{"title":"DEEP DRAINAGE ESTIMATES FOR IRRIGATED CROP ROTATIONS IN SUBHUMID, SUBTROPICAL AUSTRALIA","authors":"S. Kodur, J. B. Robinson, J. L. Foley, D. Silburn","doi":"10.1002/ird.1872","DOIUrl":null,"url":null,"abstract":"Deep drainage rates were modelled for irrigated crop rotations in terms of typical cropping sequences that differ in crop characteristics and irrigation demand. A forage–grain–pasture sequence (sorghum, wheat and lucerne) with supplementary irrigation had an average deep drainage of 11 mm yr−1, transpiration of 703 mm yr−1 and irrigation demand of 326 mm yr−1. In contrast, a vegetable sequence (broccoli, lettuce, bean and sweetcorn) with adequate irrigation had a deep drainage of 121 mm yr−1, transpiration of 602 mm yr−1 and irrigation demand of 598 mm yr−1. Under similar growing conditions, deep drainage decreased as rooting depth and cropping duration increased, and as irrigation and rainfall decreased. Deep‐rooted, stress‐ tolerant crops such as lucerne and sorghum maximised water use and minimised the deep drainage risks through the use of moisture from preceding well‐irrigated vegetable crops and extraction of moisture from deeper soil layers. The study suggests that deep drainage risks under vegetable rotations can be minimised through the selective incorporation of these crops and improved irrigation timing and application rates. These understandings will help to develop water use efficient and economic management strategies under crop rotations. Copyright © 2014 John Wiley & Sons, Ltd.","PeriodicalId":92799,"journal":{"name":"Irrigation and drainage (International Commission on Irrigation and Drainage)","volume":"12 4","pages":"692 - 697"},"PeriodicalIF":0.0000,"publicationDate":"2014-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1002/ird.1872","citationCount":"2","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Irrigation and drainage (International Commission on Irrigation and Drainage)","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1002/ird.1872","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 2
在半湿润,亚热带澳大利亚灌溉作物轮作的深排水估计
根据不同作物特性和灌溉需求的典型种植顺序,对灌溉作物轮作的深层排水速率进行了建模。补灌的牧草-谷物-牧草序列(高粱、小麦和苜蓿)平均深排水量为11 mm yr - 1,蒸腾量为703 mm yr - 1,灌溉需水量为326 mm yr - 1。相比之下,灌溉充足的蔬菜序列(西兰花、生菜、豆类和甜玉米)的深排水量为121 mm yr - 1,蒸腾量为602 mm yr - 1,灌溉需水量为598 mm yr - 1。在相同的生长条件下,随着生根深度和种植期的增加,以及灌溉和降雨量的减少,深排水减少。深根、耐胁迫的作物,如紫花苜蓿和高粱,通过利用以前灌溉良好的蔬菜作物的水分和从深层土壤中提取水分,最大限度地提高了水的利用率,并最大限度地降低了深层排水风险。研究表明,通过选择性地种植这些作物,改善灌溉时间和施用量,可以将蔬菜轮作的深层排水风险降到最低。这些理解将有助于在作物轮作下制定有效的水资源利用和经济管理战略。版权所有©2014 John Wiley & Sons, Ltd。
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