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  • 2020-2024  (3)
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  • 1
    Online Resource
    Online Resource
    Millersville :Materials Research Forum LLC,
    Keywords: Electronic books.
    Description / Table of Contents: Due to their excellent magnetic characteristics, hard ferrites have many high-tech applications.
    Type of Medium: Online Resource
    Pages: 1 online resource (214 pages)
    Edition: 1st ed.
    ISBN: 9781644902318
    Series Statement: Materials Research Foundations Series ; v.142
    Language: English
    Note: Intro -- front-matter -- Table of Contents -- Preface -- 1 -- An Overview of Hard Ferrites: Types and Structures -- 1. Introduction -- 2. Classification and characteristics of hexaferrites -- 2.1 M-type hexaferrite -- 2.2 Z-type hexaferrite -- 2.3 Y-type hexaferrite -- 2.4 W-type hexaferrite -- 2.5 X-type hexaferrite -- 2.6 U-type hexaferrite -- 3. A brief description of the solid-state chemistry of hexaferrites -- 4. Approaches for better understanding of crystal structure of hexaferrites -- 4.1 Spinel based model -- 4.2 S/R/T blocks based model -- 5. Crystal structure of hexaferrites -- 5.1 M-type hexaferrite -- 5.2 W-type hexaferrite -- 5.3 X-type hexaferrite -- 5.4 Y-type hexaferrite -- 5.5 Z-type hexaferrite -- 5.6 U-type hexaferrite -- 6. Applications of hexaferrites -- Concluding Remarks -- References -- 2 -- Recent Advances in Processing of Hard Ferrites -- 1. Introduction -- 2. Fabrication of hard ferrites nanoparticles -- 2.1 Dry synthesis methods -- 2.1.1 Combustion method -- 2.1.2 Solid-state method -- 2.2 Wet synthesis method -- 2.2.1 Co-precipitation method -- 2.2.2 Sol-gel method -- 2.2.3 Spray pyrolysis method -- 2.2.4 Microwave-assisted combustion method -- 2.2.5 Microemulsion method -- 2.2.6 Citrate precursor method -- 2.2.7 Thermal decomposition method -- 2.2.8 Hydrothermal method -- 2.2.9 Reverse micelle method -- 2.2.10 Polyol method -- 2.2.11 Spray drying method -- 2.2.12 Sonochemical method -- 3. Comparision of synthesis methodologies -- Conclusion -- References -- 3 -- Effect of Substitution on the Dielectric and Magnetic Properties of BaFe12O19 -- 1. Introduction -- 1.1 Magnetic properties and morphology of copper-substituted barium hexaferrites -- 1.2 Effect of Co-Ti substitution on magnetic properties of nanocrystalline BaFe12O19. , 1.3 Effect of rare-earth materials substitution on the micro structural and magnetic properties of BaFe12O19 -- 1.4 The effect of Nb substitution on magnetic properties of BaFe12O19 nano hexaferrites -- 1.5 Magnetic properties of Cu and Al doped nano BaFe12O19 -- Conclusion -- References -- 4 -- Effect of Substitution on the Electric and Magnetic Properties of SrFe12O19 Hexa Hard Ferrites -- 1. Introduction -- 2. Synthesis technique for hexagonal hard ferrites -- 2.1 Standard ceramic techniques -- 2.2 Co-precipitation -- 2.3 Sol-Gel -- 3. Magnetism in hexagonal ferrites -- 4. Summary of hexagonal ferrites magnetic properties -- 5. Strontium hexa ferrites (SrM) -- 6. Effect of substitution on magnetic properties of SrFe12O19 hexa hard ferrite -- 6.1 Substituted strontium hexaferrite (SrM) -- 6.2 Magnetic properties -- 7. Magneto-dielectric properties -- 7.1 Dielectric properties -- 7.2 Magneto dielectric properties -- 8. Applications of hexagonal hard ferrites -- 8.1 Advanced ceramic materials for microwave and millimeter wave engineering -- Conclusion -- Future outlook -- References -- 5 -- Hard Ferrites for Permanent Magnets -- 1. Introduction -- 2. Structure, properties, and characteristics of hard ferrites -- 3. Generation of commerciallyavailable permanent magnets -- 3.1 Carbon steel magnets -- 3.2 Alcino magnets -- 3.3 Sm-Co magnets -- 3.4 Nd-Fe-B magnets -- 3.5 Hexaferrite/ferrite based magnets -- 4. Tasks for improving the hard ferrite-based magnets -- 5. Parameters responsible for improving the performance of the hard ferrites for their utilization in permanent magnets application -- 5.1 Influence of size at the nanoscale -- 5.2 Influence of the shape (Morphology) -- 5.3 Fabrication techniques for the preparation of hard ferrite-based nanomaterials -- 5.3.1 One dimensional nanostructure. , 5.4 Controlling substitution in the structure of hard ferrites -- 5.4.1 Enhancing magnetization (Ms) by substitution -- 5.4.2 Doing substitution in hexaferrites with large anisotropy and coercive field -- Concluding remarks -- References -- 6 -- Hard Ferrites for High Frequency Antenna Applications -- 1. Introduction -- 1.1 Ferrites for antenna application -- 2. Synthesis of hard ferries for antenna applications -- 2.1 Various synthesis methods -- 2.1.1 Ceramic powder milling method -- 2.1.2 Reaction in solid state method -- 2.1.3 Chemical coprecipitation method -- 2.1.4 Sol gel synthesis method -- 2.1.5 Temperature specific combustion synthesis -- 2.1.6 Hydrothermal synthesis method -- 2.1.7 Wet chemical method -- 2.1.8 Microemulsions method -- 3. Different compositions of hard ferrites for antenna applications -- 4. Factors affecting the performance of antenna -- 4.1 Size -- 4.2 Losses in dielectric material -- 4.3 The loss in propagation -- 4.4 Return loss -- 4.5 Radiation efficiency -- 5. Artificial materials to improve efficiency -- 5.1 Use of substrate integrated waveguide (SIW) to reduce loss -- 6. Future prospects of antenna -- Conclusion -- References -- 7 -- Applications of Hard Ferrites in Memory Devices -- 1. Introduction -- 2. Classification of ferrites -- 2.1 Spinel ferrites -- 2.2 Garnet ferrites -- 2.3 Ortho ferrites -- 2.4 Hexagonal ferrites -- 3. Preparation methods for ferrites -- 4. Hard ferrites -- 4.1 Application of hard ferrites -- 4.1.1 Inductors -- 4.1.2 Power -- 4.1.3 EMI shielding -- 5. Hard ferrites for memory devices -- 5.1 Multiple state memory devices -- 5.2 Magnetic core memory -- Conclusion -- Acknowledgement -- References -- back-matter -- Keyword Index -- About the Editors.
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  • 2
    Publication Date: 2024-04-30
    Description: The application of stable oxygen isotopic ratio of surface dwelling Globigerinoides ruber (white variety) (δ¹⁸Oruber) to reconstruct past hydrological changes requires precise understanding of the effect of ambient parameters on δ¹⁸Oruber. The northern Indian Ocean, with huge freshwater influx and being a part of the Indo-Pacific Warm Pool, provides a unique setting to understand the effect of both the salinity and temperature on δ18Oruber. Here, we use a total of 400 surface samples (252 from this work and 148 from previous studies), covering the entire salinity end member region, to assess the effect of seawater salinity and temperature on δ¹⁸Oruber in the northern Indian Ocean. For δ¹⁸O analysis, 10-15 well preserved shells of Globigerinoides ruber white variety, were picked from 250-355 μm size range. The stable oxygen isotopic ratio was measured by using Finnigan MAT 253 isotope ratio mass spectrometer, coupled with Kiel IV automated carbonate preparation device. The precision of oxygen isotope measurements was better than 0.08‰. The analyzed surface δ¹⁸Oruber very well mimics the expected δ¹⁸O calcite estimated from the modern seawater parameters (temperature, salinity and seawater δ¹⁸O). We report a large diagenetic overprinting of δ18Oruber in the surface sediments with an increase of 0.18‰ per kilometer increase in water depth. The salinity exerts the major control on δ¹⁸Oruber (R2 = 0.63) in the northern Indian Ocean, with an increase of 0.29‰ per unit increase in salinity. The relationship between temperature and salinity corrected δ¹⁸Oruber (δ¹⁸Oruber - δ¹⁸Osw) in the northern Indian Ocean [T= -0.59*(δ¹⁸Oruber - δ¹⁸Osw) + 26.40] is different than reported previously based on the global compilation of plankton tow δ¹⁸Oruber data. The revised equations will help in better paleoclimatic reconstruction from the northern Indian Ocean.
    Keywords: 63KA; 905B; 93KL; A15558; A15612; AAS6GC-3; AAS6GC-6; AAS9_21; AAS9/21; AII15-596; AII15-597; AII15-612; All15-585; All15-586; All15-591; All15-592; Andaman Sea; Arabian Sea; BARP-9406; BARP-9407; BARP-9409; BARP-9412; BARP-9413; BARP-9415; BARP-9422; BARP-9426; BARP-9435; BARP-9437; BC; BC21WP7; BCR; Box corer; Box corer (Reineck); Core; CORE; DOD-200; DOD-201; DOD-204; DODO-197; Eastern Arabian Sea; Elevation of event; Event label; Foraminifera; GC; GEMINO I; Globigerinoides ruber; Globigerinoides ruber white, δ18O; Grab; GRAB; Gravity corer; Indian Ocean; IOE_143KK; KAL; Kasten corer; KL; KL-15, AS-03; KL-26, AS-02; KL-36, AS-04; KL-51, AS-07; KL-57, AS-08; KL-74, AS-12; KL-79; KL-87, AS-15; Latitude of event; Longitude of event; M5/3a; M5/3a_422QM; MAKRAN 2; Marion Dufresne (1972); Mass spectrometer MAT253; MD10; MD10-26; MD10-27; MD10-28; MD10-29; MD13; MD13-29; MD13-36; MD13-42; MD13-44; MD13-50; MD13-59; MD13-60; MD13-67; MD13-68; MD76-123; MD76-125; MD76-127; MD76-128; MD76-129; MD76-131; MD76-132; MD76-135; MD76-136; MD77-164; MD77-169; MD77-171; MD77-176; MD77-177; MD77-178; MD77-179; MD77-180; MD77-181; MD77-185; MD77-191; MD77-194; MD77-195; MD77-197; MD77-200; MD77-202; MD77-203; MD77-204; Meteor (1986); MUC; MultiCorer; NIOP_905; NIOP_929; NIOP-B0/C0; NIOP-C2; Northeastern Arabian Sea; northern Indian Ocean; ORKS_08; OSIRIS II; OSIRIS III; oxygen isotope; PAKOMIN; PC; Piston corer; Piston corer (BGR type); QM; Quantameter; RC12; RC12-328; RC12-329; RC12-331; RC12-339; RC12-340; RC12-341; RC12-343; RC12-344; RC12-347; RC14; RC14-35; RC14-36; RC14-37; RC14-39; RC17; RC17-126; RC9-155; RC9-161; RC9-162; Reference/source; Robert Conrad; RVG_167/1_3904; Sagar Kanya; Sample ID; sediment; Sindhu Sadhana; Sindhu Sankalp; Size fraction; SK117; SK117_SC_05; SK117_SC_08; SK117_SC_11; SK117_SC_12; SK117_SC_14; SK117_SC_15; SK117_SC_16; SK117_SC_17; SK117_SC_18; SK117_SC_19; SK117_SC_20; SK117_SC_23; SK117_SC_25; SK117_SC_26; SK117_SC_27; SK117_SC_30; SK117_SC_31; SK117_SC_32; SK117_SC_33; SK117_SC_34; SK117_SC_39; SK117_SC_40; SK117_SC_43; SK117_SC_44; SK117_SC_45; SK117_SC_46; SK117_SC_51; SK126-GC39; SK129-CR05; SK148-GC4; SK157_GC_12; SK157_GC_14; SK157_GC_20; SK157-GC04; SK157-GC18; SK168-GC01; SK17; SK175; SK175_GB_02; SK175_GB_102; SK175_GB_103; SK175_GB_105; SK175_GB_111; SK175_GB_113; SK175_GB_116; SK175_GB_117; SK175_GB_118; SK175_GB_119; SK175_GB_121; SK175_GB_122; SK175_GB_123; SK175_GB_125; SK175_GB_127; SK175_GB_128; SK175_GB_129; SK175_GB_14; SK175_GB_19; SK175_GB_26; SK175_GB_28; SK175_GB_29; SK175_GB_30; SK175_GB_31; SK175_GB_33; SK175_GB_41; SK175_GB_58; SK175_GB_59; SK175_GB_60; SK175_GB_76; SK175_GB_77; SK175_GB_83; SK175_GB_84; SK175_GB_85; SK175_GB_86; SK175_GB_87; SK175_GB_89; SK175_GB_90; SK175_GB_91; SK175_GB_92; SK175_GB_93; SK175_GB_94; SK175_GB_96; SK175_GB_98; SK175_GB_99; SK20-GC185; SK218_1; SK237; SK237_GC09; SK237_SC_03; SK237_SC_04; SK237_SC_05; SK237_SC_06; SK237_SC_07; SK237_SC_11; SK237_SC_12; SK237_SC_13; SK237_SC_14; SK237_SC_16; SK237_SC_21; SK237_SC_22; SK237_SC_23; SK237_SC_27; SK237_SC_29; SK237_SC_32; SK237_SC_33; SK237_SC_34; SK237_SC_36; SK237_SC_37; SK237_SC_42; SK237_SC_43; SK237_SC_44; SK237_SC_46; SK237_SC_47; SK308; SK308_MC-02; SK308_MC-03; SK308_MC-04; SK308_MC-05; SK308_MC-08; SK308_MC-12; SK308_MC-14; SK308_MC-16; SK308_MC-18; SK308_MC-19; SK308_MC-23; SK308_MC-35; SK308_MC-36; SK308_MC-37; SK308_MC-38; SK308_MC-39; SK308_MC-41; SK308_MC-43; SK308_MC-44; SK308_MC-45; SK308_MC-47; SK308_MC-51; SK308_MC-55; SK308_MC-58; SK308_MC-59; SK308_MC-61; SK308_MC-63; SK308_MC-64; SK308_MC-66; SK31_GC_11; SL-1; SL-4; SN-6; SO130; SO130_211KG; SO130_282KG; SO130_285MC; SO28; SO28-05KL; SO28-11KL; SO28-18KL; SO42; SO42-15KL; SO42-26KL; SO42-36KL; SO42-51KL; SO42-57KL; SO42-74KL; SO42-79KL; SO42-87KL; SO90; SO90_39KG; SO90_56KA; Sonne; Southeastern Arabian Sea; Southwestern Bay of Bengal; SPAC; Spade Corer; SS3827G; SSD004; SSD004_G-01; SSD004_G-02; SSD004_G-03; SSD004_G-04; SSD004_G-05; SSD004_MC-01; SSD004_MC-02; SSD004_MC-03; SSD004_MC-04; SSD004_MC-05; SSD004_MC-06; SSD004_MC-07; SSD004_MC-08; SSD004_MC-09; SSD004_MC-10; SSD004_MC-11; SSD004_MC-12; SSD004_MC-13; SSD004_MC-14; SSD004_MC-15; SSD004_MC-16; SSD004_MC-17; SSD004_MC-18; SSD004_MC-19; SSD004_MC-20; SSD004_MC-21; SSD004_MC-23; SSD004_MC-26; SSD004_MC-27; SSD004_MC-28; SSD004_MC-29; SSD004_MC-30; SSD004_MC-31; SSD004_MC-32; SSD004_MC-53; SSD004_MC-54; SSD004_MC-55; SSD004_MC-56; SSD004_MC-57; SSD004_MC-59; SSD004_MC-60; SSD055; SSD055_MC01; SSD055_MC02; SSD055_MC03; SSD055_MC04; SSD055_MC05; SSD055_MC06; SSD055_MC08; SSD055_MC09; SSD055_MC10; SSD055_MC11; SSD055_MC12; SSD067; SSD067_GR04; SSD067_GR05; SSD067_GR10; SSD067_GR11; SSD067_MC02; SSD067_MC04; SSD067_MC05; SSD067_MC06; SSD067_MC07; SSD067_MC08; SSD067_MC09; SSD067_MC10; SSD067_MC11; SSD067_MC12; SSD067_MC13; SSD067_MC14; SSD067_MC16; SSD067_MC17; SSD067_MC21; SSD067_MC22; SSD067_MC24; SSD067_MC26; SSD067_MC29; SSD067_MC30; SSD067_MC31; SSD067_MC32; SSD067_MC33; SSD067_MC34; SSD067_MC36; SSD067_MC37; SSD067_MC38; SSD067_MC41; SSD067_MC42; SSD067_MC43; SSD067_MC44; SSD067_MC45; SSD067_MC46; SSD067_MC47; SSD067_MC49; SSD067_MC50; SSD067_MC51; SSD067_MC53; SSD067_MC54; SSD067_MC55; SSD067_MC56; SSK35; SSK35_SPC-25; SSK35_SPC-26; SSK35_SPC-27; SSK35_SPC-28; SSK35_SPC-29; SSK35_SPC-32; SSK35_SPC-33; SSK35_SPC-34; SSK35_SPC-37; SSK35_SPC-39; SSK35_SPC-42; SSK35_SPC-43; SSK35_SPC-45; SSK98; SSK98_GR01; SSK98_GR02; SSK98_GR03; SSK98_GR04; SSK98_GR05; SSK98_GR06; SSK98_GR10; SSK98_SPC01; SSK98_SPC02; SSK98_SPC03; SSK98_SPC07; SSK98_SPC11; SSK98_SPC12; SSK98_SPC13; SSK98_SPC14; Surface; TN41_32MC; TN47_6GGC; Tyro; V14; V14-101; V14-103; V14-104; V14-106; V14-107; V14-108; V19; V19-176; V19-177; V19-178; V19-183; V19-185; V19-188; V29; V29-15; V29-19; V29-29; V29-30; V34; V34-80; V34-83; V34-85; V34-88; Vema; Western Bay of Bengal
    Type: Dataset
    Format: text/tab-separated-values, 1522 data points
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  • 3
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    Unknown
    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-09-12
    Description: The Himalayas which formed as a result of collision between the Indian and Eurasian plates has been a hotspot for great earthquakes. With an aim to understand the origin of seismicity in and around the northeastern state of Sikkim in India, 27 broadband seismic stations were deployed across the Sikkim Himalayas and Himalayan foreland basin (northern part of West Bengal). The continuous operation of the network since April 2019 to present day has enabled the acquisition of quality data with excellent azimuthal coverage. We have used local earthquakes (epicenter 〈 200km) detected by the network to study the seismotectonic activity of the region. Progressive relocation of these earthquakes using multiple algorithms facilitated in locating the hypocenters with great precision. We then employed full-waveform moment tensor inversion to obtain the fault plane solutions. Earthquakes concentrated in the central part of the study region are located in the upper crust along the dipping surface of the Main Himalayan Thrust. Whereas, earthquakes concentrated diagonally along the Dhubri-Chungthang Fault Zone are located at mid to lower crustal depths. These crustal earthquakes are observed to have a characteristic strike-slip mechanism. Further north of the study region, earthquakes with focal depths 〉 40km are observed to originate along an extensional plane as evidenced by the observed normal fault plane solutions. We plan to further investigate these spatially varying trends and determine its role in segmentation along the Himalayas. We will also integrate results from various studies to discern the geodynamic evolution of the Sikkim Himalayas.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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