硫酸盐还原菌修复煤矿高硫酸盐矿井水的缓释碳源筛选实验研究

An experimental study on the selection of slow-release carbon source materials for sulfate-reducing bacteria-based remediation of high-sulfate mine water in coal mines

  • 摘要:
    背景 高硫酸盐矿井水是我国煤矿区面临的主要水环境问题,其经济高效治理是矿业可持续发展的迫切需求。硫酸盐还原菌(SRB)生物修复法前景广阔,但其效能受矿井水中溶解性有机碳匮乏的限制。
    方法 针对SRB的外加缓释碳源材料初期有机物释放量可能过多、溶解性有机质(DOM)释放机理不明确和利用速率定量化困难等问题,对甘蔗渣、玉米芯和木屑3种缓释碳源进行浸泡释碳动力学和SRB利用性实验,对其释碳规律、DOM释放机理和SRB利用性进行探究。
    结果和讨论 结果表明,3种材料的释碳过程均符合二级动力学方程和Ritger−Peppas方程,0~8 h为快速释碳期,8~120 h为缓慢释碳期。120 h内甘蔗渣、玉米芯和木屑的累计释碳量分别为218.44、77.72、39.87 mg/(g·L)。三维荧光光谱表明,甘蔗渣释放的DOM大多为类富里酸和类胡敏酸,分子量较大。玉米芯和木屑释放的大多为类色氨酸、类酪氨酸和微生物降解产物,微生物利用性更好。SRB利用甘蔗渣、玉米芯和木屑处理降解\mathrmSO_4^2- 的酶促速率分别为3.88、3.21、2.67 mmol/(L·d)。因此,玉米芯释碳能力适中且酶促速率也较好,最适合作为缓释碳源材料。研究成果相关结论可以为生物碳源材料筛选和高硫酸盐矿井水的微生物修复提供理论依据。

     

    Abstract:
    Background High-sulfate mine water poses a major aquatic environmental challenge in coal mining areas across China. Accordingly, the cost-effective and efficient treatment of such water has become an urgent need for the sustainable development of the mining industry. Despite its considerable promise, microbial remediation based on sulfate-reducing bacteria (SRB) shows limited efficiency due to the scarcity of dissolved organic carbon (DOC) in mine water.
    Methods The application of external slow-release carbon source (SRC) materials for SRB faces a range of challenges, such as the potentially excessive release of organic carbon in the initial stage, the unclear release mechanisms of dissolved organic matter (DOM), and the difficulty of quantifying the utilization rate of SRB. To address these issues, this study conducted experiments on three SRC materials (i.e., bagasse, corncob, and sawdust), involving their carbon release kinetics under soaking and availability for SRB. Accordingly, the carbon release patterns, DOM release mechanisms, and availability for SRB of the three SRC materials were explored.
    Results and Conclusions The results indicate that the carbon release processes of the three SRC materials all followed the second-order kinetic and Ritger-Peppas equations, with rapid release occurring within 0‒8 h, followed by slow release from 8 h to 120 h. The cumulative carbon release amounts within 120 h of bagasse, corncob, and sawdust were determined at 218.44 mg/(g·L), 77.72 mg/(g·L), and 39.87 mg/(g·L), respectively. Three-dimensional excitation-emission matrix (3D-EEM) fluorescence spectra indicate that the DOM released from bagasse was dominated by fulvic-like and humic-like acids, characterized by high molecular weights. In contrast, the DOM released from corncob and sawdust consisted primarily of tryptophan-like and tyrosine-like compounds, along with products from microbial degradation, suggesting better bioavailability. Facilitated by bagasse, corncob, and sawdust, the SRB exhibited enzymatic rates for \mathrmSO_4^2- degradation of 3.88 mmol/(L·d), 3.21 mmol/(L·d), and 2.67 mmol/(L·d), respectively. Therefore, corncob exhibited appropriate carbon release capacity and high enzymatic rate, establishing it as the most suitable SRC material. The results of this study can provide a theoretical basis for both the selection of SRC materials and the microbial remediation of high-sulfate mine water.

     

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