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16389-88-1

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16389-88-1 Usage

Definition

Different sources of media describe the Definition of 16389-88-1 differently. You can refer to the following data:
1. A mineral, CaCO3.MgCO3, used as an ore of magnesium and for the lining of openhearth steel furnaces and Bessemer converters.
2. dolomite: A carbonate mineral consistingof a mixed calcium–magnesiumcarbonate, CaCO3.MgCO3,crystallizing in the rhombohedralsystem. It is usually white or colourless.The term is also used to denotea rock with a high ratio of magnesiumto calcium carbonate. See limestone.

Agricultural Uses

Dolomite is a carbonate of calcium and magnesium. It is a mineral of formula CaMg(CO3)2 with a rhombohedral system. It has a density of 2.8 g/cc and hardness of 4 on the Mohs scale.Dolomite has a vitreous lustre which is between transparent and translucent. It effervesces with hot concentratedh ydrochloric acid (HCl).A carbonate-rich sedimentary rock of chemical or biological origin contains 50% or more carbonate, of which at least half is in the form of dolomite. The color of dolomite is darker than limestone and does not give any effervescence with cold and dilute HCl.Dolomite may also contain iron and manganese. Depending on the proportion of dolomite and calcite, there are many transitional phases between calcareous dolomites and dolomitic limestones.Dolomite has multiple applications. It is used in the manufacture of magnesium and its compounds. It is also used as building material, as a refractory for furnaces, as a fertilizer, for the removal of sulphur dioxide from stack gases and in ceramics.

Industrial uses

Dolomite is the carbonate mineral CaMg(CO3)2,often with small amounts of iron, manganese,or excess calcium, which replace some of themagnesium; cobalt, zinc, lead, and barium aremore rarely found.Dolomite is a very common mineral, occurringin a variety of geologic settings. It is oftenfound in ultrabasic igneous rocks, notably incarbonates and serpentinites, in metamorphosedcarbonate sediments, where it may recrystallize to form dolomite marbles, and inhydrothermal veins. The primary occurrence ofdolomite is in sedimentary deposits, where itconstitutes the major component of dolomiterock and is often present in limestones.Dolomite is normally white or colorlesswith a specific gravity of 2.9 and a hardness of3.5-4 on Mohs scale.

Check Digit Verification of cas no

The CAS Registry Mumber 16389-88-1 includes 8 digits separated into 3 groups by hyphens. The first part of the number,starting from the left, has 5 digits, 1,6,3,8 and 9 respectively; the second part has 2 digits, 8 and 8 respectively.
Calculate Digit Verification of CAS Registry Number 16389-88:
(7*1)+(6*6)+(5*3)+(4*8)+(3*9)+(2*8)+(1*8)=141
141 % 10 = 1
So 16389-88-1 is a valid CAS Registry Number.
InChI:InChI=1/CH2O3.Ca.Mg/c2-1(3)4;;/h(H2,2,3,4);;/q;2*+2/p-2

16389-88-1SDS

SAFETY DATA SHEETS

According to Globally Harmonized System of Classification and Labelling of Chemicals (GHS) - Sixth revised edition

Version: 1.0

Creation Date: Aug 18, 2017

Revision Date: Aug 18, 2017

1.Identification

1.1 GHS Product identifier

Product name DOLOMITE

1.2 Other means of identification

Product number -
Other names taraspite

1.3 Recommended use of the chemical and restrictions on use

Identified uses For industry use only.
Uses advised against no data available

1.4 Supplier's details

1.5 Emergency phone number

Emergency phone number -
Service hours Monday to Friday, 9am-5pm (Standard time zone: UTC/GMT +8 hours).

More Details:16389-88-1 SDS

16389-88-1Upstream product

16389-88-1Downstream Products

16389-88-1Related news

Environments favoring DOLOMITE (cas 16389-88-1) formation at cold seeps: A case study from the Gulf of Mexico08/12/2019

Dolomite rarely occurs in modern marine environments, while it is ubiquitous in the geological record. This apparent contradiction made the formation mechanism of dolomite a long-standing problem haunting sedimentologists. However, dolomite is a constituent of many modern seep carbonates, provid...detailed

Effect of ash and DOLOMITE (cas 16389-88-1) on the migration of sulfur from coal pyrolysis volatiles08/11/2019

For investigating the effectiveness of ash and dolomite on the migration of sulfur from coal pyrolysis volatiles, pyrolysis experiments of Xinzhou high-sulfur bitumite were executed in a self-designed reactor. The influences of heat carrier species, mass ratios of ash to coal, and ash particle s...detailed

Evolution of DOLOMITE (cas 16389-88-1) composition and reactivity during biomass gasification08/10/2019

Dolomite is a cheap and robust catalyst used for biomass gasification, but its deactivation under relevant conditions of pilot-scale gasifiers has still been poorly understood. For this reason, the catalytic activity of fresh and used dolomites produced from an industrial air-blow fluidized bed ...detailed

Aerobically incubated bacterial biomass-promoted formation of disordered DOLOMITE (cas 16389-88-1) and implication for DOLOMITE (cas 16389-88-1) formation08/07/2019

With the realization that the formation of low-temperature dolomite could involve the microbial activity, a new pathway to understand the origin and mechanism of dolomite is emerging. Although microbially mediated CaMg carbonates and dolomite occur in some aerobic and high-salinity conditions, l...detailed

Genetic types and distinguished characteristics of DOLOMITE (cas 16389-88-1) and the origin of DOLOMITE (cas 16389-88-1) reservoirs08/05/2019

To find out the origin of dolomite, the precipitation of primary dolomite, and the formation of pores in dolomite, petrologic and geochemical characteristics of typical samples from Sichuan and Tarim Basin were analyzed based on the previous understandings, and three aspects of results were achi...detailed

Neoproterozoic marine DOLOMITE (cas 16389-88-1) hardgrounds and their relationship to cap DOLOMITE (cas 16389-88-1)s08/04/2019

Neoproterozoic cap dolomites are unusual and distinctive marker units that occur after large Cryogenian glaciations. Several thin dolomite units that have features resembling cap dolomites occur within the Cryogenian-Ediacaran succession of the Adelaide Geosyncline. While each of these dolomite ...detailed

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