Figure 4. Characteristics of
discharged thermal water from each microfacies. 4.1 Map of the study site
showing approximate microfacies locations. Numbers refer to localities were
measurements were taken (see Figure 4.3). (4.2) Representative examples
of glass slides with subaerially accreted silica after 67 days. Differences
between slides indicate different rates of subaerial silica accretion. Dashed
blue line marks average water level. Note the relatively large subaqueous
sulphur accumulation in Microfacies 1. A yellow-light brown substance (sulphur?
and/or organics?) accumulated subaqueously in Microfacies 2. Bar
represents ~3 cm. Silica accretion rates were unable to be measured for
Microfacies 3. (Continued below.)
Figure 4 (continued). 4.3. Temperature, pH, water level changes and silica accretion measurements. N.R. = not recorded. No significant water temperature changes were observed between seasons.
Locality
number |
Microfacies |
Water temperature
(summer/winter)
(°C) |
Water level
(summer/winter)
(mm) |
Water
pH |
Silica accumulation
over 67 days (g) |
1
|
Stream
|
30.8/17
|
150/159
|
2.03
|
N.R.
|
2
|
2
|
49
|
12/14
|
2.3
|
0.1287
|
3
|
2
|
55
|
N.R.
|
2.25
|
N.R.
|
4
|
2
|
58
|
20/23
|
2.14
|
N.R.
|
5
|
2
|
57.9
|
8/12
|
2.23
|
N.R.
|
6
|
2
|
55
|
12/18
|
2.23
|
0.1289
|
7
|
2
|
54.6
|
12/15
|
N.R.
|
N.R.
|
8
|
2
|
58
|
12/16
|
2.3
|
0.1281
|
9
|
2 and 3
|
59.8
|
6/10
|
2.13
|
N.R.
|
10
|
4
|
45
|
No change
|
2.24
|
0.0092
|
11
|
2
|
85
|
10/12
|
2.10
|
0.0802
|
12
|
1
|
64.2
|
10/14
|
2.13
|
N.R.
|
13
|
2
|
54
|
10/19
|
2.12
|
N.R.
|
14
|
2
|
38.8
|
130/136
|
N.R.
|
N.R.
|
15
|
2
|
63
|
5/8
|
2.24
|
N.R.
|
16
|
1
|
63.9
|
6/10
|
N.R.
|
N.R.
|
17
|
1
|
83.2
|
N.R.
|
2.28
|
0.2752
|
18
|
1
|
76.1
|
25/28
|
N.R.
|
N.R.
|
19
|
1
|
78.2
|
20/25
|
N.R.
|
0.2036
|
20
|
4
|
67
|
No change
|
N.R.
|
0.0098
|
21
|
1
|
84.6
|
N.R.
|
2.26
|
N.R.
|
22
|
2
|
59.4
|
18/20
|
2.23
|
N.R.
|
23
|
1
|
78.1
|
21/25
|
2.27
|
N.R.
|
24
|
4
|
52
|
No change
|
2.22
|
N.R.
|
25
|
1
|
91
|
N.R.
|
N.R.
|
N.R.
|
26
|
Stream
|
33.2/20.9
|
120/130
|
N.R.
|
N.R.
|
|