OR/19/015 Appendix 2 - Measured subsurface temperature data
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Busby, J P. 2019. Thermal conductivity and subsurface temperature data pertaining to the Glasgow Geothermal Energy Research Field Site (GGERFS). British Geological Survey Open Report, OR/19/015. |
Hallside Borehole (266940E, 659750N) Data ref. Burley et al. (1984)[1] | |||
Depth (m) | Temperature (°C) | Type | Comment |
350.0 | 11.8 | LOG | 60 hr after circulation correction applied |
Queenslie No. 4 Borehole (264660E, 665980N) Data ref. Burley et al. (1984)[1] | |||
Depth (m) | Temperature (°C) | Type | Comment |
691.0 | 36.0 | BHT | No correction applied |
Bargeddie No. 1 Borehole (269378E, 664649N) Data ref. DECC Onshore Wells | |||
Depth (m) | Temperature (°C) | Type | Comment |
720.8 | 30.3 | DST | DST 6; tight? |
773.9 | 29.5 | DST | DST 2; produced gas |
802.8 | 32.9 | DST | DST 4; tight? |
884.0 | 36.1 | DST | DST 5; produced water |
934.9 | 38.0 | DST | DST 3; produced water |
978.9 | 38.7 | DST | DST 1; produced water |
Maryhill Borehole (257180E, 668560N) Data ref. Wheildon et al. (1985)[2] | |||
Depth (m) | Temperature (°C) | Type | Comment |
6.12 | 9.36 | EQM | |
9.18 | 9.39 | EQM | |
12.24 | 9.39 | EQM | |
15.30 | 9.43 | EQM | |
18.35 | 9.50 | EQM | |
21.41 | 9.64 | EQM | |
24.47 | 9.80 | EQM | |
27.53 | 10.01 | EQM | |
30.59 | 10.17 | EQM | |
33.65 | 10.26 | EQM | |
36.71 | 10.31 | EQM | |
39.77 | 10.39 | EQM | |
42.83 | 10.49 | EQM | |
45.89 | 10.62 | EQM | |
48.95 | 10.77 | EQM | |
52.00 | 10.92 | EQM | |
55.06 | 11.01 | EQM | |
58.12 | 11.09 | EQM | |
61.18 | 11.18 | EQM | |
64.24 | 11.29 | EQM | |
67.30 | 11.36 | EQM | |
70.36 | 11.43 | EQM | |
73.42 | 11.48 | EQM | |
76.48 | 11.53 | EQM | |
79.54 | 11.61 | EQM | |
82.60 | 11.72 | EQM | |
85.65 | 11.83 | EQM | |
88.71 | 11.92 | EQM | |
91.77 | 12.00 | EQM | |
94.83 | 12.08 | EQM | |
97.89 | 12.28 | EQM | |
100.95 | 12.29 | EQM | |
104.01 | 12.40 | EQM | |
107.07 | 12.51 | EQM | |
110.13 | 12.71 | EQM | |
113.19 | 12.91 | EQM | |
116.25 | 13.09 | EQM | |
119.30 | 13.27 | EQM | |
122.36 | 13.45 | EQM | |
125.42 | 13.67 | EQM | |
128.48 | 13.87 | EQM | |
131.54 | 14.05 | EQM | |
134.60 | 14.17 | EQM | |
137.66 | 14.27 | EQM | |
140.72 | 14.37 | EQM | |
143.78 | 14.47 | EQM | |
146.84 | 14.55 | EQM | |
149.89 | 14.64 | EQM | |
152.95 | 14.73 | EQM | |
156.01 | 14.82 | EQM | |
159.07 | 14.94 | EQM | |
162.13 | 15.07 | EQM | |
165.19 | 15.23 | EQM | |
168.25 | 15.37 | EQM | |
171.31 | 15.49 | EQM | |
174.37 | 15.61 | EQM | |
177.43 | 15.73 | EQM | |
180.49 | 15.84 | EQM | |
183.54 | 15.93 | EQM | |
186.60 | 16.01 | EQM | |
189.66 | 16.09 | EQM | |
192.72 | 16.18 | EQM | |
195.78 | 16.27 | EQM | |
198.84 | 16.35 | EQM | |
201.90 | 16.43 | EQM | |
204.96 | 16.51 | EQM | |
208.02 | 16.60 | EQM | |
211.08 | 16.69 | EQM | |
214.14 | 16.77 | EQM | |
217.19 | 16.86 | EQM | |
220.25 | 16.95 | EQM | |
223.31 | 17.04 | EQM | |
226.37 | 17.13 | EQM | |
229.43 | 17.24 | EQM | |
232.49 | 17.32 | EQM | |
235.55 | 17.41 | EQM | |
238.61 | 17.50 | EQM | |
241.67 | 17.58 | EQM | |
244.73 | 17.64 | EQM | |
247.79 | 17.69 | EQM | |
250.84 | 17.73 | EQM | |
253.90 | 17.78 | EQM | |
256.96 | 17.82 | EQM | |
260.02 | 17.88 | EQM | |
263.08 | 17.97 | EQM | |
266.14 | 18.07 | EQM | |
269.20 | 18.18 | EQM | |
272.26 | 18.30 | EQM | |
275.32 | 18.40 | EQM | |
278.38 | 18.49 | EQM | |
281.44 | 18.61 | EQM | |
284.49 | 18.78 | EQM | |
287.55 | 18.96 | EQM | |
290.61 | 19.18 | EQM | |
293.67 | 19.39 | EQM | |
296.73 | 19.57 | EQM | |
299.79 | 19.80 | EQM | |
302.85 | 20.01 | EQM | |
303.12 | 20.03 | EQM |
Hurlet House borehole (250100E, 661200N) Data ref. Oxburgh (1982)[3] | |||
Depth (m) | Temperature (°C) | Type | Comment |
15 | 9.2 | LOG | |
21 | 9.3 | LOG | |
40 | 9.8 | LOG | |
75 | 10.7 | LOG | |
85 | 11.0 | LOG | |
90 | 11.2 | LOG | |
95 | 11.3 | LOG | |
105 | 11.5 | LOG | |
115 | 11.6 | LOG | |
125 | 11.9 | LOG | |
135 | 12.1 | LOG | |
145 | 12.3 | LOG | |
160 | 12.6 | LOG | |
175 | 12.9 | LOG | |
185 | 13.1 | LOG | |
195 | 13.3 | LOG | |
205 | 13.5 | LOG | |
215 | 13.6 | LOG | |
225 | 13.8 | LOG | |
235 | 14.0 | LOG | |
240 | 14.1 | LOG | |
245 | 14.2 | LOG | |
255 | 14.4 | LOG | |
260 | 14.6 | LOG | |
265 | 14.7 | LOG | |
270 | 14.8 | LOG | |
275 | 15.0 | LOG | |
280 | 15.1 | LOG | |
285 | 15.3 | LOG | |
290 | 15.5 | LOG | |
295 | 15.6 | LOG |
Blythswood Borehole (250030E, 668230N) Data ref. Burley et al. (1984)[1] | |||
Depth (m) | Temperature (°C) | Type | Comment |
105.0 | 12.0 | EQM |
Highhouse Colliery (253210E, 672020N) Data ref. Burley et al. (1984)[1] | |||
Depth (m) | Temperature (°C) | Type | Comment |
436.0 | 18.0 | MWT |
South Balgray Borehole (250000E, 675000N) Data ref. Burley et al. (1984)[1] | |||
Depth (m) | Temperature (°C) | Type | Comment |
137.0 | 14.5 | EQM | |
160.0 | 15.3 | EQM |
Salsburgh 1A Borehole (281660E, 664860N) Data ref. Burley et al. (1984)[1] | |||
Depth (m) | Temperature (°C) | Type | Comment |
874.0 | 29.0 | DST | No correction applied |
883.0 | 30.0 | BHT | No correction applied |
Salsburgh 2 Borehole (282110E, 663850N) Data ref. Rollin (1987)[4] | |||
Depth (m) | Temperature (°C) | Type | Comment |
1104.0 | 44.0 | BHT | No correction applied |
Craighead No. 1 Borehole (282670E, 662120N) Data ref. Burley et al. (1984)[1] | |||
Depth (m) | Temperature (°C) | Type | Comment |
977.0 | 35.0 | BHT | No correction applied |
Clachie Bridge Borehole (264470E, 683680N) Data ref. Burley et al. (1984)[1] & Oxburgh (1982)[3] | |||
Depth (m) | Temperature (°C) | Type | Comment |
30 | 7.0 | LOG | |
35 | 7.1 | LOG | |
45 | 7.4 | LOG | |
55 | 7.6 | LOG | |
80 | 8.3 | LOG | |
90 | 8.6 | LOG | |
120 | 9.3 | LOG | |
130 | 9.6 | LOG | |
135 | 9.7 | LOG | |
140 | 9.8 | LOG | |
145 | 9.9 | LOG | |
170 | 10.6 | LOG | |
180 | 10.8 | LOG | |
200 | 11.3 | LOG | |
205 | 11.4 | LOG | |
215 | 11.6 | LOG | |
225 | 11.8 | LOG | |
230 | 11.9 | LOG | |
235 | 12.0 | LOG | |
245 | 12.2 | LOG | |
265 | 12.6 | LOG | |
285 | 13.0 | LOG | |
290 | 13.0 | LOG | |
300 | 13.2 | LOG |
References
- ↑ 1.0 1.1 1.2 1.3 1.4 1.5 1.6 1.7 BURLEY, A J, EDMUNDS, W M, and GALE, I N. 1984. Investigation of the geothermal potential of the UK: catalogue of geothermal data for the land area of the United Kingdom; Second revision. British Geological Survey, 161pp. (WJ/GE/84/20) (Unpublished)
- ↑ WHEILDON, J, GEBSKI, J S, and THOMAS-BETTS, A. 1985. Further Investigations of the UK Heat Flow Field (1981–1984). Investigation of the Geothermal Potential of the UK. British Geological Survey, Keyworth, Nottingham.
- ↑ 3.0 3.1 OXBURGH, E R. 1982. Compilation of heat flow data measured by the Oxford University Heat Flow Group under contract to the Department of Energy. Unpublished document submitted to J D Garnish, ETSU, Harwell.
- ↑ ROLLIN, K E. 1987. Investigation of the geothermal potential of the UK: catalogue of geothermal data for the land area of the United Kingdom; Third revision. British Geological Survey, (WJ/GE/87/7) (Unpublished)