Abstract
The copper silicate and its dehydrated form exhibit a singlet ground state at low temperature, which is conditioned by the topology of the isolated edge-sharing (or ) chains. The structural analysis of the hydrated and dehydrated forms indicates a strong alternation of the exchange interaction parameter within these chains. The magnetic susceptibility and specific heat measurements confirm spin gaps for and for . The reversible dehydration of the water molecules from the microporous framework in the structure affords unique opportunity for tuning the magnetic interaction parameters in these compounds.
- Received 30 May 2005
DOI:https://doi.org/10.1103/PhysRevB.72.092403
©2005 American Physical Society