作会减缓冬小麦的早期发育和生长。但是,完成标题后,所有处理的物候和产量相似。在分生组织温度受土壤温度影响最大的那些阶段,凉爽的土壤温度会减缓发育和生长。但是,在接合后,当气温和光周期控制着发育和生长时,治疗之间的差异就消失了。小麦发育与土壤温度,气温和昼长的相互作用可能会导致作物无法始终如一地利用谷物产量,利用非倾斜和覆盖系统中储存的大量水进行谷物利用。

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