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Magnetics
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Introduction
The M-type hard ferrites have hexagonal crystal structure. The formula of hard ferrites can be generally represented as (MeO.6Fe2O3), where Me is divalent metal such as Sr, Ba, and Pb or a mixture of these [12]. Barium hexaferrites (BaFe12O19) with a magnetoplumbite structure are well known as hard magnetic materials which are based on iron oxides. Hexagonal ferrites are referred to as hard because the direction of magnetization cannot be changed easily to another axis [].Barium ferrite possesses relatively high Curie temperature, coercive force and magnetic anisotropy field, as well as its excellent chemical stability and corrosion resistivity [].The magnetic and dielectric characteristics of hexagonal ferrites strongly depend
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The weight ratio of balls to milled material was 5:1. The mechanically alloyed powders were cold pressed into pellets with a diameter of 12 mm. Cold pressed samples were annealed for 1 h at the temperatures of 800 ◦C, 900 ◦C, 1150 ◦C under air. The crystalline phase formation of barium hexaferrite, magnetite and composites powder was further investigated with X-ray diffraction (XRD) spectra using an X-Pert PANalytical diffractometer (PW3050/60) using CuKα radiation in the range 20° to 80°, the magnetization vs magnetic field (M-H) plot of barium hexaferrite was obtained using a vibrating sample magnetometer (VSM) and the average particle size was obtained from the scanning transmission electron microscope (STEM). The Room temperature
X-ray Photoelectron spectroscopy (XPS) studied by (S/N: 10001,
Prevac, Poland) spectra were taken with AlKα (hν¼51,486.6 eV) radiation and a hemispherical energy analyzer. The Rietveld analysis was performed applying DBWS-9807 program that is an update version for Rietveld refinement with PC and mainframe computers.
Results and discussion
Figure 1 shows the XRD patterns of the BaCO3
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Fig. 2b shows the deconvolution of Fe spectrum done using origin-8.5 software considering Gaussian function. The fitted peaks at 711.2 eV and at 713.6 eV of main 2p3/2 peak, corresponds to Fe2þ and Fe3þ oxidation state [28]. The satellite peak (718.8 eV) and 2p1/2 peak at 725.4 eV are indicating the presence of Fe3þ
[29,30]. The electronic state of Fe present in BaFe12O19 was determined through X-ray photoelectron spectroscopy. The survey spectrum
(Fig. 3(a)) indicates the presence of Ba, Fe and O peaks. The C 1s peak (284.5 eV) was used as the reference for charge correction.
Fig. 3(b) shows the deconvolution of Fe spectrum done using CASA
XPS software with a mixture of Gaussian and Lorentzian function and Shirley function for background. The 2p3/2 peak at 710.5 eV corresponds to Fe2O3 (Fe3þ) [19] and the satellite peak (718.8 eV) is 8.2 eV from the main 2p3/2 peak (710.5 eV), indicating the presence of Fe3þ. Moreover, the peak at 714.1 eV corresponds to surface peak [20], which can be attributed to the reduction in coordination of Fe (i.e. in hexaferrite, Fe is present in five nonequivalent crystallographic sites, three octahedral, one tetrahedral and one site surrounded by five oxygen atoms forming a
Procedure: Anisole (0.35mL, 0.0378mol) was obtained and placed in a pre-weighed 25 mL round bottom flask, along with 2.5 mL of glacial acetic acid and a magnetic stir bar. Then the reaction apparatus was assembled, the dry tube was charged with conc. sodium bi sulfate, the 25 mL round bottom was attached to the apparatus, and 5 mL of Br2/HBr mixture was obtained and placed in the round bottom. The reaction took place for 20 minutes. An orange liquid was obtained and placed in a 125 mL Erlenmeyer flask along with 25 mL of water and 2.5 mL of conc. Sodium bisulfate soln. The solution was then placed in an ice bath to precipitate and then the solid product was filter in a Buchner funnel. These crystals were then re-dissolved minimum amount of hot solvent (heptane) and recrystallized. Once a dry product was obtained, a melting point was established (2,4-Dibromoanisol mp 55-58 C) and percent yield was established (52%).
Gadolinium and its performance were limited by the use of passive regenerators and heat exchangers in the refrigeration cycle [25]. So, a magnetic refrigeration device must utilize a regenerative process to produce a large enough temperature span to be useful for refrigeration purposes [26].
In order to understand the controversy of fluoride, one must know the background . Fluoride is the ionic form of the element fluorine, an element abundant in the earth's crust (Borso 23). Fluoride is shown that is
Boron is one of the many elements on the periodic table. Its atomic number is five and its symbol is the letter B. Boron’s atomic weight is 10.811. It is a solid at room temperature. The group number for Boron is 13 and the periodic number for Boron is 2. It is also in the p block. Its element category is a metalloid. Boron came from the Arabic word Buraq and the Persian word Burah, which are both meanings for the material called “Borax.” Boron is a tough element – very hard, and very resistant to heat. In its crystalline form it is the second hardest of all the elements on the mohs scale – only carbon (diamond) is harder. Only 11 elements have higher melting points than boron: these are C, W, Re, Os, Ta, Mo, Nb, Ir, Ru, Hf, and Tc. Boron was discovered by Joseph Louis Gay-Lussac and Louis Jacques Thenard on June 30th on 1808. This element has contributed to chemistry enormously over the years. This is the history of Boron and how it has affected chemistry.
Beryllium is a highly toxic metal and if exposed to it, at or above the threshold values, it can lead to a chronic beryllium disease (CBD) (i.e. berylliosis) or an acute beryllium disease. Toxic exposure to beryllium is most often thru an inhalation pathway. Beryllium has a variety of effects. Some beryllium combines with a protein and is deposited in the liver, spleen and kidneys, but the beryllium when bound with a biological protein, a hapten, can result in the chronic form of the disease which is believed to be a delayed hypersensitivity immune response. The major toxicological effects of beryllium are on the respiratory tract,specifically the lungs and their alveoli.
Pure iron has a hardness that ranges from 4 to 5. It is soft and ductile. Iron can be easily magnetized at ordinary temperatures and at 790°C the magnetic property disappears. Pure iron melts at about 1535°C, boils at 2750°C, and has a specific gravity of 7.86. Chemically, iron is an active metal. When exposed to humid air, iron forms a reddish-brown, flaky, decay known as rust.
The basis for the understanding of the heat treatment of steels is the Fe-C phase diagram. Because it is well explained in earlier volumes of Metals Handbook and in many elementary textbooks, the stable iron-graphite diagram and the metastable Fe-Fe3 C diagram. The stable condition usually takes a very long time to develop, especially in the low-temperature and low-carbon range, and therefore the metastable diagram is of more interest. The Fe-C diagram shows which phases are to be expected at equilibrium for different combinations of carbon concentration and temperature. We distinguish at the low-carbon and ferrite, which can at most dissolve 0.028 wt% C at 727 oC and austenite which can dissolve 2.11 wt% C at 1148 oC. At the carbon-rich side we find cementite. Of less interest, except for highly alloyed steels, is the d-ferrite existing at the highest temperatures. Between the single-phase fields are found regions with mixtures of two phases, such as ferrite + cementite, austenite + cementite, and ferrite + austenite. At the highest temperatures, the liquid phase field can be found and below this are the two phase fields liquid + austenite, liquid + cementite, and liquid + d-ferrite. In heat treating of steels the liquid phase is always avoided. Some important boundaries at single-phase fields have been given special names. These include: the carbon content at which the minimum austenite temperature is attained is called the eutectoid carbon content. The ferrite-cementite phase mixture of this composition formed during cooling has a characteristic appearance and is called pearlite and can be treated as a microstructural entity or microconstituent. It is an aggregate of alternating ferrite and cementite particles dispersed with a ferrite matrix after extended holding close to A1. The Fe-C diagram is of experimental origin. The knowledge of the thermodynamic principles and modern thermodynamic data now permits very accurate calculations of this diagram.
Figure 1: The hexacyanoferrate iron (III) ion: contains 6 ligands which are bound to the central metal therefore has a coordination number of 6 (n=6¬). (Hussain,2007) [13]
The precipitateswere collected through a glass funnel filter and then washed several times by methanol and acetone. Metallization and patterning Measurement of the specific electrical resistance with the fourpoint probe technique requires samples with uniform thickness, which can be made by spin coating. Ag NPs were
V. Amarnath, D. C. Anthony, K. Amarnath, W. M. Valentine, L. A. Wetterau, D. G. J. Org. Chem. 1991, 56, p. 6924-6931.
When the generated fields pass through magnetic materials which themselves contribute internal magnetic fields, ambiguities can arise about what part of the field comes from the external currents and what comes from the material itself. It is common to define another magnetic field quantity, usually called the "magnetic field strength" designated by H. It can be defined by the relationship, H = B0/μ0 = B/μ0 – M, and has the value of unambiguously designating the driving magnetic influence from external currents in a material, independent of the material's magnetic response. The relationship for B can be written in the equivalent form, B = μ0(H + M), H and M will have the same units, amperes/meter. To further distinguish B from H, B is sometimes called the magnetic flux density or the magnetic
Fluorite was named by Carlo Antonio Galeani Napione in the year 1797. Through the years it has been known by many names, clax fluorata and spatum vitreum to name a few. Today we simply call it fluorite. Its name comes from the Latin word fluere, which means “to flow”, because of its low melting point when compared to other rocks and elements Napione collected with raw samples of fluorite. It is a halide mineral comprised of calcium and fluoride (CaF2). Small amounts of yttrium and cerium have been known to act as replacements for the calcium. Fluorite is in the isometric crystal system in the hexoctahedral class 4⁄m 3 ̅ 2⁄m which means it has a relatively high symmetry. It is usually found in cubic habit, though it can also be found as octahedral, dodecahedral, or massive aggregates. Penetration twinning is also common among fluorite crystals [INSERT PIC HERE].
Magnets refer to the internal alignment of the metals component atoms, most metallic objects can be turned into a magnet by a strong jolt or set of jolts of a very strong magnet to be suddenly attached and detached from the piece of steel you want to be permanently magnetized, what this does is more suddenly and strongly moves the internal component atoms into order, where they will stay. There are other methods in which ore can be magnetized such as with the earth and how it spins in its orbit and magnetizes the naturally occurring lodestone which is more complicated. In order for a metal object to be transformed into a magnet its internal component atoms must be aligned properly - all heading in the same direction like in the picture below, otherwise it will be weak or will not work at all!
The various types of magnets are used in countless facets in everyday life. Thousands of industries, including automotive, electronics, aerospace, craft, manufacturing, printing, therapeutic and mining utilise magnets so that their machineries, tools and equipment can properly function.