A cArbon cApture And storAge network for yorkshire And humber
A cArbon cApture And storAge network for yorkshire And humber
A cArbon cApture And storAge network for yorkshire And humber
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Table 7.1 Potential storage sites – gas field<br />
Gas Storage Field Availability Range Storage Capacity Distance from Distance from Injectivity<br />
(mt) Easington (km) Theddlethorpe (km)<br />
Leman 2013 2025+ 870 160 140 Good<br />
(Permenco + Shell)<br />
Indefatigable & SW 2012 2015 222 180 160 Reasonable<br />
Viking 2013 2018 214 180 170 Good<br />
West Sole 2020 2030 136 70 80 Tight<br />
Galleon 2022 2032 128 145 130 Tight<br />
Hewett 2010 2015 216 130 100 Good<br />
Indefatigable (Shell) 2005 2007 111 260 230 Reasonable<br />
Barque & Barque S 2020 2030 89 100 100 Good<br />
Victor 2015 2020 73 220 180 Good<br />
Ravenspurn North 2013 2018 59 70 90 Tight<br />
Vulcan 2015 2020 53 160 140 Reasonable<br />
Audrey 2012 2017 49 140 140 Reasonable<br />
Clipper N 2030 2035 46 135 125 Tight<br />
Amethyst E & W 2010 2015 46 45 55 Tight<br />
Sean N & S 2035 2040 44 220 200 Reasonable<br />
Schooner 2019 2024 41 155 170 Tight<br />
Pickerill 2008 2013 40 70 65 Tight<br />
Table 7.2 Potential storage sites - saline aquifer<br />
Carbon Capture and Storage Network 27<br />
Saline Aquifer Storage Capacity Depth Underlying Remarks<br />
(Tyndall ref) (mt) (m) Gas field(s) from Tyndall<br />
2/48 3169 1100 approximately Large normal fault cuts through<br />
congruent to the structure.<br />
West Sole<br />
3/48 2302 1200 linear under Barque Galleon nearby. Many faults in the seal on<br />
and Clipper N. the above lying Bunter sandstone.<br />
4/49 1114 1400 Viking block 48/17 Movement of salt has caused faulting on<br />
the flanks of the structure. Faults extend<br />
upwards to the seabed.
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