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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)