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1
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- Lectures # 32 & # 33
- Chapter 17
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2
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3
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- General Description
- Crystal Structure
- Thermodynamic inhibition
- Hydrate Phase Behavior And Inhibition
- Kinetic inhibition
- Prediction of the hydrate phase behavior
- Remedial Actions
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4
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- “Natural gas hydrates are ice-like structures composed of water and
natural gas molecules. Under
favorable conditions of high pressure and low temperature, water
molecules form cages which encapsulate gas molecules inside a
hydrogen-bonded solid lattice”
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5
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- Hydrates have potential as a future energy resource
- Related to climate change
- Affect strength of sediments in which they are found (care in
constructing underwater structures)
- Hydrates currently cause blocking in some underwater natural gas
pipelines
- Hydrates may be an alternative to pipeline transmission as a way to move
natural gas from deep water to the terminals of existing offshore
pipelines
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6
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- Production
- More common, est. $500 million just for inhibition in offshore
pipelines
- Drilling
- Typically during well control situations external to BOP at seafloor
- Drill Stem Testing operations
- Typically in deeper water, but definitely
possible in shallow water operations
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7
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- Plugging of choke and kill lines
- Formation of a plug at or below
BOP, preventing monitoring of pressures below BOP
- Plugging tubing, downhole tools and wireline during DST operation
- Free water tied up with hydrates can cause thickening of the mud
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8
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9
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10
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11
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12
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13
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14
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15
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- Gas Clathrates are crystalline compounds that occur when water forms a
cage-like structure around smaller guest molecules.
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16
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- Host - water molecules
- Guest - gas molecules
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17
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18
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- Different dielectric constant
- Different thermal conductivity (2.23 W/m-K à ice, vs 0.5 W/m-K hydrate)
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19
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- Hydrates can form when 4 ingredients are present:
- free water
- natural gas (N2, H2S, CO2, C1,
C2, C3, iC4)
- reduced temperature
- increased pressure
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20
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21
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- How much hydrate forms and when?
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22
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- Three-phase V-L-S equilibria
- Need models for fugacity coefficients (solid, liquid,gas)
- Hydrate formation curves f(P,T,composition) à saturation boundary
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23
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24
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25
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26
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27
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28
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- Remove One Component i.e. Water, Gas
- IncreaseTemperature
- Decrease System Pressure
- Use an Inhibitor in the Water
Phase (Thermodynamic)
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29
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30
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- Once hydrates have formed what can be done to remove them?
- reduce pressure
- increase temperature
- chemical (thermodynamic) inhibition
- kinetic inhibitors
- mechanical removal
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31
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- Mechanical
- Depressurization
- Chemical
- Thermal
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32
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- Remove any of the 4 ingredients
- Thermodynamic inhibitors
- electrolytes (salts) form ionic bonds with free water
- polar compounds (alcohols, glycols) compete with hydrates for hydrogen
bonding
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33
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34
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- Salts
- Normally sodium chloride, 20-24% by wt.
- Potassium chloride can be used but it is significantly more expensive,
and saturated KCl muds have performed poorly in offshore environments
- Calcium Chloride, very expensive and not as effective as NaCl for
hydrate suppression
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35
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- Salt Ionizes In Solution And Interacts With The Dipoles Of The Water
Molecules And Causes Clustering
- This Clustering Also Causes A Decrease In The Solubility Of Potential
Hydrate Guest Molecules In The Water
- These Combine To Require Substantially More Subcooling To Cause
Hydrates To Form
- Examples: Sodium Chloride And
Calcium Chloride.
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36
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- The Hydroxyl Group Hydrogen Bonds The Water Molecules. In Direct
Competition With The Dissolved Apolar Molecules
- Inhibition Ability - Decreases With Volatility
- Examples:
- Methanol
- Ethanol
- Isopropanol
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37
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- More Hydrogen Bonding Opportunity With Water Through One More Hydroxyl
Group Than Alcohols
- Glycols Generally Have Higher Molecular Weights Which Inhibit Volatility
- Examples
- Ethylene Glycol
- Triethylene Glycol
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38
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39
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- Glycols
- Alcohols
- Salts
- Alcohols & Glycols when dissolved in aqueous solutions form
hydrogen bond with the water molecules and make it difficult for the
water molecules to participate in the hydrate structure.
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40
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41
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42
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- Salts - Effectiveness
- NaCl > KCl > CaCl2 > NaBr >
- Na Formate > Ca Nitrate
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43
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- Equilibrium DT
- F° psi
- 20% NaCl + 10% Aqua-Col 45 5360 36.5
- 20% NaCl + 10% HF-100 44.9 5067 37.1
- 20% KCl 66.1 5580 16.7
- 10% KCl + 10% Aqua-Col 71.2 5245 11.1
- 10% KCl + 10% HF-100 70.2 5460 12.4
- 10% KCl + 10% NaCl 61.6 4936 20.2
- 10% KCl + 10% NaCl + 10% Aqua-Col 51.0 4825 30.6
- 10% Aqua-Col 79.2 5500 3.5
- 20% NaFormate + 10% Aqua-Col 50.6 4570 30.5
- Seawater 80 5500 2.7
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44
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45
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46
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47
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48
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- For a given T Hydrate formation P increases as HC size decreases
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49
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50
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51
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52
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53
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54
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55
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56
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57
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- Lots of research issues to pursue
- Be aware of hydrates
- Be prepared to prevent hydrate problems
- materials
- procedures
- contingencies
- site/job investigation
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