human | Q5 |
P6178 | Dimensions author ID | 0757632077.27 |
P2930 | INSPIRE-HEP author ID | A.Kurten.1 |
P496 | ORCID iD | 0000-0002-8955-4450 |
P108 | employer | Goethe University Frankfurt | Q50662 |
P734 | family name | Kürten | Q56025768 |
Kürten | Q56025768 | ||
Kürten | Q56025768 | ||
P735 | given name | Andreas | Q4926263 |
Andreas | Q4926263 | ||
P106 | occupation | researcher | Q1650915 |
P21 | sex or gender | male | Q6581097 |
Q56944687 | A fibre-optic UV system for H2SO4 production in aerosol chambers causing minimal thermal effects |
Q56944619 | Aerosol nucleation and growth in a mixture of sulfuric acid/alpha-pinene oxidation products at the CERN CLOUD chamber |
Q57204076 | Applicability of condensation particle counters to measure atmospheric clusters |
Q57204055 | Bisulfate – cluster based atmospheric pressure chemical ionization mass spectrometer for high-sensitivity (< 100 ppqV) detection of atmospheric dimethyl amine: proof-of-concept and first ambient data from boreal forest |
Q39648251 | Calibration of a chemical ionization mass spectrometer for the measurement of gaseous sulfuric acid |
Q56627327 | Causes and importance of new particle formation in the present-day and preindustrial atmospheres |
Q57204071 | Characterization of a Modified Expansion Condensation Particle Counter for Detection of Nanometer-Sized Particles |
Q57204077 | Characterization of an Automated, Water-Based Expansion Condensation Nucleus Counter for Ultrafine Particles |
Q57689156 | Characterization of diethylene glycol-condensation particle counters for detection of sub-3 nm particles |
Q57204050 | Characterization of the mass-dependent transmission efficiency of a CIMS |
Q116907468 | Chemical composition of nanoparticles from α-pinene nucleation and the influence of isoprene and relative humidity at low temperature |
Q57204066 | Comparison of chemical characteristics of 495 biomass burning plumes intercepted by the NASA DC-8 aircraft during the ARCTAS/CARB-2008 field campaign |
Q33469905 | Comparison of the SAWNUC model with CLOUD measurements of sulphuric acid-water nucleation |
Q57204064 | Contribution of sulfuric acid and oxidized organic compounds to particle formation and growth |
Q57204052 | Detection of dimethylamine in the low pptv range using nitrate chemical ionization atmospheric pressure interface time-of-flight (CI-APi-TOF) mass spectrometry |
Q28829189 | Effect of dimethylamine on the gas phase sulfuric acid concentration measured by Chemical Ionization Mass Spectrometry |
Q56944544 | Effect of ions on sulfuric acid-water binary particle formation: 2. Experimental data and comparison with QC-normalized classical nucleation theory |
Q57204058 | Effect of ions on the measurement of sulfuric acid in the CLOUD experiment at CERN |
Q21129046 | Elemental composition and clustering behaviour of α-pinene oxidation products for different oxidation conditions |
Q57204070 | Enhanced organic mass fraction and decreased hygroscopicity of cloud condensation nuclei (CCN) during new particle formation events |
Q56944521 | Evaporation of sulfate aerosols at low relative humidity |
Q57204074 | Evidence for ice particles in the tropical stratosphere from in-situ measurements |
Q56944644 | Evolution of particle composition in CLOUD nucleation experiments |
Q55090434 | Experimental investigation of ion–ion recombination under atmospheric conditions |
Q56944552 | Experimental particle formation rates spanning tropospheric sulfuric acid and ammonia abundances, ion production rates, and temperatures |
Q36176724 | Global atmospheric particle formation from CERN CLOUD measurements |
Q116907452 | High Gas-Phase Methanesulfonic Acid Production in the OH-Initiated Oxidation of Dimethyl Sulfide at Low Temperatures |
Q56944565 | Hygroscopicity of nanoparticles produced from homogeneous nucleation in the CLOUD experiments |
Q56944473 | Influence of temperature on the molecular composition of ions and charged clusters during pure biogenic nucleation |
Q56944506 | Influence of temperature on the molecular composition of ions and charged clusters during pure biogenic nucleation |
Q33463377 | Insight into acid-base nucleation experiments by comparison of the chemical composition of positive, negative, and neutral clusters |
Q125902777 | Iodine oxoacids enhance nucleation of sulfuric acid particles in the atmosphere |
Q31101741 | Ion-induced nucleation of pure biogenic particles. |
Q56944659 | Measurement of neutral sulfuric acid-dimethylamine clusters using CI-APi-TOF-MS |
Q56944496 | Measurement-model comparison of stabilized Criegee Intermediate and Highly Oxygenated Molecule production in the CLOUD chamber |
Q56944480 | Measurement–model comparison of stabilized Criegee intermediate and highly oxygenated molecule production in the CLOUD chamber |
Q56944572 | Modeling the thermodynamics and kinetics of sulfuric acid-dimethylamine-water nanoparticle growth in the CLOUD chamber |
Q90281454 | Molecular Composition and Volatility of Nucleated Particles from α-Pinene Oxidation between -50 °C and +25 °C |
Q37256141 | Molecular understanding of atmospheric particle formation from sulfuric acid and large oxidized organic molecules |
Q43829556 | Molecular understanding of sulphuric acid-amine particle nucleation in the atmosphere |
Q59750830 | Multicomponent new particle formation from sulfuric acid, ammonia, and biogenic vapors |
Q34409197 | Neutral molecular cluster formation of sulfuric acid-dimethylamine observed in real time under atmospheric conditions |
Q39137680 | New particle formation in the free troposphere: A question of chemistry and timing. |
Q59309434 | New particle formation in the sulfuric acid-dimethy lamine-water system: Reevaluation of CLOUD chamber measurements and comparison to an aerosol nucleation and growth model |
Q56944484 | New particle formation in the sulfuric acid–dimethylamine–water system: reevaluation of CLOUD chamber measurements and comparison to an aerosol nucleation and growth model |
Q57204063 | Numerical simulations of mixing conditions and aerosol dynamics in the CERN CLOUD chamber |
Q57204053 | Observation of new particle formation and measurement of sulfuric acid, ammonia, amines and highly oxidized organic molecules at a rural site in central Germany |
Q56944599 | On the composition of ammonia–sulfuric-acid ion clusters during aerosol particle formation |
Q56944591 | On the derivation of particle nucleation rates from experimental formation rates |
Q30821881 | Oxidation products of biogenic emissions contribute to nucleation of atmospheric particles |
Q57204068 | Performance of a corona ion source for measurement of sulfuric acid by chemical ionization mass spectrometry |
Q57204059 | Performance of diethylene glycol-based particle counters in the sub-3 nm size range |
Q94671784 | Rapid growth of new atmospheric particles by nitric acid and ammonia condensation |
Q58697490 | Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature range |
Q31139659 | Reduced anthropogenic aerosol radiative forcing caused by biogenic new particle formation |
Q116907484 | Role of iodine oxoacids in atmospheric aerosol nucleation |
Q56944672 | Role of organics in particle nucleation: From the lab to global model |
Q34210669 | Role of sulphuric acid, ammonia and galactic cosmic rays in atmospheric aerosol nucleation |
Q57204072 | Secondary organic aerosol formation from photooxidation of naphthalene and alkylnaphthalenes: implications for oxidation of intermediate volatility organic compounds (IVOCs) |
Q96231421 | Size-dependent influence of NOx on the growth rates of organic aerosol particles |
Q116907461 | Survival of newly formed particles in haze conditions |
Q115778993 | Synergistic HNO-HSO-NH upper tropospheric particle formation |
Q56944682 | Ternary H[sub 2]SO[sub 4]-H[sub 2]O-NH[sub 3] neutral and charged nucleation rates for a wide range of atmospheric conditions |
Q116907474 | The driving factors of new particle formation and growth in the polluted boundary layer |
Q36925572 | The effect of acid-base clustering and ions on the growth of atmospheric nano-particles |
Q56836096 | The radiative effect of ion-induced inorganic nucleation in the free troposphere |
Q56944527 | The role of ions in new particle formation in the CLOUD chamber |
Q56944501 | The role of ions in new-particle formation in the CLOUD chamber |
Q39137666 | The role of low-volatility organic compounds in initial particle growth in the atmosphere. |
Q56944605 | Thermodynamics of the formation of sulfuric acid dimers in the binary (H2SO4–H2O) and ternary (H2SO4–H2O–NH3) system |
Q51662477 | Trace detection of organic compounds in complex sample matrixes by single photon ionization ion trap mass spectrometry: real-time detection of security-relevant compounds and online analysis of the coffee-roasting process. |
Q43297156 | Unexpected epoxide formation in the gas-phase photooxidation of isoprene |
Q57204049 | Unexpectedly acidic nanoparticles formed in dimethylamine-ammonia-sulfuric acid nucleation experiments at CLOUD |
Q56944532 | Unexpectedly acidic nanoparticles formed in dimethylamine–ammonia–sulfuric-acid nucleation experiments at CLOUD |
Search more.