Size, shape, density Observations of stellar occultations from 2012 and 2014 show that Achlys is an elongated object. Under the assumption that Achlys is in
hydrostatic equilibrium (that is, its shape is controlled by its own gravity and rotation), its shape can be approximated by a rotationally distorted
Jacobi ellipsoid with dimensions of . With these dimensions, the equatorial diameter of Achlys is roughly twice as long as its polar diameter. This rotationally distorted shape has been seen in other large Kuiper belt objects, like and . The approximated dimensions of Achlys translate to an
area-equivalent diameter of , which is large enough that astronomers consider Achlys likely in hydrostatic equilibrium and therefore a
possible dwarf planet. Achlys is among the top 30 largest known TNOs. The mass and density of Achlys have not been measured, though the assumption of hydrostatic equilibrium with its ellipsoidal shape predicts that it should have a density in the range of , with the most likely value being . This density indicates Achlys has a mass of around .{{efn|name=mass|The mass of was calculated by Muñoz-Gutiérrez et al. (2019 & 2021) using Achlys's area-equivalent diameter of and predicted density of . Muñoz-Gutiérrez et al. give the mass in terms of
Earth masses (M🜨), which can be converted into
kilograms by multiplying by /M🜨. This calculation does not treat Achlys as an ellipsoid (which would have a volume of V = \frac{4}{3} \pi a b c \approx 1.85 \times 10^{17} \text{ m}^{3}), though the mass calculated from Achlys's ellipsoid volume and density (M = \rho V \approx 1.61 \times 10^{20} \text{ kg}) is equivalent to Muñoz-Gutiérrez et al.'s mass calculation when rounded to a single digit.}} Achlys falls within the diameter range where TNOs are typically observed with densities lower than that of water ice (); these objects are theorized to have
porous interior structures due to a lack of internal melting,
differentiation, and gravitational compression. Achlys's small size also makes it unlikely to hold much internal heat or possess
cryovolcanism.
Rotation Achlys has a
rotation period of about 6.79 hours. The apparent brightness of Achlys periodically fluctuates with a small peak-to-peak
amplitude of 0.07
magnitudes as it rotates, which could be monitored by telescopes on Earth. The rotation period of Achlys was first measured by
Scott Sheppard and
David C. Jewitt in 2003, who found a rotation period of either 6.7 and 13.4 hours. The rotation period of Achlys remained ambiguous until 2017, when it was found to have an elongated shape that was best explained by the former period. Achlys has a highly
tilted rotation axis that is pointed somewhat toward Earth, according to observations of Achlys's small rotational brightness variation, constant thermal emission, and variable
projected shape in stellar occultations. A 2017 analysis of stellar occultation observations from 2012 and 2014 suggested that Achlys's rotational pole could be oriented at an opening angle of roughly with respect to the plane of the sky and at a
position angle of eastward from the
celestial north pole.
Surface spectrum of Achlys as measured by the
James Webb Space Telescope. The spectrum of Achlys shows
absorption features caused by crystalline water ice on its surface.|alt=The near-infrared spectrum of Achlys, which plots its relative brightness over wavelength of light, shows absorption features caused by crystalline water ice on its surface. Achlys is a dark, icy object with a likely ancient surface devoid of geological activity. Its surface is dominated by water
ice and has a low, average
geometric albedo of about 10%.
Astronomical spectroscopy has shown that both
amorphous and crystalline forms of water ice are present on Achlys's surface, which make it highly
absorbent in
near-infrared wavelengths of light. Crystalline water ice is not commonly found on the surfaces of TNOs due to their cold temperatures, so its presence on Achlys suggests that the object had experienced heating, possibly by an
impact event. Spectroscopic analyses from 2010 and 2011 suggest that Achlys's surface may be darkened by
amorphous carbon, which is thought to originate from heavily
irradiated organic compounds. These analyses also suggest that water ice and amorphous carbon each comprise major portions of Achlys's surface, with amorphous water ice likely more abundant than crystalline water ice. The surface of Achlys is devoid of
volatile ices like
nitrogen and
carbon monoxide, in contrast to the largest trans-Neptunian objects like Pluto. This is expected because Achlys's gravity is too weak to hold on any
atmosphere, especially volatiles after they have
sublimated into
vapor. In
visible light, Achlys's surface is spectrally neutral with respect to the Sun, which gives it a gray color. Achlys shares its gray color and water ice-rich surface with several TNOs including the large plutino Orcus; these objects are classified as
BB ("blue")-type TNOs in terms of visible color and
"prominent water" ()-type TNOs in terms of spectra. The gray color of Achlys implies that it contains little amounts of
tholins—moderately irradiated organic compounds that would otherwise tint the surface red. Spectroscopic analyses suggest that tholins should make up roughly 10% of Achlys's surface composition. The surface of Achlys is not uniform. The albedo is suspected to vary across Achlys's surface because the object varies in brightness as it rotates. Near-infrared spectroscopy of Achlys shows variable
spectral absorption of water ice and tentative signs of
methanol ice. Visible-light spectroscopy has detected sporadic hints of
hydrated minerals such as
silicates, which are suspected to exist in localized deposits on Achlys's surface. The color of Achlys has been observed to change as it rotates, with its visible
spectral slope or redness varying between 3.5%/ and 8.5%/. This color variation may hint at localized areas of concentrated tholins on Achlys's surface, which could be explained by various phenomena such as an
impact crater left by a red TNO. In November 2014, an observation of a stellar occultation from
Yunnan, China revealed that Achlys has a
topographic feature located at its
limb—the edge of its projected shape. The observation showed a gradual dimming of the occulted star, which has been interpreted as a partial, grazing occultation by Achlys's topographic feature. Achlys is the first TNO whose topographic feature has been observed via stellar occultation. The topographic feature on Achlys could either be a
chasm at least deep and roughly wide, or a shallow-sloped
depression roughly deep and at least wide. Such features have been seen on Pluto and its moon
Charon. == Satellite ==