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The Silver Mask (Romanian: Masca de argint) is a 1985 Romanian action historical film directed by Gheorghe Vitanidis. [1] This is the fourth film in the Margelatu series, [2] after Drumul oaselor (1980), Trandafirul galben (1982), Misterele Bucureștilor (1983), followed by Colierul de turcoaze (1986) and Totul se plătește (1987).
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In 2019, Ssangyong discontinued the Rodius/Stavic without any successor planned citing poor sales and implementation of the Euro 6D-Temp standards as both the 2.0L e-XDI 200 I4 and 2.2L e-XDI 220 I4 diesel engines offered on the Rodius are unable to be modified further to comply with the new emission regulations. The discontinuation of the ...
For the ores Cu 2 S and ZnS , balanced equations for the roasting are: 2 Cu 2 S + 3 O 2 → 2 Cu 2 O + 2 SO 2 2 ZnS + 3 O 2 → 2 ZnO + 2 SO 2. The gaseous product of sulfide roasting, sulfur dioxide (SO 2) is often used to produce sulfuric acid. Many sulfide minerals contain other components such as arsenic that are released into the environment.
For sulfide ores, a different process is taken for beneficiation. The ore needs to have the sulfur removed before smelting can begin. Roasting is the primary method of separating, where wood was placed on heaps of ore and set on fire to help with oxidation. [6] [7] 2 Cu 2 S + 3 O 2 → 2 Cu 2 O + 2 SO 2
At 3% fission products by weight, one ton of used fuel will contain about 400 grams of rhodium. The longest lived radioisotope of rhodium is 102m Rh with a half-life of 2.9 years, while the ground state (102 Rh) has a half-life of 207 days. [1] Each kilogram of fission rhodium will contain 6.62 ng of 102 Rh and 3.68 ng of 102m Rh.
[1] The present church was built in 1906–1910, for the jubilee marking 40 years on the throne for King Carol I. It was inspired by Saint Nicholas Princely Church in Iași, itself built to commemorate 40 years of Stephen the Great’s reign. Nicolae Ghica-Budești was the architect, while Costin Petrescu painted the interior in 1908–1910. [1]
Cartoon cross-section showing manto ore deposits (USGS) [1] A polymetallic replacement deposit, also known as carbonate replacement deposit or high-temperature carbonate-hosted Ag-Pb-Zn deposit, [2] is an orebody of metallic minerals formed by the replacement of sedimentary, usually carbonate rock, by metal-bearing solutions in the vicinity of igneous intrusions. [3]