A METHOD FOR NEUTRALIZING WASTE SULFURIC ACID BY ADDING A SILICATE

Abstract: It has been shown that magnesiumsilicates, particularly Mg-rich olivine, is very proper to neutralize waste sulfuric acid. In said process a silicagel and a Fe/Mg-containing liquid are formed. The experiments show that a distinct separation of the silicagel from the Fe-containing liquid is possible in case the neutralization process is performed in an inert atmosphere. After separation of the SiO2-rich gel a Fe-V precipitate may be formed by means of aeration. The SiO2 gel may be rinsed well, so that an acceptable product is formed that e.g. is useful in the concrete industry. The liquids formed are MgSO4 rich. They may be drained simply into sea-water.

Description: A method for neutralizing waste sulfuric acid by adding a silicate. The invention relates to a method for neutralizing waste sulfuric acid by adding a salt of a weaker acid than sulfuric acid. As appears from "Ullmann's Enzyklop'idie der chemischen Techno- logie" 18, 579 (1982), it was common practice up to now to drain waste acid directly into the sea or into the rivers. Said draining causes an unacceptable environmental load of the surface waters. If from the waste sulfuric acid gypsum is formed by reacting it with calcium carbonate, the waste acid problem is only shoved, since in that case one obtains considerable quantities of gypsum for which an insufficient number of applications is available, particularly in view of the impurities present in that type of gypsum. (Consequently, according to the law, said gypsum is still a chemical waste). It was found now, that the waste acid problem may be solved in an environmentally friendly way by adding magnesium silicate to said waste sulfuric acid. At the reaction with sulfuric acid two separate or easily to separate phases are formed, the first of which consists of an aqueous solution of the sulphate ions and the magnesium metal ions derived from the salt and the second of which contains an Si<_2 containing precipitate, apart from the magnesium silicate that optionally is used in excess. From a practical point of view magnesium silicate will be used, that reacts sufficiently fast with sulfuric acid. Magnesium silicates are e.g.: forsterite, olivine, enstatite and chrysolite. Subsequently, the solution of sulfate ions and metal ions may be drained into surface water, or it can be used for an industrial application. This holds also for the precipitate obtained. Magnesium is the second important cation in sea-water and consequently there are no serious objections against draining thereof. A similar argument holds for the sulfate ion, which is the second important anion. Since further in case of using magnesium silicate a silicagel will be formed below the magnesium sulfate solution, and silica gel may be used for many purposes in the building area, the use of magnesium silicate is very useful. The reaction that occurs is illustrated by the following equation: 2H 2 S04 + Mg 2 Siθ4 + 2Sθ4 2" + 2Mg 2+ Said reaction occurs completely even at room temperature (18-30°C). The reaction rate depends on the surface available and on the temperature. E.g. in a series of experiments it appeared that at a temperature of 50°C the reaction time Is about 24 hours and at 85°C it is just some hours. Literature data show that magnesium-rich olivine is the most proper of all magnesium silicates. It may be expected that in case other magnesium silicates would be used, the reaction time would be at least ten times higher. Olivine occurs in high concentrations in nature in stones that can be won easily. In a preferred embodiment of the method according to the invention particularly at using it on an commercial scale, olivine Is added to the sulfuric acid. Indeed olivine contains apart from magnesium also small quantities of other metals, like nickel, but said metals may be extracted easily by means of old methods. Further Iron is present in the solution. Said iron may be advantageous, since at the precipitation of iron hydroxide heavy metals may be precipitated simultaneously and subsequently they can be separated easily. Examples: After having observed in a series of experiments that in order to achieve a fast reaction of the liquid olivine blend it has to be stirred continuously, and that a smaller grain size (higher specific surface) and a higher temperature increase the reaction rate, some experiments with waste sulfuric acid were carried out. Series I 350 g. olivine, having the following a composition: Siθ2 40.7 weight percent, MgO 50 weight percent, FeO 8.9 weight percent, NiO 0.4 weight percent, were added to 300 ml waste sulfuric acid (s.g. 1.29) having the following composition: H2SO4 29 weight percent, Fe 1.8 weight percent, Mg 0.5 weight percent, Al 0.4 weight percent, Ti 0.5 weight percent, Cr 0.017 weight percent, V 0.050 weight percent. The amount of olivine is the quintuple of the amount required for a complete neutralization of the sulfuric acid. The grain size of the olivine varied from 0.15 to 0.5 mm. At 25 W C after 45 hours a pH of 3.5 was reached. At 50°C it took 7 hours and at 80 β C l _ hour. After the reaction the mixture was not stirred for several hours. In all cases three layers were formed, the lower layer contained substantially only olivine. The middle layer was a thick layer of a brown gel and the upper layer was a thin layer of a clear, somewhat greeny coloured liquid. The analysis of the clear liquid showed that it contained 35 weight percent MgS04, while Fe and V could not be traced; the Cr percentage was 0.02 weight percent. The gel contained 55 weight percent H2O; 10 weight percent Siθ2_ 5 weight percent Fβ2θ3 30 weight percent MgSθ4; 0.07 weight percent V and 0.02 weight percent Cr. After repeated rinsing of the gel the major part of the MgS04 could be removed. Then, the gel contained about 75 weight percent H2O 12 weight percent Siθ2_ 7 weight percent Fβ2θ3; 6 weight percent MgS04; 0.1 weight percent V and 0.12 weight percent Cr. Series II This series is identical to series I but the system was kept in a reducing condition by maintaining a nitrogen atmosphere above the liquid-olivine blend. There was no difference in reaction time. After having stopped stirring the system divided itself again into three layers. The lower layer was formed by olivine. The second layer consisted of a transparent to white gel above which a clear green liquid was present. The composition of the gel was 60 weight percent H2O, 10 weight percent Siθ2 » 5 weight percent FeS04 en 30 weight percent MgSθ with 0.03 weight percent V and 0.02 weight percent Cr. After rinsing the composition of the gel was 85 weight percent H2O, 12 weight percent Si(_2, 1 weight percent FeS04 and 1 weight percent MgS0 . After centrifuging the composition of the gel was 60 weight percent H2O, 38 weight percent Siθ2, 1 weight percent FeS04 and 1 weight percent MgS0 . The green liquid was oxidized at pH 3.5 by means of H2O2- Immediately a brown precipitate was formed having the composition: 70 weight percent FeOOH, 10 weight percent MgSθ4, 20 weight percent H2O, 0.7 weight percent V and 0.03 weight percenter. The remaining liquid contained 35 weight percent MgSθ and 0.02 weight percent Cr.

Claims: CLAIMS 1. A method for neutralizing waste sulfuric acid, by adding a salt of a weaker acid than sulfuric acid, characterized in that magnesium silicate is added to the sulfuric acid and it is allowed to the magnesium silicate to react with the sulfuric acid. 2. A method according to claim 1, characterized in using olivine as said magnesium silicate * * * * *

Inventors: SCHUILING ROELOF DIRK, SCHUILING, ROELOF, DIRK
Applicants: UNIV UTRECHT, RIJKSUNIVERSITEIT UTRECHT
Application year: 1985
Main classification: C02F1
IPC codes: A62D3, A62D101, C02F1