Berndt Torsten, Böge Olaf, Stratmann Frank, Heintzenberg Jost, Kulmala Markku
Leibniz-Institut für Troposphärenforschung e.V., Permoserstrasse 15, 04318 Leipzig, Germany.
Science. 2005 Feb 4;307(5710):698-700. doi: 10.1126/science.1104054.
We investigated the formation of new particles in a laboratory study, starting from H2SO4 produced in situ through the reaction of OH radicals with SO2. Newly formed particles were observed for H2SO4 concentrations above 7 x 10(6) per cubic centimeter. At 293 kelvin, a rough estimate yielded a nucleation rate of 0.3 to 0.4 particles per cubic centimeter per second for approximately 10(7) particles per cubic centimeter of H2SO4 (particle size >/= 3 nanometers). These findings are in agreement with observations from the atmosphere. The results demonstrate that under laboratory conditions similar to the atmosphere, particle formation occurs at atmospheric H2SO4 concentration levels.
我们在一项实验室研究中,从通过羟基自由基与二氧化硫反应原位生成的硫酸出发,对新粒子的形成进行了研究。当硫酸浓度高于每立方厘米7×10⁶时,观察到了新形成的粒子。在293开尔文时,对于每立方厘米约10⁷个硫酸粒子(粒径≥3纳米),粗略估计得出的成核速率为每秒每立方厘米0.3至0.4个粒子。这些发现与大气观测结果一致。结果表明,在与大气相似的实验室条件下,在大气硫酸浓度水平会发生粒子形成。