Temperature and Field Dependence of Protonated Water Cluster Emission from Field Adsorbed Water Layers on Platinum

2001 ◽  
Author(s):  
Christopher J. Rothfuss ◽  
Valentin K. Medvedev ◽  
Eric M. Stuve
Keyword(s):  
Field Dependence ◽  
Water Cluster ◽  
Adsorbed Water ◽  
Cluster Emission ◽  
Water Layers

Temperature and field dependence of protonated water cluster emission from field adsorbed water layers on platinum

2002 ◽  
Vol 501 (3) ◽  
pp. 169-181 ◽  
Author(s):  
Christopher J. Rothfuss ◽  
Valentin K. Medvedev ◽  
Eric M. Stuve
Keyword(s):  
Field Dependence ◽  
Water Cluster ◽  
Adsorbed Water ◽  
Cluster Emission ◽  
Water Layers

Vertical and Lateral Order in Adsorbed Water Layers on Anatase TiO2(101)

Langmuir ◽  
2004 ◽  
Vol 20 (19) ◽  
pp. 8379-8384 ◽  
Author(s):  
Antonio Tilocca ◽  
Annabella Selloni
Keyword(s):  
Adsorbed Water ◽  
Anatase Tio2 ◽  
Water Layers

Contact Forces between TiO2Nanoparticles Governed by an Interplay of Adsorbed Water Layers and Roughness

Langmuir ◽  
2015 ◽  
Vol 31 (41) ◽  
pp. 11288-11295 ◽  
Author(s):  
Jens Laube ◽  
Samir Salameh ◽  
Michael Kappl ◽  
Lutz Mädler ◽  
Lucio Colombi Ciacchi
Keyword(s):  
Adsorbed Water ◽  
Contact Forces ◽  
Water Layers

Hydromechanical effects: (II) on the water-Na-smectite system

Clay Minerals ◽  
2000 ◽  
Vol 35 (3) ◽  
pp. 537-544 ◽  
Author(s):  
M. Al-mukhtar ◽  
Y. Qi ◽  
J . -F. Alcover ◽  
J . Conard ◽  
F. Bergaya
Keyword(s):  
Water Content ◽  
Mechanical Stress ◽  
Adsorbed Water ◽  
Bulk Water ◽  
Water Volume ◽  
X Ray Diffraction ◽  
Applied Water ◽  
X Ray ◽  
Water Layers ◽  
Different Types

AbstractThe localization and number of the different types of water in two Na-smectites (Laponite and hectorite) were studied as a function of the hydromechanical stresses applied. Water volume variation was obtained by macroscopic oedometric tests. Thermogravimetric analysis (TGA), X-ray diffraction (XRD) and nuclear magnetic resonance (NMR) were used to study water-smectite interactions. The TGA results show that the bulk water content decreases while the adsorbed water content remains practically constant with increasing mechanical stress; hectorite adsorbs less water than Laponite at low hydraulic stress. The proportion of adsorbed water obtained by NMR confirms the TGA data. The interlamellar space and the equivalent water layers decrease with increasing mechanical stress and is always lower in hectorite than in Laponite. Hydromechanical effects on the water-Na-smectite system are in agreement with microtexture changes measured by porosimetry. Differences in the properties of the two clays can be attributed to the higher extension of the layers in hectorite compared with Laponite.

scholarly journals Disordered Adsorbed Water Layers on TiO2 Nanoparticles under Subsaturated Humidity Conditions at 235 K

2019 ◽  
Vol 10 (23) ◽  
pp. 7433-7438 ◽  
Author(s):  
Fabrizio Orlando ◽  
Luca Artiglia ◽  
Huanyu Yang ◽  
Xiangrui Kong ◽  
Kanak Roy ◽  
...  
Keyword(s):  
Tio2 Nanoparticles ◽  
Adsorbed Water ◽  
Water Layers

Phase transitions in adsorbed water layers in confined pores

1992 ◽  
Vol 153 (1) ◽  
pp. 85-91
Author(s):  
Boris Gorbunov ◽  
Valeri Petukhov ◽  
Ludmila Lazareva
Keyword(s):  
Phase Transitions ◽  
Adsorbed Water ◽  
Water Layers
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