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291.
Yusuf M. Mohamoud 《Journal of the American Water Resources Association》2007,43(5):1280-1292
Abstract: The hydrological simulation program – FORTRAN (HSPF) is a comprehensive watershed model that employs depth‐area‐volume‐flow relationships known as the hydraulic function table (FTABLE) to represent the hydraulic characteristics of stream channel cross‐sections and reservoirs. An accurate FTABLE determination for a stream cross‐section site requires an accurate determination of mean flow depth, mean flow width, roughness coefficient, longitudinal bed slope, and length of stream reach. A method that uses regional regression equations to estimate mean flow depth, mean flow width, and roughness coefficient is presented herein. FTABLES generated by the proposed method (Alternative Method) and FTABLES generated by Better Assessment Science Integrating Point and Nonpoint Sources (BASINS) were compared. As a result, the Alternative Method was judged to be an enhancement over the BASINS method. First, the Alternative Method employs a spatially variable roughness coefficient, whereas BASINS employs an arbitrarily selected spatially uniform roughness coefficient. Second, the Alternative Method uses mean flow width and mean flow depth estimated from regional regression equations whereas BASINS uses mean flow width and depth extracted from the National Hydrography Dataset (NHD). Third, the Alternative Method offers an option to use separate roughness coefficients for the in‐channel and floodplain sections of compound channels. Fourth, the Alternative Method has higher resolution in the sense that area, volume, and flow data are calculated at smaller depth intervals than the BASINS method. To test whether the Alternative Method enhances channel hydraulic representation over the BASINS method, comparisons of observed and simulated streamflow, flow velocity, and suspended sediment were made for four test watersheds. These comparisons revealed that the method used to estimate the FTABLE has little influence on hydrologic calibration, but greatly influences hydraulic and suspended sediment calibration. The hydrologic calibration results showed that observed versus simulated daily streamflow comparisons had Nash‐Sutcliffe efficiencies ranging from 0.50 to 0.61 and monthly comparisons had efficiencies ranging from 0.61 to 0.84. Comparisons of observed and simulated suspended sediments concentrations had model efficiencies ranging from 0.48 to 0.56 for the daily, and 0.28 to 0.70 for the monthly comparisons. The overall results of the hydrological, hydraulic, and suspended sediment concentration comparisons show that the Alternative Method yielded a relatively more accurate FTABLE than the BASINS method. This study concludes that hydraulic calibration enhances suspended sediment simulation performance, but even greater improvement in suspended sediment calibration can be achieved when hydrological simulation performance is improved. Any improvements in hydrological simulation performance are subject to improvements in the temporal and spatial representation of the precipitation data. 相似文献
292.
Richard J. Schicht 《Journal of the American Water Resources Association》1972,8(1):175-187
Changes in groundwater levels due to a well discharging at a constant rate are used with various formulas to determine hydraulic properties of aquifers and their confining bed and to detect the presence of aquifer boundaries. These formulas are generally solved by graphical methods. 相似文献
293.
The feasibility of using anaerobic ba ed reactor (ABR) as onsite wastewater treatment system was discussed. The ABR consisted
of one sedimentation chamber and three up-flow chambers in series was experimented under di erent peak flow factors (PFF of 1
to 6), superficial gas velocities (between 0.6 and 3.1 cm/hr) and hydraulic retention times (HRT) (24, 36 and 48 hr). Residence time
distribution (RTD) analyses were carried out to investigate the hydraulic characteristics of the ABR. It was found that the PFF resulted
in hydraulic dead space. The dead space did not exceed 13% at PFF of 1, 2 and 4 while there was 2-fold increase (26%) at PFF of
6. Superficial gas velocities did not result in more (biological) dead space. The mixing pattern of ABR tended to be a completelymixed
reactor when PFF increased. Superficial gas velocities did not a ect mixing pattern. The e ects of PFF on mixing pattern could
be minimized by higher HRT (48 hr). The tank-in-series (TIS) model (N = 4) was suitable to describe the hydraulic behaviour of
the studied system. The HRT of 48 hr was able to maintain the mixing pattern under di erent flow patterns, introducing satisfactory
hydraulic e ciency. Chemical oxygen demand (COD) and total suspended solids (TSS) removals under all flow patterns were achieved
more than 85% and 90%, respectively. The standard deviation of e uent COD and TSS concentration did not exceed 15 mg/L. 相似文献
294.
结合姜堰市城市生活污水处理厂运行,对CASS工艺中水力停留时间对COD、TN和NH3-N去除率的影响进行了探讨。通过运行工况和进水水质的改变试验,以积累大量的试验运行数据和实际处理效果,探讨水力停留时间对去除率的影响,确定适宜的水力停留时间。实验研究表明,水力停留时间控制在18h比较适宜,这样既经济又可以获得较稳定的处理效果。 相似文献
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298.
反冲洗措施改善垂直潜流人工湿地水力特性的研究 总被引:1,自引:0,他引:1
人工湿地污水处理工程中难以解决的问题之一是湿地基质堵塞,本研究尝试用反冲洗措施解决此问题。采用不同反冲洗方案研究了反冲洗措施对人工湿地堵塞程度的改善效果,同时分析了反冲洗措施对垂直潜流人工湿地污染物去除效果的改变和水力特性的影响。结果表明,反冲洗措施对解决垂直潜流人工湿地的堵塞有明显地改善;人工湿地发生淤堵使COD去除率下降,反冲洗后随着实际水力停留时间的延长,COD去除率较反冲洗前有所提高;在几种反冲洗方案中,气水联合反冲洗方案在单位面积流量为8~10 L(/m.2s),反冲洗时间为5~7 min时反冲洗效果最好。 相似文献
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