Optimizing evapotranspiration and crop irrigation requirements of tropical forages cropping systems in Southern Brazil

IF 3 3区 地球科学 Q2 BIOPHYSICS
Ivo Z. Gonçalves, Fernando C. Mendonça, Arthur C. Sanches, Fábio R. Marin
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Abstract

Crop irrigation requirements are usually estimated based on crop evapotranspiration (ETc) as determined by the reference evapotranspiration (ETo) and crop coefficient (Kc). There is a lack of knowledge on the irrigation requirements of tropical forage crops in Brazil, contrasting with the increasing use of irrigation in pastures. The effort of this study was to investigate what would be the water needs of tropical forages in Southern Brazil, based on a robust experimental database. The study was carried out in São Paulo State-Brazil using different forages species and their combinations [Guinea grass (GG); Guinea grass + black oat + ryegrass (GOR); Bermuda grass (BG), and Bermuda + black oat + ryegrass (BOR)]. The experimental fields were fully irrigated, and the Kc values were derived from ETc measurements on lysimeters; ETo was estimated using daily data from a nearby weather station and the standard FAO56 parameterization. Mean daily ETc values for GG, GOR, BG and BOR were 4.1, 2.9, 3.6, and 3.4 mm, respectively, and respective mean Kc values were 0.99, 0.90, 1.0, and 0.94. Average Kc values for all plots decreased as ETo increased, producing a negative Kc-ETo relationship, mainly when ETo reached values greater than 5 mm d−1. This was most likely due to internal plant stomatal resistance to vapor release from the leaves diffusing to the atmosphere at high ETo. So, the time-based Kc curves described by FAO 56 manual should be adjusted for the analyzed crops considering different ranges of ETo to improve the required irrigation depth.

Abstract Image

优化巴西南部热带牧草种植系统的蒸散和作物灌溉需求。
作物灌溉需求通常根据参考蒸散量(ETo)和作物系数(Kc)确定的作物蒸发量(ETc)进行估计。与牧场日益使用灌溉相比,巴西对热带牧草的灌溉需求缺乏了解。这项研究的目的是基于一个强大的实验数据库,调查巴西南部热带牧草的用水需求。这项研究是在巴西圣保罗州进行的,使用了不同的牧草物种及其组合[几内亚草(GG);几内亚草 + 黑燕麦 + 黑麦草;百慕大草(BG)和百慕大 + 黑燕麦 + 黑麦草(BOR)]。试验田被完全灌溉,Kc值是从蒸渗仪上的ETc测量中得出的;ETo是使用附近气象站的每日数据和标准的FAO56参数化进行估计的。GG、GOR、BG和BOR的日平均ETc值分别为4.1、2.9、3.6和3.4 mm,Kc值的平均值分别为0.99、0.90、1.0和0.94。所有地块的平均Kc值随着ETo的增加而降低,产生负的Kc-ETo关系,主要是当ETo达到大于5 mm d-1的值时。这很可能是由于植物内部气孔对高ETo下叶片向大气扩散的蒸汽释放的抵抗力。因此,应根据ETo的不同范围,对FAO 56手册中描述的基于时间的Kc曲线进行调整,以提高所需的灌溉深度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
6.40
自引率
9.40%
发文量
183
审稿时长
1 months
期刊介绍: The Journal publishes original research papers, review articles and short communications on studies examining the interactions between living organisms and factors of the natural and artificial atmospheric environment. Living organisms extend from single cell organisms, to plants and animals, including humans. The atmospheric environment includes climate and weather, electromagnetic radiation, and chemical and biological pollutants. The journal embraces basic and applied research and practical aspects such as living conditions, agriculture, forestry, and health. The journal is published for the International Society of Biometeorology, and most membership categories include a subscription to the Journal.
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