圣保罗州Jales和Andradina微区大豆作物水分亏缺的空间性

IF 0.2 Q4 AGRONOMY
K. Assis, Maria Clara Lelles Moreira Begueline, João Victor Costa, F. Hernandez
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引用次数: 0

摘要

了解未来规划的土壤水分有效性是合理利用土壤水分的基础。本工作旨在研究Jales SP和Andradina SP微区夏季收获大豆种植中的降水量、作物蒸散量和水分补充需求的空间性。水平衡是通过Thortwaite和Mather(1955)方法确定的,数据由联合国教科文组织Ilha Solteira水利和灌溉区运营的农业气象站网络提供。我们考虑了40毫米的可用水量(AWC)。这项研究是通过模拟2020年11月4日播种的大豆作物的水分状况进行的。在缺水条件下,实际蒸散量(ETa)在缺水20%时被认为是零的,其他值遵循相同的数学比例。利用ArcGIS 10.7软件中的普通循环克里格法对各气象站的同期平均降雨量、作物蒸散量和缺水量进行插值。圣保罗西北地区大豆作物缺水与周期内降水分布不均以及整个地区印度夏季的显著重现有关。为了生产商的安全,对灌溉系统的投资是合理的,预计这种分配会很差。该地区的缺水情况是可变的。在降雨量分布良好的年份,它可以达到零值,在分布较差的年份,可以达到大于180毫米的值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The spatiality of the soybean crop water deficit in Jales and Andradina microregions, state of São Paulo
Knowledge about soil water availability for future planning is the basis for carrying out its rational use. This work aimed to study the spatiality of water precipitation, crop evapotranspiration, and the need for water supplementation in soybean cultivation in the microregions of Jales-SP and Andradina-SP for the summer harvest. The water balance was determined by the Thorthwaite and Mather (1955) method, with data made available by the Agrometeorological Stations Network operated by the Hydraulics and Irrigation area of UNESP Ilha Solteira. We considered an available water capacity (AWC) of 40 mm. The study took place from the simulation of the water condition of a soybean crop sown on November 4, 2020. In the water deficit condition, the actual evapotranspiration (ETa) was considered null at a 20 % deficit, and the other values followed the same mathematical proportion. The mean rainfall of the period, crop evapotranspiration, and water deficit of each weather station were interpolated through ordinary circular kriging in ArcGIS 10.7 software. The water deficit in the soybean crop in the northwest region of São Paulo is related to the poor distribution of precipitation during the cycle and the significant recurrence of Indian summers all through the area. For the producers’ safety, investment in irrigation systems anticipating this poor distribution is justified. The water deficit in the region is variable. In years with good rainfall distribution, it can reach zero values, and in years with poor distribution, it can reach values greater than 180 mm.
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