Scientific Commons: S. T. Martin

Loading-dependent elemental composition of α-pinene SOA particles (2009)

J. E. Shilling, Q. Chen, S. M. King, T. Rosenoern, J. H. Kroll, D. R. Worsnop, ...

The chemical composition of secondary organic aerosol (SOA) particles, formed by the dark ozonolysis of α-pinene, was characterized by a high-resolution time-of-flight aerosol mass spectrometer. The...

Increased cloud activation potential of secondary organic aerosol for atmospheric mass loadings (2009)

S. M. King, T. Rosenoern, J. E. Shilling, Q. Chen, S. T. Martin

The effect of organic particle mass loading from 1 to ≥100 μg m<sup>−3</sup> on the cloud condensation nuclei (CCN) properties of mixed organic-sulfate particles was...

Increased cloud activation potential of secondary organic aerosol for atmospheric mass loadings (2009)

S. M. King, T. Rosenoern, J. E. Shilling, Q. Chen, S. T. Martin

The effect of organic particle mass loading from 1 to ≥100 μg m<sup>−3</sup> on the cloud condensation nuclei (CCN) properties of mixed organic-sulfate particles was...

Cloud condensation nuclei in pristine tropical rainforest air of Amazonia: size-resolved measurements and modeling of atmospheric aerosol composition and CCN activity (2009)

S. S. Gunthe, S. M. King, D. Rose, Q. Chen, P. Roldin, D. K. Farmer, ...

Atmospheric aerosol particles serving as cloud condensation nuclei (CCN) are key elements of the hydrological cycle and climate. We have measured and characterized CCN at water vapor supersaturations...

Amorphous and crystalline aerosol particles interacting with water vapor – Part 1: Microstructure, phase transitions, hygroscopic growth and kinetic limitations (2009)

E. Mikhailov, S. Vlasenko, S. T. Martin, T. Koop, U. Pöschl

Interactions with water are crucial for the properties, transformation and climate effects of atmospheric aerosols. Here we outline characteristic features and differences in the interaction of...

Cloud condensation nuclei in pristine tropical rainforest air of Amazonia: size-resolved measurements and modeling of atmospheric aerosol composition and CCN activity (2009)

S. S. Gunthe, S. M. King, D. Rose, Q. Chen, P. Roldin, D. K. Farmer, ...

Atmospheric aerosol particles serving as cloud condensation nuclei (CCN) are key elements of the hydrological cycle and climate. We have measured and characterized CCN at water vapor supersaturations...

Particle mass yield in secondary organic aerosol formed by the dark ozonolysis of ?-pinene (2008)

Shilling, J. E., Chen, Q., King, S. M., Rosenoern, T., Kroll, J. H., Worsnop, D. R., ...

The yield of particle mass in secondary organic aerosol (SOA) formed by dark ozonolysis was measured for 0.3?22.8 ppbv of reacted ?-pinene. Most experiments were conducted using a continuous-flow...

Particle mass yield in secondary organic aerosol formed by the dark ozonolysis of ?-pinene (2008)

Shilling, J. E., Chen, Q., King, S. M., Rosenoern, T., Kroll, J. H., Worsnop, D. R., ...

The yield of particle mass in secondary organic aerosol (SOA) formed by dark ozonolysis was measured for 0.3?22.8 ppbv of reacted ?-pinene. Most experiments were conducted using a continuous-flow...

Particle mass yield in secondary organic aerosol formed by the dark ozonolysis of α-pinene (2008)

J. E. Shilling, Q. Chen, S. M. King, T. Rosenoern, J. H. Kroll, D. R. Worsnop, ...

The yield of particle mass in secondary organic aerosol (SOA) formed by dark ozonolysis was measured for 0.3–22.8 ppbv of reacted α-pinene. Most experiments were conducted using a...

Corrigendum to "The relative importance of competing pathways for the formation of high-molecular-weight peroxides in the ozonolysis of organic aerosol particles" published in Atmos. Chem. Phys., 6, 4851–4866, 2006 (2008)

M. Mochida, Y. Katrib, J. T. Jayne, D. R. Worsnop, S. T. Martin

No abstract available.

Loading-dependent elemental composition of α-pinene SOA particles (2008)

J. E. Shilling, Q. Chen, S. M. King, T. Rosenoern, J. H. Kroll, D. R. Worsnop, ...

The chemical composition of secondary organic aerosol (SOA) particles, formed by the dark ozonolysis of α-pinene, was characterized by a high-resolution time-of-flight aerosol mass spectrometer. The...

Loading-dependent elemental composition of α-pinene SOA particles (2008)

J. E. Shilling, Q. Chen, S. M. King, T. Rosenoern, J. H. Kroll, D. R. Worsnop, ...

The chemical composition of secondary organic aerosol (SOA) particles, formed by the dark ozonolysis of α-pinene, was characterized by a high-resolution time-of-flight aerosol mass spectrometer. The...

Particle mass yield in secondary organic aerosol formed by the dark ozonolysis of ?-pinene (2007)

Shilling, J. E., Chen, Q., King, S. M., Rosenoern, T., Kroll, J. H., Worsnop, D. R., ...

The yield of particle mass in secondary organic aerosol (SOA) formed by dark ozonolysis was measured for 0.3?22.8 ppbv of reacted ?-pinene. Most experiments were conducted using a continuous-flow...

Particle mass yield in secondary organic aerosol formed by the dark ozonolysis of ?-pinene (2007)

Shilling, J. E., Chen, Q., King, S. M., Rosenoern, T., Kroll, J. H., Worsnop, D. R., ...

The yield of particle mass in secondary organic aerosol (SOA) formed by dark ozonolysis was measured for 0.3?22.8 ppbv of reacted ?-pinene. Most experiments were conducted using a continuous-flow...

Particle mass yield in secondary organic aerosol formed by the dark ozonolysis of α-pinene (2007)

J. E. Shilling, Q. Chen, S. M. King, T. Rosenoern, J. H. Kroll, D. R. Worsnop, ...

The yield of particle mass in secondary organic aerosol (SOA) formed by dark ozonolysis was measured for 0.3–22.8 ppbv of reacted α-pinene. Most experiments were conducted using a...

Prompt deliquescence and efflorescence of aerosol nanoparticles (2006)

G. Biskos, D. Paulsen, L. M. Russell, P. R. Buseck, S. T. Martin

Literature reports have differed on the possibilities of discontinuous and continuous (i.e., prompt and nonprompt) deliquescence and efflorescence of aerosol particles in the nanosize regime....

The relative importance of competing pathways for the formation of high-molecular-weight peroxides in the ozonolysis of organic aerosol particles (2006)

Mochida, M., Katrib, Y., Jayne, J. T., Worsnop, D. R., Martin, S. T.

High-molecular-weight (HMW) organic compounds are an important component of atmospheric particles, although their origins, possibly including in situ formation pathways, remain incompletely...

Prompt deliquescence and efflorescence of aerosol nanoparticles (2006)

Biskos, G., Paulsen, D., Russell, L. M., Buseck, P. R., Martin, S. T.

Literature reports have differed on the possibilities of discontinuous and continuous (i.e., prompt and nonprompt) deliquescence and efflorescence of aerosol particles in the nanosize regime....

The relative importance of competing pathways for the formation of high-molecular-weight peroxides in the ozonolysis of organic aerosol particles (2006)

Mochida, M., Katrib, Y., Jayne, J.T., Worsnop, D.R., Martin, S.T.

High-molecular-weight (HMW) organic compounds are an important component of atmospheric particles, although their origins, possibly including in situ formation pathways, remain incompletely...

Prompt deliquescence and efflorescence of aerosol nanoparticles (2006)

Biskos, G., Paulsen, D., Russell, L. M., Buseck, P. R., Martin, S. T.

Literature reports have differed on the possibilities of discontinuous and continuous (i.e., prompt and nonprompt) deliquescence and efflorescence of aerosol particles in the nanosize regime....

The relative importance of competing pathways for the formation of high-molecular-weight peroxides in the ozonolysis of organic aerosol particles (2006)

Mochida, M., Katrib, Y., Jayne, J. T., Worsnop, D. R., Martin, S. T.

High-molecular-weight (HMW) organic compounds are an important component of atmospheric particles, although their origins, possibly including in situ formation pathways, remain incompletely...

Prompt deliquescence and efflorescence of aerosol nanoparticles (2006)

Biskos, G., Paulsen, D., Russell, L. M., Buseck, P. R., Martin, S. T.

Literature reports have differed on the possibilities of discontinuous and continuous (i.e., prompt and nonprompt) deliquescence and efflorescence of aerosol particles in the nanosize regime....

The relative importance of competing pathways for the formation of high-molecular-weight peroxides in the ozonolysis of organic aerosol particles (2006)

Mochida, M., Katrib, Y., Jayne, J.T., Worsnop, D.R., Martin, S.T.

High-molecular-weight (HMW) organic compounds are an important component of atmospheric particles, although their origins, possibly including in situ formation pathways, remain incompletely...

Prompt deliquescence and efflorescence of aerosol nanoparticles (2006)

Biskos, G., Paulsen, D., Russell, L. M., Buseck, P. R., Martin, S. T.

Literature reports have differed on the possibilities of discontinuous and continuous (i.e., prompt and nonprompt) deliquescence and efflorescence of aerosol particles in the nanosize regime....

Density changes of aerosol particles as a result of chemical reaction (2005)

Y. Katrib, S. T. Martin, Y. Rudich, P. Davidovits, J. T. Jayne, D. R. Worsnop

This paper introduces the capability to study simultaneously changes in the density, the chemical composition, the mobility diameter, the aerodynamic diameter, and the layer thickness of...

Aberrant Methylation of the Human Hedgehog Interacting Protein (HHIP) Gene in Pancreatic Neoplasms (2005)

Martin, S.T., Sato, N., Dhara, S., Chang, R., Hustinx, S.R., Maitra, A., ...

Density changes of aerosol particles as a result of chemical reaction (2005)

Katrib, Y., Martin, S. T., Rudich, Y., Davidovits, P., Jayne, J. T., Worsnop, D. R.

This paper introduces the capability to study simultaneously changes in the density, the chemical composition, the mobility diameter, the aerodynamic diameter, and the layer thickness of...

Density changes of aerosol particles as a result of chemical reaction (2005)

Katrib, Y., Martin, S. T., Rudich, Y., Davidovits, P., Jayne, J. T., Worsnop, D. R.

This paper introduces the capability to study simultaneously changes in the density, the chemical composition, the mobility diameter, the aerodynamic diameter, and the layer thickness of...

Effects of the physical state of tropospheric ammonium-sulfate-nitrate particles on global aerosol direct radiative forcing (2004)

S. T. Martin, R. J. Park, D. J. Jacob, K. V. Chance, ...