To double the insolation on Mars would require a mirror or array of mirrors with an area, projected onto a plan perpendicular to the Sun-Mars line, equal to that of Mars itself divided by the efficiency of the system. In principle, there appear to be three places where such a reflector could be: the first or second Lagrange point or a Sun synchronous polar orbit. In all three cases, the projection of the mirror system on the plane perpendicular to the Sun-Mars line would be an annulus with an ID slightly larger than Mars, say 8,000 km, and an OD of about 11,000 km, depending on the system's efficiency. As discussed below, only one of these is potentially feasible.
Here is a list of some relevant data:
Mean Sun-Mars distance = 2.28E8 km;
Sun's diameter = 1.39E6 km;
Mars' diameter = 6779 km;
Sun's mass = 1.99E30 kg;
Mars' mass = 6.42E23 kg;
Mars L1/2 = 1.19E6 km;
Angular Subtense of Mars from L1/2 = 2 * arctan ([Mars diam/2]/Mars L1/L2 dist) = 0.326 degrees;
Angular Subtense of Sun from Mars = 2 * arctan([Sun diam/2]/mean Sun-Mars dist) = 0.349 degrees.
(All data from Wikipedia or similar on the web, except Mars L1/2 from
the equation at bottom left of Figure 2 where R = Sun-Mars distance,
M2 = Mars' Mass, and M1 = Sun's mass -- equation derived at Ref 1).
One of the few Earthling friendly features of Mars is its day-night cycle which is very close to that of Earth. If the mirror system were placed at L2, illuminating the "dark" side of Mars, it would eliminate the day-night cycle. If it were in a dusk/dawn Sun synchronous polar orbit, the terminator would be brightly illuminated by a band of light about 1500 km wide. The only position that would retain the normal day-night cycle would be L1.
At L1, a cylindrical mirror system seems reasonable until you look at the angles involved. The radius at the middle of the annulus would be approximately 4750 km, so the angle from the Sun would be arctan(4750 km/[2.28E8 km-1.19E6 km]) = 0.0012 degrees. The angle from the middle of the annulus to Mars would be arctan(4750 km/1.19E6) =- 0.229 degrees. The sum of the angles is 0.230 degrees, so the tilt of the mirror surface at the midpoint position of the annulus would be 0.115 degrees. The mirror surface would be a section of a parabola that focuses flux from the Sun onto Mars. For the 0.115 degrees angle, it follows the equation y = 0.05274x^2 for x ranging from ±4000 km to ±5500 km. For this range, the total depth in y is 0.75E6 km (!), so an array of mirrors along this surface would not be practical. Alternatively, you could collapse the parabolic surface onto an array of mirrors on a common plane as a reflective analog to a Fresnel lens. As an example, an array of 1 meter square mirrors would be seen from the Sun as nearly end on. As the tangent of 0.115 degrees is 0.002, each 1 meter mirror would collect solar flux over a 1 meter by 2 millimeter area, so would need to be spaced 2 mm apart. Given that the actual mirrors would have a finite thickness likely greater that 2 millimeters, this doesn't work.
The concept for a Sun synchronous polar orbital mirror is shown in Figure 1 below. For simplicity, the sketch ignores the tilt of Mars' axis and the fact that, for the orbit to precess precisely 360 degrees per year, it doesn't go exactly through the poles (Ref 2). The surface of the mirror would be a slice of a 90 degree circular cone. Unfortunately, since the entire mirror could not be magically constructed all at once, it fails because any individual part of it would be unstable. For example, the section shown at the top of the sketch would immediately start rotating clockwise around it's center of mass. It would oscillate back and forth between tilting forward and backward, with the angle damping over time until it became tidally locked in the vertical position. See Ref 3 or any good explanation of tide locking or gravity gradient stabilization.
For L2, a slightly concave mirror could be used in a circular halo orbit around L2. If the mirror were collapsed onto a common plane, the concavity is so small that dividing the annulus into five sub-annuli, each with a slightly different tilt would be sufficient. This is shown in Figure 2. The minimum tilt is 0.100 degrees and the maximum is 0.129 degrees. Because of the finite angular subtense of the Sun as seen from Mars, the reflection from any point on the mirror system diverges by about ± 0.175 degrees or 0.349 degrees total. Since the angular subtense of Mars as seen from L2 is 0.326 degrees, the disk of illumination is slightly larger than Mars, causing an additional efficiency loss of approximately 11%.
For such a large structure, it must be possible to start with a sparse array of mirrors, filling in the rest over time. Initially, there would be a few unconnected islands, all orbiting at the same radius from L2. With GPS satellites around Mars, each island could use station keeping to keep at the proper radius and keep from running into each other. As one ring becomes full, all the islands at that radius could be connected and a new sparse ring could begin, etc. The biggest risk (which I can't evaluate) is, due to the million km plus lever arm, the plane of the orbit needs to remain perpendicular to the Mars-L2 line to a few arc minutes so that all of the back side of Mars remains illuminated. Also, the station keeping required for a circular halo orbit would be significant, compared to almost none for a Lissajous orbit, but probably not prohibitively so. Maybe an orbital mechanics SME could comment on this.
Radiation pressure from the Sun will produce a small, but finite, outward push on the mirror system. Although this could be compensated by additional station keeping or a slight change in the distance of the mirror from Mars, it would be useful to calculate the magnitude of this effect. At Earth (at 1.0 AU), the pressure is 4.53E-6 newtons/square meter, or 4.61E-7 kilograms force/square meter (Ref. 4). At Mars (at 1.38 AU) the value decreases to 2.42E-7 kgf/m^2. This is for absorbed radiation. The value would be doubled for a perfect reflector. For a more realistic reflection of, say, 92%, the force would be 1.92 * 2.42E-7 kgf/m^2 = 4.65E-7 kgf/m^2. Lets assume for simplicity that the areal mass density of the mirror system is 1.0 kg/m^2.
By definition, L2 is a position where the gravitational pull of Mars is just enough so that an object there can orbit the Sun at exactly the same angular velocity as Mars itself. We can calculate this pull from the gravitational force at Mars' surface and the ratio of the squared values of its mean radius and that of the L2 distance. The gravity at Mars' surface is 3.711 m/s^2, or 0.378 g, where g = 1.0 Earth gravity. The ratio of the squares of Mars mean radius and L2 is 8.11E-6. So the gravitational pull on an object at L2 from Mars is 8.11E-6 * 0.378 g = 3.066E-6 g which exerts a force on a 1.0 kg mass of 3.066E-6 kgf. So, for this case, every square meter of the mirror system is pulled toward Mars by a force of 3.066E-6 kgf (due to Mars' gravity) and pushed away from Mars by a force of 4.65E-7 kgf (due to radiation pressure from the Sun). To compensate for the radiation pressure, the mirror system must be moved slightly toward Mars. At L2, Mars exerts a gravitational force of 3.066E-6 kgf. To compensate for the radiation pressure, this must be increased by 4.65E-7 kgf to 3.066E-6 + 4.65E-7 = 3.113E-6 kgf. Solving for the adjusted distance D in the equation:
[(3,390 km)^2/D^2)] * 0.378 g) = 3.116E-6 g, which simplifies to
D = SQRT{[(3,390 km)^2 * 0.378 g]/3.116E-6} gives 1.181E6 km, or a shift toward Mars of about 9,300 km. Of course, a mirror system with a lower areal density or a higher reflectance would require a larger shift and visa versa.
Ref. 1: Derivation of approximate L1 calculation.
Ref. 2: Sun synchronous polar orbit.
https://en.wikipedia.org/wiki/Sun-synchronous_orbit
Ref. 3: Tidal forces on an orbiting bar.
https://en.wikipedia.org/wiki/Tidal_force
or
https://ocw.mit.edu/courses/earth-atmospheric-and-planetary-sciences/12-808-introduction-to-observational-physical-oceanography-fall-2004/lecture-notes/course_notes_15n.pdf
Ref. 4: https://www.grc.nasa.gov/WWW/K-12/Numbers/Math/Mathematical_Thinking/sunlight_exerts_pressure.htm