ATMOSPHERIC AEROSOL-PARTICLES AND THEIR ROLE IN THE FORMATION OF DEW ON THE SURFACE OF PLANT-LEAVES

被引:23
作者
EIDEN, R
BURKHARDT, J
BURKHARDT, O
机构
[1] Lehrstuhl für Hydrologie, Abteilung Meteorologie, University of Bayreuth, 8580 Bayreuth
[2] Lehrstuhl für Hydrologie, Abteilung Meteorologie, University of Bayreuth, 8580 Bayreuth, Crailsheim
关键词
D O I
10.1016/0021-8502(94)90087-6
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
Measurements of the electrical conductivity along the surface of leaves or conifer needles show that the wetting of such surfaces coated with wax already starts below a relative humidity of 100%. To explain the observations, the deposition of water soluble atmospheric aerosol particles on these surfaces is taken into account. It is shown that the capillary space between particle and settling surface and, as an additional indispensable condition, the water solubility of at least some constituents of the atmospheric aerosol particle (i.e. a combined capillary solution effect), permits the formation of condensate or dew water significantly below a r.h. of 100%.
引用
收藏
页码:367 / 376
页数:10
相关论文
共 8 条
[1]  
Burkhardt J, 1990, TREES-STRUCT FUNCT, V4, P22, DOI 10.1007/BF00226236
[2]  
EUTENAUERMACHER T, 1990, DISSERATIONES BOTANI, V150
[3]   TOWARDS MODELING THE MENISCUS GEOMETRY AND VOLUME OF CAPILLARY WATER BETWEEN 2 CONTACTING MICROSPHERES IN MOISTAIR [J].
GLASSTETTER, R ;
RICKETTS, CI ;
WILHELM, JG .
JOURNAL OF AEROSOL SCIENCE, 1991, 22 :S195-S198
[4]   MODELING THE DRY DEPOSITION VELOCITY OF AEROSOL-PARTICLES TO A SPRUCE FOREST [J].
PETERS, K ;
EIDEN, R .
ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS, 1992, 26 (14) :2555-2564
[5]  
Rogers R. R., 1996, SHORT COURSE CLOUD P
[6]  
WILLMORE TJ, 1972, INTRO DIFFERENTIAL G
[7]  
Winkler P., 1973, Journal of Aerosol Science, V4, P373, DOI 10.1016/0021-8502(73)90027-X
[8]  
WOLF KL, 1959, PHYSIK CHEM GRENZFLA, V2