You Ben-Sheng, Wang Tong-Cheng, Fan Cheng-Xin, Zhong Ji-Cheng, Yin Hong-Bin, Li Bao
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography & Limnology, Chinese Academy of Sciences, Nanjing 210008, China.
Huan Jing Ke Xue. 2008 Jan;29(1):26-31.
Internal nutrient loading caused by sediment resuspension is becoming a key issue in studying water eutrophication of shallow lakes. A Y-shape apparatus was used to simulate sediment resuspension and sedimentation process under hydrodynamic conditions in situ in grass type zone of Lake Taihu, and effects on aqueous nutrient loading were investigated. The results indicated that, in the light and moderate wind processes, content of ammonia nitrogen and phosphate had remarkably reduced with the increase of the amount of suspended sediments in water column, with the maximal change of -0.140 g x m(-2) and -1.59 mg x m(-2) at the sediment-water interface for the two nutrients respectively, and in the strong wind process, concentration of aqueous phosphate had a significant increase, with the maximal flux of 0.81 mg x m(-2) at the sediment-water interface, while concentration of aqueous ammonia nitrogen showed a small decrease. And in the later sedimentation process after wind, content of aqueous ammonia nitrogen was lower than that before the light and moderate wind processes, but approximated to that before the strong wind process. Content of aqueous phosphate was close to that before the light and moderate wind processes, but had a marked increase compared to that before the strong wind condition, with the maximal increment of 1.36 mg x m(-2). Consequently, sediment resuspension and sedimentation processes impact nutrients loading of overlaying water evidently. Comparison of the results with those from non-grass type zone in Lake Taihu illustrates that the presence of aquatic macrophytes played some roles in reducing the release of nutrients during the sediment resuspension process.
由沉积物再悬浮引起的内源营养负荷正成为研究浅水湖泊水体富营养化的关键问题。利用Y形装置原位模拟太湖草型湖区水动力条件下的沉积物再悬浮和沉降过程,并研究其对水体营养负荷的影响。结果表明,在小风及中风过程中,水柱中悬浮沉积物量增加,氨氮和磷酸盐含量显著降低,两种营养物质在沉积物-水界面处的最大变化分别为-0.140 g·m(-2)和-1.59 mg·m(-2);在大风过程中,水体磷酸盐浓度显著增加,沉积物-水界面处的最大通量为0.81 mg·m(-2),而水体氨氮浓度略有下降。且在大风过后的沉降过程中,水体氨氮含量低于小风及中风过程前,但接近大风过程前;水体磷酸盐含量接近小风及中风过程前,但与大风前相比有显著增加,最大增量为1.36 mg·m(-2)。因此,沉积物再悬浮和沉降过程对上层水体营养负荷有明显影响。将结果与太湖非草型湖区的结果进行比较表明,水生植物的存在对减少沉积物再悬浮过程中营养物质的释放起到了一定作用。