She Yingjun, Li Ping, Qi Xuebin, Rahman Shafeeq Ur, Guo Wei
Farmland Irrigation Research Institute, Chinese Academy of Agricultural Sciences, Xinxiang, Henan, China.
Graduate School of Chinese Academy of Agricultural Sciences, Beijing, China.
Front Plant Sci. 2023 Mar 7;14:1114611. doi: 10.3389/fpls.2023.1114611. eCollection 2023.
Shallow groundwater plays a vital role in physiology morphological attributes, water use, and yield production of winter wheat, but little is known of its interaction with nitrogen (N) application. We aimed to explore the effects of N fertilization rate and shallow groundwater table depth (WTD) on winter wheat growth attributes, yield, and water use. Experiments were carried out in micro-lysimeters at WTD of 0.6, 0.9, 1.2, and 1.5 m with 0, 150, 240, and 300 kg/ha N application levels for the winter wheat ( L.). The results showed that there was an optimum groundwater table depth (Op-wtd), in which the growth attributes, groundwater consumption (GC), yield, and water use efficiency (WUE) under each N application rate were maximum, and the Op-wtd decreased with the increase in N application. The Op-wtd corresponding to the higher velocity of groundwater consumption (Gv) appeared at the late jointing stage, which was significantly higher than other WTD treatments under the same N fertilization. WTD significantly affected the Gv during the seeding to the regreening stage and maturity stage; the interaction of N application, WTD, and N application was significant from the jointing to the filling stage. The GC, leaf area index (LAI), and yield increased with an increase of N application at 0.6-0.9-m depth-for example, the yield and the WUE of the NF300 treatment with 0.6-m depth were significantly higher than those of the NF150-NF240 treatment at 20.51%, and 14.81%, respectively. At 1.2-1.5-m depth, the N application amount exceeding 150-240 kg/ha was not conducive to wheat growth, groundwater use, grain yield, and WUE. The yield and the WUE of 150-kg/ha treatment were 15.02% and 10.67% higher than those of 240-300-kg/ha treatment at 1.2-m depth significantly. The optimum N application rate corresponding to yield indicated a tendency to decrease with the WTD increase. Considering the winter wheat growth attributes, GC, yield, and WUE, application of 150-240 kg/ha N was recommended in our experiment.
浅层地下水对冬小麦的生理形态特征、水分利用及产量形成起着至关重要的作用,但关于其与施氮量之间的相互作用却知之甚少。我们旨在探究施氮量和浅层地下水位深度(WTD)对冬小麦生长特征、产量及水分利用的影响。针对冬小麦(品种未提及),在地下水位深度分别为0.6、0.9、1.2和1.5米的微型蒸渗仪中开展试验,施氮水平分别为0、150、240和300千克/公顷。结果表明,存在一个最佳地下水位深度(Op-wtd),在此深度下,各施氮量水平下的生长特征、地下水消耗量(GC)、产量及水分利用效率(WUE)均达到最大值,且Op-wtd随施氮量增加而降低。在拔节后期出现了对应地下水消耗速度(Gv)较高的Op-wtd,在相同施氮条件下,该深度显著高于其他WTD处理。在播种至返青期和成熟期,WTD对Gv有显著影响;从拔节期到灌浆期,施氮量、WTD及其交互作用显著。在0.6 - 0.9米深度,GC、叶面积指数(LAI)和产量随施氮量增加而增加,例如,0.6米深度的NF300处理的产量和WUE分别比NF150 - NF240处理显著高出20.51%和14.81%。在1.2 - 1.5米深度,施氮量超过150 - 240千克/公顷不利于小麦生长、地下水利用、籽粒产量及WUE。在1.2米深度,150千克/公顷处理的产量和WUE分别比240 - 300千克/公顷处理显著高出15.02%和10.67%。对应产量的最佳施氮量呈现出随WTD增加而降低的趋势。综合考虑冬小麦生长特征、GC、产量及WUE,本试验推荐施氮量为150 - 240千克/公顷。