TABLE 82
Summary of the Thermodynamic Data Computed from the Balloon Ascension to 30,000 Meters
Made at Huron, South Dakota, September 1, 1910
z
T
P
p
Cp
Q
Wi—Wo
Ui—Uo
Kio
log c
a
Height,
in
Meters
Tempera
ture
Pressure
Density
Specific
Heat
Ratio
Velocity
m. p. s.
External
Work of
Expansion
Inner
Kinetic
Energy
Radiation.
Coefficient
in the
Law
Exponent
in the
Law
50000
49
0 0
7.86
-174.
+808.
-9033.
-5.074
3.600
2.6
4.18 X 10 -6
4.900 X10 -8
113.66
-7600.
.0003
-5.295
3.700
48
6.3
1.48X10- 2
1.637 x10 -5
497.19
2002.
-5370.
.1156
-5.448
3.770
47
11.9
0.717
2.586X10-*
807.42
3379.
-4615.
1.501
-5.585
3.830
46
19.6
6.56
.001247
929.28
6204.9
-6689.1
- 13.063
-5.738
3.905
45000
28.7
27.47
.003452
959.75
5616.5
-7042.3
- 51.36
-5.618
3.843
44
48.5
67.69
.006555
738.48
4321.4
-7830.8
- 158.0
-5.427
3.760
43
78.0
117.63
.009710
537.55
3245.2
-8281.1
- 348.2
-5.274
3.691
42
108.7
170.2
.01263
429.16
2731.6
-8651.1
- 614.5
-5.161
3.640
41
140.9
224.
.01539
358.49
2336.3
-8815.8
- 934.6
-5.077
3.602
40000
170.5
279.
.01796
315.71
2141.7
-8931.6
-1278.2
-5.025
3.578
39
192.3
337.
.02054
295.59
2016.1
-8948.6
-1607.9
-4.999
3.567
38
208.2
400.
.02373
286.81
1993.1
-8955.7
-1919.4
-4.992.
3.564
37
216.1
470.
.02600
289.48
2036.8
-8960.1
-2218.7
-5.000
3.568
36
222.0
549.
.02905
294.77
0.0
2108.2
-8958.0
-2522.
-5.011
3.573
35000
224.8
640.
.03239
304.28
1.0
2153.0
-8894.8
-2830.
-5.028
3.580
34
225.8
744.
.03607
316.45
2.0
2281.7
-8904.9
-3155.
-5.046
3.588
33
227.4
866.
.04015
328.22
2.8
2324.7
-8832.4
-3517.
-5.066
3.596
32
229.2
1005.
.04466
340.02
3.2
2428.0
-8818.5
-3926.
-5.081
3.604
31
231.1
1166.
.04963
352.02
3.6
2527.8
-8792.4
-4388.
-5.095
3.610
30000
232.3
1352.
.05512
365.58
3.8
2599.2
-8722.9
-4849.
-5.120
3.622
29
1 232.5
1565.
.06118
380.93
3.5
2748.1
-8718.2
-5357.
-5.140
3.630
28
232.9
1814.
.06795
396.82
3.0
2809.0
-8619.8
-5960.
-5.157
3.638
27
233.3
2098.
.07536
413.15
2.5
2955.5
-8579.9
-6539.
-5.181
3.649
26
232.0
2429.
.08363
433.41
3.0
3128.3
-8546.5
-7155.
-5.201
3.658
25000
230.4
2817.
.09290
455.48
3.5
3258.1
-8455.6
-7807.
-5.226
3.670
24
229.1
3267.
.10320
478.10
4.0
3430.5
-8403.4
-8656.
-5.252
3.681
23
228.3
3794.
.1148
500.94
4.5
3524.0
-8267.0
-9337.
-5.270
3.689
22
227.7
4411.
.1278
524.64
5.0
3781.7
-8255.8
-10363.
-5.295
3.700
21
224.7
5130.
.1423
555.35
5.5
3986.1
-8155.0
-11295.
-5.323
3.713
20000
222.6
5975.
.1586
585.83
6.5
4229.2
-8107.5
-12366.
-5.344
3.723
19
221.8
6972.
.1770
614.77
7.0
4400.0
-79S6.7
-13643.
-5.375
3.737
18
220.9
8132.
.1974
645.31
7.2
4653.1
-7908.8
-14931.
-5.398
3.747
17
220.0
9500.
.2205
677.75
9.8
4832.6
-7711.4
-16248.
-5.417
3.755
16
218.9
11095.
.2463
712.38
15.2
5156.9
-7724.3
-17972.
-5.442
3.767
15000
218.2
12986.
.2754
747.92
17.2
5339.8
-7549.7
-19764.
-5.461
3.775
14
219.0
15183.
.3078
779.60
20.3
5559.4
-7428.8
-21817.
-5.482
3.784
13
218.5
17742.
.3439
817.34
22.9
5851.8
-7489.2
-24012.
-5.504
3.795
12
220.9
20731.
.3841
845.63
21.2
5998.7
-7424.6
-27704.
-5.514
3.799
11
226.5
24151.
.4282
861.92
18.9
6096.6
-7351.7
-31391.
-5.517
3.800
10000
233.0
28024.
.4760
874.46
17.9
6172.5
-7317.5
-35695.
-5.525
3.804
9
240.1
32376.
.5274
884.96
16.7
6246.0
-7285.2
-40495.
-5.523
3.803
8
247.5
37249.
.5827
893.96
16.0
6315.2
-7283.7
-46012.
-5.526
3.805
7
254.4
42679.
.6419
903.88
13.7
6391.6
-7237.1
-51620.
-5.532
3.807
6
260.8
48729.
.7054
916.86
11.8
6441.1
-7205.5
-58156.
-5.535
3.808
5000
270.0
55421.
.7730
919.18
10.1
6472.7
-7193.2
-65570.
-5.534
3.808
4
278.4
62779.
.8446
924.12
9.0
6522.4
-7164.9
-73187.
-5.531
3.806
3
285.1
70873.
.9207
934.58
8.0
3337.9
-3589.0
-78707.
-5.538
3.810
2500
284.8
75278.
.9611
952.03
7.6
3369.9
-3532.6
-81358.
-5.547
3.814
2000
284.4
79932.
1.0029
970.04
7.3
3427.9
-3522.1
-84746.
-5.548
3.815
1500
286.1
84868.
1.0465
981.12
6.5
3457.6
-3505.6
-88614.
-5.554
3.817
1000
288.8
90064.
1.0917
988.78
5.6
3437.4
-3453.2
-92283.
-5.555
3.818
500
292.6
95508.
1.1385
992.66
5.3
754.8
- 756.9
-96298.
-5.556
3.818
392
293.4
96723.
1.1485
993.58
5.0
-5.557
3.819
366 EXTENSION OF THERMODYNAMIC COMPUTATIONS FIRST DISTRIBUTION OF TEMPERATURE