Post-anthesis water use and biomass accumulation in winter wheat under subsoiling and microsprinkler irrigation

IF 6.1 1区 农林科学 Q1 SOIL SCIENCE
Chao Huang , Yanyan Zhang , Xuchen Liu , Yang Gao , Shoutian Ma , Anzhen Qin , Ying Li , Qifeng Zhang , Zile Gao , Guanghui Wu , Kai Wang , Zhandong Liu
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Abstract

The advancement of agricultural mechanization has led to soil compaction and an increased thickness of the plow layer in the North China Plain. By contrast, subsoiling tillage can disrupt the plow layer, enhance the cultivation environment of the soil, and promote crop growth. Nevertheless, such changes in tillage methods often disrupt conventional irrigation systems, highlighting the need to explore alternative approaches. This study employed microsprinkler irrigation, a prevalent irrigation method in crop production, to evaluate how different irrigation regimes affect crop growth in subsoiled fields. Three irrigation lower limits are established in subsoil plots: 70 %FC (MS-H), 60 %FC (MS-M), and 50 %FC (MS-L). For comparison, the study included a 70 %FC surface irrigation treatment with subsoiling (ST) and a 70 %FC surface irrigation treatment without subsoiling (RT). Results indicated that subsoiling border irrigation (ST) increased topsoil moisture and water uptake in the 0–60-cm soil layer. This enhanced water availability led to greater overall water consumption during grain filling, a delayed post-anthesis biomass accumulation, and an extended grain-filling stage, ultimately contributing to increased grain yield. The MS-L treatment increased the utilization of deep soil water owing to lower topsoil water content. However, this limited biomass accumulation leads to early termination of post-anthesis biomass accumulation, a drop in the rate of grain filling, a reduction in the length of grain filling, and a decrease in grain weight. The MS-M treatment, which mainly absorbs water from the 0–30-cm soil layer, considerably increased deep soil water consumption and the duration of post-anthesis biomass accumulation, resulting in a 4.5-day extension of the grain-filling stage and a notable increase in grain weight. While MS-H maintained adequate topsoil moisture, its deep soil water consumption was lower than that of MS-M, resulting in shorter biomass accumulation and grain-filling duration, though still longer than ST, as well as a grain weight not notably different from that of MS-M. Comprehensive TOPSIS analysis identified MS-M as the optimal irrigation regime. Consequently, establishing a 60 % field capacity irrigation threshold for microsprinkler regimes in subsoiled wheat fields effectively promotes deep soil water absorption, boosts biomass accumulation following anthesis, and enhances grain filling, ultimately improving winter wheat yields.
底播和微喷灌条件下冬小麦的花后用水和生物量积累
农业机械化的发展导致华北平原土壤板结,犁层厚度增加。相比之下,深松耕作可以打破耕作层,改善土壤耕作环境,促进作物生长。然而,这种耕作方式的改变往往会破坏传统的灌溉系统,因此有必要探索其他方法。本研究利用微喷灌这种作物生产中普遍采用的灌溉方式,来评估不同灌溉制度对底土田作物生长的影响。在底土地块中设定了三个灌溉下限:70 %FC (MS-H)、60 %FC (MS-M) 和 50 %FC (MS-L)。为了进行比较,该研究还包括 70 %FC 的地表灌溉处理,同时进行底土翻耕(ST)和 70 %FC 的地表灌溉处理,同时不进行底土翻耕(RT)。结果表明,畦灌(ST)增加了表土湿度和 0-60 厘米土层的吸水率。水分供应量的增加导致谷物灌浆期总耗水量增加,花后生物量积累延迟,谷物灌浆期延长,最终导致谷物产量增加。由于表土含水量较低,MS-L 处理提高了土壤深层水分的利用率。然而,这种有限的生物量积累导致花后生物量积累提前结束,谷物灌浆速度下降,谷物灌浆期缩短,谷物重量减少。MS-M 处理主要吸收 0-30 厘米土层的水分,大大增加了土壤深层的耗水量和花后生物量积累的持续时间,使谷粒灌浆期延长了 4.5 天,谷粒重量明显增加。虽然 MS-H 保持了充足的表土水分,但其土壤深层耗水量低于 MS-M,导致生物量积累和谷粒饱满期缩短,但仍长于 ST,谷粒重量与 MS-M 没有明显差异。综合 TOPSIS 分析确定 MS-M 为最佳灌溉制度。因此,在底播麦田中为微喷灌制度设定 60% 的田间灌溉能力阈值,可有效促进土壤深层吸水,促进花后生物量积累,提高籽粒充实度,最终提高冬小麦产量。
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来源期刊
Soil & Tillage Research
Soil & Tillage Research 农林科学-土壤科学
CiteScore
13.00
自引率
6.20%
发文量
266
审稿时长
5 months
期刊介绍: Soil & Tillage Research examines the physical, chemical and biological changes in the soil caused by tillage and field traffic. Manuscripts will be considered on aspects of soil science, physics, technology, mechanization and applied engineering for a sustainable balance among productivity, environmental quality and profitability. The following are examples of suitable topics within the scope of the journal of Soil and Tillage Research: The agricultural and biosystems engineering associated with tillage (including no-tillage, reduced-tillage and direct drilling), irrigation and drainage, crops and crop rotations, fertilization, rehabilitation of mine spoils and processes used to modify soils. Soil change effects on establishment and yield of crops, growth of plants and roots, structure and erosion of soil, cycling of carbon and nutrients, greenhouse gas emissions, leaching, runoff and other processes that affect environmental quality. Characterization or modeling of tillage and field traffic responses, soil, climate, or topographic effects, soil deformation processes, tillage tools, traction devices, energy requirements, economics, surface and subsurface water quality effects, tillage effects on weed, pest and disease control, and their interactions.
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