Jin Xiangcan, Jiang Xia, Yao Yang, Li Lihe, Wu F C
Chinese Research Academy of Environmental Science, Beijing 100012, China.
Sci Total Environ. 2006 Mar 15;357(1-3):231-6. doi: 10.1016/j.scitotenv.2005.04.027. Epub 2005 Jun 2.
Effects of oxygen and light on the uptake and distribution of phosphorus at the sediment-water interface were investigated in this study. The experimental water and sediment samples were collected from East Taihu Lake, China. The results show that phosphorus can be taken up from the overlying water to the sediments with high nutrient loading in both anoxic and aerobic conditions. The transformation between different phosphorus fractions in the sediments and in the overlying water was observed. Effects of dissolved oxygen on the phosphorus distribution at the sediment and overlying water interface were mainly due to the inorganic processes, while effects of light were mainly due to the biological activity. This study indicates that oxygen concentration had a predominant control on the distribution and uptake of phosphorus in the sediments, and light had obvious effect on the dissolved inorganic phosphorus (DIP) concentration in the overlying water.
本研究调查了氧气和光照对沉积物-水界面磷吸收和分布的影响。实验用水和沉积物样本采自中国太湖东部。结果表明,在缺氧和好氧条件下,高营养负荷时磷均可从上覆水被吸收至沉积物中。观察到沉积物和上覆水中不同磷组分之间的转化。溶解氧对沉积物与上覆水界面磷分布的影响主要源于无机过程,而光照的影响主要源于生物活性。本研究表明,氧浓度对沉积物中磷的分布和吸收起主要控制作用,光照对上覆水中溶解无机磷(DIP)浓度有明显影响。