THE DISSOCIATION-CONSTANT OF AMMONIUM-NITRATE AND ITS DEPENDENCE ON TEMPERATURE, RELATIVE-HUMIDITY AND PARTICLE-SIZE

被引:236
作者
MOZURKEWICH, M
机构
[1] Department of Chemistry, York University, North York, Ont. M3J 1P3
来源
ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS | 1993年 / 27卷 / 02期
关键词
DISSOCIATION CONSTANT; AMMONIUM NITRATE; GAS PARTICLE EXCHANGE; AEROSOL EQUILIBRIA;
D O I
10.1016/0960-1686(93)90356-4
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The dissociation constant of NH4NO3(c, IV) is determined from the evaluation of literature data from a variety of sources. Three different methods of calculation using five independent data sets lead to accurate values of the dissociation constant; these are in excellent agreement with each other. The recommended value of the standard free energy of dissociation of NH4NO3(c, IV) to NH3(g) and HNO3(g) is 93.4 +/- 0.3 kJ mol-1. Over the temperature range for which crystalline phase IV is stable(-17 to 32-degrees-C), the temperature dependence of the dissociation constant (in units of nb2) is given to within +/- 12% by ln (K(p)) = 118.87 - 24084/T - 6.025 ln (T). Equations are also given for the computation of the dissociation constant of NH4NO3(aq) to NH3(g) and HNO3(g) as a function of temperature and either solution concentration or equilibrium relative humidity. For saturated solutions these equations are consistent with the results for the solid, and for dilute solutions they are consistent with data on dilute solutions of NH3(aq) and HNO3(aq). For particles with radii less than 0.1 mum, the Kelvin effect has a substantial effect on the dissociation constant. However, particle size has little effect on the deliquescence point.
引用
收藏
页码:261 / 270
页数:10
相关论文
共 43 条
[1]   FIELD-MEASUREMENTS OF THE DISSOCIATION OF AMMONIUM-NITRATE AND AMMONIUM-CHLORIDE AEROSOLS [J].
ALLEN, AG ;
HARRISON, RM ;
ERISMAN, JW .
ATMOSPHERIC ENVIRONMENT, 1989, 23 (07) :1591-1599
[2]   DISSOCIATION CONSTANT OF AQUEOUS AMMONIA AT 0 TO 50-DEGREES FROM EMF STUDIES OF THE AMMONIUM SALT OF A WEAK ACID [J].
BATES, RG ;
PINCHING, GD .
JOURNAL OF THE AMERICAN CHEMICAL SOCIETY, 1950, 72 (03) :1393-1396
[3]  
Brandner J.D., 1962, J CHEM ENG DATA, V7, P227, DOI DOI 10.1021/JE60013A020
[4]   NUMERICAL MODELING OF CONCENTRATIONS AND FLUXES OF HNO3, NH3, AND NH4NO3 NEAR THE SURFACE [J].
BROST, RA ;
DELANY, AC ;
HUEBERT, BJ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1988, 93 (D6) :7137-7152
[5]  
Chase M.W., 1985, JANAF THERMOCHEMICAL, Vthird
[6]   EQUILIBRIUM PARTIAL PRESSURES AND MEAN ACTIVITY AND OSMOTIC COEFFICIENTS OF 0-100-PERCENT NITRIC-ACID AS A FUNCTION OF TEMPERATURE [J].
CLEGG, SL ;
BRIMBLECOMBE, P .
JOURNAL OF PHYSICAL CHEMISTRY, 1990, 94 (13) :5369-5380
[7]  
Cox J.D., 1989, CODATA KEY VALUES TH
[8]   STANDARD ENTHALPY OF FORMATION OF AMMONIUM-NITRATE AND OF THE NITRATE ION [J].
COX, JD ;
HARROP, D ;
HEAD, AJ .
JOURNAL OF CHEMICAL THERMODYNAMICS, 1979, 11 (08) :811-814
[9]   SOLUBILITY OF AMMONIA IN LIQUID WATER AND GENERATION OF TRACE LEVELS OF STANDARD GASEOUS AMMONIA [J].
DASGUPTA, PK ;
DONG, S .
ATMOSPHERIC ENVIRONMENT, 1986, 20 (03) :565-570