“…Regardless of the oxidation state at the involved arsenic atoms, rare-earth metal oxoarsenates can serve well as either host materials or concentrated phosphors for lumogenious applications. This holds for the monazite -, xenotime -, and scheelite -type oxoarsenates(V) RE [AsO 4 ] ( Schäfer and Will, 1971 ; Lohmüller et al, 1973 ; Long and Stager, 1977 ; Schäfer et al, 1979 ; Brahim et al, 2002 ; Kang et al, 2005a ; Kang, 2009 ; Kang and Schleid, 2005 ; Schmidt et al, 2005 ; Hartenbach et al, 2006 ; Golbs et al, 2009 ; Metzger, 2012 ; Metzger et al, 2016 ; Ledderboge et al, 2018 ; Goerigk, 2021 ; Adala et al, 2022 ) ( RE = rare-earth metal: Sc, Y, La, Ce–Lu), where O 2− -to-As 5+ ligand-to-metal charge-transfer processes (LMCT) within the tetrahedral [AsO 4 ] 3− anions have a beneficial impact on the necessary energy transfer as well as for the oxoarsenates(III) RE [AsO 3 ] and RE 4 [As 2 O 5 ] 2 [As 4 O 8 ] ( Ben Hamida et al, 2005 ; Kang, 2009 ; Kang and Schleid, 2006 ; Ben Hamida, 2007 ; Metzger, 2012 ; Metzger et al, 2012 ; Ledderboge et al, 2014 ; Ledderboge, 2016 ; Locke et al, 2023 ), where the O 2− -to-As 3+ LMCT is supported by the lone-pair antenna at the trivalent arsenic centers. The latter occur as ψ 1 -tetrahedral [AsO 3 ] 3− groups either isolated in the first cases (Pb[SeO 3 ]- or K[ClO 3 ]-type RE [AsO 3 ]) or vertex-condensed to di- and tetranuclear anions ( pyro -[As 2 O 5 ] 4− and cyclo- [As 4 O 8 ] 4− ) for the latter ones ( RE 4 [As 2 O 5 ] 2 [As 4 O 8 ] ≡ 2 × RE 2 As 4 O 9 ).…”