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Oil and gas production handbook An introduction to oil ... - ABB Group

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3.1.3 Condensates<br />

While the ethane, propane, butane, <strong>and</strong> pentanes must be removed from<br />

natural <strong>gas</strong>, this does not mean that they are all waste products. In fact,<br />

associated hydrocarbons, known as natural <strong>gas</strong> liquids (NGL), can be very<br />

valuable byproducts of natural <strong>gas</strong> processing. NGLs include ethane,<br />

propane, butane, iso-butane, <strong>and</strong> natural <strong>gas</strong>oline. These are sold<br />

separately <strong>and</strong> have a variety of different uses such as raw materials for <strong>oil</strong><br />

refineries or petrochemical plants, as sources of energy, <strong>and</strong> for enhancing<br />

<strong>oil</strong> recovery in <strong>oil</strong> wells. Condensates are also useful as diluents for heavy<br />

crude.<br />

3.2 The reservoir<br />

The <strong>oil</strong> <strong>and</strong> <strong>gas</strong> bearing structure is typically porous rock, such as s<strong>and</strong>s<strong>to</strong>ne<br />

or washed out limes<strong>to</strong>ne. The s<strong>and</strong> may have been laid down as desert s<strong>and</strong><br />

dunes or seafloor. <strong>Oil</strong> <strong>and</strong> <strong>gas</strong> deposits form as organic material (tiny plants<br />

<strong>and</strong> animals) deposited in earlier geological periods, typically 100 <strong>to</strong> 200<br />

million years ago, under, over or with the s<strong>and</strong> or silt, are transformed by<br />

high temperature <strong>and</strong> pressure in<strong>to</strong> hydrocarbons.<br />

<strong>An</strong>ticline Fault Salt dome<br />

Gas<br />

Porous rock<br />

<strong>Oil</strong><br />

Impermeable rock<br />

Fossil water in porous reservoir rock<br />

Figure 5. Reservoir formations<br />

For an <strong>oil</strong> reservoir <strong>to</strong> form, porous rock needs <strong>to</strong> be covered by a nonporous<br />

layer such as salt, shale, chalk or mud rock that prevent the<br />

hydrocarbons from leaking out of the structure. As rock structures become<br />

folded <strong>and</strong> raised as a result of tec<strong>to</strong>nic movements, the hydrocarbons<br />

migrate out of the deposits <strong>and</strong> upward in porous rock <strong>and</strong> collect in crests<br />

under the non-permeable rock, with <strong>gas</strong> at the <strong>to</strong>p <strong>and</strong> <strong>oil</strong> <strong>and</strong> fossil water at<br />

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