Skip to main content

ANTIMONY ORE

Antimony (pronounced /ˈæntɨmɵnɪ/ AN-ti-mo-nee);[note 2] Latinstibium) is a chemical element with the symbol Sb and an atomic number of 51. It has two stable isotopes, one with seventy neutrons, the other with seventy-two. A silvery lustrous grey metalloid, it is found mainly as antimony sulfide, commonly known as stibnite.
Elemental antimony has applications in electronics and as an alloy with other metals it is used for small arms ammunition.

Detailed descriptin:
Etymology
The ancient words for antimony mostly have, as their chief meaning, kohl, the sulfide of antimony. Pliny the Elder, however, distinguishes between male and female forms of antimony; his male form is probably the sulfide, while the female form, which is superior, heavier, and less friable, is probably native metallic antimony.
History
Antimony's sulfide compound, antimony(III) sulfide, Sb2S3 was recognized in antiquity, at least as early as 3000 BC.
An artifact made of antimony dating to about 3000 BC was found at TelloChaldea (part of present-day Iraq), and a copper object plated with antimony dating between 2500 BC and 2200 BC has been found in Egypt. There is some uncertainty as to the description of the artifact from Tello. Although it is sometimes reported to be a vase, a recent detailed discussion reports it to be rather a fragment of indeterminate purpose. The first European description of a procedure for isolating antimony is in the book De la pirotechnia of 1540 by Vannoccio Biringuccio, written in Italian. This book precedes the more famous 1556 book in Latin by AgricolaDe re metallica, even though Agricola has been often incorrectly credited with the discovery of metallic antimony.
Characteristics
Physical properties
There are four known allotropes of antimony: a stable metallic form, and three meta-stable forms which are explosive, black and yellow. Each has its own distinct physical properties, the most common of which is metallic antimony, a brittle, silver-white shiny metal. When molten antimony is slowly cooled to metallic antimony, it forms with an hexagonal crystal structure, isomorphic with that of the grey form of arsenic.

The explosive form of antimony is formed from the electrolysis of antimony(III) trichloride, under specific temperatures and concentration. In a bath of hydrochloric with an antimony anode and platinum foil cathode, explosive antimony is deposited on the latter. When scratched with a sharp implement, an exothermic reaction occurs and white fumes given off as metallic antimony is formed; alternatively, when rubbed with a pestle in a mortar, an strong detonation occurs. Black antimony is formed when gaseous metallic antimony is rapidly cooled. It oxidies in air and is sometimes spontaneously combustible. At 100 °C, it gradually transforms into the stable form. Finally, the yellow allotrope of antimony is the most unstable. While it cannot be produced as the black allotrope by rapid cooling, it can only be formed by introducing oxygen into antimony hydride at -90 °C. Above this temperature and in ordinary light, it transforms into the stabler black allotrope.

PRICE
$2.23/KG OR $1.01/IB

For more information:

mobile: +2348039721941

e-mail: emeabau@yahoo.com


contact person: emeaba uche



Comments

Popular posts from this blog

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...

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...

GERMANIUM ORE

Germanium (pronounced /dʒərˈme ɪ niəm/ , jər-MAY-nee-əm ) is a chemical element with the symbol Ge and atomic number 32. It is a lustrous, hard, grayish-white metalloid in the carbon group , chemically similar to its group neighbors tin and silicon . Germanium has five naturally occurring isotopes ranging in atomic mass number from 70 to 76. It forms a large number of organometallic compounds, including tetraethylgermane and isobutylgermane Detailed description Germanium was discovered comparatively late because very few minerals contain it in high concentration. Germanium ranks near fiftieth in relative abundance of the elements in the Earth's crust . In 1869, Dmitri Mendeleev predicted its existence and some of its properties based on its position on his periodic table and called the element eka-silicon . Nearly two decades later, in 1886, Clemens Winkler found it in the mineral argyrodite . Winkler found that experimental observations agreed with Mendeleev...