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[Effect of the invention of claim 2 of the present application]The invention of claim 2 of the present application is the waste paper remaining in the second crushing gypsum crushed by the second crusher between the second crusher and the return passage in the recycled raw material production apparatus of claim 1. A vibration sieving machine for separating the slab is provided so that only fine gypsum from which scrap paper has been removed by the vibration sieving machine is returned to the return passage.
07. doi:10.008.Li D, Guo X, Xu Z, Tian Q, Feng Q (2015) Leaching behavior of metals from copper anode slime using an alkali fusion-leaching process.2015.hydromet.1016/j. Hydrometallurgy 157:9–12.
89% (Table 4). The mixture of these carbonate phases is visible in BSE image as a fair grey mass (Fig.95 to 10.28% and O: from 43. The median value of magnesium calculated for high-Mg calcite averages 9.In lower Biohermal limestone: low-Mg calcite and high-Mg calcite form the micritic rock mass.51 to 46. The content of MgCO3 in protodolomite is lower than the stoichiometric value for dolomite—46.61 to 36.25% MgCO3). The difference in the magnesium content in carbonate phases is only possible to observe in Table 4 which includes the results of the chemical analysis executed in selected points of the microarea.60 to 43. 5B), but there is no difference in colour shades between low-Mg calcite and high-Mg calcite.42 to 1. It is represented by crystals in which the content of MgCO3 ranges from 40. Sparry dark grey dolomite crystals (Table 4) are euhedral and rhombohedral in shape (Fig.46 to 10. Protodolomite was also identified in this limestone. 5B).18%, Mg: from 8.5% (33. In lower Biohermal limestone the content of MgCO3 in low magnesium calcite ranges from 0.92% (Table 4).46 to 36. The amount of Ca in high magnesium calcite ranges from 33. Like in lower Crinoidea limestone, also in these rocks protodolomite is probably present.13%.86%. The crystals of this carbonate phase are similar to protodolomite crystals of lower Crinoidea limestone.54%, C: from 7.19%, in high-Mg calcite—from 29.
106 for each sample. However, for widely dispersed samples, it can sometimes prove impossible to evidence all particles with the same lens. Samples were dispersed in 90% (v/v) ethanol added with 10% of methanol. Here, the lenses M5 (measuring range: 1.105 and 1. From the recorded images, we determined the median equivalent particle size and the aspect ratio (Equation (3))AR= FeretminFeretmax,. The lens needs to be selected to make the smallest particles visible and to find the right depth of field to focus on both larger and smaller particles.8–3755 µm) and M3 (range: 0.The QicPic granulomorphometer (Sympatec, Germany) with the MIWCELL cell dispersion module (wet analysis configuration) was used to measure the particle shapes by dynamic image analysis. The number of particles analyzed was between 1. The device is equipped with various lenses, and a digital camera captures the particles within the field of the lens.55–1126 µm) were used.
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