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ZHANG Shao-yuan Renze van Houten Dick H. Eikelboom JIANG Zhao-chun FAN Yao-bo WANG Ju-si 《环境科学学报(英文版)》2002,14(4):501-507
Based on the microorganism kinetic model, the formula for computing hydraulic retention time in a membrane bioreactor system (MBR) is derived. With considering HRT as an evaluation index a combinational approach was used to discuss factors which have an effect on MBR. As a result, the influencing factors were listed in order from strength to weakness as: maximum specific removal rate K, saturation constant Ks, maintenance coefficient m, maximum specific growth rate ,ua and observed yield coefficient Yobs. Moreover, the formula was simplified, whose parameters were experimentally determined in petrochemical wastewater treatment. The simplified formula is θ= 1.1( 1/β -1)(Ks S)/KXo , for oetroehemical wastewater treatment K and Ko eaualed 0.185 and 154.2, resoectively. 相似文献
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Christopher I. Thornton Steven R. Abt Warren P. Clary 《Journal of the American Water Resources Association》1997,33(6):1279-1288
ABSTRACT: A meandering stream channel was simulated in the Hydraulics Laboratory at Colorado State University and a series of tests was conducted using four types of vegetation to evaluate the potential effects of vegetation on sediment deposition and retention in a stream channel. The data collected included average flow velocity, flow depth, length of vegetation, density of vegetation, cross-sectional area of the vegetative stem, wetted perimeter of the vegetative stem, and injection and flushing time. The findings indicated that the vegetation could retain from 30 to 70 percent of the deposited sediments. The ability of vegetation to entrap and retain sediment is related to the length and cross-sectional area of the vegetation. The variables describing the flow and the vegetative properties were combined to form a predictive parameter, the sedimentation factor (Sd) that can be compared with the amount of sediment entrapped by vegetation in a stream system. A relation was developed correlating vegetation length to sediment retention after flushing for flexibility and rigid vegetation. 相似文献
15.
In multiphase systems capillary pressures play a significant role on fluid movement and retention. The facility to predict
the effect of different thermal remediation strategies requires the knowledge of the effect of temperature on capillary pressure-saturation
relationships in the soils.
The objective of recent study was (a) to develop a technique for routinely measuring the pressure-saturation curves of soil
samples saturated with a nonpolar liquid at different regulated temperatures (b) to build a database using the measured pressure-saturation
curves and the physical, chemical properties of the model soils (c) to establish the dependence of nonaqueous phase liquid
retention on the soil properties and the temperature.
The retention curves (extraction isotherms) with nonaqueous phase liquid were determined using a modified
pressure plate extractor. The wetting phase was a non-aromatic hydrocarbon distillation product. Pressure plates were designed and constructed in
the laboratory of our department. The temperature was held constant at 20, 40 and 60 ∘C.
Statistical analysis was performed involving selected soil parameters and the measured nonaqueous phase liquid retention data.
The results show that knowing some easily measurable soil parameters (bulk density, particle size distribution, humus and
lime content) we can estimate the nonaqueous phase liquid retention of the soils. The measured “extraction isotherms” provide
essential information about the temperature-dependency of pressure-saturation curves. 相似文献
16.
Four sequence batch reactors (SBRs) fed by fermented sugar cane wastewater were continuously operated under the aerobic dynamic feeding (ADF) mode with different configurations of sludge retention time (SRT), carbon and initial biomass concentrations to enrich polyhydroxyalkanoate (PHA) accumulating mixed microbial cultures (MMCs) from municipal activated sludge. The stability of SBRs was investigated besides the enrichment performance. The microbial community structures of the enriched MMCs were analyzed using terminal restriction fragment length polymorphism (T-RFLP). The optimum operating conditions for the enrichment process were: SRT of 5 days, carbon concentration of 2.52 g COD/L and initial biomass concentration of 3.65 g/L. The best enrichment performance in terms of both operating stability and PHA storage ability of enriched cultures (with the maximum PHA content and PHA storage yield (YPHA/S) of 61.26% and 0.68 mg COD/mg COD, respectively) was achieved under this condition. Effects of the SRT, carbon concentration and initial biomass concentration on the PHA accumulating MMCs selection process were discussed respectively. A new model including the segmentation of the enrichment process and the effects of SRT on each phase was proposed. 相似文献
17.
玉米秸秆生物炭对贵州黄壤持水能力的影响 总被引:1,自引:0,他引:1
生物炭具有丰富的微孔结构,能够影响土壤的持水性能,对植物生长和土壤中养分的保持有着重要意义。而土壤水分特征曲线又是表征土壤持水能力的一个重要指标。本文通过压力膜法测定添加不同比例生物炭的黄壤水分特征曲线,并结合van Genuchten模型对实测结果进行拟合,推导水动力学参数。结果表明,随着生物炭施入量的增加(0、5%、10%),土壤的田间持水量增加,凋萎含水量降低,土壤有效含水量增加。生物炭添加能够显著提高土壤的持水能力,增强水分的可利用性。同时,van Genuchten模型拟合结果同实测值高度相似,可以用作预测生物炭改良土壤的水动力学参数。 相似文献
18.
目的研究典型环境对丁腈橡胶-铝合金带垫卡箍的损伤效应。方法通过模拟铝合金-丁腈橡胶航空带垫卡箍使用时的装配结构和应力状态,应用GJB 150A—2009中的湿热和太阳辐射两种典型老化环境,采用宏观形貌观察、卡箍保持力测试和橡胶衬垫拉伸性能测试方法,结合扫描电子显微镜和傅里叶红外光谱技术,分析带垫卡箍的性能劣化过程。结果带垫卡箍在湿热和太阳辐射环境中老化50 d后,卡箍橡胶衬垫表面出现大量微孔缺陷,拉伸性能大幅降低,导致卡箍保持力分别下降了35%和51%。结论带垫卡箍在模拟装配状态下进行湿热和太阳辐射环境暴露实验,卡箍橡胶衬垫内部结构由致密逐渐变得疏松,部分碳碳双键发生氧化交联反应,并在一定程度上提高了聚合物的交联密度,材料硬度提高,回弹性能减弱,橡胶衬垫对芯轴的包裹能力降低,导致卡箍保持力性能降低。 相似文献
19.
海水生物滤器氨氮沿程转化规律模型 总被引:4,自引:2,他引:2
生物滤器是海水循环水养殖系统中的核心水处理单元,其主要用于去除对养殖生物有害的氨氮、有机物等.本研究基于吸附原理和一级反应生物膜理论构建了氨氮在生物滤器中沿程转化规律的数学模型,并通过实验加以验证.实验所用生物滤器采用竹制空心生化球填料,装填高度为70 cm,在pH为7.1~7.6,DO为5~7 mg.L-1,气水比20∶1左右,有机负荷约为4g.(m3.h)-1,水力停留时间(HRT)为1 h条件下,生物滤器中氨氮的去除主要发生在填料高度0~10 cm处,10~70 cm处氨氮去除量很少.进水氨氮质量浓度的增大和水力停留时间的降低都会导致出水氨氮质量浓度增大.此外,模型对进水氨氮质量浓度较低时的沿程出水氨氮质量浓度具有很好的预测效果;当进水氨氮质量浓度较高时,预测值略低于实际结果. 相似文献
20.
垦殖对湿地土壤有机碳垂直分布及可溶性有机碳截留的影响 总被引:7,自引:3,他引:4
通过测定和计算兴凯湖地区沼泽湿地及由其垦殖而来的旱田和水田土壤剖面有机碳含量和密度及土壤剖面不同深度土壤溶液中可溶性有机碳含量,分析了垦殖对兴凯湖周边沼泽湿地土壤有机碳垂直分布及土壤剖面截留可溶性有机碳的影响.结果表明,垦殖显著影响湿地0~40 cm土壤有机碳含量,大豆田和水稻田0~10、10~20、20~30、30~40 cm土壤有机碳含量与湿地相比分别降低了79.07%和82.01%、79.01%和82.28%、79.86%和92.90%、37.49%和78.05%;40 cm以下土层土壤有机碳含量垦殖前后差异不显著.大豆田和水稻田有机碳密度相比沼泽湿地分别降低了25.50%和47.35%,但三者1 m深土壤中大部分的有机碳均是储存在0~50 cm土层中.垦殖前后土壤有机碳含量与深度之间的关系均可用指数函数来描述,垦殖改变了土壤有机碳含量但并未改变其随土壤深度的变化规律.垦殖为大豆田土壤剖面对可溶性有机碳的截留效果较湿地和水稻田更明显,沼泽湿地和水稻田对可溶性有机碳的截留效果大致相当. 相似文献