Fluid composition or bottom currents: What drives extremes in behavior of plumes at ASHES vent field, Axial Volcano?

2019 ◽  
Author(s):  
Karen Bemis ◽  
Guangyu Xu ◽  
Darrell Jackson ◽  
Anatoliy Ivakin
2017 ◽  
Author(s):  
Melissa R. Luna ◽  
◽  
Suzanne O'Connell ◽  
Joseph D. Ortiz ◽  
Michael C. Wizevich

Pharmaceutics ◽  
2021 ◽  
Vol 13 (2) ◽  
pp. 272
Author(s):  
Arik Dahan ◽  
Isabel González-Álvarez

The gastrointestinal tract (GIT) can be broadly divided into several regions: the stomach, the small intestine (which is subdivided to duodenum, jejunum, and ileum), and the colon. The conditions and environment in each of these segments, and even within the segment, are dependent on many factors, e.g., the surrounding pH, fluid composition, transporters expression, metabolic enzymes activity, tight junction resistance, different morphology along the GIT, variable intestinal mucosal cell differentiation, changes in drug concentration (in cases of carrier-mediated transport), thickness and types of mucus, and resident microflora. Each of these variables, alone or in combination with others, can fundamentally alter the solubility/dissolution, the intestinal permeability, and the overall absorption of various drugs. This is the underlying mechanistic basis of regional-dependent intestinal drug absorption, which has led to many attempts to deliver drugs to specific regions throughout the GIT, aiming to optimize drug absorption, bioavailability, pharmacokinetics, and/or pharmacodynamics. In this Editorial we provide an overview of the Special Issue "Regional Intestinal Drug Absorption: Biopharmaceutics and Drug Formulation". The objective of this Special Issue is to highlight the current progress and to provide an overview of the latest developments in the field of regional-dependent intestinal drug absorption and delivery, as well as pointing out the unmet needs of the field.


2021 ◽  
Vol 41 (1) ◽  
Author(s):  
Yi-Ching Yeh ◽  
Chung-Lin Tsai ◽  
Shu-Kun Hsu ◽  
Hsiao-Shan Lin ◽  
Kuan-Ting Chen ◽  
...  

1992 ◽  
Vol 11 (7) ◽  
pp. 589-590 ◽  
Author(s):  
William A. Bonadio ◽  
Lynn Stanco ◽  
Robert Bruce ◽  
Darcy Barry ◽  
Douglas Smith

1962 ◽  
Vol 99 (6) ◽  
pp. 558-569 ◽  
Author(s):  
Peter J. Wyllie

AbstractBowen's petrogenetic grid is a PT projection containing univariant curves for decarbonation, dehydration, and solid-solid reactions, with vapour pressure (Pf) equal to total pressure (Ps). Analysis of experimental data in the system MgO–CO2–H2O leads to an expansion of this grid. Three of the important variables in metamorphism when Pf = Ps are P, T, and variation of the pore fluid composition between H2O and CO2. These can be illustrated in a three-dimensional petrogenetic model; one face is a PT plane for reactions occurring with pure H2O, and the opposite face is a similar plane for reactions with pure CO2; these are separated by an axis for pore fluid composition varying between H2O and CO2. Superposition of the PT faces of the model provides the petrogenetic grid. The reactions within the model are represented by divariant surfaces, which may meet along univariant lines. For dissociation reactions, the surfaces curve towards lower temperatures as the proportion of non-reacting volatile increases, and solid-solid reaction surfaces are parallel to the vapour composition axis and perpendicular to the PT axes. The relative temperatures of reactions and the lines of intersections of the surfaces can be illustrated in isobaric sections. Isobaric sections are used to illustrate reactions proceeding at constant pressure with (1) pore fluid composition remaining constant during the reaction, with temperature increasing (2) pore fluid composition changing during the reaction, with temperature increasing, and (3) pore fluid changing composition at constant temperature. The petrogenetic model provides a convenient framework for a wide range of experimental data.


Sign in / Sign up

Export Citation Format

Share Document