Physical characteristics, composition and features of iron metal

Pure iron (99.97%), purified by electrolysis

Iron

- a malleable silver-white metal with high chemical reactivity: iron quickly corrodes at high temperatures or high humidity in the air. Iron burns in pure oxygen, and in a finely dispersed state it spontaneously ignites in air. Denoted by the symbol Fe (Latin Ferrum). One of the most common metals in the earth's crust (second place after aluminum).

1. Structure
2. Properties
3. Reserves and production
4. Origin
5. Application
6. Classification
7. Physical properties
8. Optical properties
9. Crystallographic properties

See also:

Aluminum

– structure and physical properties

STRUCTURE

Two modifications of the iron crystal lattice

Several polymorphic modifications have been established for iron, of which the high-temperature modification - γ-Fe (above 906°) forms a lattice of a face-centered cube of the Cu type (a0 = 3.63), and the low-temperature modification - the α-Fe lattice of a centered cube of the α-Fe type (a0 = 2.86). Depending on the heating temperature, iron can be found in three modifications, characterized by different crystal lattice structures:

1. In the temperature range from the lowest to 910 ° C - a-ferrite (alpha ferrite), which has a crystal lattice structure in the form of a centered cube;
2. In the temperature range from 910 to 1390°C - austenite, the crystal lattice of which has the structure of a face-centered cube;
3. In the temperature range from 1390 to 1535 ° C (melting point) - d-ferrite (delta ferrite). The crystal lattice of d-ferrite is the same as that of a-ferrite. The only difference between them is the different (larger for d-ferrite) distances between the atoms.

When liquid iron is cooled, primary crystals (crystallization centers) appear simultaneously at many points in the cooled volume. With subsequent cooling, new crystalline cells are built around each center until the entire supply of liquid metal is exhausted. The result is a granular structure of the metal. Each grain has a crystal lattice with a certain direction of its axes. With subsequent cooling of solid iron, during the transitions of d-ferrite to austenite and austenite to a-ferrite, new crystallization centers may appear with a corresponding change in grain size

Story

The history of iron goes back thousands of years. About 3500 years ago, as A. Azimov wrote,

“iron smelting technology was developed in the Caucasian foothills.”

Ultra-pure iron
The Hittite kingdom was located there. The warlike Hittites guarded the secret of smelting as closely as they could, which is why the price of iron was tens of times higher than the price of gold. Those who wielded iron weapons almost automatically emerged victorious in battles. And the wars were mainly fought over territories.

With the invention of welded weapons came the age of ferrous metal.

In peaceful life, iron tools had enough to do: cut down a hut, hew stone, plow a field.

PROPERTIES

Iron ore

In its pure form under normal conditions it is a solid. It has a silver-gray color and a pronounced metallic luster. The mechanical properties of iron include its level of hardness on the Mohs scale. It is equal to four (average). Iron has good electrical and thermal conductivity. The last feature can be felt by touching an iron object in a cold room. Because this material conducts heat quickly, it removes most of it from your skin in a short period of time, which is why you feel cold. If you touch, for example, wood, you will notice that its thermal conductivity is much lower. The physical properties of iron include its melting and boiling points. The first is 1539 degrees Celsius, the second is 2860 degrees Celsius. We can conclude that the characteristic properties of iron are good ductility and fusibility. But that's not all. Also, the physical properties of iron include its ferromagnetism. What it is? Iron, whose magnetic properties we can observe in practical examples every day, is the only metal that has such a unique distinctive feature. This is explained by the fact that this material is capable of magnetization under the influence of a magnetic field. And after the end of the action of the latter, the iron, the magnetic properties of which have just been formed, remains a magnet for a long time. This phenomenon can be explained by the fact that in the structure of this metal there are many free electrons that are able to move.

Melting point table

It is important for anyone involved in the metallurgical industry, whether a welder, foundry worker, smelter or jeweler, to know the temperatures at which the materials they work with melt. The table below shows the melting points of the most common substances.

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Table of melting temperatures of metals and alloys

In addition to the melting table, there are many other supporting materials. For example, the answer to the question what is the boiling point of iron lies in the table of boiling substances. In addition to boiling, metals have a number of other physical properties, such as strength.

RESERVES AND PRODUCTION

Iron is one of the most common elements in the solar system, especially on the terrestrial planets, in particular on Earth. A significant part of the iron of the terrestrial planets is located in the cores of the planets, where its content is estimated to be about 90%. The iron content in the earth's crust is 5%, and in the mantle about 12%.

Iron

Iron is quite widespread in the earth's crust - it accounts for about 4.1% of the mass of the earth's crust (4th place among all elements, 2nd among metals). In the mantle and earth's crust, iron is concentrated mainly in silicates, while its content is significant in basic and ultrabasic rocks, and low in acidic and intermediate rocks. A large number of ores and minerals containing iron are known. Of greatest practical importance are red iron ore (hematite, Fe2O3; contains up to 70% Fe), magnetic iron ore (magnetite, FeFe2O4, Fe3O4; contains 72.4% Fe), brown iron ore or limonite (goethite and hydrogoethite, respectively FeOOH and FeOOH nH2O ). Goethite and hydrogoethite are most often found in weathering crusts, forming so-called “iron hats”, the thickness of which reaches several hundred meters. They can also be of sedimentary origin, falling out of colloidal solutions in lakes or coastal areas of the seas. In this case, oolitic, or legume, iron ores are formed. Vivianite Fe3(PO4)2·8H2O is often found in them, forming black elongated crystals and radial aggregates. The iron content in sea water is 1·10−5-1·10−8%. In industry, iron is obtained from iron ore, mainly from hematite (Fe2O3) and magnetite (FeO·Fe2O3). There are various ways to extract iron from ores. The most common is the domain process. The first stage of production is the reduction of iron with carbon in a blast furnace at a temperature of 2000 °C. In a blast furnace, carbon in the form of coke, iron ore in the form of agglomerate or pellets, and flux (such as limestone) are fed from above, and are met by a stream of forced hot air from below. In addition to the blast furnace process, the process of direct iron production is common. In this case, pre-crushed ore is mixed with special clay, forming pellets. The pellets are fired and treated in a shaft furnace with hot methane conversion products, which contain hydrogen. Hydrogen easily reduces iron without contaminating the iron with impurities such as sulfur and phosphorus, which are common impurities in coal. Iron is obtained in solid form and is subsequently melted in electric furnaces. Chemically pure iron is obtained by electrolysis of solutions of its salts.

Biological effects

For humans, iron as a microelement (0.02%) is of special importance: it regulates cellular respiration and is part of the blood.

Health Importance

The adult human body contains 3.5 grams of iron. Of these, three quarters are included in the hemoglobin of the blood, the rest is distributed to other structures of the body.

Lack of microelement causes anemia in humans or animals, chlorosis in plants.

Nutrition

Iron is supplied to the body by food.

The foods richest in micronutrients are found in all food groups:

• Bread, cereals.
• Liver, meat.
• Eggs.
• Beets, leafy greens.
• Legumes.
• Dried fruits, nuts, seeds.

Foods contain different types of iron: heme and non-heme. Heme contains the “animal” assortment, while non-heme contains the plant variety.

Need

Daily iron requirement (mg):

• children – 4-18;
• women – 18;
• men – 10.

During pregnancy, the norm doubles. More is required for anemic people and donors.

It is easier for the body to absorb heme iron, so vegans or vegetarians need 30-33 mg daily.

The danger of oversupply

However, an excess of the substance is not welcome, since it “suppresses” the formation of antioxidants in the body.

The use of water with an iron content of more than 2 mg per liter is undesirable. If the metal content is more than 200 mg, the water is toxic.

According to Russian standards, a liter of water should contain no more than 0.3 mg of iron.

ORIGIN

Native iron

Origin telluric (terrestrial) iron is rarely found in basalt lavas (Uifak, Disko Island, off the western coast of Greenland, near Kassel, Germany). At both locations, pyrrhotite (Fe1-xS) and cohenite (Fe3C) are associated with it, which is explained by both the reduction by carbon (including from the host rocks) and the decomposition of carbonyl complexes such as Fe(CO)n. In microscopic grains, it has more than once been established in altered (serpentinized) ultrabasic rocks, also in paragenesis with pyrrhotite, sometimes with magnetite, due to which it arises during reduction reactions. Very rarely found in the oxidation zone of ore deposits, during the formation of swamp ores. Findings have been recorded in sedimentary rocks associated with the reduction of iron compounds with hydrogen and hydrocarbons. Almost pure iron was found in lunar soil, which is associated with both meteorite falls and magmatic processes. Finally, two classes of meteorites - stony-iron and iron - contain natural iron alloys as a rock-forming component.

When was it open

The history of man's acquaintance with iron begins with Space. Judging by the ancient (for example, ancient Egyptian) names of the element, it was meteorite iron. Hittite texts refer to him as "fallen from the sky."

Man has been using metal for 6 thousand years.

Archaeologists have unearthed tools used by the ancient Sumerians and Egyptians. They are made from meteorite iron.

Iron products conquered the world. The poems of Homer's Iliad are dedicated to metal, and it is mentioned by Aristotle and Strabo.

The ancient name of iron is due to its celestial origin: “sider” (“starry”).

Scientists are constantly exploring the potential of metal. Thus, in 1868, the Russian scientist D.K. Chernov discovered crystalline modifications of matter.

APPLICATION

Iron ring

Iron is one of the most used metals, accounting for up to 95% of global metallurgical production. Iron is the main component of steels and cast irons - the most important structural materials. Iron can be part of alloys based on other metals - for example, nickel. Magnetic iron oxide (magnetite) is an important material in the production of long-term computer memory devices: hard drives, floppy disks, etc. Ultrafine magnetite powder is used in many black and white laser printers mixed with polymer granules as a toner. This uses both the black color of the magnetite and its ability to stick to the magnetized transfer roller. The unique ferromagnetic properties of a number of iron-based alloys contribute to their widespread use in electrical engineering for magnetic cores of transformers and electric motors. Iron(III) chloride (ferric chloride) is used in amateur radio practice for etching printed circuit boards. Ferrous sulfate heptate (ferrous sulfate) mixed with copper sulfate is used to combat harmful fungi in gardening and construction. Iron is used as an anode in iron-nickel batteries and iron-air batteries. Aqueous solutions of ferrous and ferric chlorides, as well as its sulfates, are used as coagulants in the purification processes of natural and waste water in the water treatment of industrial enterprises.

Iron – Fe

Alloys

Markings help to navigate the sea of ​​iron alloys (steels, cast irons). It will help determine the composition of the alloy, the amount of carbon and alloying elements, and distinguish their properties.

A general description can be given by chemical composition: these are carbon and alloy steels.

Steels are divided by application:

PHYSICAL PROPERTIES

Crystallographic characteristics

Cubic system

Class hexoctahedral

Crystal structure of native iron – Body-centered cubic lattice (for low-temperature modification)

Form of being in nature

The appearance of crystals. Only microscopically small ferrite crystals are known.

Twins in native iron at (111) with a fusion plane (211), often repeated.

Aggregates.

Grains, scales, wire-like sticks, curved ribbons, impregnations in rocks, sometimes large continuous deposits weighing up to several tons (ferrite), often intergrown with cohenite.

Chemical composition

Telluric iron contains impurities of nickel (Ni) 0.6-2%, cobalt (Co) up to 0.3%, copper (Cu) up to 0.4%, platinum (Pt) up to 0.1%, carbon. Native iron usually contains Ni in solid solution. The composition of individual varieties has not been precisely established; the analyzes are mostly old, performed on material not verified by mineragraphic and x-ray studies. Minor admixtures of Co, Cu, S, C, Mn, P, Pt, As, Ge have been identified, partly associated, apparently, with a mechanical admixture of cohenite; the presence of gas inclusions (CO and CO2) was noted.

Varieties

Ferrite (Vernadsky, 1912) is the purest, almost Ni-free native iron. Awaruite - awaruite (Skei, 1885) 6 -(Ni, Fe). Native nickel-iron with a high Ni content (Ni: Fe from 4: 1 to 2: 1). Hardness. 5. Density 8.1. It resembles polyxene in luster and color. In reflected light, pure white or light cream, isotropic, highly reflective. Named for its location in Avarua Bay (New Zealand), where it is associated with gold, platinum, cassiterite, chromite, and magnetite. It is found as a secondary mineral in peridotites that have undergone serpentinization, serpentinites, trachytes, and quartz porphyries. Varieties of nickel-iron of terrestrial origin close to or identical to awaruite, found in placers and in serpentinized peridotites, are described under the names: josephinite (Melville, 1892), souesite-souesite (Hofman, 1905), octibbehite (Taylor, 1905). 1857), catarinite - satarinite (Damur, 1877). Under the name bobrovkite (Vysotsky, 1913), nickel-iron (iron-nickel) is described, found in the form of fine-scaled grains together with platinum (polyxene) in the placers of M. Bobrovka (Ural). Contains Ni 71.93, Fe 28.07, as well as Co, Mn.

B. Meteoric iron

Kamacite – Kamacite – nickel iron (6-9% Ni). The name kamacite comes from the Greek - beam, rod (Reichenbach, 1861),

A synonym for kamacite is beam iron, taenite is band iron (Reichenbach, 1861), edmonsonite (Flight, 1882). Plessite (Reichenbach, 1861) is a fine mixture of kamacite and taenite.

Taenite – Taenite – nickel-iron (up to 48% Ni), taenite – from Taivia - ribbon, strip (Reichenbach, 1861).

For taenite of the Fe2Ni composition, the following names have been proposed: nikdiferrite (Chirvinsky, 1928), orthotenite (Badhu, 1936) and chirvinite (Astapovich, 1950); a compound of this composition is established in the Fe-Ni system. Metakamacite is a metastable a-modification of pickled iron, and, in addition, a granular variety of plessite (Owen, 1940). Metatenite is taenite with an admixture of kamacite (Badhyo, 1936).

Native iron of cosmic origin makes up the mass of iron meteorites. Found in most stony meteorites. Forms:

a) a solid mass of a meteorite;

b) a spongy mass in which grains of olivine or other silicates are immersed;

c) grains and scales scattered throughout the meteorite;

d) separate crystalline individuals with numerous twin plates. Kamacite and taenite are always closely intergrown. Iron meteorites from the octahedrite group are characterized by systems of intersecting stripes, which are called Widmanstätten figures: individual stripes consist of kamacite with taenite rims, with plessite between the intersecting stripes. Widmanstätten figures arise as a result of the decomposition of a solid solution of γ-iron and nickel. In intergrowths of kamacite and taenite, the plane of the rhombic dodecahedron (110) of kamacite is parallel to the plane of the octahedron (111) of taenite, which is explained by their structural similarity.

Strength of metals

In addition to the ability to transition from a solid to a liquid state, one of the important properties of a material is its strength - the ability of a solid body to resist destruction and irreversible changes in shape. The main indicator of strength is the resistance that occurs when a pre-annealed workpiece breaks. The concept of strength does not apply to mercury because it is in a liquid state. The designation of strength is adopted in MPa - Mega Pascals.

There are the following strength groups of metals:

• Fragile. Their resistance does not exceed 50MPa. These include tin, lead, soft-alkaline metals
• Durable, 50−500 MPa. Copper, aluminum, iron, titanium. Materials of this group are the basis of many structural alloys.
• High strength, over 500 MPa. For example, molybdenum and tungsten.

Metal strength table