Where does rain come from? The first experimental evidence for the existence of the (H2O+O2−) charge transfer complex, predicted to play a key role as a nucleation center for atmospheric vapor photonucleation (see picture), is provided by the powerful neutralization – reionization mass spectrometric technique.

Direct Experimental Evidence for the H2O+O2- Charge Transfer Complex: Crucial Support to Atmospheric Photonucleation Theory / Cacace, Fulvio; De Petris, Giulia; Troiani, Anna; Pepi, Federico. - In: ANGEWANDTE CHEMIE. INTERNATIONAL EDITION. - ISSN 1433-7851. - STAMPA. - 39:2(2000), pp. 367-367. [10.1002/(SICI)1521-3773(20000117)39:2<367::AID-ANIE367>3.0.CO;2-I]

Direct Experimental Evidence for the H2O+O2- Charge Transfer Complex: Crucial Support to Atmospheric Photonucleation Theory

CACACE, Fulvio;DE PETRIS, GIULIA;TROIANI, Anna;PEPI, Federico
2000

Abstract

Where does rain come from? The first experimental evidence for the existence of the (H2O+O2−) charge transfer complex, predicted to play a key role as a nucleation center for atmospheric vapor photonucleation (see picture), is provided by the powerful neutralization – reionization mass spectrometric technique.
2000
01 Pubblicazione su rivista::01a Articolo in rivista
Direct Experimental Evidence for the H2O+O2- Charge Transfer Complex: Crucial Support to Atmospheric Photonucleation Theory / Cacace, Fulvio; De Petris, Giulia; Troiani, Anna; Pepi, Federico. - In: ANGEWANDTE CHEMIE. INTERNATIONAL EDITION. - ISSN 1433-7851. - STAMPA. - 39:2(2000), pp. 367-367. [10.1002/(SICI)1521-3773(20000117)39:2<367::AID-ANIE367>3.0.CO;2-I]
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11573/48792
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