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首页> 外文期刊>Journal of arid environments >Soil water extraction and use by winter wheat cultivars under limited irrigation in a semi-arid environment
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Soil water extraction and use by winter wheat cultivars under limited irrigation in a semi-arid environment

机译:半干旱环境下有限灌溉条件下冬小麦品种对土壤水分的提取和利用

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摘要

Water supply and distribution are the main limiting factors to wheat (Triticum aestivum) yield in a semi-arid region of the U.S. southern Great Plains. To manage crop water demand, limited irrigation (also called deficit irrigation) is commonly practiced in the region. A 4-yr study was conducted to evaluate yield in winter wheat cultivars as influenced by the depth and amount of net soil water extraction (SWE) under limited irrigation. For timing the irrigation application, we considered critical growth stages (jointing, tillering, and anthesis) as well as soil water depletion at the crop root zone below 50%. Volumetric soil water content was measured in 0.2 m increments to the depth of 2.4 m at planting, jointing, anthesis, and physiological maturity. Since the irrigation capacity was limited, seasonal precipitation was still an important factor for determining SWE. The 2011 season was one of the historic drought seasons with only 60 mm of seasonal precipitation and the net SWE in that season was limited to the upper 1.2 m profile. In contrast, the 2016 season was more favorable for crop growth with 315 mm of seasonal precipitation and the net SWE in that season reached to 2.0 m deep. Grain yield was largely influenced by the amount of net SWE during the growing season. For the wheat with grain yield of 4807 kg ha(-1), net SWE was 165 mm (2016). However, wheat with grain yield of 2933 kg ha(-1) only extracted 70 mm stored soil water (2011). The 2012 and 2017 seasons remained intermediate in terms of seasonal precipitation, SWE, and yield. Although the 2011 and 2016 seasons had similar stored soil moisture at planting, more early-season as well as total precipitation in 2016 appears to have enabled plant growth to access the deeper water. In contrast, a greater amount of stored soil water was left unused at the end of the 2011 season due to drought and poor plant growth. Hence, in addition to adding water at critical growth stages, ensuring early plant growth to promote root development for extracting soil water from the deeper profile later in the season should be a key strategy to take full advantage of limited irrigation.
机译:在美国南部大平原的半干旱地区,水的供应和分配是限制小麦(Triticum aestivum)产量的主要限制因素。为了管理作物的需水量,该地区通常实行有限灌溉(也称为赤字灌溉)。进行了为期4年的研究,以评估受限灌溉下冬小麦净水提取量(SWE)的深度和数量对冬小麦品种产量的影响。为了确定灌溉时间,我们考虑了关键的生长阶段(拔节,分er和花期)以及作物根部低于50%的土壤水分枯竭。在种植,拔节,开花和生理成熟时,以0.2 m的增量测量深度土壤中的水分含量为2.4 m。由于灌溉能力有限,季节性降水仍然是确定SWE的重要因素。 2011年是历史上的干旱季节之一,只有60毫米的季节性降水,该季节的净西南偏西地区仅限于高1.2 m剖面。相比之下,2016年季节更有利于作物生长,季节性降水量为315毫米,该季节的净西南偏西深度达到2.0 m。在生长季节,谷物单产主要受净SWE量的影响。对于谷物产量为4807 kg ha(-1)的小麦,净SWE为165 mm(2016)。但是,谷物产量为2933 kg ha(-1)的小麦仅提取了70 mm存储的土壤水(2011年)。就季节降水量,SWE和产量而言,2012年和2017年季节仍处于中间水平。尽管2011年和2016年季节在播种时储存的土壤水分相似,但2016年更多的早期季节和总降水量似乎使植物生长能够获取更深的水。相比之下,由于干旱和植物生长不良,2011赛季末大量未利用的土壤水被闲置。因此,除了在关键的生长阶段添加水以外,确保植物早生长以促进根系发育,以便在季节后期从较深的剖面中抽取土壤水,这应该是充分利用有限灌溉的一项关键策略。

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