Spontaneous symmetry breaking: formation of Janus micelles (2009)
Voets, I.K., Fokkink, R.G., Hellweg, T., King, S.M., ...
We describe the preparation and solution properties of Janus micelles, i.e., non-centrosymmetric nanoparticles with compartmentalized shells, via co-assembly of two fully water-soluble block...
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...
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...
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...
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...
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...
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...
Double-faced micelles from water-soluble polymers (2006)
Voets, I.K., Frederik, P.M., Bomans, P.H.H., Schmalz, H., ...
SANS2D at the ISIS Second Target Station (2006)
Heenan, R K, King, S M, Turner, DS, Treadgold, JR
Los Alamos National Laboratory Report, June 2006, pp780-785, Eds. G J Russell, J J Rhyne, B V Maes
The Structure of Metallomicelles (2004)
Griffiths, Peter Charles, Fallis, Ian Andrew, Willock, David James, Paul, Alison, Barrie, C. L., Griffiths, P. M., ...
The Structure of Metallomicelles (2004)
Griffiths, Peter Charles, Fallis, Ian Andrew, Willock, David James, Paul, Alison, Barrie, C. L., Griffiths, P. M., ...
The port of Wanganui and its influence on the City of Wanganui / (1964)
King, S. M. (Stafford Merrill)
Thesis (M.A.)--Victoria University of Wellington, 1964.