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引用次数: 0
摘要
利用有机废水制氢具有产生清洁能源和生物修复的双重优势,可持续时间更长。为了最大限度地从富含淀粉的废水中回收能量,采用了一种由嗜热暗发酵和微生物燃料电池组成的两级系统。采用单参数优化策略对批处理系统进行了优化。在初始底物浓度(COD)为35 g L−1、温度为60℃、pH为6.5的最佳条件下,最大累积产氢量为2.56 L L−1,COD降低48%。H2产率和H2产率分别为6.8 mol H2/kg coreduced和731.3 mL L−1 h−1。在连续搅拌槽式反应器(CSTR)中研究了有机负载率(OLR)对产氢率的影响。在OLR为5.6 g L−1 h−1时,最大产氢率为913 mL L−1 h−1。出水回用对提高产氢率有重要作用。在循环倍率为0.6的条件下,最大产氢率为1224 mL L−1 h−1。利用碳酸盐缓冲液中和的深色发酵废培养基,在最佳pH为7时,MFC观察到功率密度为4.2 W m−3。总COD降低了86%。
Maximization of Energy Recovery from Starch Processing Wastewater by Thermophilic Dark Fermentation Coupled with Microbial fuel Cell Technology
Utilization of organic wastewater for hydrogen production has dual advantages of clean energy generation and bioremediation, which is sustainable for a longer period. To maximize the energy recovery from starch rich wastewater, a two stage system comprising of thermophilic dark fermentation coupled with microbial fuel cell was employed. A single parameter optimization strategy was implemented for the operation of the batch system. The maximum cumulative hydrogen production obtained was 2.56 L L−1 with a 48% reduction in COD under the optimal conditions of 35 g L−1 initial substrate concentration (COD), temperature 60 °C, and pH 6.5. The H2 yield and H2 production rate were 6.8 mol H2/kg CODreduced and 731.3 mL L−1 h−1, respectively. The effect of the organic loading rate (OLR) on H2 production rate was studied in a continuous stirred tank reactor (CSTR). A maximum hydrogen production rate of 913 mL L−1 h−1 was observed at an OLR of 5.6 g L−1 h−1. Effluent recycle played an important role in the improvement of H2 production. A maximum H2 production rate of 1224 mL L−1 h−1 was observed at a recycle ratio of 0.6. Power density of 4.2 W m−3 was observed with MFC using the dark fermentative spent media neutralized with carbonate buffer at an optimal pH of 7. A total COD reduction of 86% was observed.
期刊介绍:
Geomicrobiology Journal is a unified vehicle for research and review articles in geomicrobiology and microbial biogeochemistry. One or two special issues devoted to specific geomicrobiological topics are published each year. General articles deal with microbial transformations of geologically important minerals and elements, including those that occur in marine and freshwater environments, soils, mineral deposits and rock formations, and the environmental biogeochemical impact of these transformations. In this context, the functions of Bacteria and Archaea, yeasts, filamentous fungi, micro-algae, protists, and their viruses as geochemical agents are examined.
Articles may stress the nature of specific geologically important microorganisms and their activities, or the environmental and geological consequences of geomicrobiological activity.
The Journal covers an array of topics such as:
microbial weathering;
microbial roles in the formation and degradation of specific minerals;
mineralization of organic matter;
petroleum microbiology;
subsurface microbiology;
biofilm form and function, and other interfacial phenomena of geological importance;
biogeochemical cycling of elements;
isotopic fractionation;
paleomicrobiology.
Applied topics such as bioleaching microbiology, geomicrobiological prospecting, and groundwater pollution microbiology are addressed. New methods and techniques applied in geomicrobiological studies are also considered.