The objective of this section is to provide the investigator with a method of procuring, processing, and interpreting the thermal signature recorded by gypsum wallboard exposed to fire environments.
Determine subject area prior to identifying sample location (that is, make a photo overview).
Evaluate subject area recognizing distinguishing variations in gypsum wallboard surface conditions:
2.1 Plume/Thermal signatures
2.1.1 Variation of these patterns - that is, levels of calcination
Select sampling locations
3.1 Greatest degree of observable calcination
3.2 A systematic sampling survey of adjoining regions to those specifically targeted
3.3 Areas related to potentially conflicting patterns of calcination
3.4 Control specimens protected from thermally induced change as a function of the fire
Mark the selected specimen location and map
4.1 Marking for pre-removal photos
4.2 Mapping for specimen location identification accuracy
Cut 6 cm x 6 cm using a sheet rock knife or similar tool. Place specimen into poly bag for protection.
Fracture the specimen by hand, preferably halving the piece - resulting in two 3 cm x 6 cm pieces.
Photograph fracture surface.
Identify coloration and/or apparent density changes in the cross-section of the specimen. Measure the depths of these distinguishable layers from the back of the affected surface.
Prepare power diffraction specimens by extracting material from each distinguishable layer.
9.1 Example: the top/exposed surface to 2 mm below the surface
9.2 The middle region (8-10 mm) from the unexposed surface
9.3 The back side of the specimen
Perform XRD on the prepared specimens. Suggested methodology: 2-q range: 10° -60° with steps of 0.1°.
Identify the top 6 peaks based on percent intensity (percent intensity is also known as height). Capture the d-spacing and percent intensity for use in the analysis.
Compare test data to that established by experimental testing and external standards.
9.2 List of gypsum samples and test conditions
Table 14 List of gypsum samples and test conditions
|
Sample ID |
Depth of sample |
Heat Flux (kW/m2) |
Duration (seconds) |
|
1GYP2_5X |
16 mm |
25 |
1500 |
|
1GYP5_5X |
16 mm |
25 |
4500 |
|
1GYP6_5X |
16 mm |
50 |
1500 |
|
1GYP7_5X |
16 mm |
50 |
1500 |
|
1GYP8_5x_2 |
16 mm |
63 |
1500 |
|
1GYP9_5x_2 |
16 mm |
63 |
1500 |
|
1GYP1_5X |
16 mm |
75 |
1500 |
|
1GYP3_5X |
16 mm |
75 |
1500 |
|
1GYP4_5X |
16 mm |
75 |
1500 |
|
1GYP10_5x |
16 mm |
83 |
1500 |
|
1GYP11_5x |
16 mm |
83 |
1500 |
|
1GYP12_5x |
16 mm |
83 |
1500 |
|
1GYP8_5X |
16 mm |
90 |
1500 |
|
1GYP9_5X |
16 mm |
90 |
1500 |
|
1GYP2_1 |
25 mm |
25 |
1500 |
|
1GYP5_1 |
25 mm |
25 |
4500 |
|
1GYP6_1 |
25 mm |
50 |
1500 |
|
1GYP7_1 |
25 mm |
50 |
1500 |
|
1GYP10_1 |
25 mm |
63 |
1500 |
|
1GYP11_1 |
25 mm |
63 |
1500 |
|
1GYP1_1 |
25 mm |
75 |
1500 |
|
1GYP14_1 |
25 mm |
75 |
1500 |
|
1GYP3_1 |
25 mm |
75 |
1500 |
|
1GYP4_1 |
25 mm |
75 |
1500 |
|
1GYP12_1 |
25 mm |
83 |
1500 |
|
1GYP13_1 |
25 mm |
83 |
1500 |
|
1GYP8_1 |
25 mm |
90 |
1500 |
|
1GYP9_1 |
25 mm |
90 |
1500 |
9.3 Data, measurements, and analysis
This section contains the raw data, the analysis, and the results which were shown in the main body of the dissertation in the figures. It is intended as a supplement to the final results shown in the body of the thesis.
9.3.1 Graphs of gypsums response to heat
It is useful to see exactly how all the data was taken. One of the central tenets of this dissertation is that the gypsum burns more steadily than wood. The next figures, Figure 169 through Figure 176, show the results of both 16 mm and 25 mm gypsum when heated in the cone calorimeter. It is useful to note the low variability between the samples at both low and high heat fluxes, both near and far away from the surface.
Figure 169 Temperature versus time profiles: 16 mm gypsum, 25 kW/m2 heat flux
Figure 170 Temperature versus time profiles: 25 mm gypsum, 25 kW/m2 heat flux
Figure 171 Temperature versus time profiles: 16 mm gypsum, 50 kW/m2 heat flux
Figure 172 Temperature versus time profiles: 25 mm gypsum, 50 kW/m2 heat flux
Figure 173 Temperature versus time profiles: 16 mm gypsum, 75 kW/m2 heat flux
Figure 174 Temperature versus time profiles: 25 mm gypsum, 75 kW/m2 heat flux
Figure 175 Temperature versus time profiles: 16 mm gypsum, 90 kW/m2 heat flux
Figure 176 Temperature versus time profiles: 25 mm gypsum, 90 kW/m2 heat flux
9.3.2 Analysis: rate of isotherm progression
In this section, we detail the calculations which were performed to draw our conclusions about the rate of isotherm progression. The manner of analysis is detailed below.
There were three isotherms which were followed. They were the 80° C isotherm (corresponding to dihydrate), the 200 ° C isotherm (corresponding to b-hemihydrate), and the 500° C isotherm (corresponding to anhydrous). For each thermocouple, the time between insertion into the calorimeter and the time when the thermocouple hit the isotherm was measured. The distance between the exposed surface and the thermocouple was already known. Because we used the 4 mm and the 12 mm thermocouples for these measurements, there were three different zones generated. 47
With a known distance, and a measured time, the rate of isotherm progression could be calculated. The detailed calculations are shown in Table 15 and closely parallel those of the wood samples shown in Table 7 and Table 8.
Table 15 Time required for isotherm to progress through Zone 0 and Zone 1 in gypsum
(TC=thermocouple)
|
COL. LABEL |
B |
C |
D |
E |
F |
G |
H |
I |
|
|
|
|
Time until hemihydrate forms48 (sec) |
Time until Insoluble b -CaSO4 forms49 (sec) |
Time until anhydrous |
|||
|
Gypsum Thickness |
Heat Flux (kW/m2) |
Sample ID |
4 mm TC |
12 mm TC |
4 mm TC |
12 mm TC |
4 mm TC |
12 mm TC |
|
16 mm |
25 |
1gyp2_5x |
22 |
114 |
159 |
975 |
|
|
|
16 mm |
25 |
1gyp5_5x |
27 |
130 |
220 |
1139 |
|
3206 |
|
16 mm |
50 |
1gyp6_5x |
18 |
96 |
108 |
879 |
1177 |
1313 |
|
16 mm |
50 |
1gyp7_5x |
14 |
94 |
96 |
867 |
805 |
1276 |
|
16 mm |
63 |
1gyp8_5x_2 |
13 |
65 |
74 |
566 |
536 |
1113 |
|
16 mm |
63 |
1gyp9_5x_2 |
11 |
52 |
84 |
734 |
592 |
1119 |
|
16 mm |
75 |
1gyp1_5x |
9 |
45 |
60 |
496 |
415 |
1089 |
|
16 mm |
75 |
1gyp3_5x |
10 |
44 |
50 |
499 |
377 |
1086 |
|
16 mm |
75 |
1gyp4_5x |
9 |
49 |
53 |
547 |
330 |
1070 |
|
16 mm |
83 |
1gyp10_5x |
|
|
|
|
|
|
|
16 mm |
83 |
1gyp11_5x |
4 |
56 |
33 |
611 |
126 |
982 |
|
16 mm |
83 |
1gyp12_5x |
16 |
54 |
191 |
|
834 |
|
|
16 mm |
90 |
1gyp8_5x |
10 |
70 |
79 |
659 |
344 |
913 |
|
16 mm |
90 |
1gyp9_5x |
7 |
70 |
55 |
590 |
184 |
884 |
|
25 mm |
25 |
1gyp2_1 |
30 |
146 |
226 |
1394 |
|
|
|
25 mm |
25 |
1gyp5_1 |
17 |
153 |
184 |
1443 |
|
|
|
25 mm |
50 |
1gyp6_1 |
15 |
136 |
122 |
1327 |
1550 |
|
|
25 mm |
50 |
1gyp7_1 |
10 |
110 |
82 |
1335 |
1052 |
|
|
25 mm |
63 |
1gyp10_1 |
15 |
|
|
|
994 |
|
|
25 mm |
63 |
1gyp11_1 |
|
|
|
|
|
|
|
25 mm |
75 |
1gyp1_1 |
8 |
67 |
70 |
536 |
500 |
|
|
25 mm |
75 |
1gyp14_1 |
15 |
130 |
122 |
1199 |
794 |
|
|
25 mm |
75 |
1gyp3_1 |
7 |
60 |
50 |
471 |
383 |
|
|
25 mm |
75 |
1gyp4_1 |
7 |
84 |
24 |
590 |
185 |
|
|
25 mm |
83 |
1gyp12_1 |
8 |
123 |
70 |
980 |
439 |
|
|
25 mm |
83 |
1gyp13_1 |
13 |
152 |
118 |
1336 |
637 |
|
|
25 mm |
90 |
1gyp8_1 |
17 |
99 |
116 |
938 |
568 |
|
|
25 mm |
90 |
1gyp9_1 |
11 |
85 |
110 |
818 |
510 |
|
Table 16 Calculation of rate of isotherm progression through gypsum Zone 0
This table uses the raw data set forth in Table 15 and calculates the rate of isotherm progression. The column labels refer to Table 15.
|
Gypsum Thickness |
Heat Flux (kW/m2) |
Sample ID |
Rate of hemi-hydrate isotherm51 moving through Zone 052 (mm/s)53 |
Rate of Insoluble b CaSO4 isotherm54 moving through Zone 0 (mm/s) |
Rate of anhydrous isotherm55 moving through Zone 0 (mm/s) |
|
|
|
|
=4 mm / Column D |
=4 mm / Col F |
=4 mm / Col H |
|
16 mm |
25 |
1gyp2_5x |
0.181818 |
0.025157 |
|
|
16 mm |
25 |
1gyp5_5x |
0.148148 |
0.018182 |
|
|
16 mm |
50 |
1gyp6_5x |
0.222222 |
0.037037 |
0.003398 |
|
16 mm |
50 |
1gyp7_5x |
0.285714 |
0.041667 |
0.004969 |
|
16 mm |
63 |
1gyp8_5x_2 |
0.307692 |
0.054054 |
0.007463 |
|
16 mm |
63 |
1gyp9_5x_2 |
0.363636 |
0.047619 |
0.006757 |
|
16 mm |
75 |
1gyp1_5x |
0.444444 |
0.066667 |
0.009639 |
|
16 mm |
75 |
1gyp3_5x |
0.400000 |
0.080000 |
0.010610 |
|
16 mm |
75 |
1gyp4_5x |
0.444444 |
0.075472 |
0.012121 |
|
16 mm |
83 |
1gyp10_5x |
|||
|
16 mm |
83 |
1gyp11_5x |
1.000000 |
0.121212 |
0.031746 |
|
16 mm |
83 |
1gyp12_5x |
0.250000 |
0.020942 |
0.004796 |
|
16 mm |
90 |
1gyp8_5x |
0.400000 |
0.050633 |
0.011628 |
|
16 mm |
90 |
1gyp9_5x |
0.571429 |
0.072727 |
0.021739 |
|
25 mm |
25 |
1gyp2_1 |
0.133333 |
0.017699 |
|
|
25 mm |
25 |
1gyp5_1 |
0.235294 |
0.021739 |
|
|
25 mm |
50 |
1gyp6_1 |
0.266667 |
0.032787 |
0.002581 |
|
25 mm |
50 |
1gyp7_1 |
0.400000 |
0.048780 |
0.003802 |
|
25 mm |
63 |
1gyp10_1 |
0.266667 |
0.004024 |
|
|
25 mm |
63 |
1gyp11_1 |
|||
|
25 mm |
75 |
1gyp1_1 |
0.500000 |
0.057143 |
0.008000 |
|
25 mm |
75 |
1gyp14_1 |
0.266667 |
0.032787 |
0.005038 |
|
25 mm |
75 |
1gyp3_1 |
0.571429 |
0.080000 |
0.010444 |
|
25 mm |
75 |
1gyp4_1 |
0.571429 |
0.166667 |
0.021622 |
|
25 mm |
83 |
1gyp12_1 |
0.500000 |
0.057143 |
0.009112 |
|
25 mm |
83 |
1gyp13_1 |
0.307692 |
0.033898 |
0.006279 |
|
25 mm |
90 |
1gyp8_1 |
0.235294 |
0.034483 |
0.007042 |
|
25 mm |
90 |
1gyp9_1 |
0.363636 |
0.036364 |
0.007843 |
Table 17 Calculation of rate of isotherm progression through gypsum Zone 1
This table is a parallel of Table 16 for Zone 1. It uses the raw data set forth in Table 15 and calculates the rate of isotherm progression. The column labels refer to Table 15.
|
Gypsum Thickness |
Heat Flux (kW/m2) |
Sample ID |
Rate of hemi-hydrate isotherm moving through Zone 156 (mm/s) |
Rate of Insoluble b CaSO4 isotherm moving through Zone 1 (mm/s) |
Rate of anhydrous isotherm moving through Zone 1 (mm/s) |
|
|
|
|
=8 mm /(Col E - Col. D) |
=8 mm /(Col G - Col. F) |
=8 mm /(Col I - Col. H) |
|
16 mm |
25 |
1gyp2_5x |
0.086957 |
0.009804 |
|
|
16 mm |
25 |
1gyp5_5x |
0.077670 |
0.008705 |
|
|
16 mm |
50 |
1gyp6_5x |
0.102564 |
0.010376 |
0.058824 |
|
16 mm |
50 |
1gyp7_5x |
0.100000 |
0.010376 |
0.016985 |
|
16 mm |
63 |
1gyp8_5x_2 |
0.153846 |
0.016260 |
0.013865 |
|
16 mm |
63 |
1gyp9_5x_2 |
0.195122 |
0.012308 |
0.015180 |
|
16 mm |
75 |
1gyp1_5x |
0.222222 |
0.018349 |
0.011869 |
|
16 mm |
75 |
1gyp3_5x |
0.235294 |
0.017817 |
0.011283 |
|
16 mm |
75 |
1gyp4_5x |
0.200000 |
0.016194 |
0.010811 |
|
16 mm |
83 |
1gyp10_5x |
|||
|
16 mm |
83 |
1gyp11_5x |
0.153846 |
0.013841 |
0.009346 |
|
16 mm |
83 |
1gyp12_5x |
0.210526 |
||
|
16 mm |
90 |
1gyp8_5x |
0.133333 |
0.013793 |
0.014060 |
|
16 mm |
90 |
1gyp9_5x |
0.126984 |
0.014953 |
0.011429 |
|
25 mm |
25 |
1gyp2_1 |
0.068966 |
0.006849 |
|
|
25 mm |
25 |
1gyp5_1 |
0.058824 |
0.006354 |
|
|
25 mm |
50 |
1gyp6_1 |
0.066116 |
0.006639 |
|
|
25 mm |
50 |
1gyp7_1 |
0.080000 |
0.006385 |
|
|
25 mm |
63 |
1gyp10_1 |
|||
|
25 mm |
63 |
1gyp11_1 |
|||
|
25 mm |
75 |
1gyp1_1 |
0.135593 |
0.017167 |
|
|
25 mm |
75 |
1gyp14_1 |
0.069565 |
0.007428 |
|
|
25 mm |
75 |
1gyp3_1 |
0.150943 |
0.019002 |
|
|
25 mm |
75 |
1gyp4_1 |
0.103896 |
0.014134 |
|
|
25 mm |
83 |
1gyp12_1 |
0.069565 |
0.008791 |
|
|
25 mm |
83 |
1gyp13_1 |
0.057554 |
0.006568 |
|
|
25 mm |
90 |
1gyp8_1 |
0.097561 |
0.009732 |
|
|
25 mm |
90 |
1gyp9_1 |
0.108108 |
0.011299 |
|
9.3.3 Determination of exposure time and heat flux
In this section, we present tables showing the isotherm progression calculated using the rates observed in Table 16 and Table 17. They are presented for three isotherms (the 80° isotherm, the 200° isotherm, and the 500° isotherm) for two depths of gypsum (16 mm and 25 mm depths) in Table 18 through Table 23 below.
Table 18 Average time for 80 C isotherm to progress to depths of 4 and 12 mm in 16 mm gypsum
|
Heat flux (kW/m2) |
Depth from exposed surface (mm) |
Average time until 80° isotherm reaches depth (seconds) 57 |
Max time until 80° isotherm reaches depth (seconds) |
Min time until 80° isotherm reaches depth (seconds) |
|
25 |
0 |
0.00 |
0.00 |
0.00 |
|
25 |
4 |
24.24 |
27.00 |
22.00 |
|
25 |
12 |
121.43 |
130.00 |
114.00 |
|
|
|
|
|
|
|
50 |
0 |
0.00 |
0.00 |
0.00 |
|
50 |
4 |
15.75 |
18.00 |
14.00 |
|
50 |
12 |
94.74 |
98.00 |
92.00 |
|
|
|
|
|
|
|
63 |
0 |
0.00 |
0.00 |
0.00 |
|
63 |
4 |
11.92 |
13.00 |
11.00 |
|
63 |
12 |
57.77 |
65.00 |
52.00 |
|
|
|
|
|
|
|
75 |
0 |
0.00 |
0.00 |
0.00 |
|
75 |
4 |
9.31 |
10.00 |
9.00 |
|
75 |
12 |
45.81 |
50.00 |
43.00 |
|
|
|
|
|
|
|
83 |
0 |
0.00 |
0.00 |
0.00 |
|
83 |
4 |
6.40 |
16.00 |
4.00 |
|
83 |
12 |
50.31 |
68.00 |
42.00 |
|
|
|
|
|
|
|
90 |
0 |
0.00 |
0.00 |
0.00 |
|
90 |
4 |
8.24 |
10.00 |
7.00 |
|
90 |
12 |
69.70 |
73.00 |
67.00 |
Table 19 Average time for 80 C isotherm to progress to depths of 4 and 12 mm in 25 mm gypsum
|
Heat flux (kW/m2) |
Depth from exposed surface (mm) |
Average time until 80° isotherm reaches depth (seconds) 58 |
Max time until 80° isotherm reaches depth (seconds) |
Min time until 80° isotherm reaches depth (seconds) |
|
25 |
0 |
0.00 |
0.00 |
0.00 |
|
25 |
4 |
21.70 |
30.00 |
17.00 |
|
25 |
12 |
146.91 |
166.00 |
133.00 |
|
|
|
|
|
|
|
50 |
0 |
0.00 |
0.00 |
0.00 |
|
50 |
4 |
12.00 |
15.00 |
10.00 |
|
50 |
12 |
121.50 |
136.00 |
110.00 |
|
|
|
|
|
|
|
63 |
0 |
0.00 |
0.00 |
0.00 |
|
63 |
4 |
N/A59 |
N/A |
N/A |
|
63 |
12 |
N/A |
N/A |
N/A |
|
|
|
|
|
|
|
75 |
0 |
0.00 |
0.00 |
0.00 |
|
75 |
4 |
8.38 |
15.00 |
7.00 |
|
75 |
12 |
77.94 |
130.00 |
60.00 |
|
|
|
|
|
|
|
83 |
0 |
0.00 |
0.00 |
0.00 |
|
83 |
4 |
9.90 |
13.00 |
8.00 |
|
83 |
12 |
135.77 |
152.00 |
123.00 |
|
|
|
|
|
|
|
90 |
0 |
0.00 |
0.00 |
0.00 |
|
90 |
4 |
13.36 |
17.00 |
11.00 |
|
90 |
12 |
91.15 |
99.00 |
85.00 |
Table 20 Average time for 200 C isotherm to progress to depths of 4 and 12 mm in 16 mm gypsum
|
Heat flux (kW/m2) |
Depth from exposed surface (mm) |
Average time until 200° isotherm reaches depth (seconds) 60 |
Max time until 200° isotherm reaches depth (seconds) |
Min time until 200° isotherm reaches depth (seconds) |
|
25 |
0 |
0.00 |
0.00 |
0.00 |
|
25 |
4 |
184.59 |
220.00 |
159.00 |
|
25 |
12 |
1049.03 |
1139.00 |
975.00 |
|
|
|
|
|
|
|
50 |
0 |
0.00 |
0.00 |
0.00 |
|
50 |
4 |
101.65 |
108.00 |
96.00 |
|
50 |
12 |
872.65 |
879.00 |
867.00 |
|
|
|
|
|
|
|
63 |
0 |
0.00 |
0.00 |
0.00 |
|
63 |
4 |
78.68 |
84.00 |
74.00 |
|
63 |
12 |
638.75 |
734.00 |
566.00 |
|
|
|
|
|
|
|
75 |
0 |
0.00 |
0.00 |
0.00 |
|
75 |
4 |
54.02 |
60.00 |
50.00 |
|
75 |
12 |
512.38 |
554.00 |
486.00 |
|
|
|
|
|
|
|
83 |
0 |
0.00 |
0.00 |
0.00 |
|
83 |
4 |
56.28 |
191.00 |
33.00 |
|
83 |
12 |
634.28 |
769.00 |
611.00 |
|
|
|
|
|
|
|
90 |
0 |
0.00 |
0.00 |
0.00 |
|
90 |
4 |
64.85 |
79.00 |
55.00 |
|
90 |
12 |
621.44 |
659.00 |
590.00 |
Table 21 Average time for 200 C isotherm to progress to depths of 4 and 12 mm in 25 mm gypsum
|
Heat flux (kW/m2) |
Depth from exposed surface (mm) |
Average time until 200° isotherm reaches depth (seconds)61 |
Max time until 200° isotherm reaches depth (seconds) |
Min time until 200° isotherm reaches depth (seconds) |
|
25 |
0 |
0.00 |
0.00 |
0.00 |
|
25 |
4 |
202.85 |
226.00 |
184.00 |
|
25 |
12 |
1414.64 |
1485.00 |
1352.00 |
|
|
|
|
|
|
|
50 |
0 |
0.00 |
0.00 |
0.00 |
|
50 |
4 |
98.08 |
122.00 |
82.00 |
|
50 |
12 |
1326.61 |
1375.00 |
1287.00 |
|
|
|
|
|
|
|
63 |
0 |
0.00 |
0.00 |
0.00 |
|
63 |
4 |
N/A |
N/A |
N/A |
|
63 |
12 |
N/A |
N/A |
N/A |
|
|
|
|
|
|
|
75 |
0 |
0.00 |
0.00 |
0.00 |
|
75 |
4 |
47.53 |
122.00 |
24.00 |
|
75 |
12 |
601.82 |
1199.00 |
445.00 |
|
|
|
|
|
|
|
83 |
0 |
0.00 |
0.00 |
0.00 |
|
83 |
4 |
87.87 |
118.00 |
70.00 |
|
83 |
12 |
1129.58 |
1336.00 |
980.00 |
|
|
|
|
|
|
|
90 |
0 |
0.00 |
0.00 |
0.00 |
|
90 |
4 |
112.92 |
116.00 |
110.00 |
|
90 |
12 |
873.67 |
938.00 |
818.00 |
Table 22 Average time for 500 C isotherm to progress to depths of 4 and 12 mm in 16 mm gypsum
|
Heat flux (kW/m2) |
Depth from exposed surface (mm) |
Average time until 200° isotherm reaches depth (seconds) 62 |
Max time until 200° isotherm reaches depth (seconds) |
Min time until 200° isotherm reaches depth (seconds) |
|
25 |
0 |
0.00 |
0.00 |
0.00 |
|
25 |
4 |
N/A |
N/A |
N/A |
|
25 |
12 |
N/A |
N/A |
N/A |
|
|
|
|
|
|
|
50 |
0 |
0.00 |
0.00 |
0.00 |
|
50 |
4 |
956.09 |
1177.00 |
805.00 |
|
50 |
12 |
1167.15 |
1648.00 |
941.00 |
|
|
|
|
|
|
|
63 |
0 |
0.00 |
0.00 |
0.00 |
|
63 |
4 |
562.61 |
592.00 |
536.00 |
|
63 |
12 |
1113.48 |
1169.00 |
1063.00 |
|
|
|
|
|
|
|
75 |
0 |
0.00 |
0.00 |
0.00 |
|
75 |
4 |
370.72 |
415.00 |
330.00 |
|
75 |
12 |
1077.35 |
1155.00 |
1004.00 |
|
|
|
|
|
|
|
83 |
0 |
0.00 |
0.00 |
0.00 |
|
83 |
4 |
218.93 |
834.00 |
126.00 |
|
83 |
12 |
1074.93 |
1690.00 |
982.00 |
|
|
|
|
|
|
|
90 |
0 |
0.00 |
0.00 |
0.00 |
|
90 |
4 |
239.76 |
344.00 |
184.00 |
|
90 |
12 |
867.50 |
1044.00 |
753.00 |
Table 23 Average time for 500 isotherm to progress to 4 and 12 mm depth in 25 mm gypsum
|
Heat flux (kW/m2) |
Depth from exposed surface (mm) |
Average time until 500° isotherm reaches depth (seconds) 63 |
Max time until 500° isotherm reaches depth (seconds) |
Min time until 500° isotherm reaches depth (seconds) |
|
25 |
0 |
0.00 |
0.00 |
0.00 |
|
25 |
4 |
N/A |
N/A |
N/A |
|
25 |
12 |
N/A |
N/A |
N/A |
|
|
|
|
|
|
|
50 |
0 |
0.00 |
0.00 |
0.00 |
|
50 |
4 |
1253.34 |
1550.00 |
1052.00 |
|
50 |
12 |
N/A |
N/A |
N/A |
|
|
|
|
|
|
|
63 |
0 |
0.00 |
0.00 |
0.00 |
|
63 |
4 |
994.00 |
994.00 |
994.00 |
|
63 |
12 |
N/A |
N/A |
N/A |
|
|
|
|
|
|
|
75 |
0 |
0.00 |
0.00 |
0.00 |
|
75 |
4 |
354.74 |
794.00 |
185.00 |
|
75 |
12 |
N/A |
N/A |
N/A |
|
|
|
|
|
|
|
83 |
0 |
0.00 |
0.00 |
0.00 |
|
83 |
4 |
519.78 |
637.00 |
439.00 |
|
83 |
12 |
N/A |
N/A |
N/A |
|
90 |
0 |
0.00 |
0.00 |
0.00 |
|
90 |
4 |
537.44 |
568.00 |
510.00 |
|
90 |
12 |
N/A |
N/A |
N/A |
This dissertation has shown how X-ray diffraction can be used to determine the heat flux, and hence the time, to which a gypsum sample was exposed. The X-ray diffraction has shown three distinct areas of peaks, which are outlined in Table 24 below.
This table breaks the XRD data down into the three regions, defined as follows:
H: hydrate: 2q =11-16 degrees.
HH: hemihydrate: 2q =28-33 degrees
A: anhydrous: 2q = 37-42 degrees
For each type of material, the data in the table shows the approximate height of any peaks which were in the corresponding degree ranges. Note: peak heights are very approximate, and not all peaks are registered here.
Table 24 XRD peaks analysis table, showing three crystalline forms
|
Type of material |
Region à |
|
Hydrate region (one range) |
|
Hemihydrate region (two ranges) |
|
Anhydrous region (two ranges) |
||
|
|
Degree rangeà |
|
2q =11-16 |
|
2q = 28-30 |
2q = 30-33 |
|
2q = 37-40 |
2q = 40-42 |
|
|
|
|
|
|
|
|
|
|
|
|
H |
Control |
|
3200 |
|
2700 |
1300 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
HH |
222 C |
|
1800 |
|
2100 |
1800 |
|
|
|
|
HH |
280 C |
|
1800 |
|
2100 |
1800 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
HH, A |
350 C |
|
1900 |
|
2200 |
2100 |
|
|
|
|
HH, A |
380 C |
|
|
|
1000 |
|
|
600 |
600 |
|
HH, A |
400 C |
|
|
|
800 |
800 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
A |
500 C |
|
|
|
|
1200 |
|
700 |
700 |
|
A |
600 C |
|
|
|
|
1200 |
|
700 |
700 |
|
A |
700 C |
|
|
|
|
1300 |
|
900 |
800 |
|
A |
800 C |
|
|
|
|
2200 |
|
1300 |
1200 |
|
A |
900 C |
|
|
|
|
2200 |
|
1500 |
1200 |
|
A |
1000 C |
|
|
|
|
2500 |
|
1600 |
1600 |
|
A |
1100 C |
|
|
|
|
N/A |
|
2000 |
1600 |
|
A |
1200 C |
|
|
|
|
2100 |
|
1600 |
1300 |