The role of a nanoparticle monolayer on the flow of polymer melts in nanochannels

Nanoscale ◽  
2014 ◽  
Vol 6 (19) ◽  
pp. 11013-11018 ◽  
Author(s):  
Long-Biao Huang ◽  
Ye Zhou ◽  
Su-Ting Han ◽  
Yan Yan ◽  
Li Zhou ◽  
...  

The flowing behaviour of polymer melts in nanochannels with diverse surface conditions were experimentally investigated and the results are presented in this paper.

2007 ◽  
Vol 40 (17) ◽  
pp. 6325-6332 ◽  
Author(s):  
Regis Schach ◽  
Yvette Tran ◽  
Alain Menelle ◽  
Costantino Creton

2012 ◽  
Vol 9 (6) ◽  
pp. 7257-7289 ◽  
Author(s):  
L. Durantou ◽  
A. Rochon ◽  
D. Ledu ◽  
G. Massé

Abstract. Dinoflagellate cyst (dinocyst) assemblages have been widely used over the Arctic Ocean to reconstruct sea-surface parameters on a quantitative basis. Such reconstructions provide insights into the role of anthropogenic vs natural forcings in the actual climatic trend. Here, we present the palynological analysis of a 36 cm-long core collected from the Mackenzie Through in the Canadian Beaufort Sea. Dinocyst assemblages were used to quantitatively reconstruct the evolution of sea surface conditions (temperature, salinity, sea ice) and freshwater palynomorphs influxes were used as local paleo-river discharge indicators over the last ~150 yr. Dinocyst assemblages are dominated by autotrophic taxa (68 to 96 %). Pentapharsodinium dalei is the dominant specie throughout most of the core, except at the top where the assemblages are dominated by Operculodinium centrocarpum. Quantitative reconstructions of sea surface parameters display a serie of relatively warm, lower sea ice and saline episodes in surface waters, alternately with relatively cool and low salinity episodes. The warm episodes are characterized with high dinocyst productivity. Variations of dinocyst influxes and reconstructed sea surface conditions are closely linked to large scale atmospheric circulation patterns such as the Pacific Decadal Oscillation (PDO) and to a lesser degree, the Arctic Oscillation (AO). Positive phases of the PDO correspond to increases of dinocyst influxes, warmer and saltier surface waters, which we associate with upwelling events of warm and relatively saline water from Pacific origin. Freshwater palynomorph influxes increased in three phases from AD 1857 until reaching maximum values in AD 1991, suggesting that the Mackenzie River discharge followed the same trend when its discharge peaked between AD 1989 and AD 1992. The PDO mode seems to dominate the climatic variations at multi-annual to decadal timescales in the Western Canadian Arctic and Beaufort Sea areas.


2010 ◽  
Vol 10 (7) ◽  
pp. 17815-17851 ◽  
Author(s):  
N. A. Brunsell ◽  
D. B. Mechem ◽  
M. C. Anderson

Abstract. The role of land-atmosphere interactions under heterogeneous surface conditions is investigated in order to identify mechanisms responsible for altering surface heat and moisture fluxes. Twelve coupled land surface – large eddy simulation scenarios with four different length scales of surface variability under three different horizontal wind speeds are used in the analysis. The base case uses Landsat ETM imagery over the Cloud Land Surface Interaction Campaign (CLASIC) field site for 3 June 2007. Using wavelets, the surface fields are band-pass filtered in order to maintain the spatial mean and variances to length scales of 200 m, 1600 m, and 12.8 km as lower boundary conditions to the model. The simulations exhibit little variation in net radiation. Rather, a change in the partitioning of the surface energy between sensible and latent heat flux is responsible for differences in boundary layer dynamics. The sensible heat flux is dominant for intermediate surface length scales. For smaller and larger scales of surface heterogeneity, which can be viewed as being more homogeneous, the latent heat flux becomes increasingly important. The results reflect a general decrease of the Bowen ratio as the surface conditions transition from heterogeneous to homogeneous. Air temperature is less sensitive to surface heterogeneity than water vapor, which implies that the role of surface heterogeneity in modifying the local temperature gradients in order to maximize convective heat fluxes. More homogeneous surface conditions, on the other hand, tend to maximize latent heat flux. Scalar vertical profiles respond predictably to the partitioning of surface energy. Fourier spectra of the vertical wind speed, air temperature and specific humidity (w, T and q) and associated cospectra (w'T', w'q' and T'q'), however, are insensitive to the length scale of surface heterogeneity, but the near surface spectra are sensitive to the mean wind speed.


1991 ◽  
Vol 35 (6) ◽  
pp. 985-998 ◽  
Author(s):  
Bernard Tremblay
Keyword(s):  

1979 ◽  
Vol 36 (3) ◽  
pp. 340-345
Author(s):  
A. N. Prokunin ◽  
N. G. Proskurnina
Keyword(s):  

2006 ◽  
Vol 45 (4) ◽  
pp. 393-402 ◽  
Author(s):  
Thomas Schweizer ◽  
André Bardow

2012 ◽  
Vol 78 (24) ◽  
pp. 8849-8853 ◽  
Author(s):  
Ralf Moeller ◽  
Andrew C. Schuerger ◽  
Günther Reitz ◽  
Wayne L. Nicholson

ABSTRACTSpores of wild-type and mutantBacillus subtilisstrains lacking various structural components were exposed to simulated Martian atmospheric and UV irradiation conditions. Spore survival and mutagenesis were strongly dependent on the functionality of all of the structural components, with small acid-soluble spore proteins, coat layers, and dipicolinic acid as key protectants.


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