Li Guolian, Xie Fazhi, Zhang Jin, Wang Jingrou, Yang Ying, Sun Ruoru
School of Environment and Energy Engineering, Anhui Jianzhu University Provincial Key Laboratory of Water Pollution Control and Waste Water Utilization, Hefei, Anhui 230601, China E-mail:
School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China.
Water Sci Technol. 2016 Sep;74(6):1266-1273. doi: 10.2166/wst.2016.277.
Phosphorus (P) in a water body is mainly controlled by the interaction between surface sediment and the overlying water column after the complete control of external pollution. Significant enhancement of P in a water body would cause eutrophication of lakes. Thus, a better understanding is needed of the occurrences of P between the sediment and water column in eutrophic lakes. Here, we measured total phosphorus (TP) and major elements (Fe, Al, Ca, Mn, Si) in the water column, and total nitrogen, organic matter, TP and major oxides (FeO, AlO, CaO, SiO) in surface sediment of Chaohu Lake, a continuously eutrophic lake. The results showed that the rank of TP levels was western lake > eastern lake > southern lake. There were significantly positive correlations between TP (including water TP and sedimentary TP) and Fe, Al, Mn, while the correlation coefficients between water TP and sedimentary TP were -0.43, -0.41 and 0.18 for the western, eastern and southern lake respectively. The negative and significant correlations of water TP and sedimentary TP may indicate that the risk of sedimentary P release was great in the western and eastern lake during algae bloom sedimentation, while the southern lake showed weak P exchange between the sediment and water column.
在完全控制外源污染后,水体中的磷(P)主要受表层沉积物与上覆水体之间相互作用的控制。水体中磷的显著增加会导致湖泊富营养化。因此,需要更好地了解富营养化湖泊中沉积物与水体之间磷的赋存情况。在此,我们测定了连续富营养化湖泊巢湖的水柱中的总磷(TP)和主要元素(Fe、Al、Ca、Mn、Si),以及表层沉积物中的总氮、有机质、TP和主要氧化物(FeO、AlO、CaO、SiO)。结果表明,TP水平的排序为:西湖>东湖>南湖。TP(包括水体TP和沉积TP)与Fe、Al、Mn之间存在显著正相关,而西湖、东湖和南湖水体TP与沉积TP之间的相关系数分别为-0.43、-0.41和0.18。水体TP与沉积TP之间的负相关且显著,这可能表明在藻类沉降期间,西湖和东湖沉积物中磷释放的风险很大,而南湖沉积物与水柱之间的磷交换较弱。