中国环境科学
中國環境科學
중국배경과학
CHINA ENVIRONMENTAL SCIENCE
2014年
4期
966-975
,共10页
王鹍%夏平平%刘凡%谭文峰%邱国红%冯雄汉
王鹍%夏平平%劉凡%譚文峰%邱國紅%馮雄漢
왕곤%하평평%류범%담문봉%구국홍%풍웅한
As(III)%δ-MnO2%搅拌流动法%动力学%速率常数%反应位点
As(III)%δ-MnO2%攪拌流動法%動力學%速率常數%反應位點
As(III)%δ-MnO2%교반류동법%동역학%속솔상수%반응위점
As (III)%δ-MnO2%stirred-flow technique%kinetics%rate constant%reactive site
采用搅拌流动法研究了酸性水钠锰矿及水羟锰矿2种δ-MnO2矿物氧化As(Ⅲ)的动力学过程,构建了可用于多相体系的搅拌-流动氧化还原反应动力学模型.经过As吸附量的校正后,该模型对酸性水钠锰矿及水羟锰矿氧化As(III)动力学数据拟合度分别为0.980和0.951,模型拟合得到pH 7时2种矿物单位比表面上氧化As(III)的初始反应速率常数k分别为0.131,0.014min-1?m-2.相比而言,该速率常数明显高于批量法得到的表观速率常数kobs,0.021,0.001min-1?m-2更接近真实的化学动力学参数.搅拌流动法与批量法得到的不同矿物的速率常数大小趋势一致,即尽管酸性水钠锰矿对 As(III)的氧化率低于水羟锰矿,单位比表面上酸性水钠锰矿氧化 As(III)初始反应速率却远高于水羟锰矿.反应过程分析表明,反应初始阶段,As(III)的吸附为主要限速步骤;而随着反应的进行,矿物表面反应位点逐渐钝化或减少,反应位点数量成为限速步骤.
採用攪拌流動法研究瞭痠性水鈉錳礦及水羥錳礦2種δ-MnO2礦物氧化As(Ⅲ)的動力學過程,構建瞭可用于多相體繫的攪拌-流動氧化還原反應動力學模型.經過As吸附量的校正後,該模型對痠性水鈉錳礦及水羥錳礦氧化As(III)動力學數據擬閤度分彆為0.980和0.951,模型擬閤得到pH 7時2種礦物單位比錶麵上氧化As(III)的初始反應速率常數k分彆為0.131,0.014min-1?m-2.相比而言,該速率常數明顯高于批量法得到的錶觀速率常數kobs,0.021,0.001min-1?m-2更接近真實的化學動力學參數.攪拌流動法與批量法得到的不同礦物的速率常數大小趨勢一緻,即儘管痠性水鈉錳礦對 As(III)的氧化率低于水羥錳礦,單位比錶麵上痠性水鈉錳礦氧化 As(III)初始反應速率卻遠高于水羥錳礦.反應過程分析錶明,反應初始階段,As(III)的吸附為主要限速步驟;而隨著反應的進行,礦物錶麵反應位點逐漸鈍化或減少,反應位點數量成為限速步驟.
채용교반류동법연구료산성수납맹광급수간맹광2충δ-MnO2광물양화As(Ⅲ)적동역학과정,구건료가용우다상체계적교반-류동양화환원반응동역학모형.경과As흡부량적교정후,해모형대산성수납맹광급수간맹광양화As(III)동역학수거의합도분별위0.980화0.951,모형의합득도pH 7시2충광물단위비표면상양화As(III)적초시반응속솔상수k분별위0.131,0.014min-1?m-2.상비이언,해속솔상수명현고우비량법득도적표관속솔상수kobs,0.021,0.001min-1?m-2경접근진실적화학동역학삼수.교반류동법여비량법득도적불동광물적속솔상수대소추세일치,즉진관산성수납맹광대 As(III)적양화솔저우수간맹광,단위비표면상산성수납맹광양화 As(III)초시반응속솔각원고우수간맹광.반응과정분석표명,반응초시계단,As(III)적흡부위주요한속보취;이수착반응적진행,광물표면반응위점축점둔화혹감소,반응위점수량성위한속보취.
In this study, As (III) oxidation at the surfaces of two δ-MnO2 minerals, birnessite and vernadite, was investigated using stirred-flow technique, and the corresponding model was established to describe the kinetics of the redox reactions in the stirred-flow heterogeneous system. Following correction of As adsorption, the degree of fitting of the stirred-flow kinetic data of As (III) oxidation by birnessite and vernadite using the established model was 0.980and 0.951, respectively. The obtained initial rate constants (k) per unit specific area at pH 7were 0.131 and 0.014min-1m-2, respectively, which were much greater than apparent initial rate constant (kobs), 0.021min-1m-2 and 0.001min-1m-2, derived from the batch experiments. This indicated that rate constant (k) is much closer to the real chemical kintics that could be obtained using the stirred-flow technique. Both stirred-flow and the batch experiments showed that birnessite exhibited the greater reaction rate on a per surface area basis in As (III) oxidation than on vernadite, although birnessite had a relatively lower suface area and As (III) oxidation capacity. Analysis of the reaction process suggested that As (III) absorption was the rate determining step in the initial stage, and then the number of suface Mn reactive sites gradually became the rate determining step with the passivation and decrease of the sites.