159edo/Interval names and harmonies: Difference between revisions
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Line 138: | Line 138: | ||
| 160/153 | | 160/153 | ||
| Rkm2, rKuA1 | | Rkm2, rKuA1 | ||
| Wide Subminor Second, | | Wide Subminor Second, Lesser Sub-Augmented Prime | ||
| Eb↓/, Dt<↑ | | Eb↓/, Dt<↑ | ||
| This interval acts as a type of semitone, however, whether it's a diatonic or chromatic semitone depends on the situation. | | This interval acts as a type of semitone, however, whether it's a diatonic or chromatic semitone depends on the situation. | ||
Line 150: | Line 150: | ||
| ? | | ? | ||
| rm2, KuA1 | | rm2, KuA1 | ||
| Narrow Minor Second, | | Narrow Minor Second, Greater Sub-Augmented Prime | ||
| Eb\, Dt>↑ | | Eb\, Dt>↑ | ||
| Not only does this interval serve as a type of leading tone, but it should be noted that six of these add up to a Perfect Fourth. | | Not only does this interval serve as a type of leading tone, but it should be noted that six of these add up to a Perfect Fourth. | ||
Line 174: | Line 174: | ||
| [[18/17]] | | [[18/17]] | ||
| Rm2, RkA1 | | Rm2, RkA1 | ||
| Artomean Minor Second, | | Artomean Minor Second, Artomean Augmented Prime | ||
| | | | ||
| | | | ||
Line 186: | Line 186: | ||
| '''[[17/16]]''' | | '''[[17/16]]''' | ||
| rKm2, rA1 | | rKm2, rA1 | ||
| Tendomean Minor Second, | | Tendomean Minor Second, Tendomean Augmented Prime | ||
| | | | ||
| | | |
Revision as of 15:51, 11 January 2022
159edo contains all the intervals of 53edo, however, as some of the interpretations differ due 159edo having different mappings for certain primes, those differences show up in how harmonies are constructed. It should be noted that since 159edo does a better job of representing the 2.3.11 subgroup than 24edo, some of the chords listed on the page for 24edo interval names and harmonies carry over to this page, even though the exact sets of enharmonics differ between the two systems.
Step | Cents | 5 limit | 7 limit | 11 limit | 13 limit | 17 limit | Interval Names | Notes | ||
---|---|---|---|---|---|---|---|---|---|---|
0 | 0 | 1/1 | P1 | Perfect Unison | D | The root of any chord. | ||||
1 | 7.5471698 | 225/224 | 243/242 | 196/195, 351/350 | 256/255 | R1 | Wide Prime | D/ | Useful for slight dissonances that convey something less than satisfactory, however it can also add to the bandwidth of a sound. | |
2 | 15.0943396 | ? | 121/120, 100/99 | 144/143 | 120/119 | rK1 | Narrow Superprime | D↑\ | Useful for slight dissonances that create more noticeable tension. | |
3 | 22.6415094 | 81/80 | ? | ? | 78/77 | 85/84 | K1 | Lesser Superprime | D↑ | Useful for appoggiaturas, and acciaccaturas, and quick passing tones. |
4 | 30.1886792 | 64/63 | 56/55, 55/54 | ? | 52/51 | S1, kU1 | Greater Superprime, Narrow Inframinor Second | Dt<↓ | Useful for various types of subchromatic gestures, as well as for appoggiaturas, and acciaccaturas, and quick passing tones. | |
5 | 37.7358491 | ? | 45/44 | ? | 51/50 | um2, RkU1 | Inframinor Second, Wide Superprime | Edb>, Dt>↓ | By default, this interval is a type of paradiatonic quartertone and is used in much the same way as 24edo's own Inframinor Second. | |
6 | 45.2830189 | ? | ? | ? | 40/39 | 192/187 | kkm2, Rum2, rU1 | Wide Inframinor Second, Narrow Ultraprime, Semilimma | Eb↓↓, Dt<\ | This interval is particularly likely to be used as a cross between an Ultraprime and an Inframinor Second. |
7 | 52.8301887 | ? | 33/32 | ? | 34/33 | U1, rKum2 | Ultraprime, Narrow Subminor Second | Dt< | By default, this interval is a type of parachromatic quartertone and is thus used in much the same way as 24edo's own Ultraprime. | |
8 | 60.3773585 | 28/27 | ? | ? | 88/85 | sm2, Kum2, uA1 | Lesser Subminor Second, Wide Ultraprime, Infra-Augmented Prime | Eb↓\, Dt> | Although this interval can act as a leading tone, it can also act as a trienstone- that is, a third of a tone- since it's one third of the Ptolemaic Major Second. | |
9 | 67.9245283 | 25/24 | ? | ? | 26/25, 27/26 | ? | km2, kkA1 | Greater Subminor Second, Diptolemaic Augmented Prime | Eb↓, D#↓↓ | Although this interval frequently acts as the Diptolemaic Chroma, it can also act as a trienstone- that is, a third of a tone- since it's one third of the Pyth Major Second. |
10 | 75.4716981 | ? | ? | ? | 160/153 | Rkm2, rKuA1 | Wide Subminor Second, Lesser Sub-Augmented Prime | Eb↓/, Dt<↑ | This interval acts as a type of semitone, however, whether it's a diatonic or chromatic semitone depends on the situation. | |
11 | 83.0188679 | 21/20 | 22/21 | ? | ? | rm2, KuA1 | Narrow Minor Second, Greater Sub-Augmented Prime | Eb\, Dt>↑ | Not only does this interval serve as a type of leading tone, but it should be noted that six of these add up to a Perfect Fourth. | |
12 | 90.5660377 | 256/243, 135/128 | ? | ? | ? | ? | m2, kA1 | Pythagorean Minor Second, Ptolemaic Augmented Prime | Eb, D#↓ | As the approximation of both the Pythagorean Minor Second and the Ptolemaic Augmented Prime, this interval is used accordingly. |
13 | 98.1132075 | ? | 128/121 | 55/52 | 18/17 | Rm2, RkA1 | Artomean Minor Second, Artomean Augmented Prime | |||
14 | 105.6603774 | ? | ? | ? | 17/16 | rKm2, rA1 | Tendomean Minor Second, Tendomean Augmented Prime | |||
15 | 113.2075472 | 16/15 | ? | ? | ? | ? | Km2, A1 | Ptolemaic Minor Second, Pythagorean Augmented Prime | ||
16 | 120.7547170 | 15/14 | 275/256 | ? | ? | |||||
17 | 128.3018868 | ? | ? | 14/13 | 128/119 | |||||
18 | 135.8490566 | 27/25 | ? | ? | 13/12 | ? | ||||
19 | 143.3962264 | ? | 88/81 | ? | ? | |||||
20 | 150.9433962 | ? | 12/11 | ? | ? | |||||
21 | 158.4905660 | ? | ? | ? | 128/117 | 561/512, 1024/935 | ||||
22 | 166.0377358 | ? | 11/10 | ? | ? | |||||
23 | 173.5849057 | 567/512 | 243/220 | ? | 425/384 | |||||
24 | 181.1320755 | 10/9 | ? | 256/231 | ? | ? | ||||
25 | 188.6792458 | ? | ? | 143/128 | 512/459 | |||||
26 | 196.2264151 | 28/25 | 121/108 | ? | ? | |||||
27 | 203.7735849 | 9/8 | ? | ? | ? | ? | ||||
28 | 211.3207547 | ? | ? | 44/39 | 289/256 | |||||
29 | 218.8679245 | ? | ? | ? | 17/15 | |||||
30 | 226.4150943 | 256/225 | ? | 154/135 | ? | ? | ||||
31 | 233.9622642 | 8/7 | 55/48 | ? | ? | |||||
32 | 241.5094340 | ? | 1024/891 | ? | ? | |||||
33 | 249.0566038 | ? | ? | ? | 15/13 | ? | ||||
34 | 256.6037736 | ? | 297/256 | ? | ? | |||||
35 | 264.1509434 | 7/6 | 64/55 | ? | ? | |||||
36 | 271.6981132 | 75/64 | ? | ? | ? | ? | ||||
37 | 279.2452830 | ? | ? | ? | 20/17 | |||||
38 | 286.7924528 | ? | 33/28 | 13/11 | 85/72 | |||||
39 | 294.3396226 | 32/27 | ? | ? | ? | ? | ||||
40 | 301.8867925 | 25/21 | 144/121 | ? | ? | |||||
41 | 309.4339622 | ? | ? | 512/429 | 153/128 | |||||
42 | 316.9811321 | 6/5 | ? | 77/64 | ? | ? | ||||
43 | 324.5283019 | 135/112 | ? | ? | 512/425 | |||||
44 | 332.0754717 | ? | 40/33, 121/100 | ? | 144/119, 165/136 | |||||
45 | 339.6226415 | ? | ? | ? | 39/32 | 17/14 | ||||
46 | 347.1698113 | ? | 11/9 | ? | ? | |||||
47 | 354.7169811 | ? | 27/22 | ? | ? | |||||
48 | 362.2641509 | ? | ? | ? | 16/13 | 21/17 | ||||
49 | 369.8113208 | ? | ? | ? | 68/55 | |||||
50 | 377.3584906 | 56/45 | 1024/825 | ? | ? | |||||
51 | 384.9056604 | 5/4 | ? | 96/77 | ? | ? | ||||
52 | 392.4528302 | ? | ? | ? | 64/51 | |||||
53 | 400 | 63/50 | 121/96 | ? | ? | |||||
54 | 407.5471698 | 81/64 | ? | ? | ? | ? | ||||
55 | 415.0943396 | ? | 14/11 | 33/26 | 108/85 | |||||
56 | 422.6415094 | ? | ? | 143/112 | 51/40 | |||||
57 | 430.1886792 | 32/25 | ? | ? | ? | ? | ||||
58 | 437.7358491 | 9/7 | 165/128 | ? | ? | |||||
59 | 445.2830189 | ? | 128/99 | ? | 22/17 | |||||
60 | 452.8301887 | ? | ? | ? | 13/10 | ? | ||||
61 | 460.3773585 | ? | 176/135 | ? | ? | |||||
62 | 467.9245283 | 21/16 | 55/42, 72/55 | ? | 17/13 | |||||
63 | 475.4716981 | 320/243, 675/512 | ? | ? | ? | ? | ||||
64 | 483.0188679 | ? | 33/25 | ? | 45/34 | |||||
65 | 490.5660377 | ? | ? | ? | 85/64 | |||||
66 | 498.1132075 | 4/3 | ? | ? | ? | ? | ||||
67 | 505.6603774 | 75/56 | 162/121 | ? | ? | |||||
68 | 513.2075472 | ? | 121/90 | ? | ? | |||||
69 | 520.7547170 | 27/20 | ? | ? | 104/77 | ? | ||||
70 | 528.3018868 | ? | 110/81 | ? | ? | |||||
71 | 535.8490566 | ? | 15/11 | ? | ? | |||||
72 | 543.3962264 | ? | ? | ? | 160/117 | 256/187 | ||||
73 | 550.9433962 | ? | 11/8 | ? | ? | |||||
74 | 558.4905660 | 112/81 | ? | ? | ? | |||||
75 | 566.0377358 | 25/18 | ? | ? | 18/13 | ? | ||||
76 | 573.5849057 | ? | ? | ? | 357/256 | |||||
77 | 581.1320755 | 7/5 | ? | ? | ? | |||||
78 | 588.6792458 | 1024/729, 45/32 | ? | ? | ? | ? | ||||
79 | 596.2264151 | ? | ? | ? | 24/17 | |||||
80 | 603.7735849 | ? | ? | ? | 17/12 | |||||
81 | 611.3207547 | 729/512, 64/45 | ? | ? | ? | ? | ||||
82 | 618.8679245 | 10/7 | ? | ? | ? | |||||
83 | 626.4150943 | ? | ? | ? | 512/357 | |||||
84 | 633.9622642 | 36/25 | ? | ? | 13/9 | ? | ||||
85 | 641.5094340 | 81/56 | ? | ? | ? | |||||
86 | 649.0566038 | ? | 16/11 | ? | ? | |||||
87 | 656.6037736 | ? | ? | ? | 117/80 | 187/128 | ||||
88 | 664.1509434 | ? | 22/15 | ? | ? | |||||
89 | 671.6981132 | ? | 81/55 | ? | ? | |||||
90 | 679.2452830 | 40/27 | ? | ? | 77/52 | ? | ||||
91 | 686.7924528 | ? | 180/121 | ? | ? | |||||
92 | 694.3396226 | 112/75 | 121/81 | ? | ? | |||||
93 | 701.8867925 | 3/2 | ? | ? | ? | ? | ||||
94 | 709.4339622 | ? | ? | ? | 128/85 | |||||
95 | 716.9811321 | ? | 50/33 | ? | 68/45 | |||||
96 | 724.5283019 | 243/160, 1024/675 | ? | ? | ? | ? | ||||
97 | 732.0754717 | 32/21 | 84/55, 55/36 | ? | 26/17 | |||||
98 | 739.6226415 | ? | 135/88 | ? | ? | |||||
99 | 747.1698113 | ? | ? | ? | 20/13 | ? | ||||
100 | 754.7169811 | ? | 99/64 | ? | 17/11 | |||||
101 | 762.2641509 | 14/9 | 256/165 | ? | ? | |||||
102 | 769.8113208 | 25/16 | ? | ? | ? | ? | ||||
103 | 777.3584906 | ? | ? | 224/143 | 80/51 | |||||
104 | 784.9056604 | ? | 11/7 | 52/33 | 85/54 | |||||
105 | 792.4528302 | 128/81 | ? | ? | ? | ? | ||||
106 | 800 | 100/63 | 192/121 | ? | ? | |||||
107 | 807.5471698 | ? | ? | ? | 51/32 | |||||
108 | 815.0943396 | 8/5 | ? | 77/48 | ? | ? | ||||
109 | 822.6415094 | 45/28 | 825/512 | ? | ? | |||||
110 | 830.1886792 | ? | ? | ? | 55/34 | |||||
111 | 837.7358491 | ? | ? | ? | 13/8 | 34/21 | ||||
112 | 845.2830189 | ? | 44/27 | ? | ? | |||||
113 | 852.8301887 | ? | 18/11 | ? | ? | |||||
114 | 860.3773585 | ? | ? | ? | 64/39 | 28/17 | ||||
115 | 867.9245283 | ? | 33/20, 200/121 | ? | 119/72, 272/165 | |||||
116 | 875.4716981 | 224/135 | ? | ? | 425/256 | |||||
117 | 883.0188679 | 5/3 | ? | 128/77 | ? | ? | ||||
118 | 890.5660377 | ? | ? | 429/256 | 256/153 | |||||
119 | 898.1132075 | 42/25 | 121/72 | ? | ? | |||||
120 | 905.6603774 | 27/16 | ? | ? | ? | ? | ||||
121 | 913.2075472 | ? | 56/33 | 22/13 | 144/85 | |||||
122 | 920.7547170 | ? | ? | ? | 17/10 | |||||
123 | 928.3018868 | 128/75 | ? | ? | ? | ? | ||||
124 | 935.8490566 | 12/7 | 55/32 | ? | ? | |||||
125 | 943.3962264 | ? | 512/297 | ? | ? | |||||
126 | 950.9433962 | ? | ? | ? | 26/15 | ? | ||||
127 | 958.4905660 | ? | 891/512 | ? | ? | |||||
128 | 966.0377358 | 7/4 | 96/55 | ? | ? | |||||
129 | 973.5849057 | 225/128 | ? | 135/77 | ? | ? | ||||
130 | 981.1320755 | ? | ? | ? | 30/17 | |||||
131 | 988.6792458 | ? | ? | 39/22 | 512/289 | |||||
132 | 996.2264151 | 16/9 | ? | ? | ? | ? | ||||
133 | 1003.7735849 | 25/14 | 216/121 | ? | ? | |||||
134 | 1011.3207547 | ? | ? | 256/143 | 459/256 | |||||
135 | 1018.8679245 | 9/5 | ? | 231/128 | ? | ? | ||||
136 | 1026.4150943 | 1024/567 | 440/243 | ? | 768/425 | |||||
137 | 1033.9622642 | ? | 20/11 | ? | ? | |||||
138 | 1041.5094340 | ? | ? | ? | 117/64 | 1024/561, 935/512 | ||||
139 | 1049.0566038 | ? | 11/6 | ? | ? | |||||
140 | 1056.6037736 | ? | 81/44 | ? | ? | |||||
141 | 1064.1509434 | 50/27 | ? | ? | 24/13 | ? | ||||
142 | 1071.6981132 | ? | ? | 13/7 | 119/64 | |||||
143 | 1079.2452830 | 28/15 | 512/275 | ? | ? | |||||
144 | 1086.7924528 | 15/8 | ? | ? | ? | ? | ||||
145 | 1094.3396226 | ? | ? | ? | 32/17 | |||||
146 | 1101.8867925 | ? | 121/64 | 104/55 | 17/9 | |||||
147 | 1109.4339622 | 243/128, 256/135 | ? | ? | ? | ? | ||||
148 | 1116.9811321 | 40/21 | 21/11 | ? | ? | |||||
149 | 1124.5283019 | ? | ? | ? | 153/80 | |||||
150 | 1132.0754717 | 48/25 | ? | ? | 25/13, 52/27 | ? | ||||
151 | 1139.6226415 | 27/14 | ? | ? | 85/44 | |||||
152 | 1147.1698113 | ? | 64/33 | ? | 33/17 | |||||
153 | 1154.7169811 | ? | ? | ? | 39/20 | 187/96 | ||||
154 | 1162.2641509 | ? | 88/45 | ? | 100/51 | |||||
155 | 1169.8113208 | 63/32 | 55/28, 108/55 | ? | 51/26 | |||||
156 | 1177.3584906 | 160/81 | ? | ? | 77/39 | 168/85 | ||||
157 | 1184.9056604 | ? | 240/121, 99/50 | 143/72 | 119/60 | |||||
158 | 1192.4528302 | 448/225 | 484/243 | 195/98, 700/351 | 255/128 | |||||
159 | 1200 | 2/1 | P8 | Perfect Octave | D | Reduplication of the root. |