VIEWS & COMMENTS

Impacts of CO2 and H2S on the risk of hydrate formation during pipeline transport of natural gas

  • Solomon A. Aromada , 1 ,
  • Bjørn Kvamme 2
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  • 1. Department of Physics and Technology, University of Bergen, 5007 Bergen, Norway
  • 2. Strategic Carbon LLC, Vestre Holbergsallmenningen 17, 5011 Bergen, Norway

Received date: 20 Apr 2018

Accepted date: 01 Nov 2018

Published date: 15 Sep 2019

Copyright

2019 Higher Education Press and Springer-Verlag GmbH Germany, part of Springer Nature

Abstract

Evaluation of maximum content of water in natural gas before water condenses out at a given temperature and pressure is the initial step in hydrate risk analysis during pipeline transport of natural gas. The impacts of CO2 and H2S in natural gas on the maximum mole-fractions of water that can be tolerated during pipeline transport without the risk of hydrate nucleation has been studied using our novel thermodynamic scheme. Troll gas from the North Sea is used as a reference case, it contains very negligible amount of CO2 and no H2S. Varying mole-fractions of CO2 and H2S were introduced into the Troll gas, and the effects these inorganic impurities on the water tolerance of the system were evaluated. It is observed that CO2 does not cause any distinguishable impact on water tolerance of the system, but H2S does. Water tolerance decreases with increase in concentration of H2S. The impact of ethane on the system was also investigated. The maximum mole-fraction of water permitted in the gas to ensure prevention of hydrate formation also decreases with increase in the concentration of C2H6 like H2S. H2S has the most impact, it tolerates the least amount of water among the components studied.

Cite this article

Solomon A. Aromada , Bjørn Kvamme . Impacts of CO2 and H2S on the risk of hydrate formation during pipeline transport of natural gas[J]. Frontiers of Chemical Science and Engineering, 2019 , 13(3) : 616 -627 . DOI: 10.1007/s11705-019-1795-2

Electronic Supplementary Material

Supplementary material is available in the online version of this article at https://doi.org/10.1007/s11705-019-1795-2 and is accessible for authorized users.
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