Hydrates
were first discovered by Sir Humphrey Davy in 1810 but remained
a scientific curiosity until Hammerschmidt reported in 1934 that
they could form in natural gas pipelines leading to blockages
and reduced or zero gas flow. The initial work by Hammerschmidt motivated
considerable research activity into the formation of hydrates
and their prevention in pipelines and led to the development of
the first hydrate prediction methods and inhibition techniques.
Gas
hydrates are crystalline ice-like solids formed from water and
a range of lower molecular weight molecules, typically methane,
ethane, propane, hydrogen sulphide and carbon dioxide. The structures of the crystals fall into the class of clathrates
with the water molecules forming a hydrogen-bonded cage-like structure
which is stabilized by ‘guest’ molecules located within
the lattice. For more detail please refer to our recent
paper on hydrates.
To
date there are three known hydrate structures referred to as structures
I, II and H. The figure below presents schematics of
the three different structures together with a picture of a pure
crystal.
Although
the most common form of hydrate is structure II, the others may
form under certain circumstances. For example, structure I may form in a gas-water
system where the gas is rich in methane. Maximus is able to predict the dissociation curve of all three hydrate
structures and so allow engineers to select operating envelopes
that avoid the formation of these solids. An example phase diagram is provided below:
Example Showing Structure
I, II and H Hydrate Loci Overlaid on Hydrocarbon Phase Envelope