Sulfur-based denitrification: Effect of biofilm development on denitrification fluxes

被引:83
|
作者
Wang, Yue [1 ]
Bott, Charles [2 ]
Nerenberg, Robert [1 ]
机构
[1] Univ Notre Dame, Dept Civil & Environm Engn & Earth Sci, 156 Fitzpatrick Hall, Notre Dame, IN 46556 USA
[2] Hampton Rd Sanitat Dist, POB 5911, Virginia Beach, VA 23471 USA
关键词
Sulfur; Denitrification; Biofilm; Fluxes; Nitrite accumulation; WASTE-WATER TREATMENT; AUTOTROPHIC DENITRIFICATION; ELEMENTAL-SULFUR; NITRATE REMOVAL; DRINKING-WATER; CHEMOLITHOTROPHIC DENITRIFICATION; MICROBIAL COMMUNITY; KINETIC-PARAMETERS; GROUNDWATER; REDUCTION;
D O I
10.1016/j.watres.2016.05.020
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Elemental sulfur (S-o) can serve as an electron donor for denitrification. However, the mechanisms and rates of S-o-based denitrification, which depend on a biofilm development on a solid S-o surface, are not well understood. We used completely-mixed reactors packed with S-o chips to systematically explore the behavior of S-o-based denitrification as a function of the bulk nitrate (NO3-) concentration and biofilm development. High-purity (99.5%) and agricultural-grade (90% purity) S-o chips were tested to explore differences in performance. NO3- fluxes followed a Monod-type relationship with the bulk NO3- concentration. For high-purity S-o, the maximum NO3- flux increased from 0.4 gN/m(2)-d at 21 days to 0.9 g N/m(2)-d at around 100 days, but then decreased to 0.65 gN/m(2)-d at 161 days. The apparent (extant) half saturation constant for NO3- K-Sapp, based on the bulk NO3- concentration and NO3- fluxes into the biofilm, increased from 0.1 mgN/L at 21 days to 0.8 mgN/L at 161 days, reflecting the increasing mass transfer resistance as the biofilm thickness increased. Nitrite (NO2-) accumulation became significant at bulk NO3- concentration above 0.2 mgN/L. The behavior of the agricultural-grade S-o was very similar to the high-purity S-o. The kinetic behavior of S-based denitrification was consistent with substrate counter-diffusion, where the soluble sulfur species diffuse from the S-o particle into the base of the biofilm, while NO3- diffuses into the biofilm from the bulk. Initially, the fluxes were low due to biomass limitation (thin biofilms). As the biofilm thickness increased with time, the fluxes first increased, stabilized, and then decreased. The decrease was probably due to increasing diffusional resistance in the thick biofilm. Results suggest that fluxes comparable to heterotrophic biofilm processes can be achieved, but careful management of biofilm accumulation is important to maintain high fluxes. (C) 2016 Elsevier Ltd. All rights reserved.
引用
收藏
页码:184 / 193
页数:10
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