scholarly journals Shallow gas and gas hydrate occurrences on the northwest Greenland shelf margin

2021 ◽  
Vol 432 ◽  
pp. 106382 ◽  
Author(s):  
David R. Cox ◽  
Mads Huuse ◽  
Andrew M.W. Newton ◽  
Arka D. Sarkar ◽  
Paul C. Knutz
Keyword(s):  
2021 ◽  
Author(s):  
P. V. Suryanarayana ◽  
Miodrag Bogdanovic ◽  
Kuhanesapathy Thavaras Pathy ◽  
M. Razali Paimin

Abstract Shallow gas hydrate zones are present in some deepwater fields. During production, the shallow hydrates may dissociate due to heat-up of the near wellbore formation, which can extend radially to several meters from the wellbore. This can compromise structural integrity of the well (particularly structural strings), cause subsidence, and impact subsea equipment installations. This problem is well known, and has been addressed in the literature. An enthalpy-based transient thermal simulation is required to determine the dissociation front. Further, post-dissociation formation mechanics and well integrity assessment are complex, requiring numerical approaches such as Finite Element Analyses. In this paper, we present an approach that allows a preliminary assessment of the severity of the impact of dissociation on well integrity, so that a more complex assessment may be undertaken only for severe situations. The main objectives of the preliminary assessment are: to model hydrate dissociation front and the radial extent of dissociation as a function of depth; evaluate response of formation to this dissociation; analyze mechanical response of the well to the modified mechanical properties within dissociated zone; and confirm well integrity. The paper describes the approach, and introduces two thermal metrics to assess the likely severity of the integrity impact of hydrate dissociation. Using these metrics, the need for a more detailed analysis can be determined. Further, load analysis and integrity checks of the structural strings and the wellhead that can be performed as part of the preliminary assessment are discussed. An illustrative example is used to demonstrate the approach.


2019 ◽  
Vol 46 (24) ◽  
pp. 14459-14468 ◽  
Author(s):  
Jun Yoneda ◽  
Masato Kida ◽  
Yoshihiro Konno ◽  
Yusuke Jin ◽  
Sumito Morita ◽  
...  

Geosciences ◽  
2019 ◽  
Vol 9 (3) ◽  
pp. 134 ◽  
Author(s):  
Claudio Argentino ◽  
Stefano Conti ◽  
Chiara Fioroni ◽  
Daniela Fontana

The occurrence of seep-carbonates associated with shallow gas hydrates is increasingly documented in modern continental margins but in fossil sediments the recognition of gas hydrates is still challenging for the lack of unequivocal proxies. Here, we combined multiple field and geochemical indicators for paleo-gas hydrate occurrence based on present-day analogues to investigate fossil seeps located in the northern Apennines. We recognized clathrite-like structures such as thin-layered, spongy and vuggy textures and microbreccias. Non-gravitational cementation fabrics and pinch-out terminations in cavities within the seep-carbonate deposits are ascribed to irregularly oriented dissociation of gas hydrates. Additional evidences for paleo-gas hydrates are provided by the large dimensions of seep-carbonate masses and by the association with sedimentary instability in the host sediments. We report heavy oxygen isotopic values in the examined seep-carbonates up to +6‰ that are indicative of a contribution of isotopically heavier fluids released by gas hydrate decomposition. The calculation of the stability field of methane hydrates for the northern Apennine wedge-foredeep system during the Miocene indicated the potential occurrence of shallow gas hydrates in the upper few tens of meters of sedimentary column.


2009 ◽  
Vol 118 (1) ◽  
pp. 111-127 ◽  
Author(s):  
Hitoshi TOMARU ◽  
Hirotsugu MINAMI ◽  
Hitoshi SHOJI ◽  
Akihiro HIRUTA ◽  
Ryo MATSUMOTO ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document