College of Geography and Environment, Shandong Normal University, Jinan, Shandong, PR China.
The Natural Resources and Planning Bureau of Weishan, Jining, PR China.
PLoS One. 2023 Oct 11;18(10):e0292705. doi: 10.1371/journal.pone.0292705. eCollection 2023.
The South-to-North Water Diversion East Project (SNWDP-E) is an effective way to realize the optimal allocation of water resources in China. The North Dasha River (NDR) is the reverse recharge section that receives water from the Yufu River to the Wohushan Reservoir transfer project line in the SNWDP. However, the dissolved organic matter (DOM) evolution mechanism of seasonal water transfer projects on tributary waters has not been fully elucidated. In this paper, the NDR is the main object, and the changes in the composition and distribution of spectral characteristics during the winter water transfer period (WT) as well as during the summer non-water transfer period (NWT) are investigated by parallel factor analysis (PARAFAC). The results showed that the water connectivity caused by water transfer reduces the environmental heterogeneity of waters in the basin, as evidenced by the ammonia nitrogen (NH4+-N) and total phosphorus (TP) in the water body were significantly lower (p<0.05, p<0.01) during the water transfer period than the non-water transfer period. In addition, the fluorescence intensity of DOM was significantly lower in the WT than the NWT (p<0.05) and was mainly composed of humic substances generated from endogenous sources with high stability. While the NWT was disturbed by anthropogenic activities leading to significant differences in DOM composition in different functional areas. Based on the redundancy analysis (RDA) and multiple regression analysis, it was found that the evolution of the protein-like components is dominated by chemical oxygen demand (COD) and NH4+-N factors during the WT. While the NWT is mainly dominated by total nitrogen (TN) and TP factors for the evolution of the humic-like components. This study helps to elucidate the impact of water transfer projects on the trunk basin and contribute to the regulation and management of inter-basin water transfer projects.
南水北调东线工程(SNWDP-E)是实现中国水资源优化配置的有效途径。北沙河(NDR)是反向补给段,从御府河接收水到 SNWDP 的乌呼山水库转输工程线。然而,支流季节性调水工程中溶解有机物(DOM)的演变机制尚未完全阐明。本文以北沙河为主要对象,采用平行因子分析(PARAFAC)研究了冬季调水期(WT)和夏季非调水期(NWT)DOM 组成和分布光谱特征的变化。结果表明,调水引起的水体连通性降低了流域内水体的环境异质性,水体中的氨氮(NH4+-N)和总磷(TP)在调水期明显低于非调水期(p<0.05,p<0.01)。此外,DOM 的荧光强度在 WT 期显著低于 NWT 期(p<0.05),主要由内源性来源产生的稳定性较高的腐殖物质组成。而 NWT 期受到人为活动的干扰,导致不同功能区 DOM 组成存在显著差异。基于冗余分析(RDA)和多元回归分析,发现 WT 期蛋白样组分的演化主要受化学需氧量(COD)和 NH4+-N 因子的控制,而 NWT 期腐殖质样组分的演化主要受总氮(TN)和 TP 因子的控制。本研究有助于阐明调水工程对干流域的影响,为流域间调水工程的调控和管理提供依据。