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Responses of Grain Sorghum to Varying Irrigation Frequency in the Ord Irrigation Area. PI* Evapotranspiration, Water Use Efficiency and Root Distribution of Different Cultivars

机译:Ord灌区谷物高粱对不同灌溉频率的响应。不同品种的PI *蒸散量,水分利用效率和根系分布

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摘要

Four grain sorghum cultivars (Quicksilver, Texas 610SR, E57 and Q7844), representing early-to-late nmaturity types, were grown under different irrigation frequencies (7-day, 14-day, 28-day or 42-day nintervals or once-only-at-sowing) in the dry season in the Ord Irrigation Area. Soil water distribution, nroot distribution and evapotranspiration were determined periodically. nFrequent irrigation resulted in shallow root development and most water use was from the surface n40 cm of soil. Depth of water extraction increased with plant age and with less frequent irrigation. The ndepth of root penetration determined by direct measurement was similar to that inferred from soil water nprofiles. Water uptake per unit length of root was related to soil water content only in the 0-40 cm soil nlayers. E,/Ep (actual evapotranspiration/pan evaporation) was classified into three stages according to nthe degree of soil drying after irrigation. During the first stage, immediately after irrigation, EJEp was ngenerally close to 0.75 irrespective of cultivar, leaf area index (LAI) or irrigation interval. During the nsecond stage, linear functions adequately described E,/E, as a function of LA1 for LA1 less than 5. nDuring the third stage, which commenced when total soil water to 1.8 m declined to 545 mm, poor nrelationships between EJE, and soil water were observed. nFollowing an analysis of the soil water use data, it is believed that maximum yields of sorghum may nbe attainable with irrigation at sowing followed by three carefully timed irrigations.
机译:在不同灌溉频率下(分别是7天,14天,28天或42天间隔或一次间隔),种植了代表早至晚期成熟度类型的四种谷物高粱品种(Quicksilver,Texas 610SR,E57和Q7844)。仅在Ord灌溉区的旱季播种)。定期确定土壤水分分布,根系分布和蒸散量。 n频繁灌溉导致根系发育较浅,大部分用水来自土壤40厘米处。抽水深度随植物年龄和灌溉频率的降低而增加。通过直接测量确定的根部渗透深度与从土壤水分剖面中推断的深度相似。单位长度的根部吸水仅与0-40 cm的土壤层中的土壤水分有关。根据灌溉后土壤干燥的程度,E / Ep(实际蒸散/蒸发皿蒸发)分为三个阶段。在第一阶段,灌水后,无论品种,叶面积指数(LAI)或灌水间隔如何,EJEp通常都接近0.75。在第二阶段中,线性函数充分描述了E,/ E,对于LA1小于5而言,它是LA1的函数。n在第三阶段,即当土壤总水量降至1.8 m降至545 mm时开始,EJE之间的相关性很差,并且观察土壤水。 n在对土壤水分利用数据进行分析之后,据信在播种后再进行三个精心安排的灌溉,可能无法达到高粱的最大产量。

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    《Crop and Pasture Science》 |1984年第1期|p.31-42|共12页
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    Division of Tropical Crops and Pastures, CSIRO, Cunningham Laboratory, 306 Carmody Road, St Lucia, Qld 4067. Division of Tropical Crops and Pastures, CSIRO, Cooper Laboratory and Field Station, Lawes, Qld 4345. Division of Tropical Crops and Pastures, CSIRO, Charles Darwin Laboratories, Private Bag No. 44, Winnellie, N.T. 5789. .;

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