The relationship between global warming and methane gas hydrates in the earth

1993 ◽  
Vol 48 (23) ◽  
pp. 3963-3969 ◽  
Author(s):  
Savvas G. Hatzikiriakos ◽  
Peter Englezos
Soundings ◽  
2021 ◽  
Vol 78 (78) ◽  
pp. 50-63
Author(s):  
Dipesh Chakrabarty ◽  
Ashish Ghadiali

The notion of the planetary allows us to distinguish between the global of globalisation and the global of global warming. Globalisation is the process through which humans created the world we live in, how we converted the planet into a spherical human domain, at the centre of which are the human stories of technology, empires, capitalism and inequality. Global warming is what has resulted at the planetary level as intensified human consumption of the globe's resources has turned humanity into a geological agent of change. The global is 500 years old, while the planetary is as old as the age of the earth. The physical world has its own deep history: over time it has experienced profound changes. If climate change is to be addressed this mutability must be recognised – the unchanging nature of the world can no longer be taken for granted. The interview covers the rise of atmospheric sciences during the Cold War, when the Earth became, effectively, part of a comparative study of planets; the relationship between Marxism and the idea of 'deep history'; the human-made ecological disaster of bush-fires in Australia; the influence of Rohith Vemula and Rabindranath Tagore on planetary thinking and ideas about connectivity; biopower, zoe and the pandemic; and the difficulty of thinking politically about deep history.


2021 ◽  
pp. 132-151
Author(s):  
Jorge Daniel Taillant

This chapter examines the warming of permafrost found in the Earth’s coldest regions. It relates how this warming results in the release of large amounts of methane gas from gas hydrates buried in frozen grounds and discusses the implications for climate change of this release. The chapter outlines the categories of permafrost and the role that thawing and freezing cycles play in the local environment. It also describes how to use online GIS tools to locate permafrost regions on the Earth. Finally, the chapter reviews the common impacts of melting permafrost such as subsidence, sinkholes, destruction of infrastructure, as well as the possible release of human and animal disease agents.


1990 ◽  
Vol 27 (1) ◽  
pp. 148-157 ◽  
Author(s):  
E. G. Nisbet

Methane-gas hydrates may have contributed to the rapid rise in atmospheric CH4, CO2, and global temperatures at the end of the last major glaciation about 13 500 years ago. Given suitable orbital conditions and insolation at high latitude, a small triggering event, such as the release of one or more Arctic gas pools, may have initiated massive release of methane from hydrate under ice and in permafrost. The consequent greenhouse warming would have provided strong positive feedback, amplifying emission. This warming, driven by CH4, may have induced the release of CO2 from the oceans to the biosphere, stabilizing the interglacial carbon cycle.


2007 ◽  
Vol 34 (1) ◽  
Author(s):  
Charles K. Paull ◽  
William Ussler ◽  
Scott R. Dallimore ◽  
Steve M. Blasco ◽  
Thomas D. Lorenson ◽  
...  

2021 ◽  
Vol 230 ◽  
pp. 01004
Author(s):  
Olena Svietkina ◽  
Iryna Kovalevska ◽  
Kateryna Sai ◽  
Kostiantyn Prokopenko

The crystallization process of gas hydrates during their formation in the presence of surface-active substances (SAS) is studied. The research is conducted in two directions – theoretical and experimental. Experimental data on the crystallization rate of methane gas hydrates formation in the presence of surfactants have been obtained: high-molecular compounds are used on the basis of polymeric quaternary ammonium salts containing side aliphatic radicals of various lengths in the acyl fragment, as well as a number of specific surfactants. The process of methane gas hydrates formation is performed using a laboratory setup of the NPO modification for the gas hydrates creation. To analyse the experimental data, technical and metrological instruments are used: stalagmometric method with automatic photoelectric drop counting, conductometric method, Wheatstone bridge, spectrophotometric titration of amino end-groups, viscometer VPZh-1. It has been substantiated that the crystal formation rate depends on the surfactant concentration. New experimental dependences of the gas hydrates formation on surfactants under thermobaric conditions in the presence of surfactants have been found. It has been revealed that the crystallization process during the methane gas hydrates formation is accelerated in the presence of a surfactant. As a result of their application, the effect of solubilization and catalysis arises with the formation of the so-called “diffusion zone”, the size of which decreases in the presence of surfactants, thereby accelerating the substance transfer to the surface on which crystallization occurs. An increase in the surfactant concentration leads to an increase in the rate of molecular diffusion, and also creates a more intense turbulent diffusion.


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