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→Core analysis reports
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{{Table 8
{| class = "wikitable"
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|+ {{table number|2}}A typical core analysis report
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! colspan = 8|Core 1 2244.80-2300.10 m (7364.82-7546.25 ft) Drilled Depth
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! Sample || Depth || KH<sup>1</sup> || KV<sup>2</sup> || CPOR<sup>3</sup> || CSO<sup>4</sup> || CSW<sup>5</sup> || RHOG<sup>6</sup>
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| 1 || 2244.95 || 838.00 || - || 15.7 || 52.30 || 3.4 || 2.65
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| 2 || 2245.24 || 2180.00 || - || 16.1 || 46.20 || 3.3 || 2.64
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| 3 || 2245.51 || 995.00 || - || 15.0 || 50.30 || 3.6 || 2.64
|-
| 4 || 2245.78 || 766.00 || - || 14.9 || 48.50 || 3.5 || 2.65
|-
| 5 || 2246.25 || 165.00 || - || 12.2 || 41.20 || 10.2 || 2.65
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| 6 || 2246.50 || 474.00 || 390.00 || 15.9 || 51.50 || 3.4 || 2.65
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| 7 || 2246.95 || 521.00 || - || 15.3 || 42.60 || 8.1 || 2.64
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| 8 || 2247.75 || 260.00 || - || 12.4 || 49.70 || 7.2 || 2.65
|-
| 9 || 2248.05 || 374.00 || - || 15.7 || 52.40 || 6.8 || 2.64
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| 10 || 2248.25 || 88.90 || - || 14.1 || 50.10 || 10.2 || 2.65
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| 11 || 2248.45 || 42.20 || - || 10.9 || 49.70 || 8.2 || 2.65
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| 12 || 2250.42 || 672.00 || - || 15.3 || 51.30 || 1.2 || 2.65
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| 13 || 2250.75 || colspan = 5|Preserved sample
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| 14 || 2300.00 || 76.30 || - || 9.5 || 47.90 || 5.6 || 2.54
|}
''<sup>1 = horizontal permeability to air (md.) 2 = vertical permeability to air (md). 3 = core porosity (%). 4 = core oil saturation (%). 5 = core water saturation (%). 6 = grain density (g/cm<sup>3</sup>).</sup>''
The depths at which preserved core samples have been picked will also be listed. These are selected pieces of core that are kept to preserve the conditions of the rock as close to those in the reservoir as possible. They may be required for special core analysis such as wettability studies (Bajsarowicz, 1992). One preservation method is to store the samples in sealed jars containing simulated formation brine.
The depths at which preserved core samples have been picked will also be listed. These are selected pieces of core that are kept to preserve the conditions of the rock as close to those in the reservoir as possible. They may be required for special core analysis such as wettability studies (Bajsarowicz, 1992). One preservation method is to store the samples in sealed jars containing simulated formation brine.