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Magnesium hydroxide natural form

Aluminium and magnesium hydroxides are difficult to produce directly in any useable form from their natural ores. Filler grade calcium carbonate is widely produced from natural sources, but grinding costs appear to become prohibitive when ultra-fine particles are required and precipitation procedures then become competitive. Further details of precipitation procedures will be found under the specific filler types. [Pg.78]

The nature of silicate scaling is often complex and can involve the nucle-ation of calcium carbonate crystals (which tends to provide seeding points for silicate precipitation) and magnesium hydroxide (which can form at the heat-transfer surfaces, especially at cathodic sites where localized pH levels may exceed 10.0, then reacting with colloidal silica from the bulk water to form silicate scale). [Pg.111]

Magnesium hydroxide (mag-NEE-zee-um hye-DROK-side) is a white powder with no odor, found in nature as the mineral brucite. Perhaps the best known form of the compound is a milky liquid known as milk of magnesia, a product used to treat upset stomach and constipation. Milk of magnesia was invented in 1817 by the Irish pharmacist Sir James Murray (1788-1871). Murray built a plant to produce a mixture of magnesium hydroxide in water that he sold for the treatment of a variety of ailments, including heartburn, stomach acidity, bladder and bowel problems, and female problems. He said that the liquid mixture was much more effective than powdery magnesium hydroxide which had previously been used for the same purposes. [Pg.415]

Magnesium Hydroxid—MgHgOi—58—occurs in nature, and is-formed when a solution of a Mg salt is precipitated with excess, of NaHO, in absence of ammoniacal salts. It is a heavy, white-powder, insoluble in HjO absorbs COi. [Pg.205]

Magnesium oxide (MgO, magnesia) occurs naturally as the mineral periclase, a metamorphic mineral formed by the breakdown of dolomite, CaMg(C03)2, and other magnesium minerals. Occurrences of periclase are rare and are of no commercial importance. The principal commercial sources of MgO are magnesite (MgCOs) and magnesium hydroxide [Mg(OH)2]. [Pg.352]

Coagulants are often added in conjunction with lime to increase the settling rate of calcium carbonate and magnesium hydroxide. Most of these coagulants are acidic in nature and react with the alkalinity of the water. Commonly used coagulants include aluminium sulphate (alum), sodium aluminate, ferric sulphate and ferrous sulphate (Table 6.8). Alum reacts with natural alkalinity in water to form aluminium hydroxide floe (Equations 2.5—2.8) [14]. About 1 ppmofalumdecreaseswater alkahnity by 0.5 ppm and produces 0.44 ppm of CO2 ... [Pg.92]

Hydrotalcite, Mg5A 2(0H)26C03.4H20, is one of the naturally occurring anionic clay minerals (Reichle 1986). The magnesium-aluminium hydroxide octahedra form positively charged layers and are stacked on top of each other. The carbonate ions are located between the layers as interlayer anions. These clays after heat treatment have been found to be catalysts for base catalyzed reactions. [Pg.170]

In principle, there are a variety of routes to generate a desirable form of magnesium hydroxide. These range from milling of naturally occurring forms, such as bmcite, to precipitation and recrystallisation techniques. The target or guide is the property envelope of a typical finely precipitated ATH as shown in Table 4.2. [Pg.44]

Magnesium hydroxide is a white crystalline material. Its specific gravity is 2.4. Like ATH, it is soft and non-abrasive with a Mohs hardness about 3. It starts to decompose at about 300 °C. The naturally occurring mineral is known as brucite. The natural crystal form is as a flat hexagonal shaped plate. [Pg.88]

Magnesium hydroxide is potentially available in a number of product forms, which are all being developed and optimised for flame-retardant uses. Three distinct types of magnesium hydroxide can be recognised natural, synthetic seawater or brine, and synthetic large crystal. [Pg.88]

A number of new processes have recently been developed based on both precipitation and hydration methods [118]. Surface are acn be controlled in the range 1-25 mVg and the particle size from 0.5 to 5.0 micron. Magnesium hydroxide has a natural tendency to form platy, hexagonal crystals but this can also be controlled to some extent resulting in products with varying aspect of ratio. [Pg.90]

Magnesium Oxide n (ca. 1909) (magnesia, periclase) A white powder used as filler and as a thickening agent in polyester resins. It occurs naturally as the mineral periclase, but it is usually made in purer form by calcining magnesium hydroxide or carbonate. [Pg.440]

The ubiquity of water and metals that are ever present in the water means that hydrolysis reactions are essential aspects of many areas of science, industry and nature. Hydrolysis is an important component in water purification and treatment. In water treatment, many metals are removed from solution by precipitation as solid hydroxide phases which, in turn, may remove other metals and metalloids via adsorption onto the formed solids. In many countries, arsenic is removed from groundwater recovered for drinking via adsorption onto solid iron hydroxide, and knowledge ofthe precipitation behaviour of magnesium hydroxide is important in thermal desalination processes. [Pg.2]


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Magnesium forms

Magnesium hydroxide

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