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磷酸鹽分解鉬酸鈣的熱力學

Thermodynamic analysis on phosphate decomposition of calcium molybdate

  • 摘要: 針對磷酸鹽分解鉬酸鈣的過程,根據同時平衡原理和質量守恒定律,繪制了25℃時Ca-Mo-P-H2O體系溶解組分的lgC-pH圖,以及不同總磷濃度條件下溶液中總鈣、總鉬的lgC-pH圖和鉬酸鈣穩定區.結果表明,在溶液中總磷濃度一定的條件下,隨著pH的增大體系中會依次出現H2MoO4(s)、CaMoO4(s)、Ca5(OH)(PO4)3(s)和Ca(OH)2(s)穩定存在的區域.總磷濃度直接影響到鉬酸鈣的分解過程,隨著總磷濃度的增加,鉬酸鈣的穩定區域不斷減小甚至消失,使得鉬酸鈣更加易于分解,因此溶液中總鉬濃度不斷增大,而總鈣濃度不斷降低;但總磷濃度過高會導致溶液中殘留游離含磷離子過高.從熱力學角度來看,在鉬酸鈣分解過程中,添加磷酸鹽比碳酸鹽更加有利于鉬酸鈣的分解.

     

    Abstract: According to the laws of simultaneous equilibria and mass conservation, the logarithm concentration-pH diagram of a Ca-Mo-P-H2O system, the logarithm eoncentration-pH diagrams of total calcium and total molybdenum at different total phosphate concentrations, and the stabile area of calcium molybdate at 25℃ were obtained on the basis of thermodynamic data. The results show that the stabile areas of H2MoO4(s), CaMoO4(s), Ca5(OH) (PO4)3(s) and Ca(OH)2(s) are distinguished orderly with increasing pH values at a constant total phosphate concentration. Calcium molybdate can be easily decomposed since the stabile area of calcium molybdate shrinks or even disappears with increasing total phosphate concentration; at the same time, the total molybdenum concentration increases, and the total calcium concentration decreases. However, high phosphate concentration is unnecessary for calcium molybdate can be decomposed at a very low phosphate concentration. Compared to carbonate, phosphate is more propitious to the decomposition of calcium molybdate.

     

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