USAC is a publicly traded (NYSE: UAMY) natural resource company and the only significant antimony producer in the United States — vertically integrated across mining, milling, smelting, and sales.
United States Antimony Corporation is the major domestic producer of antimony products, operating one of only three antimony smelters in North and Central America — located in the Burns Mining District of Sanders County, Montana. USAC produces antimony oxide, sodium antimonate, and antimony metal, each serving distinct industrial markets. Antimony oxide is a fine white powder widely used as a flame retardant in plastics, rubber, fiberglass, textiles, paints, and coatings, as well as a catalyst in polyester resin and PET bottle production, and an opacifier for porcelains. Sodium antimonate serves as a fining agent for glass in cathode ray tubes and as a flame retardant. Antimony metal is sold for use in bearings, storage batteries, and ordnance. Emerging research also points to antimony’s promise as a next-generation semiconductor material, with charge mobility significantly higher than silicon, positioning it as a potential building block for post-silicon electronics.
ANTIMONY METAL: a silvery-white element belonging to Group VA of the periodic table, atomic number 51, atomic weight 121.76, density 6.73, melting point 630 degrees centigrade, boiling point 1380 degrees centigrade.
ANTIMONY OXIDE: “Antimony Oxides”, are antimony trioxides, (Sb2O3), and are fine white odorless powders. Antimony trioxide has two crystalline forms, either senarmontite which is cubic, or valentinite which is orthorhombic. Antimony trioxide (Sb2O3) has a molecular weight of 291.52, a melting point of 656° C, a boiling point of 1,425° C, and a refractive index of 2.087. Montana Brand antimony oxides are formed exclusively by the sublimation of antimony metal under extremely rigid furnace conditions. The physical and chemical properties are remarkably consistent due to a comprehensive quality control program. Sb2O3is practically insoluble in water (approximately 0.001 grams/100ml of H2O at 25° C.) It is soluble in HCl to form antimony tri-chloride, SbCl3; in HNO3 to form SbONO3; in H2SO4 to form SbOhSO4; in NaOH to form NaSbO3; and in KOH to form KSbO3.
Antimony trisulfide (Sb2S3) is found in nature as the crystalline mineral stibnite and the amorphous red mineral (actually a mineraloid) metastibnite. It is manufactured for use in safety matches, military ammunition, explosives and fireworks. It also is used in the production of ruby-colored glass and in plastics as a flame retardant.[5] Historically the stibnite form was used as a grey pigment in paintings produced in the 16th century.[6] In 1817, the dye and fabric chemist, John Mercer discovered the non-stoichiometric compound Antimony Orange (approximate formula Sb2S3·Sb2O3), the first good orange pigment available for cotton fabric printing.
Antimony trisulfide was also used as the image sensitive photoconductor in vidicon camera tubes. It is a semiconductor with a direct band gap of 1.8–2.5 eV. With suitable doping, p and n type materials can be produced.
Not everything is bigger in Texas — some things are really, really small. A group of engineers at The University of Texas at Austin may have found a new material for manufacturing even smaller computer chips that could replace silicon and help overcome one of the biggest challenges facing the tech industry in decades: the inevitable end of Moore’s Law.
In 1965, Gordon Moore, founder of Intel, predicted the number of transistors that could fit on a computer chip would double every two years, while the cost of computers would be cut in half. Almost a quarter century later and Moore’s Law continues to be surprisingly accurate. Except for one glitch.
Silicon has been used in most electronic devices because of its wide availability and ideal semiconductor properties. But chips have shrunk so much that silicon is no longer capable of carrying more transistors. So, engineers believe the era of Moore’s Law may be coming to an end, for silicon at least. There simply isn’t enough room on existing chips to keep doubling the number of transistors.
Researchers in the Cockrell School of Engineering are searching for other materials with semiconducting properties that could form the basis for an alternative chip. Yuanyue Liu, an assistant professor in the Walker Department of Mechanical Engineering and a member of UT’s Texas Materials Institute, may have found that material.
In a paper published in the Journal of the American Chemical Society, Liu and his team, postdoctoral fellow Long Cheng and graduate student Chenmu Zhang, outline their discovery that, in its 2D form, the chemical element antimony may serve as a suitable alternative to silicon.
Antimony is a semi-metal that is already used in electronics for some semiconductor devices, such as infrared detectors. As a material, it is only a couple of atomic layers thick and has a high charge mobility — the speed a charge moves through a material when being pulled by an electric field. Antimony’s charge mobility is much higher than other semiconductors with similar size, including silicon. This property makes it promising as the building block for post-silicon electronics.
Liu has only demonstrated its potential through theoretical computational methods but is confident it can exhibit the same properties when tested with physical antimony samples, which is the team’s next step. But the findings have even broader significance than simply identifying a potential replacement for silicon in the race to maintain Moore’s Law into the future.
“More importantly, we have uncovered the physical origins of why antimony has a high mobility,” Liu said. “These findings could be used to potentially discover even better materials.”
Date:
November 4, 2019
Source:
University of Texas at Austin
Summary:
Researchers are searching for alternative material to silicon with semiconducting properties that could form the basis for an alternative chip.
Bear River Zeolite (BRZ™) is almost pure clinoptilolite zeolite that originates from volcanic ash that settled in a fresh water lake and solidified into rock over thousands of years. Clinoptilolite zeolite is one of over 50 minerals in the zeolite group, which are basically hydrated calcium potassium sodium aluminosilicates, commonly referred to as molecular sieves.
BRZ™ clinoptilolite zeolite is regarded as one of the best zeolites due to its high cation exchange capacity (CEC), low sodium content, high potassium content, superior hardness, and uniformity.
*Cation-exchange capacity is a measure of the number of cations per unit weight available for exchange, usually expressed as milliequivalents per 100 grams of material.
University at Buffalo’s department of Civil, Structural and Environmental Engineering tested zeolite from two sources for possible use – Column studies were conducted for more than a year at UB using simulated (nonradioactive) groundwater and at WVDP using actual (radioactive) groundwater – Using data collected conducted modeling to assist in estimating PTW longevity.
Bear River Zeolite was the chosen zeolite for the remediation of radioactive ground water
