The method grew out of years of crystallography and coordination chemistry in Óscar Castillo’s group at the University of the Basque Country (UPV/EHU). Rubén Pérez-Aguirre was building the porous metal-organic materials there, and he wanted to know what they really held in solution, not what a dry gas-phase test guessed they might hold.
His answer was a force balance. Suspend the particle in a magnetic field, then watch the field shift as mass adsorbs onto it; that shift calibrates into a captured-mass number. It reads the solid in virtually any liquid at normal temperature and pressure — water and ethanol are the proven examples — and it does so independent of particle size, even on materials a dry test would write off as non-porous.
The proof came when CO₂ was captured straight from water and weighed on the solid. After that it stopped being a curiosity and became a measurement worth a company. The same question turns up across pharma, CO₂ capture and CCUS, water and PFAS, membranes, direct air capture, academic labs, and high-throughput screening: what does this solid hold in its working liquid?