Most solid combinations of helium with other substances require high pressure. Helium does not bond with the other atoms, but the substances can have a well defined crystal structure.
Disodium helide Disodium helide (Na2He) is a compound of helium and sodium that is stable at high pressures above . Disodium helide was first
predicted using USPEX code and was first synthesised in 2016. It was predicted to be
thermodynamically stable over 160 GPa and
dynamically stable over 100 GPa. Na2He has a
cubic crystal structure, resembling
fluorite. At 300 GPa the edge of a
unit cell of the crystal has . Each unit cell contains four helium atoms on the centre of the cube faces and corners, and eight sodium atoms at coordinates a quarter cell in from each face. Double electrons (2e−) are positioned on each edge and the centre of the unit cell. Each pair of electrons is spin paired. The presence of these isolated electrons makes this an
electride. The helium atoms do not participate in any bonding. However the electron pairs can be considered as an eight-centre two-electron
bond. Cristobalite He II (SiO2He) is stable between 1.7 and 6.4 GPa. It has a rhombohedral space group R-3c with unit cell dimensions and at 4 GPa. Cristobalite He I (SiO2He) can be formed under higher helium pressures over 6.4 GPa. It has a monoclinic space group P21/C with unit cell dimensions and at 10 GPa. Helium penetrates into fused silica at high pressure, reducing its compressibility.
Chibaite, another natural silica clathrate has its structure penetrated by helium under pressures higher than 2.5 GPa. The presence of guest hydrocarbons does not prevent this happening. Neon requires a higher pressure, 4.5 GPa to penetrate, and unlike helium shows hysteresis. Linde-type A zeolites are also rendered less compressible when penetrated by helium between 2 and 7 GPa.
Arsenolite helium inclusion compound Arsenolite helium inclusion compound is stable from pressures over 3 GPa and up to at least 30 GPa.
Arsenolite is one of the softest and most compressible minerals. Helium prevents amorphization that would otherwise occur in arsenolite under pressure. The solid containing helium is stronger and harder, with a higher sound velocity than plain arsenolite. The helium that is included into the crystal causes a more uniform stress on the As4O6 molecules. No actual bond is formed from arsenic to helium despite the lone pairs of electrons available. The diffusion of helium into arsenolite is a slow process taking days at a pressure around 3 GPa. However, if the pressure on the crystal is too high (13 GPa) helium penetration does not take place, as the gaps between arsenolite molecules become too small. At 1 GPa all the A sites are filled by helium, yielding He2CaZrF6.
Formates Under pressure helium penetrates
dimethylammonium iron formate (CH3)2NH2Fe(HCOO)3. It affects this by causing a change to a monoclinic ordered state at a lower pressure (around 4 GPa) than if helium were absent.
Small molecule is a van der Waals compound with hexagonal crystals. At 10 GPa the unit cell of 22 nitrogen atoms has a unit cell volume of 558 Å3, and about 512 Å3 at 15 GPa. These sizes are around 10 Å3 smaller than the equivalent amount of solid δ-N2 nitrogen at these pressures. The substance is made by compressing nitrogen and helium in a diamond anvil cell. NeHe2 has a crystal structure of hexagonal MgZn2 type at 13.7 GPa. The unit cell has dimensions and at 21.8 GPa, There are four atoms in each unit cell. It melts at 12.8 GPa and 296 K, stable to over 90 GPa.
Clathrates Helium clathrates only form under pressure. With
ice II at pressures between 280 and 480 MPa a solid helium hydrate with He:H2O ratio of 1:6 exists. Another clathrate with a water to helium ratio of 2.833 has been made in the SII clathrate structure. It has two different cages in the ice, the small one can contain one helium atom, and the large can contain four atoms. It was produced from neon clathrate that lost its neon, and then replaced by helium at 141 K and 150 MPa Other helium hydrates with the ice-I
h, ice-I
c 1:1, and ice-I
c 2:1 He to H2O ratio have been predicted.
Fullerites Helium can form intercalation compounds with the
fullerites, including
buckminsterfullerene C60 and C70. In solid C60 there are spaces between the C60 balls, either tetrahedral or octahedral in shape. Helium can diffuse into the solid fullerite even at one atmosphere pressure. Helium enters the lattice in two stages. The first rapid stage takes a couple of days, and expands the lattice by 0.16% (that is 2.2 pm) filling the larger octahedral sites. The second stage takes thousands of hours to absorb more helium and expands the lattice twice as much again (0.32%) filling the tetrahedral sites. However the solid C60•3He is not stable and loses helium on a timescale of 340 hours when not under a helium atmosphere. When the helium intercalated fullerite is cooled, it has an
orientational phase transition that is 10 K higher than for pure solid C60. The actual discontinuous change in volume at that point is smaller, but there are more rapid changes near the transition temperature, perhaps due to varying occupancy of the voids by helium.
Endohedral Helium atoms can be trapped inside molecular cages such as the
fullerenes He@C60, He@C70, He2@C60 and He2@C70 have all been made using compressed helium and fullerenes. When using only pressure and heat, the yield is quite low, under 1%. However, by breaking and reforming the carbon ball, much higher concentrations of He@C60 or He@C70 can be made. High-performance liquid chromatography can concentrate the helium containing material. HeN@C60 and HeN@C70 have also been made. These have a lower symmetry due to the two atoms being trapped together in the same cavity. This causes
ESR line broadening.
Dodecahedrane can trap helium from a helium ion beam to yield He@C20H20. Other cage like inorganic or organic molecules may also trap helium, for example C8He with He inside a cube, or He@Mo6Cl8F6. ==Impurity helium condensates==