FeS2(lattice)+2Li++2e−→Li2FeS2(amporhous) ---(1)
and then a second discharge equation,
Li2FeS2+2Li++2e−↔Fe+2Li2S --- (2)
On recharge, equation (2) reverses,
Fe+2Li2S−2e−↔Li2FeS2+2Li+ --- (3)
then,
Li2FeS2−xe−↔Li2−xFeS2+xLi+ --- (4)
but on further recharge,
Li2−xFeS2−(2−x)e−→(2−x)Li++FeSn+(2−n)S ---(5)
where x≥0.8
With these background materials...
This is Li2 when two unpaired orbits, each from one Li, pairs up,
This is the FeS2 lattice, where each member has six neighbors and each lattice unit is attached to another at two points,
At the cathode, the Li with an unpaired orbit pairs up another Li to form Li2 and attaches itself to the lattice of FeS2. This is an ionic bond.
Li2 replaces one Fe atom around S and the replaced Fe is reduced.
Under lower temperature 21oC to 30oC, the lattice starts to crack. This is the first discharge when a new battery come into use. Upon a second discharge via equation (2), hole forms in the lattice with the formation of Fe and Li2S. At this point if a recharge is attempted, the amporhous Li2FeS2 (1) reforms within the hole in the lattice. Upon further recharge, we obtain Li, but we do not return to the ionic lattice of FeS2, instead we obtain, FeSn and free elemental S. The presence of elemental S causes havoc at the anode.
Structurally the cathode has disintegrated.
Recharging is not a problem at 400oC with a salt electrolyte, the FeS2 lattice (melting point 1,177−1,188oC is reformed upon full recharge. Heat increases the orbital radii of the members of the lattice Fe and S, and makes the FeS2 lattice more malleable but not melting it completely. At this temperature the FeS2 lattice can accommodate Li2.
Increasing the distance between the ionic elements can also be done using a polar solvent infused into the lattice. This solvent should not dissolve the compound but space out the members of the lattice as when the
temperature is at 400oC. FeS2 is not soluble in water, but water introduced into the lattice when the crystal forms might space themselves between the lattice members and make the crystal soft. Otherwise a more polar solvent has to be found. Since, Pyrite is soluble in acids, a good candidate is HCl, other acids are physically too big. FeS2 doped with HCl.
CuS2−FeS2 has wider lattice spacing √3.(3.966×10−10) m, compared to FeS2 of √3.(3.38×10−10) m. And with Arsenic As in the mix, √3.(3.8488×10−10) m.(2)
If the lattice is intact after the first discharge via equation (1). The Li2 member are simply hanging in the lattice of FeS2 slightly expanded to accommodate the new member. And subsequent discharge,
Li2FeS2−2e−↔FeS2+2Li+
pucks the Li2 as 2Li+ after removing the two electrons, from the lattice.
The crux of the problem is to keep the lattice structure of FeS2 intact during the charge and discharge cycle. A backing lattice that holds onto the FeS2 lattice and stretches it to accommodate Li2 but
itself does not part-take in the redox reactions can be the solution. Stacked layers of the two lattices will then build the bulk of the cathode. The backing lattice need not stretch the FeS2 lattice if a single layer of the bounded lattice (FeS2+backing) are use. In this case, the expose surface of the FeS2 lattice allows Li2 to bond freely. A transport layer that allows Li+ to move freely can be sandwiched between two bounded lattices to build bulk. Many binary metal chalcogenides (compounds with S, Se or Te) have the FeS2 structure, as do oxides like CdO2, α−K2O, β−Na2O(3). And "Late" transition metal disulfides (Mn, Fe, Co, Ni) almost always adopt the pyrite or the related marcasite motif. There are many material options for a backing lacttice, insulated from the redox reactions by a few layers of FeS2 to provide structural integrity.
Note: It is likely that instead of Li+ we have LiH+. Since, H after loosing its electron sit inside Li, Li+ and LiH+ is likely to be of comparable in size.
There is no reversing entropy but entropy can be preserved.
References:
(1) In situ Fe K-EDGE X-ray absorption fine structure of a pyrite electrode in a Li/Polyethylene oxide (LiClO4)/FeS2 battery environment. Dana Totir, In Tae Bae, Yining Hu, Mark R. Antonio and Daniel A. Scherson. Proceeding Symposium Lithium Battery CONF-961040--23
(2)Schmid-Beurmann P, Lottermoser W Physics and Chemistry of Minerals 19 (1993) 571-577
57Fe-Moessbauer spectra, electronic and crystal structure of members of the CuS2-FeS2
solid solution series.
One set of data from reference (2), (http://rruff.geo.arizona.edu/AMS/AMC_text_files/20081_amc.txt) repeated below, suggests, an atomic center to center of √3.(6.25×10−10)m.
Pyrite
Oftedal I
Zeitschrift fur Physikalische Chemie 135 (1928) 291-299
Uber die Kristallstrukturen der verbindungen RuS2, OsS2, MnTe2 und AuSb2.
Mit einem Anhang uber die Gitterkonstant von Pyrit
_database_code_amcsd 0017728
5.414 5.414 5.414 90 90 90 Pa3
atom x y z
Fe 0 0 0
S .625 .625 .625
(3)"Ceramic Materials: Science and Engineering" By C. Barry Carter, M. Grant Norton publisher: Springer Science & Business Media, 4 Jan 2013.
(1) In situ Fe K-EDGE X-ray absorption fine structure of a pyrite electrode in a Li/Polyethylene oxide (LiClO4)/FeS2 battery environment. Dana Totir, In Tae Bae, Yining Hu, Mark R. Antonio and Daniel A. Scherson. Proceeding Symposium Lithium Battery CONF-961040--23
(2)Schmid-Beurmann P, Lottermoser W Physics and Chemistry of Minerals 19 (1993) 571-577
57Fe-Moessbauer spectra, electronic and crystal structure of members of the CuS2-FeS2
solid solution series.
One set of data from reference (2), (http://rruff.geo.arizona.edu/AMS/AMC_text_files/20081_amc.txt) repeated below, suggests, an atomic center to center of √3.(6.25×10−10)m.
Pyrite
Oftedal I
Zeitschrift fur Physikalische Chemie 135 (1928) 291-299
Uber die Kristallstrukturen der verbindungen RuS2, OsS2, MnTe2 und AuSb2.
Mit einem Anhang uber die Gitterkonstant von Pyrit
_database_code_amcsd 0017728
5.414 5.414 5.414 90 90 90 Pa3
atom x y z
Fe 0 0 0
S .625 .625 .625
(3)"Ceramic Materials: Science and Engineering" By C. Barry Carter, M. Grant Norton publisher: Springer Science & Business Media, 4 Jan 2013.