Skip to main content

CINNABAR[HgS]

Cinnabar  and cinnabarite, likely deriving from the Ancient Greek: κιννάβαρι[6] (kinnabari), refer to the common bright scarlet to brick-red form of mercury(II) sulfide, formula HgS, that is the most common source ore for refining elemental mercury, and is the historic source for the brilliant red or scarlet pigment termed vermilion and associated red mercury pigments.
Detailed description
Cinnabar generally occurs as a vein-filling mineral associated with recent volcanic activity and alkaline hot springs. The mineral resembles quartz in symmetry and in its exhibiting birefringence; cinnabar has a mean refractive index of ~3.2, a hardness between 2 and 2.5, and a specific gravity of ~8.1. The color and properties derive from a structure that is a rhombohedral crystalline latticebelonging to the hexagonal crystal system, crystals that sometimes exhibit twinning.
Cinnabar has been used for its color since antiquity in the Near East, including as a rouge-type cosmetic, in the New World since the Olmec culture, and in China since as early as the Song dynasty, where it was used in coloring lacquerware.
Associated modern precautions for use and handling of cinnabar arise from the toxicity of the mercury component, which was recognized as early as ancient Rome.

Mining and extraction of mercury

As the most common source of mercury in nature,[14] cinnabar has been mined for thousands of years, even as far back as the Neolithic Age.[15] During the Roman Empire it was mined both as a pigment,[16][17] and for its mercury content.
To produce liquid mercury (quicksilver), crushed cinnabar ore is roasted in rotary furnaces. Pure mercury separates from sulfur in this process and easily evaporates. A condensing column is used to collect the liquid metal, which is most often shipped in iron flasks.

Toxicity


Associated modern precautions for use and handling of cinnabar arise from the toxicity of the mercury component, which was recognized as early as in ancient Rome.[18] Because of its mercury content, cinnabar can be toxic to human beings. Though people in ancient South America often used cinnabar for art, or processed it into refined mercury (as a means to gild silver and gold to objects) "the toxic properties of mercury were well known. It was dangerous to those who mined and processed cinnabar, it caused shaking, loss of sense, and death. Data suggest that mercury was retorted from cinnabar and the workers were exposed to the toxic mercury fumes."[19][page needed] Overexposure to mercury, mercurialism, was seen as an occupational disease to the ancient Romans, "Mining in the Spanish cinnabar mines of Almadén, 225 km (140 mi) southwest of Madrid, was regarded as being akin to a death sentence due to the shortened life expectancy of the miners, who were slaves or convicts."[20]

Decorative use

Cinnabar has been used for its color since antiquity in the Near East, including as a rouge-type cosmetic,[18] in the New World since the Olmec culture, and in China since as early as the Song dynasty, where it was used in coloring lacquerware.
Cinnabar's use as a color in the New World, since the Olmec culture,[21] is exemplified by its use in royal burial chambers during the peak of Maya civilization, most dramatically in the Tomb of the Red Queen in Palenque (600–700 AD), where the remains of a noble woman and objects belonging to her in her sarcophagus were completely covered with bright red powder made from cinnabar.[22]

The most popularly known use of cinnabar is in Chinese carved lacquerware, a technique that apparently originated in the Song dynasty.[23] The danger of mercury poisoning may be reduced in ancient lacquerware by entraining the powdered pigment in lacquer,[24][page needed] but could still pose an environmental hazard if the pieces were accidentally destroyed. In the modern jewelry industry, the toxic pigment is replaced by a resin-based polymer that approximates the appearance of pigmented lacquer.

PRICE
$4,090/FLASK

For more information:

mobile: +2348039721941

contact person: emeaba uche

e-mail: emeabau@yahoo.com



Comments

Popular posts from this blog

MAGNESIUM ORES

Magnesium is a chemical element with the symbol Mg , atomic number 12 and common oxidation number +2. It is an alkaline earth metal and the eighth most abundant element in the Earth's crust , where it constitutes about 2% by mass, [2] and ninth in the known Universe as a whole. [3] [4] This preponderance of magnesium is related to the fact that it is easily built up in supernova stars from a sequential addition of three helium nuclei to carbon (which in turn is made from three helium nuclei). Magnesium ion's high solubility in water helps ensure that it is the third most abundant. Detailed description: Magnesium is the 11th most abundant element by mass in the human body; its ions are essential to all living cells , where they play a major role in manipulating important biological polyphosphate compounds like ATP , DNA , and RNA . Hundreds of enzymes thus require magnesium ions to function. Magnesium is also the metallic ion at the center of chlorophyll...

BERYLLIUM ORE

A  divalent  element, beryllium is found naturally only combined with other elements in minerals. Notable gemstones which contain beryllium include  beryl  ( aquamarine ,  emerald ) and  chrysoberyl . The free element is a steel-gray, strong, lightweight brittle  alkaline earth metal . It is primarily used as a hardening agent in  alloys , notably  beryllium copper . Structurally, beryllium's very low density (1.85 times that of water), high melting point (1287 °C), high temperature stability and low coefficient of thermal expansion, make it in many ways an ideal aerospace material, and it has been used in rocket nozzles and is a significant component of planned space telescopes. Detailed description Because of its relatively high transparency to X-rays and other  ionizing radiation  types, beryllium also has a number of uses as filters and windows for radiation and particle physics experiments. Commercial use of beryllium m...

SPODUMENE [LiAl(SiO3)2]

Spodumene   is a   pyroxene   mineral   consisting of   lithium   aluminium   inosilicate ,   Li Al ( Si O 3 ) 2 , and is a source of lithium. It occurs as colorless to yellowish, purplish, or lilac kunzite (see below), yellowish-green or emerald-green   hiddenite , prismatic crystals, often of great size.   Detailed d Single crystals of 14.3 m (47 ft) in size are reported from the   Black Hills   of   South Dakota ,   United States . [5] [6] The normal low-temperature form α-spodumene is in the   monoclinic   system whereas the high-temperature β-spodumene crystallizes in the   tetragonal   system. The normal α-spodumene converts to β-spodumene at temperatures above 900 °C. [4]   Crystals are typically heavily striated parallel to the principal axis. Crystal faces are often etched and pitted with triangular markings. Discovery and occurrence Spodumene was first des...