Why does ordinary water have a triple point?
Summarizing the relevant point (pun intended) of my answer to a related post: a mixture does not exhibit a &quot;triple line&quot; if its composition is constant. It is only a &quot;triple line&quot; insofar as you get to vary the proportion (mole fractions) of the components. Therefore different samples of water with different isotopic composition will differ in the value of the TP, but for a given sample the TP is just that, a single constant point (not a line).
This question however does point out a very important problem for the implementation of the standards adopted during establishment of an absolute temperature scale based on the triple point of water. A good discussion of this is provided in white papers (1,2) from Isotech (manufaturers of triple point measurement apparatuses):

There are 3 main sources of error in a water triple point cell[6,
7] (excluding errors associated with measurement):

The isotopic composition of the cell’s water may not be that of SMOW.

There may be air trapped inside the cell.

There will be impurities in the water.


Isotopic composition can be measured to great accuracy from a
small sample of the cell’s contents.

SMOW and V-SMOW are water samples of standard composition (this is amply discussed in Isotech white papers, referring also to the documentation behind the International Temperature Scale established in 1990 (ITS-90)):
\begin{array} {|r|r|}
\hline
\text{Component}  &amp;  \text{Mole Fraction} \\
\hline
\ce{^1H} &amp; 0.999 842 \\
\ce{^2H} (\text{deuterium}) &amp; 0.000 158 \\
\ce{^3H} (\text{tritium}) &amp; 0 \\
\ce{^{16}O}  &amp; 0.997 640 \\
\ce{^{17}O} &amp; 0.000 371 \\
\ce{^{18}O} &amp; 0.001 989 \\
\hline
\end{array}
A second white paper provides guidelines on consideration of these effects (see the section &quot;Isotopic Composition&quot;):

We think of water as $\ce{H2O}$, more precisely we should write $\ce{^1H2^{16}O}$. This has been termed ‘light’ water and is unobtainable. If it were obtainable it’s triple point would be approximately +0.008°C. In practice what we drink from the tap, and what is in the ocean is a soup of $\ce{^1H}$, $\ce{^2H}$ with $\ce{^{16}O}$, $\ce{^{17}O}$ and $\ce{^{18}O}$. This means real water does not have a single triple point temperature. Its ‘combination triple point’ will vary as the isotopic composition varies. This  was  understood  more  than  50  years  ago  and  after  much  analysis  of  water  from  different  sources recent temperature scales state that  the water in a triple point cell shall have the isotopic composition  of ocean water.  Although not explicitly stated, there is a Standard Mean Ocean Water (SMOW) and it is assumed that the isotopic content of SMOW fulfils the ITS-90 requirements.

concluding:

Analysing the cell contents for isotopic composition is a useful and valid addition to the usual techniques of intercomparing cells and gives an accurate indication of the cells ideal triple point value.
[...]
Such cells, complete with isotopic analysis provide the closest association to the ITS-90 value of the water triple point and hence the KTTS Scale. It is now possible to produce cells, based on Stimpson’s original design which can be associated to V-SMOW within ±3mK and this is a smaller uncertainty than can be provided by traditional measurements.

References

The Establishment  of  ITS-90 Water Triple Point References  to  ±2μK,  and  the Assessment of 100 Water Triple Point Cells Made Between 2001 and 2006, John P. Tavener and Nick Davies, Isothermal Technology Ltd. (England).

The Water Triple Point - A Reference Cell Close to the ITS-90 Value. John P. Tavener &amp; Anne Blundell. Northern Temperature Primary Laboratory, Pine Grove, Southport, Merseyside, PR9 9AG, England.

Supplementary Information for the International Temperature Scale of 1990, BIPM. ISBN 92-822-2111-3.