Ning Yihong, Gao Bin, Wang Haiyan, Hou Wenning
State Key Laboratory of Efficient Production of Forest Resources, Key Laboratory of Forest Cultivation and Protection, Ministry of Education, College of Forestry, Beijing Forestry University, Beijing, China.
College of Smart Urban Construction, Guangzhou City Polytechnic, Guangzhou, China.
PeerJ. 2025 Mar 26;13:e19161. doi: 10.7717/peerj.19161. eCollection 2025.
To clarify the influence of changes in the overlying water environment on internal nitrogen release from reservoir sediments, we collected surface sediments at a depth of approximately 10 cm from the Sunxi River in the tail area of the Three Gorges Reservoir area for simulation experiments. By using orthogonal simulation experiments in the laboratory, we studied the effects of water pH, temperature and hydraulic disturbance on nitrogen release in the sediment and established a quantitative linear relationship between the nitrogen release rate from the sediment and the environmental factors of the overlying water. The results indicated that the average concentrations of total nitrogen (TN) and total phosphorus (TP) in the sediment were 430 mg/kg and 200 mg/kg, respectively. The sediment TN concentration had a very significant positive correlation with the sediment organic matter content ( < 0.001). The sediment TN, NO-N and NH-N release intensities gradually increased with increasing incubation time, with maximum release rates of 29.24 mg/((m⋅d), 23.11 mg/(m⋅d) and 4.32 mg/((m⋅d), respectively. Range analysis revealed that the significance of the effects of environmental factors on sediment TN and NH-N release were ranked as follows: temperature > pH > disturbance, and that of NO-N release was ranked as pH > temperature > disturbance. Temperature plays the most important role in the behavior of different forms of nitrogen release from sediments. The capacity and potential for nitrogen release from sediments offer crucial insights for assessing the risks posed to the overlying water and highlighting the importance of these factors in water quality management and prediction in the reservoir area.
为阐明上覆水环境变化对水库沉积物内源氮释放的影响,我们在三峡库区尾部的孙溪河采集了深度约为10厘米的表层沉积物进行模拟实验。通过在实验室进行正交模拟实验,研究了水体pH值、温度和水力扰动对沉积物中氮释放的影响,并建立了沉积物氮释放速率与上覆水环境因子之间的定量线性关系。结果表明,沉积物中总氮(TN)和总磷(TP)的平均浓度分别为430毫克/千克和200毫克/千克。沉积物TN浓度与沉积物有机质含量呈极显著正相关(<0.001)。沉积物TN、NO-N和NH-N的释放强度随培养时间的增加而逐渐增大,最大释放速率分别为29.24毫克/(平方米·天)、23.11毫克/(平方米·天)和4.32毫克/(平方米·天)。极差分析表明,环境因子对沉积物TN和NH-N释放影响的显著性排序为:温度>pH值>扰动,对NO-N释放影响的显著性排序为:pH值>温度>扰动。温度在沉积物中不同形态氮释放行为中起最重要作用。沉积物氮释放的能力和潜力为评估对上覆水的风险以及突出这些因素在库区水质管理和预测中的重要性提供了关键见解。