Global warming-induced drought threatens the micronutrient quality of agricultural products, as water availability governs nutrient translocation and partitioning within plants. However, the effects of supplemental irrigation on wheat micronutrient dynamics under warming conditions remain poorly characterised. Here, a 3-year field experiment was conducted to investigate the effects of warming treatments (CK: ambient temperature; WS: winter-spring warming; FF: flowering-grain filling warming) and irrigation regimes (CI: conventional irrigation; SI: supplemental irrigation) on metal micronutrients (Fe, Mn, Cu, and Zn) in winter wheat and their driving factors. Results showed that warming slightly increased grain Fe, Mn, and Zn concentrations (0.3–5.8 %) but reduced their total accumulations (17.1–34.6 %). Compared to CK, FF decreased soil available micronutrients (9–35.7 %), with Fe and Zn availability strongly correlated with microbial taxa (Chloroflexi, Proteobacteria, and Firmicutes). SI increased grain Fe (3.1 %) and Zn (7.1 %) concentrations, enhanced total micronutrient uptake (6.8–22.6 %), and elevated soil-available micronutrients (6.2–25.8 %) relative to CI. Structural equation modelling revealed that soil temperature, moisture, pH, nutrients, available micronutrients, and microbiota jointly regulated grain micronutrients through direct pathways, with microbes being a key driver (total direct effect value = 0.619, p < 0.001). We conclude that supplemental irrigation effectively mitigates warming-induced micronutrient depletion, whereas the soil microbiota plays a pivotal role in mediating wheat micronutrient acquisition. These findings advance adaptive strategies to safeguard crop nutritional security under changing climate conditions.
扫码关注我们
求助内容:
应助结果提醒方式:
