School of Water Resources and Environment, MOE Key Laboratory of Groundwater Circulation and Environmental Evolution, China University of Geosciences (Beijing), Beijing, 100083, People's Republic of China.
The Key Laboratory of Orogenic Belts and Crustal Evolution, Beijing Key Laboratory of Mineral Environmental Function, School of Earth and Space Sciences, Peking University, Beijing, 100871, People's Republic of China.
Environ Res. 2024 Dec 15;263(Pt 3):120166. doi: 10.1016/j.envres.2024.120166. Epub 2024 Oct 16.
Nitrate pollution in groundwater is a global environmental issue that poses significant threats to human health and ecological security. This study focuses on elucidating the mechanisms of heterotrophic-autotrophic cooperative denitrification (HAD) by employing wheat straw and elemental sulfur as electron donors in varying proportions. The research initially underscores that heterotrophic denitrification (HD) accelerates the denitrification process due to its high-energy metabolism. However, as readily degradable organic matter diminished, reliance on more complex substrates such as lignocellulose posed a challenge to HD. This marks a pivotal transition towards autotrophic denitrification (AD), which, despite a slower initial rate, exhibits a more sustained denitrification performance. A low proportion of heterotrophic denitrification layer (e.g., 3:1) at the bottom facilitating efficient and sustainable denitrification. HD is capable of simultaneous removal of nitrates and nitrites, whereas AD demonstrates a higher affinity for nitrates, with nitrite accumulation reaching 100% at high influent nitrate concentrations (100 mg/L). HD not only provides the necessary alkaline environment for AD but also reduces sulfate production, whereas AD utilizes the residual organic carbon and ammonia produced by HD. The heterotrophic layer is characterized by a diverse community, whereas the autotrophic layer is predominantly composed of Thiobacillus. By delineating the interactive mechanisms and characteristics of HAD, this study highlights the importance of balancing heterotrophic and autotrophic activities for the effective remediation of groundwater nitrates.
地下水硝酸盐污染是一个全球性的环境问题,对人类健康和生态安全构成了重大威胁。本研究重点探讨了以小麦秸秆和单质硫为电子供体,按不同比例组合时异养-自养协同反硝化(HAD)的作用机制。研究首先强调了异养反硝化(HD)由于其高能量代谢而加速反硝化过程。然而,随着易降解有机物质的减少,依赖更复杂的底物(如木质纤维素)对 HD 提出了挑战。这标志着向自养反硝化(AD)的关键转变,尽管初始速率较慢,但 AD 表现出更持续的反硝化性能。底部异养反硝化层(例如 3:1)的低比例有利于高效和可持续的反硝化。HD 能够同时去除硝酸盐和亚硝酸盐,而 AD 对硝酸盐具有更高的亲和力,在高进水硝酸盐浓度(100mg/L)下,亚硝酸盐积累达到 100%。HD 不仅为 AD 提供必要的碱性环境,还减少了硫酸盐的产生,而 AD 则利用 HD 产生的残余有机碳和氨。异养层具有多样化的群落,而自养层主要由硫杆菌组成。通过描述 HAD 的相互作用机制和特性,本研究强调了平衡异养和自养活动对于有效修复地下水中硝酸盐的重要性。