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作 者:袁辉[1] 黄川[2] 崔志强[3] 胡刚[2] 包亮[2]
机构地区:[1]重庆大学图书馆,重庆400030 [2]重庆大学资源及环境科学学院,重庆400030 [3]重庆大学人事处,重庆400030
出 处:《重庆大学学报(自然科学版)》2007年第9期134-138,共5页Journal of Chongqing University
基 金:重庆市发展和改革委员会资助项目;重庆市科学技术委员会资助项目(03-26)
摘 要:随着三峡工程蓄水的完成,三峡库区消落带将逐渐形成并进入淹没期。消落带初次进入淹没期后,长期吸附在消落带土壤中的氮磷等营养物质将逐渐进入水体,并由此对三峡水库水质产生一定的影响。模拟消落带土壤淹没后氮磷释放实验,根据实验结果和一级动力学方程,计算出消落带土壤进入淹水期后的氮磷释放速率方程,并分别预测了在高、中、低水平下库区各区县消落带土壤释放的氮磷总量。以典型的开县消落带为例,预测了开县消落带氮磷释放与水环境之间的响应关系,结果表明高水平条件下开县消落带土壤全淹后对水环境中TP、TN和氨氮浓度的贡献值均较小,但其所占预测负荷总量的百分比分分别为93.79%,69.65%和51.61%,As the water storage plans of the Three Gorges Project come into action, the shore area along the reservoir will gradually be submerged and a wet-dry alternation environment will form, where the nutriments of the P and N absorbed in the soil during long period will leach out and diffuse in the water environment. With the simulated submerging experiments of the soil conduct, the leaching amounts of the P and N under three different conditions (High, Medium and Low) were calculated. Based on the experiments data and kinetic equation, the leaching models of N and Pwere established.Furthermore, the relationships between the leached P, N and the water quality were also projected as taken Kaixian County' s wet-dry area as an example.
分 类 号:X524[环境科学与工程—环境工程]
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