We were able to follow the formation reaction of high-temperature superconductors in the system Bi-Pb-Sr-Ca-Cu-O by using in-situ high-temperature X-ray diffraction. We first observed reactions in the confined system Bi-Sr-Cu-O, and then investigated modifications in the reaction path introduced by lead and calcium. We found that the addition of Ca does not modify reactions below 850°C but lowers the melting point of Bi 2Sr 2CuO 6+ x , Calcium also extends the stability range of the latter phase which, in contrast to Ca-free samples, does not decompose before melting. The addition of lead lowers the formation temperature of some intermediate phases, and introduces strontium lead oxide as a new phase stable up to 880°C. The addition of calcium and lead leads to the formation of very stable Ca 2PbO 4 early in the process (550°C). This reaction consumes, depending on stoichiometry, most of the lead. We found that Ca 2PbO 4 decomposes when the high-temperature superconductor Bi 2Sr 2CaCu 2O 8+x is formed above 830°C. Up to this temperature, Ca 2PbO 4 acts therefore as a reservoir for calcium and keeps the lead oxide from acting as a flux.
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