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Eng. Andrei ALEXANDRU-DINU

Assistant Researcher

Data Analysis Fluorescence Spectroscopy Magnetic

2010-2014 : National College Spiru Haret, Ploiesti (Romania)

2014-2018 : Bachelor's Degree - Politehnica University  of Bucharest, Faculty of Applied Sciences, Physics Engineering, Bucuresti (Romania)

2018-2020 : Master Degree - Politehnica University  of Bucharest, Faculty of Applied Sciences, Engineering and Applications of Lasers and Accelerators, Bucuresti (Romania)

2020-present : PhD - University of Bucharest, Faculty of Physics, Condensed Matter and Materials Physics, Magurele (Romania)

2018-present : Assistant Researcher - National Institute of Materials Physics, Laboratory of Magnetism and Superconductivity, Magurele (Romania)

My research interests are in the area of magnetic materials, in particular, the design and the morpho-structural characterization of iron oxides and the analysis of their magnetic properties by magnetometers and Mossbauer Spectroscopy. I am also interested in intermetallics alloys, synthesized by non-equilibrium techniques such as Spark Plasma Sintering, Melt Spinning and Optical Floating Zone. My research in this area mainly contributes to the literature on magnetic materials characterization but also to the fundamental approach on this kind of systems.

X-Ray Fluorescence, Magnetic Materials, Materials Science, Materials Engineering, Magnetic Measurements, Melt Spinning, Intermetallic Alloys, Oxides

In the present studies, I'm focused on three types of compounds: 1) Iron intermetallics with and without rare earth elements (Ex: GdFeB, FeSiB). As an example, in the last years, amorphous intermetallics containing rare earth elements and transition metals, scientists discovered they have different characteristics depending on the ionic anisotropy of the rare earth element.

                                                                                                                      2) Aluminosilicates presenting clusterization processes and rare earth based oxides (Ex: Ancient Roman ceramics or composites, RIG - rare earth iron garnets). As an example, a complex archaeometric characterization combined with materials characterization techniques (XRD, XRF, SEM, Mossbauer Spectroscopy and others) on a foreign material (Roman brick - 2nd to 3rd century AD), had led to the understanding of the historical theories but also of the ancient materials and how this affected the society.

                                                                                                                      3) Nanocomposites (borides or carbides containing transition metals or rare earths). The research is focused on the investigation of the local properties of the nanostructures and nanocomposites of different borides/carbides systems (Ex: High magnetic order temperature). 

In resume, my research is based on different classes of materials containing rare earth elements or transition metals which allows the getting of multi-functional properties. In particular, the focus is set on the local nanometric level of effects and events followed by the extrapolation to the macro-scales needed for the practical applications.

1

Cation distribution and its magnetic implications in gadolinium-iron garnets for an enhanced control of compensation temperature

Bartha, C; Locovei, C; Alexandru-Dinu, A; Comanescu, C; Grigoroscuta, MA; Kuncser, A; Iacob, N; Galatanu, M; Leca, A; Badica, P; Kuncser, V

2025 OCT 16 2025, PHYSICAL CHEMISTRY CHEMICAL PHYSICS

DOI: 10.1039/d5cp02696b

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The precise control of the magnetic compensation temperature (theta c) in ferrimagnetic garnets is essential for the development of cutting-edge ultrafast customizable spintronic devices. In this work we demonstrate how fine variation in stoichiometry and cation distribution in iron gadolinium garnets significanty influences theta c. Two samples of Gd3Fe5O112 garnets synthesized via a new hydrothermal method and a conventional solid-state reaction, respectively, were considered. The complex study was carried out using a complex approach combining X-ray diffraction, magnetometry, and M & ouml;ssbauer spectroscopy. Atomic-scale analysis revealed with unprecedent accuracy a cationic inversion between Fe3+ ang Gd3+ at octahedral and dodecahedral sites in both samples, and their chemical compositions were determined as Gd2.70Fe4.76O11.9 and Gd2.96Fe4.68O11.5, respectively. These local rearrangements have been shown to have a consistent influence on theta c (290 K and 317 K, respectively) around room temperature, emphasizing the high sensitivity of exchange interactions to internal atomic order. Results clearly illustrate the strong correlation between the processing, atomic configuration and macroscopic magnetic behavior, establishing a new paradigm for the design of garnet-based materials with tunable theta c. The strategy for the accurate determination of cation inversion illustrated in this work exhibits great potential in guiding material innovations for next-generation spintronics.

2 Open Access

Microstructure and coupling mechanisms in MnBi-FeSiB nanocomposites obtained by spark plasma sintering

Alexandru-Dinu, A; Locovei, C; Bartha, C; Grigoroscuta, MA; Burdusel, M; Kuncser, A; Palade, P; Schinteie, G; Iacob, N; Lu, W; Batalu, D; Badica, P; Kuncser, V

JUL 24 2024, SCIENTIFIC REPORTS, 14, 17029

DOI: 10.1038/s41598-024-67353-7

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Fabrication and extensive characterization of hard-soft nanocomposites composed of hard magnetic low-temperature phase LTP-MnBi and amorphous Fe70Si10B20 soft magnetic phase for bulk magnets are reported. Samples with compositions Mn55Bi45 + x center dot(Fe70Si10B20) (x = 0, 3, 5, 10, 20 wt.%) were prepared by spark plasma sintering of powder mixtures. Characterization has been performed by X-ray diffraction, scanning and transmission electron microscopy, magnetometry and Fe-57 Mossbauer spectroscopy. It was shown that samples contain crystallized and nanometric LTP-MnBi phases with various elemental compositions depending on the degree of Bi clustering. Complex correlations between starting compositions, processes during fabrication, and functional magnetic characteristics were observed. Unexpected special situations of the relation between microstructure and magnetic coupling mechanisms are discovered. Exchange spring effects of different strengths occur, being very sensitive to morpho-structural and compositional features, which in turn are controlled by processing conditions. An in-depth analysis of related microscopic characteristics is provided. Results of this work suggest that fabrication by powder metallurgy routes, such as spark plasma sintering of hard and soft magnetic powder mixtures, of MnBi-based composites with exchange spring phenomena have a high potential in designing and optimization of suitable materials with tunable magnetic properties towards rare-earth-free permanent magnet applications.

3

Two Roman Glass Furnaces Discovered at Resca-Romula (Romania)

Negru, M; Badica, P; Alexandru-Dinu, A; Galatanu, M; Kuncser, A; Patroi, D; Artene, I

OCT 1 2023, AMERICAN JOURNAL OF ARCHAEOLOGY, 127

DOI: 10.1086/726009

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Romula (today Resca, Dobrosloveni Village, Romania) was the largest urban and economic center of Dacia Inferior (Malvensis), a Roman province located in the north of the Lower Danube region. In this context, the city market included workshops for the production of ceramic, metal, stone, bone, and glass objects. In 2013, 2015, and 2018, during excavations of the former Roman city, two rectangular glass furnaces were discovered. One has only one chamber, the other has two chambers. A melted glass layer was found on the walls of furnace no. 1, as well as in one room of furnace no. 2. Broken fragments of glass were also found in both. The furnaces are located in the central area of the Roman city. The evidence suggests that the furnaces belong to secondary glass workshops. The glass may have arrived in raw form, where it was remelted and processed. The discovery of these furnaces contributes to the growing body of evidence for Roman glass production around the empire.1

4 Open Access

Mud and burnt Roman bricks from Romula

Badica, P; Alexandru-Dinu, A; Grigoroscuta, MA; Burdusel, M; Aldica, GV; Sandu, V; Bartha, C; Polosan, S; Galatanu, A; Kuncser, V; Enculescu, M; Locovei, C; Porosnicu, I; Tiseanu, I; Ferbinteanu, M; Savulescu, I; Negru, M; Batalu, ND

SEP 23 2022, SCIENTIFIC REPORTS, 12, 15864

DOI: 10.1038/s41598-022-19427-7

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Sesquipedalian mud and burnt bricks (second to third century AD) were excavated from the Roman city of Romula located in the Lower Danube Region (Olt county, Romania). Along with local soils, bricks are investigated by petrographic analysis, X-ray fluorescence (XRF), X-ray diffraction (XRD), Fourier transformed infrared spectroscopy (FT-IR), electron microscopy (SEM/EDX), X-ray microtomography (XRT), thermal analysis (DTA-TG), M.ssbauer spectroscopy, magnetometry, colorimetry, and mechanical properties assessment. The results correlate well with each other, being useful for conservation/restoration purposes and as reference data for other ceramic materials. Remarkably, our analysis and comparison with literature data indicate possible control and wise optimization by the ancient brickmakers through the recipe, design (size, shape, and micro/ macrostructure), and technology of the desired physical-chemical-mechanical properties. We discuss the Roman bricks as materials that can adapt to external factors, similar, to some extent, to modern "smart" or "intelligent" materials. These features can explain their outstanding durability to changes of weather/climate and mechanical load.

5

Influence of erbium doping on the structural, magnetic and optical properties of hematite (?-Fe2O 3) nanorods

Popov, N; Ristic, M; Kuncser, V; Zadro, K; Velinov, N; Badica, P; Alexandru-Dinu, A; Iacob, N; Krehula, LK; Music, S; Krehula, S

OCT 2022, JOURNAL OF PHYSICS AND CHEMISTRY OF SOLIDS, 169, 110857

DOI: 10.1016/j.jpcs.2022.110857

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Pure and Er-doped hematite (alpha-Fe2O3) nanorods were prepared by a two-step method involving hydrothermal synthesis and calcination of pure and Er-doped goethite (alpha-FeOOH) nanorods. Substitution of Fe3+ by Er3+ in the crystal structure of hematite caused morpho-structural changes such as expansion of the unit cell and gradual shortening and rounding of hematite nanorods towards formation of nanoellipsoids. These changes induced modification of magnetic and optical properties suggesting the possibility of a systematic control of physical properties via rare earth substitution. A decrease in the hyperfine magnetic field, coercive field and Morin transition temperature, as well as an increase of the magnetic susceptibility and a narrowing of the optical band gap were observed by substitution. Intimate mechanisms related to the formation of more and more defect-like hematite phases with decreased temperatures for the transition to the low temperature antiferromagnetic phase at increased doping level were evidenced via temperature dependent Mo center dot ssbauer spectroscopy.

6

Kaolin clay pottery discovered in the Roman city of Romula (Olt County, Romania)

Badica, P; Alexandru-Dinu, A; Grigoroscuta, M; Locovei, C; Kuncser, A; Bartha, C; Aldica, G; Negru, M; Batalu, D; Cruceru, N; Savulescu, I

APR 2021, JOURNAL OF ARCHAEOLOGICAL SCIENCE-REPORTS, 36, 102899

DOI: 10.1016/j.jasrep.2021.102899

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Pottery vessels made of kaolin clay from the Roman Period (2nd, 3rd centuries CE) found in Romula (Re?ca village, Olt County, Romania) from Dacia Inferior (Malvensis) were investigated by petrographic, X-ray diffraction, X-ray fluorescence, thermal analysis, electron microscopy, and mechanical tests. Our results are compared with available data on kaolin clays and pottery vessels from other sites located along the lower course of Danube river and near the Black Sea, namely in Moesia Superior, Moesia Inferior, and Thracia. Archeological and geographical contexts are addressed. Results of our analysis suggest a local production of ceramics in Romula, by using raw materials from the north of Lower Danube, in opposition to the idea that kaolin ware was imported from the provinces south of the Danube.