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In [[13-limit]] [[just intonation]], '''13/10''', the '''tridecimal semisixth''' is an [[interseptimal]] interval measuring about 454.2 [[cent]]s. It falls in an ambiguous zone between a wide major third such as [[9/7]] and a flat perfect fourth such as [[21/16]]. The descriptor "interseptimal" comes from [[Margo Schulter]], and indicates its position between those two septimal (7-based) extremes. | |||
In [[ | In many notation systems based on the [[5L 2s|diatonic]] [[chain-of-fifths notation]] with commatic alterations (e.g. [[FJS]], [[HEJI]]), 13/10 is a fourth, as it is a [[4/3|perfect fourth (4/3)]] minus an instance of [[40/39]], which is a [[2187/2048|Pythagorean apotome]] minus a stack consisting of an [[81/80|syntonic comma (81/80)]] and a [[1053/1024|tridecimal quartertone (1053/1024)]], none of which changes the [[scale|scale degree]]. It functions as such in the harmonic thirteenth chord, [[4:5:6:7:9:11:13]]. | ||
However, 13/10 also appears in the relatively simple [[10:13:15]] triad, which consists of 13/10 and [[15/13]] that stack to make a [[3/2]] perfect fifth. This makes 13/10 function as an ultramajor third (if the chord is not taken as a suspension). It is well-approximated in [[16edo]], [[21edo]], [[24edo]], [[29edo]], [[37edo]], and of course, infinitely many other [[edo]] systems. | |||
== Interval chain == | |||
Because 13/10 is an interseptimal interval, stacking it four times will result in a good approximation of a septimal interval. In this case, (13/10)<sup>4</sup> approximates 20/7 (compound [[10/7]]) remarkably well, with less than 1{{cent}} error. | |||
Additionally, while it may seem as though (13/10)<sup>2</sup> does not approximate 17/10 very well at first glance, it allows for an elegant interpretation of the tetrad formed by stacking 13/10 three times on top of itself: [[~]]10:13:17:22. | |||
{| class="wikitable" | |||
|+ [[Interval chain]] generated by 13/10 | |||
! # | |||
! [[Cent]]s | |||
! Approximated [[ratio]]s | |||
! Associated [[comma]]s | |||
|- | |||
| 1 | |||
| 454.2 | |||
| 13/10<br>[[17/13]] (+10.2{{cent}}) | |||
| <br>[[170/169]] (major naiadma) | |||
|- | |||
| 2 | |||
| 908.4 | |||
| [[27/16]] (-2.6{{cent}})<br>[[22/13]] (+2.4{{cent}})<br>[[17/10]] (+10.2{{cent}}) | |||
| [[676/675]] (island comma)<br>[[2200/2197]] (petrma)<br>[[170/169]] (major naiadma) | |||
|- | |||
| 3 | |||
| 1362.6 | |||
| [[11/5]] (+2.4{{cent}}) | |||
| [[2200/2197]] (petrma) | |||
|- | |||
| 4 | |||
| 1816.9 | |||
| [[20/7]] (+0.6{{cent}}) | |||
| [[200000/199927]] | |||
|- | |||
| 5 | |||
| 2271.1 | |||
| [[26/7]] (+0.6{{cent}}) | |||
| [[200000/199927]] | |||
|} | |||
== Approximation == | |||
{{Interval edo approximation|13/10}} | |||
== See also == | == See also == | ||
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[[Category:Third]] | [[Category:Third]] | ||
[[Category:Supermajor third]] | [[Category:Supermajor third]] | ||
[[Category:Over-5]] | [[Category:Over-5 intervals]] | ||