State Key Laboratory of Eco-Hydraulics in Northwest Arid Region of China, Xi'an University of Technology, Xi'an, Shaanxi, 710048, China.
State Key Laboratory of Eco-Hydraulics in Northwest Arid Region of China, Xi'an University of Technology, Xi'an, Shaanxi, 710048, China.
Chemosphere. 2024 Sep;364:143002. doi: 10.1016/j.chemosphere.2024.143002. Epub 2024 Aug 2.
Lanthanum-modified bentonite (LMB) combined with submerged macrophytes (SM) has been a conventional means of eutrophication management in lakes in recent years, and is one of the most important methods for P removal. However, trends in nutrients and sediment enzymes at the water-sediment interface during this process have not been systematically assessed, and there are still some gaps in how abiotic properties drive changes in enzyme activity. Here, we show changes in aquatic environmental conditions under the action of different ratios of modified bentonite (0, 10%, 20%, and 30%) in combination with SM (Vallisneria natans, Potamogeton lucens, and Hydrilla verticillate) and quantify their effects on sediment enzyme activities. The results showed that the nutrient cycling at the water-sediment interface was facilitated by the combined effect of SM and LMB, which effectively reduced the overlying water nutrient concentration, increased the sediment enzyme activity and enhanced the N cycling process. Partial least squares structural equation model (PLS-SEM) showed that sediment parameters strongly influenced changes in enzyme activity, with NO-N as the main controlling factors. Our study fills in the process of changing environmental conditions in lake water under geoengineered materials combined with macrophyte measures, especially the changes in biological properties enzyme activities, which contributes to a clearer understanding of nutrient fluxes during the management of eutrophication in lakes.
近年来,镧改性膨润土(LMB)与沉水植物(SM)相结合已成为湖泊富营养化管理的常规手段,是去除磷的最重要方法之一。然而,在这个过程中,水-沉积物界面处的营养物质和沉积物酶的趋势尚未得到系统评估,并且对于非生物特性如何驱动酶活性变化仍然存在一些差距。在这里,我们展示了在不同比例的改性膨润土(0、10%、20%和 30%)与 SM(苦草、菹草和黑藻)结合作用下,水生态环境条件的变化,并定量它们对沉积物酶活性的影响。结果表明,SM 和 LMB 的联合作用促进了水-沉积物界面的养分循环,有效降低了上覆水营养盐浓度,增加了沉积物酶活性,增强了氮循环过程。偏最小二乘结构方程模型(PLS-SEM)表明,沉积物参数强烈影响酶活性的变化,以硝态氮(NO-N)为主要控制因素。本研究填补了在地质工程材料与沉水植物措施相结合的情况下,湖水环境条件变化的过程,特别是生物特性酶活性的变化,有助于更清楚地了解湖泊富营养化管理过程中的养分通量。