LASER-BASED STUDIES OF REACTIONS OF THE NITRATE RADICAL IN AQUEOUS-SOLUTION

被引:72
作者
EXNER, M
HERRMANN, H
ZELLNER, R
机构
来源
BERICHTE DER BUNSEN-GESELLSCHAFT-PHYSICAL CHEMISTRY CHEMICAL PHYSICS | 1992年 / 96卷 / 03期
关键词
ATMOSPHERIC CHEMISTRY; CHEMICAL KINETICS; PHOTOCHEMISTRY; RADICALS IN AQUEOUS SOLUTION;
D O I
10.1002/bbpc.19920960347
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
A new experimental technique for temperature dependent studies of the kinetics of the nitrate radical (NO3) in aqueous solution has been developed. In this technique NO3 is produced by excimer laser photolysis of peroxodisulfate anions at 351 nm in the presence of excess nitrate and detected by time-resolved long-path laser absorption using the 632.8 nm line of a HeNe-laser. - For the generation reaction of NO3, viz. (1) SO4- + NO3- --> SO42- + NO3 a rate constant of k1 = (5.0 +/- 0.5) . 10(4) l/mol . s at T = 298 K and zero ionic strength was found. For the reactions (2) NO3 + OH- --> NO3- + OH and (3) NO3 + Cl- --> NO3 + Cl rate coefficients of k2 = (8.2 +/- 0.9) - 10(7) and k3 = (1.0 +/- 0.2) . 10(7) l/mol . s were determined at T = 298 K. In temperature dependent experiments the Arrhenius expressions k2 (T) (8.1 +/- 0.4) . 10(11) exp[-(2700 +/- 400)K/T] l/mol . s and k3 (T) = (1.9 +/- 0.2) - 10(13) exp[-(4300 +/- 500) K/T] l/mol . s were derived. - The rate constant of the reaction of NO3 with dissolved sulfur (IV) has been studied over a range of pH-values and temperature. For the reactions with SO2(aq) (4), and HSO3-(5) rate coefficients of k4 = (2.3 +/- 0.5) . 10(8) and k5 = (1.4 +/- 0.1) . 1O(9) l/mol . s, respectively, at 298 K were obtained. The corresponding temperature dependences are described by: k4(T) = (5.6 +/- 0.7) . 10(13) exp[-(3700 +/- 1100)K/T] l/mol . s and k5(T) = (1.1 +/- 0.2) . 10(12) exp[-(2000 +/- 400)K/T] l/mol . s. For the reaction of NO3 with SO32- (6) a rate constant of k6 = (3.0 +/- 0.4) . 10(8) l/mol . s was derived at T = 278 K.
引用
收藏
页码:470 / 477
页数:8
相关论文
共 33 条
[1]  
BERDNIKOV VM, 1970, ZH FIZ KHIM+, V44, P395
[2]   POSSIBLE ROLE OF NO3 IN THE NIGHTTIME CHEMISTRY OF A CLOUD [J].
CHAMEIDES, WL .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1986, 91 (D5) :5331-5337
[3]   THE FREE-RADICAL CHEMISTRY OF CLOUD DROPLETS AND ITS IMPACT UPON THE COMPOSITION OF RAIN [J].
CHAMEIDES, WL ;
DAVIS, DD .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1982, 87 (NC7) :4863-4877
[4]   POSSIBLE ROLE OF NO3 IN THE NIGHTTIME CHEMISTRY OF A CLOUD - REPLY [J].
CHAMEIDES, WL .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1986, 91 (D13) :14571-14572
[5]   THE PHOTOCHEMISTRY OF A REMOTE MARINE STRATIFORM CLOUD [J].
CHAMEIDES, WL .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1984, 89 (ND3) :4739-4755
[6]  
CHAMEIDES WL, 1983, PRECIPITATION SCAVEN
[7]   The extent of dissociation of salts in water. Part VIII. An equation for the mean ionic activity coefficient of an electroltye in water, and a revision of the dissociation constants of some sulphates [J].
Davies, CW .
JOURNAL OF THE CHEMICAL SOCIETY, 1938, :2093-2098
[8]  
Debye V.P., 1925, PHYS Z, V26, P22
[9]  
Finlayson-Pitts B.J., 1986, ATMOSPHERIC CHEM
[10]  
FROST AA, 1961, KINETICS MECHANISMS