2020
DOI: 10.3390/jmse8010022
|View full text |Cite
|
Sign up to set email alerts
|

The Performance of Low-Pressure Seawater as a CO2 Solvent in Underwater Air-Independent Propulsion Systems

Abstract: Air-independent propulsion systems have improved the performance and decreased the vulnerability of underwater weapon systems. Reforming systems, however, generates large amounts of water and CO2. The recovery or separation of CO2, a residual gas component generated in vessels, entails considerable cost and energy consumption. It is necessary to understand the characteristics of the interaction between CO2 and seawater under the conditions experienced by underwater weapon systems to design and optimize a CO2 t… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

2020
2020
2024
2024

Publication Types

Select...
3
1

Relationship

0
4

Authors

Journals

citations
Cited by 4 publications
(1 citation statement)
references
References 43 publications
0
1
0
Order By: Relevance
“…84 Representative diffusion coefficients ranging from 7 × 10 -5 cm 2 s -1 to 1 × 10 -5 cm 2 s -1 demonstrate the lower and upper bounds for several atmospheric gases in a range of ocean relevant temperatures. [85][86][87][88][89] Seemingly, as the film becomes more concentrated throughout the bloom and the film thickness increases, the film permeability decreases. Interestingly, gases with larger diffusion coefficients show a more apparent exponential decrease in their permeability concurrent with film thickness, and are more greatly impeded by film thickness possibly due to the longer elapse of time required to permeate the film and the abrupt nature of physical aging resulting from the inherent kinetic nature of transitioning through the film.…”
Section: Gas Transport and Atmospheric Implicationsmentioning
confidence: 99%
“…84 Representative diffusion coefficients ranging from 7 × 10 -5 cm 2 s -1 to 1 × 10 -5 cm 2 s -1 demonstrate the lower and upper bounds for several atmospheric gases in a range of ocean relevant temperatures. [85][86][87][88][89] Seemingly, as the film becomes more concentrated throughout the bloom and the film thickness increases, the film permeability decreases. Interestingly, gases with larger diffusion coefficients show a more apparent exponential decrease in their permeability concurrent with film thickness, and are more greatly impeded by film thickness possibly due to the longer elapse of time required to permeate the film and the abrupt nature of physical aging resulting from the inherent kinetic nature of transitioning through the film.…”
Section: Gas Transport and Atmospheric Implicationsmentioning
confidence: 99%