Yunnan Ecological and Environmental Monitoring Center, Kunming 650034, China.
School of Resources and Environmental Engineering, Anhui University, Hefei 230601, China; Anhui Shengjin Lake Wetland Ecology National Long-term Scientific Research Base, Dongzhi 247230, China.
J Contam Hydrol. 2023 Feb;253:104127. doi: 10.1016/j.jconhyd.2022.104127. Epub 2022 Dec 28.
Large deep lakes in plateau regions provide crucial ecosystem services but are susceptible to eutrophication due to their long water residence time. To date, the water quality of deep lakes has not received as much attention as that of shallow lakes owing to logistical challenges. This study investigated the seasonal variation and vertical distribution of phosphorus and related environmental variables in a large deep lake in the Yunnan Plateau, China (Fuxian Lake). Generally, the concentrations of total phosphorus (TP, R = 0.862), total dissolved phosphorus (TDP, R = 0.922), and dissolved inorganic phosphorus (DIP, R = 0.889) exhibited a linear increase with the greater water depth, whereas the pH and dissolved oxygen (DO) showed decreasing trends. The TP, TDP, and DIP values were 0.012, 0.006, and 0.004 mg/L, respectively, in surface waters (0.5 m depth), and increased to 0.074, 0.065, and 0.062 mg/L, respectively, at 140.0 m depth. The averaged over ordering method demonstrated that DO and air temperature accounted for a higher proportion of the explained variance of TP, TDP, and DIP in the shallow water layer (0.5-20.0 m). In contrast, DO and pH accounted for a higher proportion of the explained variance of TP, TDP, and DIP in deeper water layers (40.0-150.0 m). As a warm monomictic lake, the higher observed phosphorus concentrations in deeper water and sediment potentially pose a risk of future eutrophication in the Fuxian Lake. Our findings demonstrate that more efficient technical and management measures should be taken to reduce the external phosphorus load to Fuxian Lake, so that the load to and from the sediment will decrease eventually.
高原地区的大型深水湖泊提供了至关重要的生态系统服务,但由于其水停留时间长,容易发生富营养化。迄今为止,由于后勤方面的挑战,深水湖泊的水质尚未像浅水湖泊那样受到关注。本研究调查了中国云南高原大型深水湖泊抚仙湖(Fuxian Lake)的磷及相关环境变量的季节性变化和垂直分布。一般来说,总磷(TP,R=0.862)、总溶解磷(TDP,R=0.922)和溶解无机磷(DIP,R=0.889)的浓度随水深的增加呈线性增加,而 pH 值和溶解氧(DO)呈下降趋势。表层水(0.5 米深度)的 TP、TDP 和 DIP 值分别为 0.012、0.006 和 0.004mg/L,而在 140.0 米深度处分别增加到 0.074、0.065 和 0.062mg/L。平均排序法表明,在浅层水层(0.5-20.0m)中,DO 和空气温度对 TP、TDP 和 DIP 的解释方差的比例较高。相比之下,在更深的水层(40.0-150.0m)中,DO 和 pH 值对 TP、TDP 和 DIP 的解释方差的比例较高。作为一个温暖的单型湖泊,在更深的水层和沉积物中观察到的较高磷浓度可能会增加抚仙湖未来富营养化的风险。我们的研究结果表明,应采取更有效的技术和管理措施,减少抚仙湖的外部磷负荷,从而最终减少从沉积物输入和输出的磷负荷。