Definition:Submagma
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Definition
If:
then $\left({T, \circ}\right)$ is a submagma of $\left({S, \circ}\right)$, and we can write:
- $\left({T, \circ}\right) \subseteq \left({S, \circ}\right)$
If $\left({S, \circ}\right)$ is a magma and $\left({T, \circ}\right) \subseteq \left({S, \circ}\right)$, then we can say that:
- $\left({T, \circ}\right)$ is contained in $\left({S, \circ}\right)$ algebraically
- $\left({S, \circ}\right)$ algebraically contains $\left({T, \circ}\right)$
- $\left({S, \circ}\right)$ is an extension of $\left({T, \circ}\right)$
- $\left({T, \circ}\right)$ is embedded in $\left({S, \circ}\right)$
- $\left({T, \circ}\right)$ is closed (or stable) in $\left({S, \circ}\right)$.
Induced Operation
Let $\left({S, \circ}\right)$ be a magma.
Let $\left({T, \circ}\right) \subseteq \left({S, \circ}\right)$.
That is, let $T$ be a subset of $S$ such that $\circ$ is closed in $T$.
Then the restriction of $\circ$ to $T$, namely $\circ \restriction_T$, is called the (binary) operation induced on $T$ by $\circ$.
Examples
If $\left({S, \circ}\right)$ is a magma, then $\left({S, \circ}\right)$ is always a submagma of $\left({S, \circ}\right)$. That is, all magmas are submagmas of themselves.
If $\left({S, \circ}\right)$ is a magma, then $\left({\varnothing, \circ}\right)$ is always a submagma of $\left({S, \circ}\right)$. That is, the empty set is always a submagma of any magma:
| \(\displaystyle \) | \(\displaystyle \) | \(\displaystyle \) | \(\displaystyle \neg \ \exists x, y\) | \(\in\) | \(\displaystyle \varnothing\) | \(\displaystyle \) | \(\displaystyle \) | \(\displaystyle \) | |||
| \(\displaystyle \) | \(\displaystyle \implies\) | \(\displaystyle \) | \(\displaystyle \neg \ \exists x, y\) | \(\in\) | \(\displaystyle \varnothing:\) | \(\displaystyle \) | \(\displaystyle x \circ y \notin \varnothing\) | \(\displaystyle \) | |||
| \(\displaystyle \) | \(\displaystyle \implies\) | \(\displaystyle \) | \(\displaystyle \forall x, y\) | \(\in\) | \(\displaystyle \varnothing:\) | \(\displaystyle \) | \(\displaystyle x \circ y \in \varnothing\) | \(\displaystyle \) |
Subset which is not a submagma
Note the following.
Suppose $\left({S, \circ}\right)$ is a magma.
Suppose $T \subseteq S$.
Suppose $\exists s, t \in T: s \circ t \notin T$, although of course $s \circ t \in S$.
Then $\left({T, \circ}\right)$ is not closed, and it is not true to write $\left({T, \circ}\right) \subseteq \left({S, \circ}\right)$.
This is because $\left({T, \circ}\right)$ is not actually a magma itself, through dint of it not being closed.
Also known as
An older term for this concept is subgroupoid (or sub-gruppoid), from groupoid.
A groupoid is now often understood to be a concept in category theory.
Also see
Sources
- J.A. Green: Sets and Groups (1965)... (previous)... (next): $\S 5.1$
- Seth Warner: Modern Algebra (1965)... (previous)... (next): $\S 8$