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    石灰性土壤-小麦系统中铜的迁移、分配与累积健康风险评估

    Copper transport, distribution, accumulation and health risk assessment in the calcareous soil–wheat system

    • 摘要:
      研究目的 铜是维持动植物正常生命活动不可或缺的微量元素之一,在光合作用、抗氧化防御及能量代谢等关键生理过程中发挥着核心作用。华北平原石灰性土壤的高pH值与碳酸钙组分强烈抑制铜的生物有效性,制约小麦产量与品质并提示潜在膳食风险。本研究通过开展对照试验,系统揭示铜在土壤-小麦系统中的转运分配机制,评估籽实累积的健康风险,为安全生产与精准调控提供理论依据。
      研究方法 以小麦“石新828”为供试材料,设置0~3.6 mg/kg铜浓度梯度开展盆栽试验,测定不同生育期土壤与植株各部位铜含量,结合富集系数、转运系数及相关性分析,阐明铜的迁移分配规律。
      研究结果 石灰性土壤(pH 8.48)对铜具有强烈固持作用。拔节期铜主要向叶片富集,成熟期转为根系主导的储存模式,根系铜含量从8.7 mg/kg升至12.9 mg/kg,富集系数从0.36升至0.56,转运系数从2.11降至1.01。籽实铜含量稳定在5.5~7.7 mg/kg,低于国家限量标准(10 mg/kg),但在3.6 mg/kg外源铜处理下膳食摄入量达成人可耐受最高摄入量的10.4%。相关分析表明土壤有效铜与籽实铜含量呈显著正相关(r=0.457,p<0.01)。
      结论 石灰性土壤-小麦系统中,土壤化学固定与根系生理屏障共同构建了保障籽实铜安全的双重机制。小麦通过生育期特异的分配策略,在生殖生长阶段显著抑制铜向籽实的转运。建议高铜背景区严格控制外源铜输入以规避风险,低铜区实施精准施肥以发挥铜的营养强化潜力。

       

      Abstract:
      This paper is the result of agricultural geological survey engineering.
      Objective Copper (Cu) is an essential micronutrient for plants and animals, playing a central role in key physiological processes such as photosynthesis, antioxidant defense, and energy metabolism. In the North China Plain, the high pH and calcium carbonate content of calcareous soils strongly inhibit the bioavailability of Cu, constraining wheat yield and quality while posing potential dietary risks. This study aimed to systematically elucidate the transport and partitioning mechanisms of Cu in the soil-wheat system and assess the health risks associated with its accumulation in grains, thereby providing a theoretical basis for safe production and precision management.
      Methods A pot experiment was conducted using the wheat cultivar "Shixin 828" exposed to a gradient of exogenous Cu concentrations (0–3.6 mg/kg). The transport processes of Cu were systematically investigated by measuring its concentrations in soil and various plant tissues at different growth stages. The mechanisms governing Cu migration and partitioning were elucidated using bioconcentration factors, translocation factors, and correlation analyses.
      Results The alkaline calcareous soil (pH 8.48) exhibited a strong immobilizing effect on Cu, significantly inhibiting its bioavailability. The allocation of Cu in wheat varied markedly between growth stages: at jointing, Cu was primarily enriched in leaves, whereas at maturity, it shifted to a root-dominated sequestration pattern. The Cu concentration in roots increased from 8.7 mg/kg at jointing to 12.9 mg/kg at maturity, with the bioconcentration factor rising from 0.36 to 0.56, while the translocation factor decreased from 2.11 to 1.01. The Cu concentration in grains remained stable within the range of 5.5–7.7 mg/kg, below the national food safety limit (10 mg/kg). However, under the 3.6 mg/kg exogenous Cu treatment, dietary intake reached 10.4% of the Tolerable Upper Intake Level for adults. Correlation analysis revealed a significant positive relationship between soil available Cu and grain Cu concentration (r=0.457, p<0.01).
      Conclusions In the calcareous soil-wheat system, soil chemical immobilization and root physiological barriers synergistically form a dual mechanism safeguarding grain Cu safety. Wheat employs growth-stage-specific allocation strategies, significantly inhibiting Cu translocation to grains during the reproductive stage. Based on these findings, we recommend strictly controlling exogenous Cu inputs in high-background areas to mitigate risks, while implementing precision fertilization in low-background areas to harness the potential of Cu for nutritional biofortification.

       

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