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[长江水臭氧氧化过程中溴酸盐生成的影响因素]

[Influence factors of bromate formation in Yangtze River water during ozonation process].

作者信息

Lu Ning, Gao Nai-Yun, Huang Xin

机构信息

State Key Laboratory of Pollution Control and Resources Reuse, Tongji University, Shanghai 200092, China.

出版信息

Huan Jing Ke Xue. 2009 May 15;30(5):1386-90.

Abstract

A serial bench-scale experiments were conducted to study the effect of ammonia, pH, initial dissolved ozone and temperature on bromate formation during ozonation process in Yangtze river water, where bromide anion (Br(-)) was detected. Ammonia has little suppression effects on bromate production in Yangtze water at pH 7.35 and 0.6 mg/L ammonia background concentration, for it can't block the indirect-direct path. Within our experiment's conditions, at the initial dissolved ozone from 0.8 mg/L to 2.5 mg/L, it should be kept below 1.2 mg/L in order to avoid bromate standard violation. BrO3(-) formation is sensitive to pH variation. BrO3(-) production is 8 microg/L when pH decreases to 6.3. Lower temperature leads to both slower ozone decomposition and lower production of bromate. BrO3(-) production is 9.1 microg/L at 10 degrees C, 100 microg/L initial Br(-) and 1.6 mg/L initial dissolved ozone.

摘要

进行了一系列实验室规模的实验,以研究氨、pH值、初始溶解臭氧和温度对长江水臭氧氧化过程中溴酸盐形成的影响,长江水中检测到了溴离子(Br(-))。在pH值为7.35且氨背景浓度为0.6mg/L的长江水中,氨对溴酸盐生成的抑制作用很小,因为它无法阻断间接-直接路径。在我们的实验条件下,初始溶解臭氧浓度在0.8mg/L至2.5mg/L之间时,为避免溴酸盐超标,应将其保持在1.2mg/L以下。BrO3(-)的形成对pH值变化敏感。当pH值降至6.3时,BrO3(-)的生成量为8μg/L。较低的温度导致臭氧分解速度减慢,溴酸盐生成量降低。在10℃、初始Br(-)为100μg/L和初始溶解臭氧为1.6mg/L的条件下,BrO3(-)的生成量为9.1μg/L。

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