1. Introduction
A porism is a theorem about a closure property of a geometric figure or construction, as explained in [
1] (pp. 412–417). A well-known example comes from the elementary triangle geometry. Any triangle in the Euclidean plane has a circumcircle
u and incircle
i. It turns out that there are infinitely many triangles with the same circumcircle
u and incircle
i. In other words, if we pick a point
on
u and draw a tangent
from
to
i, then
intersects
u in points
and
. Now, we draw a tangent
from
to
i that intersects
u in
and
. Finally, we draw a tangent
from
to
i that intersects
u in
and
. It turns out that
. The one-parameter family of triangles with a common incircle and a common circumcircle is usually called a porisitic system of triangles. In the Euclidean plane, the poristic family of triangles interscribed in between the incircle and the circumcircle is called Chapple’s porism. The fact that such families exist even in some non-Euclidean planes is due to the projective nature of the problem. Hence, it is not necessary to prove the existence of a closed triangular path between two isotropic circles (Euclidean parabolas with parallel axes). Nevertheless, in
Section 3.1, in order to obtain a parametrization of the poristic family, we offer the proof that the described property is also valid in an isotropic plane.
In [
2], the author showed that many triangle centers move on circles while the triangle traces the poristic family. Some centers move on conics, and some centers move on curves of a higher degree. In this paper, in
Section 3.2, we study the loci of some triangle centers in the isotropic plane. A further investigation of the loci of triangle centers in the Euclidean plane is given in [
3], where the authors studied a poristic family defined by two confocal ellipses.
In
Section 3.3, we study the traces of the vertices of the contact triangle, tangential triangle and anticomplementary triangle associated with the triangle of the poristic family in the isotropic plane.
2. Methods
An isotropic plane is a projective plane with a distinct line f and a distinct point . Lines incident with the absolute point F are called isotropic lines, and points incident with the absolute line f are called isotropic points. Two lines are said to be parallel if their intersection point is an isotropic point, while two points are said to be parallel if they are joined by an isotropic line.
The basic facts about the isotropic plane can be found in [
4]. Here, we highlight the ones that are important for our study.
The standard affine model of the isotropic plane, where the coordinates of points are given by and , is obtained by setting and . In this model, the isotropic lines have equations of the form with . The isotropic distance of a pair of two non-parallel points and is defined by , while two non-parallel lines p and q, given by the equations and , respectively, form the isotropic angle defined by . The midpoint of points P and Q is defined in a natural way as the point with coordinates , while the bisector of lines p and q is the line with the equation .
According to their position with respect to the absolute figure, conics are ellipses, hyperbolas, special hyperbolas, parabolas and circles, as explained in [
4]. The most interesting conics for us are circles, conics that touch
f at
F.Therefore, a circle has an equation of the form
with
.
A curve in the isotropic plane is said to be circular if it passes through the absolute point
F. If the curve intersects
f only at
F, then it is entirely circular, as explained in [
5]. Thus, circles are entirely circular conics.
It was shown in [
6] that any allowable triangle
(triangle whose sides are non-isotropic lines) in the isotropic plane can be set in the so-called standard position by choosing an appropriate affine coordinate system and having the circumcircle
u with the equation
and vertices
with
.
Let
,
and
be elementary symmetric functions in three variables
a,
b and
c; in other words, let
The centroid, the symmedian point, the Gergonne point, the Feuerbach point and the Steiner point of the triangle
are labeled
,
,
,
and
, respectively, according to Kimberling’s encyclopedia [
7].
The coordinates of the centroid
of the triangle
are
It was shown in [
8] that the incircle
i
and the Euler circle
touch each other externally at the Feuerbach point
The symmedians are the reflections of medians in the bisectors. According to [
9], they intersect at the symmedian point
of the triangle
having the coordinates
The Gergonne point
of the triangle
is the intersection point of three lines
,
and
, where
,
and
are the contact points of the triangle and its incircle
i. In [
10], the coordinates of the Gergonne point
of the standard triangle
were determined as follows:
The Steiner point
of the triangle
is defined as the fourth (in addition to
A,
B and
C) common point
of the circumscribed circle
u and circumscribed Steiner ellipse of that triangle, as explained in [
11]. In the case of the standard triangle
, this point has the coordinate vector
For every triangle in the isotropic plane, there is the first and the second Brocard point, and they are unique. The first Brocard point is defined as the point such that its connections with the vertices
A,
B and
C form equal angles with the sides
,
and
, respectively. Analogously, the second Brocard point is defined as the point such that its connection lines with the vertices
A,
B and
C form equal angles with the sides
,
and
, respectively. According to [
12], the Brocard points
and
of the standard triangle are given by
where
In
Section 3.2, we will show that in the isotropic plane, all triangles in a poristic system share the centroid and the Feuerbach point. The symmedian point and the Gergonne point of all triangles move on straight lines. The Steiner point traces a circle, while Brocard points trace a quartic curve.
4. Discussion
Any triangle in the isotropic plane has a circumcircle u and incircle i. We showed that there are infinitely many triangles with the same circumcircle u and incircle i. We also proved that all triangles in a poristic system share a centroid and Feuerbach point. The symmedian point and the Gergonne point trace straight lines, the Steiner point traces a circle, and the Brocard points trace a quartic curve.
To make this study simpler, we put the initial triangle in the so-called standard position by choosing its vertices to be , and , with . Assuming that , we would obtain the same results, but the calculations would be much more complicated, and the formulas and equations would be much longer.