文献类型： 外文期刊

作者： Gao, Xiaoyu ¹ ; Tang, Pengcheng ² ; Wang, Ziwei ² ; Yao, Yutao ³ ; Qu, Zhongyi ¹ ; Yang, Wei ¹ ; Du, Bin ⁴ ;

作者机构： 1.Inner Mongolia Agr Univ, Water Conservancy & Civil Engn Coll, Hohhot 010018, Peoples R China

2.China Inst Water Resources & Hydropower Res, Inst Water Resources Pastoral Area, Hohhot 010020, Peoples R China

3.Hebei Acad Agr & Forestry Sci, Coastal Agr Inst, Tangshan 063200, Peoples R China

4.Ningxia Inst Water Resources Res, Yinchuan 750021, Peoples R China

关键词： crop coefficient; soil water balance; sunflower; hydrological year; water-saving environment

期刊名称：WATER （ 影响因子：3.4； 五年影响因子：3.5 ）

ISSN：

年卷期： 2024 年 16 卷 2 期

页码：

收录情况： SCI

摘要： An accurate assessment of crop water requirements during the crop growth period can help organize irrigation schedules and investigate the hydrological environments in irrigation districts, especially in shallow groundwater districts. In irrigation scheduling, crop coefficients, representing three development stages, play a critical role in modeling evapotranspiration. Therefore, in this study, the crop coefficient (Kc) of sunflowers under drip irrigation in different hydrological years in the Hetao irrigation district with shallow groundwater is determined. Based on the analysis of rainfall frequency, the experimental situations of 2012, 2013, and 2014 are adopted as high, normal, and low flow years. Using the water balance method, groundwater recharge and crop evapotranspiration in different hydrological years were investigated. The results showed that the groundwater recharge in a high-flow year was larger than that in normal and low-flow years with values of 67.47, 66.75, and 42.61 mm, respectively. Crop evapotranspiration is directly related to the irrigation amount at the same growth stage. The Kc of sunflowers in a high-flow year is higher by 0.1 and 0.15 than that in normal and low-flow years. The Kc of sunflowers under drip irrigation is lower than that under surface irrigation by 8.9% in the initial and late stages of sunflower growth, but higher than that by 10.6% in the mid-stage, which is due to differences in small water potential differences and less evapotranspiration in the initial and late stages under drip irrigation. The study is of great significance for formulating a reasonable schedule of drip irrigation with shallow groundwater and improving the field environment.