外源复合有机酸对酸性土壤水稻硒吸收积累的调控效应

Regulatory effects of exogenous combined organic acid on selenium uptake and accumulation in rice under acidic soil conditions

  • 摘要: 鉴于酸性土壤中有机酸活化硒的研究相对匮乏, 本研究采用盆栽试验研究了酸性土壤条件下添加外源复合有机酸对水稻硒的吸收转运及土壤性质的影响机制, 为富硒大米生产提供技术支撑。本研究共设4个处理, 分别为不添加有机酸处理(CK), 0.23 mg∙kg–1复合有机酸处理(LOA), 1.14 mg∙kg–1复合有机酸处理(MOA)和2.28 mg∙kg–1复合有机酸处理(HOA)。结果表明, 等量施硒0.5 mg(Se)∙kg–1条件下, 不同用量复合有机酸添加处理与对照的籽粒产量和地上部生物量均无显著差异, 但LOA和MOA处理较对照显著提高水稻籽粒中硒含量和水稻整株硒的累积量, 增幅分别为28.7%、27.3%和40.1%、34.1%, 而HOA处理较对照显著降低了水稻茎中硒含量和累积量, 降幅分别为23.5%和46.7%。此外, 复合有机酸处理显著增加了根际土壤有效磷含量和非根际土壤有效硒含量, 降低了根际与非根际土壤中有效硫含量, 提高植株根系过氧化氢酶(CAT)和过氧化物酶(POD)活性, 尤其在MOA处理下土壤脲酶活性显著提高。LOA处理降低了根系活动对高岭石矿物的溶解作用, 而HOA处理促进了根系活动对高岭石矿物的溶解作用。主成分分析表明, 土壤脲酶活性和根系CAT活性对植株硒的吸收积累具有重要贡献。综上, 外源添加0.23~1.14 mg∙kg–1复合有机酸能改善土壤硒的有效性, 促进水稻对硒的吸收, 提高水稻根系CAT和POD活性, 并显著增加水稻植株各部位硒含量及植株硒累积量(177.2~185.2 μg∙株–1), 但高添加量复合有机酸(2.28 mg∙kg–1)则抑制硒从根系向地上部中的转运, 该结果为酸性土壤背景下富硒大米生产提供重要的技术支撑。

     

    Abstract: Given the scarcity research on the activation of selenium (Se) by organic acids in acidic soils, a pot experiment was conducted to investigate the effects of different amounts of exogenous compound organic acids (COA) on the uptake and transport of Se in rice as well as soil properties under acidic soil conditions, providing technical support for the production of Se-enriched rice. This study consisted of four treatments: 0 COA (CK), 0.23 mg∙kg–1 COA (LOA), 1.14 mg∙kg–1 COA (MOA), and 2.28 mg∙kg–1 COA (HOA). The results showed no significant difference in grain yield or aboveground biomass of rice between CK and COA treatments under the equal application of Se 0.5 mg(Se)∙kg–1. However, LOA and MOA treatments significantly increased the Se content in rice grains by 28.7% and 27.3% and the accumulative amount of Se in the whole plant by 40.1% and 34.1%, respectively, compared with CK. In contrast, the HOA treatment significantly decreased the Se content and accumulation in rice stems compared with CK, with reductions of 23.5% and 46.7%, respectively. The data indicated that the LOA and MOA treatments effectively enhanced Se uptake and transport, while the HOA treatment inhibited the transport of Se from the roots to stems. Additionally, the COA treatments significantly increased the available phosphorus content in the rhizosphere soil and the available Se content in the non-rhizosphere soil, decreased the available sulfur content in both the rhizosphere and non-rhizosphere soils, and enhanced the activities of catalase (CAT) and peroxidase (POD) in the roots. Particularly, the MOA treatment significantly increased soil urease activity (UE). The LOA treatment reduced the dissolution effect of root activities on kaolinite minerals, while the HOA treatment exerted a promoting effect. Principal component analysis indicated that soil UE activity and root CAT activity made significant contributions to the uptake and accumulation of Se in plants. In conclusion, exogenous addition of 0.23–1.14 mg∙kg–1 COA can improve the availability of soil Se, enhance the activities of CAT and POD in rice roots, and significantly increase the Se content in various parts of rice (2.52–8.56 mg∙kg–1) and the Se accumulation in plants (177.2–185.2 μg∙plant–1). This study provides new ideas and approaches for enhancing the Se content in rice grains and has important theoretical and practical significance for meeting the human need for Se.

     

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