排序方式: 共有49条查询结果,搜索用时 31 毫秒
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复合塘-湿地系统水生植物时空分布对氮磷去除的影响 总被引:1,自引:0,他引:1
利用复合生态塘-湿地处理系统水生植物时空格局异质性,研究了水生植物分布对氮、磷去除影响.结果表明,水生植物种类和数量的分布差异导致各单元氮、磷去除呈现不同的周期变化;水生植物主要通过改变硝化/反硝化进程、自身代谢和化学沉降速率影响NH3、NOx-、有机氮和总磷的去除.系统不同单元中氮、磷去除机制差异决定了NH3和总磷主要在曝气养鱼塘(去除率分别为29.5%、30.1%)、鱼塘(16.9%、17.8%)和水生植物塘(24.5%、19.4%)去除;NOx-主要在芦苇湿地(出水<0.4 mg/L)去除;而有机氮则主要在复合兼性塘(32.3%)和鱼塘(28.1%)去除.此外,生态塘出水中水生植物绝大部分被芦苇湿地所截滤,它们的腐败/释放导致湿地中NH3和总磷的表观去除率偏低(分别小于8.5%和11.5%). 相似文献
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填料是流离生化技术处理污水的关键材料。文中模拟试验污水处理过程,测试污泥流离球填料的挂膜情况和污染物去除能力。确定运行适应性参数DO水平为4~5mg/L,水力停留时间4h,反应温度22℃,反应pH值7~9时,实施处理配制污水试验的结果表明,净化后污水CODcr和NH3-N去除效果良好,污水净化后符合国家"污水综合排放标准"二级标准的要求,污泥陶粒流离球填料应用于污水处理可行。 相似文献
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应用灰色系统理论预测拉林河总磷浓度变化趋势 总被引:1,自引:0,他引:1
本文利用灰色系统理论,根据以前监测数据,通过建立GM(1,1)模型和模型群,预测出拉林河水体中总磷浓度及其变化趋势. 相似文献
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Zhaohua Dai Carl C. Trettin Changsheng Li Devendra M. Amatya Ge Sun Harbin Li 《Journal of the American Water Resources Association》2010,46(5):1036-1048
Dai, Zhaohua, Carl C. Trettin, Changsheng Li, Devendra M. Amatya, Ge Sun, and Harbin Li, 2010. Sensitivity of Streamflow and Water Table Depth to Potential Climatic Variability in a Coastal Forested Watershed. Journal of the American Water Resources Association (JAWRA) 1–13. DOI: 10.1111/j.1752-1688.2010.00474.x Abstract: A physically based distributed hydrological model, MIKE SHE, was used to evaluate the effects of altered temperature and precipitation regimes on the streamflow and water table in a forested watershed on the southeastern Atlantic coastal plain. The model calibration and validation against both streamflow and water table depth showed that the MIKE SHE was applicable for predicting the streamflow and water table dynamics for this watershed with an acceptable model efficiency (E > 0.5 for daily streamflow and >0.75 for monthly streamflow). The simulation results from changing temperature and precipitation scenarios indicate that climate change influences both streamflow and water table in the forested watershed. Compared to current climate conditions, the annual average streamflow increased or decreased by 2.4% with one percentage increase or decrease in precipitation; a quadratic polynomial relationship between changes in water table depth (cm) and precipitation (%) was found. The annual average water table depth and annual average streamflow linearly decreased with an increase in temperature within the range of temperature change scenarios (0-6°C). The simulation results from the potential climate change scenarios indicate that future climate change will substantially impact the hydrological regime of upland and wetland forests on the coastal plain with corresponding implications to altered ecosystem functions that are dependent on water. 相似文献
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