Gas Hydrates recovery methods, issues and solution for its prevention
Recovery of Gas Hydrates
We can recover gas
hydrates through various methods;
- Thermal Stimulation Method.
- Depressurization Method.
- Inhibitor Injection Method.
- Carbon Dioxide Injection Method.
Thermal
Stimulation Method
The thermal stimulation
approach involves raising the hydrate temperature above the stability point,
causing the hydrate to dissociate. Thermal stimulation requires a continuous
energy source to overcome the endothermic heat of dissociation.
Depressurization
Method
Depressurization
involves lowering the hydrate pressure below the stability point, causing the
hydrate to dissociate. Depressurization results in rapid hydrate dissociation,
but with an associate drop in the hydrate temperature. Without an external heat
source, depressurization lowers the hydrate temperature to a new equilibrium
condition, halting the depressurization process.
Disadvantages
There are the following
disadvantages of the depressurization methods; i.e., Production of water and disturbing the marine life.
Inhibitor
Injection Method
Inhibitor injection
involves the injection of an organic or inorganic compound that shifts the
hydrate equilibrium point to lower temperatures for isobaric conditions. As
with depressurization, inhibitor injection could require additional inhibitor
or a heat source to compensate for the decrease in hydrate temperature with
dissociation.
The most common
thermodynamic organic inhibitors are methanol, monoethylene glycol (MEG) and
diethylene glycol (DEG) commonly referred to as glycol. Dissolved salts (e.g.,
NaCl, CaCl2, KCl, NaBr) can also be inhibitors.
Disadvantages
The disadvantages of
the inhibitor injection method are; environmental impact, economic costs and thermal
self regulation of gas hydrates.
Carbon
dioxide Injection Method
Under high pressure,
low temperature sub oceanic conditions the hydrate structure can accommodate
small molecules other than methane (CH4), such as carbon dioxide (CO2) and
nitrogen (N2) in both the small and large cages. Although CO2 and N2 clathrates generally are not naturally as
abundant as those of CH4, their occurrence forms the foundation of an
unconventional approach for producing natural gas hydrates that involves the
exchange of CO2 with CH4 in the hydrate structure.
Gas
Hydrate Resource Pyramid
The methane hydrate
resource pyramid depicts hydrate resources according to reservoir type, gas
recoverability, and estimated total in-place gas quantity.
Hydrate resources that
are considered to be the most easily recoverable are found at the peak of the
pyramid, while those that are the most technically challenging to extract lie
at the base.
For example, hydrate in
arctic sandstone reservoirs contains an in-place gas volume estimated to be in
the 100’s of Tcf, while hydrate in marine sands is estimated to contain 1,000’s
to 10,000’s of Tcf, and hydrate dispersed through marine muds is estimated to
contain 100,000’s of Tcf.
Issues of Gas Hydrates
Drilling in offshore regions: Increasingly complex challenges will be faced in offshore oil and gas drilling with increasing water depths. One of these challenges is the formation of gas hydrates. If shallow sediments that contain natural gas are encountered during deep-water drilling, this gas will enter into the drilling fluid leading to gas hydrate formation under low temperature and high pressure. Gas hydrate could easily formed when mud circulation was stopped and gas entered into the drilling fluid, Resulting in an unexpected gas kick during drilling operation, which will block the pipe, annular clearance or blowout preventer (BOP).
Therefore, since the
1990s, strict measures have been taken to prevent gas from forming hydrates in
deep-water drilling. The main preventive measure is to add certain chemical
compounds that cause drilling fluid to inhibit formation of gas hydrates like
thermodynamic inhibitors and low-dosage hydrate inhibitors (LDHI). During
deep-water oil and hydrate drilling, thermodynamic inhibitors normally are
added to the drilling fluid, whereas kinetic hydrate inhibitors (KHI) are still
under investigation.
Resource
information: Although the Hikurangi Margin has been
surveyed to some degree, more research is still required to map and appraise
gas hydrate sweet spots in the area, and prioritize sweet spots for future
development when the technology becomes available. More research into the characterization
of the New Zealand gas hydrate resource is also required as methane
compositions in hydrates can vary geographically, with resulting implications
for extraction and production.
Technology
& equipment: Commercial production technology is
currently unavailable, although conventional oil and gas technologies could be
adapted. Significant technical issues currently exist around extraction and
transportation of gas hydrates.
Investment:
The
high levels of gas hydrate research may be an indicator of the potentially high
cost of extraction and production technology when they become available. Access
to the technology may require some level of government involvement or support,
as occurred with the development of Maui. Attracting inwards private investment
on the scale anticipated will require attractive policies and incentives, or
better promotion of the higher prospectivity of the New Zealand gas hydrate
resources relative to Alaska and Gulf of Mexico (the current focus of hydrate
research by USA, Japan and Canada).
Infrastructure:
Existing
onshore Taranaki infrastructure could be utilized if the technical issues
around extraction and transportation are successfully addressed. There may also
be a business case for the development of new infrastructure on the East Coast
of the North Island to be in closer proximity to the sweet spots on the
Hikurangi Margin. Such infrastructure is likely to follow successful petroleum
development in the region.
Environmental
impacts: Negative feedback: Global
warming leads to sea level rise and in increase of pressure. This leads to an
increased hydrate stability and a decrease of the methane amount released from
gas hydrates. Cooling results. Positive feedback: Global warming leads to an increase
of bottom water temperature. This decreases hydrate stability and leads in turn
to an increase of the methane amount released from gas hydrate. Further warming
is the result. There are a number of environmental issues currently being
debated internationally around gas hydrates. The ‘Smoking Gun’ hypothesis
suggests that the release of methane into the atmosphere from disassociating
gas hydrates creates one of two climate change scenarios.
Solutions for Prevention of Gas Hydrates
By the use of model: The first step in controlling hydrate formation is to know the¡ pressure and temperature conditions in the well by PVT simulators. A number of computer simulators are available for this purpose usually as adjuncts to more general phase PVT simulators. The models vary in how well they compute the chemical activity of the water phase, the effect of higher-molecular-weight hydrocarbons, and the effect of hydrate inhibitors. The second control step is the comparison of this information with the measured or expected PT profile within the production system. A method of coping with hydrate formation is then selected.
Environmental
Inhibitors: The conceptually simplest “environmental
inhibition” method is to dry the gas before it is cooled remove the
water and hydrates so they cannot form. This involves adsorption onto, for
example, silica gel, or cooling and condensation, absorption of water into
alcohols, or adsorption onto hydroscopic salts.
Drilling
Fluids and strings: Hydrates can plug drill strings, blowout
preventers, chokes, and other equipment, sometimes requiring the abandonment of
drilling operations because of safety constraints. Water-based drilling fluids
are particularly susceptible to hydrate formation. The most important variable
affecting hydrate formation is the activity of the water, which is decreased by
chemicals that dissolve by bonding to water molecules.
It is important to
recognize that other non soluble drilling-fluid components (e.g., mud solid
particles or fluidizers) may affect the kinetics or rate of hydrate formation
to determine how rapidly hydrates will form or decompose.
Kinetic
inhibitors: These chemicals are polymers with carbon
backbones and pendant groups, which adsorb into partially formed hydrate cages
to keep the polymer anchored along the hydrate-crystal surface. Growing hydrate
crystals are forced to grow around the polymer, stabilizing the hydrates as
small particles in the aqueous phase. No liquid hydrocarbon need be present. Field
tests have shown these chemicals to be effective at sub coolings up to ΔT =
20°F, at dosages from 550 to 3,000 ppm in the water phase. There is
concern about these chemicals with respect to performance on shut-in and
restart; also, a substantial amount of hydrate normally forms upon inhibitor
failure.
Emulsifiers:
These
chemicals work by stabilizing small hydrate particles in an oil phase. Some
oils contain natural emulsifiers such that, even with favorable hydrate
formation conditions, the water, which might convert to hydrates, is stabilized
within the oil phase. Artificial emulsifiers have been shown to be effective,
preventing hydrate plugs in flow loops. There are concerns about these
chemicals regarding the expense of tailoring them for each oil application and
the cost associated with emulsion breaking.
Insulation
and heating: Because fluids come from the reservoir
at high temperatures, a low cost solution is to preserve the reservoir
temperature (or add heat to the line) to keep the system out of the hydrate
region. There are three types of insulation listed in ascending order of cost:
coatings applied to pipes; pipe-in-pipe (PIP) or bundling; and vacuum-insulated
pipes or pipes with insulating gases. In combination with insulation, line
heating may be done through resistance or induction heating, with practice
favoring the former. Heating costs are very high, second only to chemical
treatment, and the power for heating is generated on platforms, where typically
only 5 to 10 MW may be available.
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