scholarly journals Experimentally probing the libration of interfacial water: the rotational potential of water is stiffer at the air/water interface than in bulk liquid

2016 ◽  
Vol 18 (27) ◽  
pp. 18424-18430 ◽  
Author(s):  
Yujin Tong ◽  
Tobias Kampfrath ◽  
R. Kramer Campen

Vibrational sum frequency spectroscopy measurements reveal that the libration frequency of interfacial water is significantly higher than bulk liquid water, suggesting that water's rotational potential stiffens on moving from the bulk liquid to the air/water interface.

2018 ◽  
Vol 122 (15) ◽  
pp. 3837-3849 ◽  
Author(s):  
Brittany P. Gordon ◽  
Frederick G. Moore ◽  
Lawrence F. Scatena ◽  
Nicholas A. Valley ◽  
Sumi N. Wren ◽  
...  

Soft Matter ◽  
2019 ◽  
Vol 15 (1) ◽  
pp. 38-46
Author(s):  
Petru Niga ◽  
Petra M. Hansson-Mille ◽  
Agne Swerin ◽  
Per M. Claesson ◽  
Joachim Schoelkopf ◽  
...  

Propofol adsorbs at the water interface forming a dense film, sitting tilted and oriented with the OH-group towards the water.


2020 ◽  
Author(s):  
Mokhtar Rashwan ◽  
Benjamin Rehl ◽  
Adrien Sthoer ◽  
Akemi Darlington ◽  
Md. Shafiul Azam ◽  
...  

The molecular origin of overcharging at mineral oxide surfaces remains a cause of contention within the geochemistry, physics, and colloidal chemistry communities owing to competing “chemical” vs “physical” interpretations. Here, we combine vibrational sum frequency spectroscopy and streaming potential measurements to obtain molecular and macroscopic insights into the pH-dependent interactions of calcium ions with a fused silica surface. In 100 mM CaCl<sub>2</sub> electrolyte, we observe evidence of charge neutralization at pH~10.5, as deducted from a minimum in the interfacial water signal. Concurrently, adsorption of calcium hydroxide cations is inferred from the appearance of a spectral feature at ~3610 cm<sup>-1</sup>. However, the interfacial water signal increases at higher pH, while adsorbed calcium hydroxide appears to remain constant, indicating that overcharging results from hydrated Ca<sup>2+</sup> ions present within the Stern layer. These findings suggest that both specific adsorption of hydrolyzed ions and ion-ion correlations of hydrated ions govern silica overcharging with increasing pH.


2016 ◽  
Vol 18 (43) ◽  
pp. 29756-29770 ◽  
Author(s):  
Garold Murdachaew ◽  
Gilbert M. Nathanson ◽  
R. Benny Gerber ◽  
Lauri Halonen

Formic acid has a lower barrier to deprotonation at the air–water interface than in bulk liquid water.


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