湘南稻田土壤-稻米系统中硒的含量与富硒机制

Contents of Selenium and Its Enrichment Mechanism in the Paddy Soil-Rice System in Southern Hunan.

  • 摘要:
    目的 弄清稻田土壤-稻米系统中硒的含量与富集规律及其相互关系的作用机制,高效利用和挖潜土壤硒资源和开发富硒农产品。
    方法 采集湘南地区24278组稻田土壤-稻米对应样品,测定了土壤全硒、有机质、阳离子交换量、pH、全铜、全锌与稻米全硒、全铜与全锌含量,通过普通克里金插值、极端梯度提升模型与Shaply加性解释、相关性分析等方法,分析了成土母质、土壤特性、气候因素(日照时数,降水量)与土壤硒、稻米硒的关系。
    结果 湘南地区土壤硒平均含量为0.514 mg kg−1,稻米硒平均为0.053 mg kg−1,富集系数平均为0.118,表明该地区土壤硒含量较高,富硒水稻资源丰富。土壤硒的空间分布呈现中、南部高,东、西和北部低的特征,稻米硒含量分布与土壤硒高度吻合,富集系数自西南向东北呈带状分布特征。成土母质对土壤、稻米硒含量和富集系数(P < 0.05)有显著影响;土壤硒含量与有机质、土壤铜、锌含量呈极显著正相关(P < 0.01),与pH、稻米铜呈显著负相关关系(P < 0.05);稻米硒含量与土壤铜、稻米铜和稻米锌呈极显著正相关(P < 0.01),而与土壤有机质和阳离子交换量显著呈极显著负相关(P < 0.01);富集系数与稻米铜、稻米锌呈极显著正相关关系(P < 0.01),而与土壤有机质、铜呈极显著负相关关系(P < 0.01)。XGBoost模型预测显示,土壤锌和有机质是影响土壤硒含量的关键因素;稻米铜对稻米硒含量影响最大;土壤有机质和稻米铜对富集系数的影响较大。
    结论 湘南地区稻田土壤硒资源丰富,稻米富硒能力较强,可采取提升土壤有机质含量、改善土壤阳离子交换量和调控pH的农艺栽培措施,进一步合理和科学开发富硒农产品。

     

    Abstract:
    Objective The aims were to clarify the contents and enrichment patterns of selenium (Se) in the paddy soil-rice system, as well as their interrelationship mechanisms, is of great significance for the efficient utilization and potential development of soil Se resources and the development of Se-rich agricultural products.
    Method This paper collected 24,278 sets of corresponding paddy soil-rice samples from the southern Hunan region, and measured the total Se, organic matter, cation exchange capacity, pH, total copper, and total zinc in the soil, as well as the total Se, total copper, and total zinc in the rice. Through ordinary kriging interpolation, extreme gradient boosting model and Shapley additive explanation, correlation analysis and other methods, the relationships between parent material, soil properties, climatic factors (sunshine duration, precipitation) and soil Se and rice Se were analyzed.
    Result The average Se content in the soil of southern Hunan was 0.514 mg kg−1, and the average Se content in rice was 0.053 mg kg−1, with an average enrichment coefficient of 0.118, indicating that the region had high soil Se content and abundant Se rice resources. The spatial distribution of soil Se showed a pattern of being high in the middle and southern parts, and low in the eastern, western and northern parts. The distribution of rice Se content was highly consistent with that of soil Se, and the enrichment coefficient showed a belt-like distribution from the southwest to the northeast. Parent material had a significant effect on the Se content and enrichment coefficient of soil and rice (P < 0.05). The soil Se content was extremely significantly positively correlated with organic matter, soil copper and zinc content (P < 0.01), and significantly negatively correlated with pH and rice copper (P < 0.05). The rice Se content was extremely significantly positively correlated with soil copper, rice copper and rice zinc (P < 0.01), and extremely significantly negatively correlated with soil organic matter and cation exchange capacity (P < 0.01). The enrichment coefficient was extremely significantly positively correlated with rice copper and rice zinc (P < 0.01), and extremely significantly negatively correlated with soil organic matter and copper (P < 0.01). The XGBoost model prediction showed that soil zinc and organic matter were key factors affecting the soil Se content. Rice copper had the greatest impact on the rice selenium content. Soil organic matter and rice copper had a greater impact on the enrichment coefficient.
    Conclusion The paddy soil Se resources in southern Hunan are abundant, and the rice's selenium-enriching ability is strong. Agronomic cultivation measures such as improving soil organic matter, cation exchange capacity and pH can be taken to further develop selenium-rich agricultural products in a reasonable and scientific way.

     

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