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Crystallization of mixed gas hydrates under equilibrium and non-equilibrium conditions: PVTx measurements and thermodynamic modeling

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HAL Id: hal-01973527

https://hal.archives-ouvertes.fr/hal-01973527

Submitted on 10 Jan 2019

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Crystallization of mixed gas hydrates under equilibrium

and non-equilibrium conditions: PVTx measurements

and thermodynamic modeling

Saheb Maghsoodloo, Baptiste Bouillot, Jérome Douzet, Son Ho-Van,

Jean-Michel Herri

To cite this version:

Saheb Maghsoodloo, Baptiste Bouillot, Jérome Douzet, Son Ho-Van, Jean-Michel Herri. Crystalliza-tion of mixed gas hydrates under equilibrium and non-equilibrium condiCrystalliza-tions: PVTx measurements and thermodynamic modeling. Journée Scientifique 2018 du Codegepra, Nov 2018, Saint-Etienne, France. Journée scientifique du CODEGEPRA - Le Génie des Procédés en Rhône-Alpes Auvergne, pp.P9. �hal-01973527�

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Crystallization of mixed gas hydrates under equilibrium and non-equilibrium

conditions: PVTx measurements and thermodynamic modeling

Introduction

MAGHSOODLOO Saheb*, BOUILLOT Baptiste, Douzet Jérôme, HO-VAN Son, HERRI Jean-Michel

Ecole des Mines de Saint-Etienne, SPIN, CNRS 5307, LGF, F-42023 Saint-Etienne, France

* Corresponding author: saheb.m@emse.fr

What are the gas hydrates?

Experimental set-up and procedures

Research and problematics

Schematic diagram of the experimental procedures: a) Quick crystallization process. b) Slow crystallization

process

Experimental and modeling results

Conclusion

Mines-Hydrates

Water

molecules

Gas

molecules

High pressure

Low temperature

How much (volume) do gas hydrates form?

How is the guest distribution in hydrate phase?

How does the rate of crystallization affect the final state?

Hydrate composition

simulation

Average absolute deviation

Slow < Quick

More homogeneous phase

Gas hydrates, an issue in oil and gas industry

Natural gas hydrates in permafrost and seafloor sediments;

an unconventional energy resource

Potential applications of gas hydrates

CO

2

capture and sequestration

Gas separation

Water desalination

Hydrate composition

Experimental data

Experimental

difficulties

𝒙

𝑯

= 𝒇(𝑻, 𝑷, 𝒚)

𝒙

𝑪

≥𝟑

≥ 𝒚

𝑪

≥𝟑

Thermodynamic modeling

𝑨𝑨𝑫

𝒅𝒊𝒓𝒆𝒄𝒕

< 𝑨𝑨𝑫

𝒊𝒏𝒅𝒊𝒓𝒆𝒄𝒕

Modelling limits

𝒙

𝑪𝑶𝟐

> 𝟎, 𝟔 𝒐𝒓

𝑷 < 𝟕𝟎 𝒃𝒂𝒓𝒔

→ 𝑨𝑨𝑫 < 𝟎, 𝟎𝟐

Hydrate volume

Storage capacity

Slow crystallization

Less kinetic effects

Thermodynamic

equilibrium

Lower crystallization rate

Different final pressure and

Composition

Less hydrate volume and more

storage capacity

These elucidations could have a significant impact on clathrate hydrate

applications which thermodynamic equilibrium is essentially taken into

account such as energy storage and transportation or CCS.

Références

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