Liu Zhe-Zhe, Ni Zhao-Kui, Liu Si-Ru, Li Xiao-Xiu, Wang Sheng-Rui
College of Resource Environment and Tourism, Capital Normal University, Beijing 100084, China.
Guangdong-Hong Kong Joint Laboratory for Water Security, Center of Water Research, Beijing Normal University at Zhuhai, Zhuhai 519087, China.
Huan Jing Ke Xue. 2022 Jun 8;43(6):3058-3065. doi: 10.13227/j.hjkx.202110121.
To reveal the characteristics of organic phosphorus release from lake sediments and its potential impact on water quality, six lake sediments from Yunnan Plateau and the middle and lower reaches of the Yangtze River in China were selected. We studied the differences in the kinetics of dissolved organic phosphorus (DOP) and dissolved inorganic phosphorus (SRP) release from sediments. The effects of organic phosphorus morphology and dissolved organic matter (DOM) characteristics on sediment phosphorus release were investigated, and the water quality risks of sediment DOP release were discussed. The results showed that:① the release kinetics of sediment DOP and SRP were similar; both followed the second-order kinetic model, starting with a rapid release phase, followed by a slow release, and the release curve gradually leveled off and reached the maximum release. ② The release of organic phosphorus was related to organophosphorus morphology and organic matter. Active organic phosphorus (LOP) and medium active organic phosphorus (MLOP) were the DOP forms mainly released into the overlying water during the rapid release phase. The proportion of LOP and MLOP to total organic phosphorus (DTP) decreased in the late release stage, whereas the proportion of non-active organic phosphorus (NLOP) increased; further, the degree of humification and aromaticity of organic matter gradually increased with phosphorus release, and its activity decreased, resulting in a slower release rate at the later stage. ③ Compared with that of SRP, the risk of DOP release was higher, accounting for 47%-77% of the total amount of DTP. It was also found that the higher the nutrient level of the lake, the greater the release of DOP and the higher the water quality risk. Therefore, not only the release of inorganic phosphorus but also that of organic phosphorus should be of concern in the process of phosphorus release from lake sediments to prevent the underestimation of phosphorus release and water quality risk.
为揭示湖泊沉积物中有机磷释放特征及其对水质的潜在影响,选取了中国云南高原及长江中下游地区的6个湖泊沉积物。研究了沉积物中溶解有机磷(DOP)和溶解性无机磷(SRP)释放动力学的差异。探讨了有机磷形态和溶解有机物(DOM)特征对沉积物磷释放的影响,并讨论了沉积物DOP释放的水质风险。结果表明:①沉积物DOP和SRP的释放动力学相似;均遵循二级动力学模型,开始为快速释放阶段,随后缓慢释放,释放曲线逐渐趋于平缓并达到最大释放量。②有机磷的释放与有机磷形态和有机质有关。活性有机磷(LOP)和中等活性有机磷(MLOP)是快速释放阶段主要释放到上覆水中的DOP形态。在释放后期,LOP和MLOP占总有机磷(DTP)的比例下降,而非活性有机磷(NLOP)的比例增加;此外,随着磷的释放,有机质的腐殖化程度和芳香性逐渐增加,其活性降低,导致后期释放速率减慢。③与SRP相比,DOP释放风险更高,占DTP总量的47%-77%。还发现湖泊营养水平越高,DOP释放量越大,水质风险越高。因此,在湖泊沉积物磷释放过程中,不仅应关注无机磷的释放,还应关注有机磷的释放,以防止低估磷释放量和水质风险。