We analyze the formation of transition metal (TM) carbides, as determined by the strength of TM–TM and
TM–C bonds, as well as lattice distortions induced by C interstitials. With increasing filling of the d-band of
TMs, TM–C bonds become increasingly weak from the left of the periodic table to the right, with fewer and
fewer C atoms entering the TMs lattice. Technetium (Tc) turns out to be a critical point for the formation of
carbides, guiding us to resolve a long-standing dispute. The predicted Tc carbides, agreeing with measured
X-ray absorption spectra, should decompose to cubic Tc and graphite above 2000 K. Consequently, we
show that what has been claimed as TcC (with rocksalt structure) is actually a high-temperature cubic
phase of elemental technetium.