Oxygen transport in the submerged freshwater macrophyte Egeria densa planch. I. Oxygen production, storage and release

1987 ◽  
Vol 28 (1) ◽  
pp. 63-80 ◽  
Author(s):  
B.K. Sorrell ◽  
F.I. Dromgoole
2019 ◽  
Vol 108 ◽  
pp. 01021
Author(s):  
Konrad Świerczek ◽  
Hailei Zhao ◽  
Zijia Zhang ◽  
Zhihong Du

Mixed ionic-electronic conducting ceramic membrane-based oxygen separation technology attracts great attention as a promising alternative for oxygen production. The oxygen-transport membranes should not only exhibit a high oxygen flux but also show good stability under CO2-containing atmospheres. Therefore, designing and optimization, as well as practical application of membrane materials with good CO2 stability is a challenge. In this work, apart from discussion of literature data, authors’ own results are provided, which are focused on materia - related issues, including development of electrode materials exhibiting high ionic and electronic conductivities.


2014 ◽  
Vol 2 (22) ◽  
pp. 8174-8178 ◽  
Author(s):  
Jong Hoon Joo ◽  
Kyong Sik Yun ◽  
Chung-Yul Yoo ◽  
Ji Haeng Yu

A novel oxygen permeation membrane with a tunable segmented configuration with high oxygen permeation is a promising alternative for industrial oxygen production.


Author(s):  
Donald Eugene Canfield

This chapter discusses the modeling of the history of atmospheric oxygen. The most recently deposited sediments will also be the most prone to weathering through processes like sea-level change or uplift of the land. Thus, through rapid recycling, high rates of oxygen production through the burial of organic-rich sediments will quickly lead to high rates of oxygen consumption through the exposure of these organic-rich sediments to weathering. From a modeling perspective, rapid recycling helps to dampen oxygen changes. This is important because the fluxes of oxygen through the atmosphere during organic carbon and pyrite burial, and by weathering, are huge compared to the relatively small amounts of oxygen in the atmosphere. Thus, all of the oxygen in the present atmosphere is cycled through geologic processes of oxygen liberation (organic carbon and pyrite burial) and consumption (weathering) on a time scale of about 2 to 3 million years.


1992 ◽  
Author(s):  
CHRISTIAN KNUDSEN ◽  
MICHAEL GIBSON ◽  
DAVID BRUENEMAN ◽  
SEISHI SUZUKI ◽  
TETSUJI YOSHIDA ◽  
...  

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