Uji Karakteristik Magnesium Fosfat dari Pelarutan Mineral Dolomit dengan Asam Fosfat

Bayu Sastra Dewangga, Mochammad Alief Setyanugraha, L. Edahwati
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Abstract

Magnesium phosphate (Mg3(PO4)2) is an organic compound formed from magnesium salts derived from phosphoric acid (H3PO4) in other words, elemental magnesium that is sandwiched between the phosphate anions. In addition, magnesium phosphate has been needed by industry, especially in the field of advanced and biological materials. However, what is currently needed is the high price of basic materials that require imports. The mineral dolomite is widely distributed in Indonesia, contains calcium (Ca) and magnesium (Mg) in it so that it can be used as an alternative base material for the synthesis of
测试多洛米特矿物溶解法的磷酸镁特性和磷酸
磷酸镁(Mg3(PO4)2)是由磷酸(H3PO4)衍生的镁盐形成的有机化合物,换句话说,是夹在磷酸阴离子之间的元素镁。此外,磷酸镁在工业上也有很大的需求,特别是在先进材料和生物材料领域。然而,目前需要的是需要进口的基础材料的高价格。白云石矿物在印度尼西亚分布广泛,其中含有钙(Ca)和镁(Mg),因此可以作为合成的替代基材
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