Made available in DSpace on 2015-03-26T13:53:26Z (GMT). No. of bitstreams: 1 texto completo.pdf: 1409063 bytes, checksum: 1b46633b4d780080208be250b7d7981d (MD5) Previous issue date: 2013-02-08 / Coordenação de Aperfeiçoamento de Pessoal de Nível Superior / Aiming to quantify the magnetic susceptibility and the total contents of trace elements both in the TFSA, as in sand, silt and clay fractions, and evaluate the desorption of P by Mehlich-1 and mixed ion exchange resin samples were collected B horizons of ferric and hyper-ferric Red Oxisols developed from different parent materials of Minas Gerais. The samples were characterized physically, chemically and mineralogically, with priority to the analysis of magnetic susceptibility and sequential extractions with Mehlich-1 and mixed ion exchange resin. The main results were: a) the value 8 to the molar ratio Fe2O3/TiO2, obtained from the results of digestion sulfur, can be used as a threshold for distinction of Red Oxisols developed itabirite those from tuffite, basalt, diabase, gabbro and amphibolites; b) the constitution mineralogical clay fraction of the soil samples studied is composed by kaolinite, gibbsite, anatase, goethite, hematite and maghemita; c) the correlation coefficient positive at 1 % significance level (r = 0.94**) found between the values of magnetic susceptibility of sand and clay fractions indicate that maghemite in the soils is formed from the oxidation of magnetite and the same goes for their titano-structural forms; d) the contents of Fe2O3 obtained by sulfuric attack presented positive correlation at 1 % probability to the values of magnetic susceptibility, reflecting the importance of the parent material in the manifestation of the magnetic properties of soils; e) the contents of Fe2O3 obtained by sulfuric digestion and magnetic susceptibility values exhibited trends of correlation the content of trace elements, however, cannot be generalized for all parent materials; f) the isomorphous substitution of Fe3+ by Al3+ in the structure of the goethite was higher to hematite; g) the hematite showed morphology predominantly placoid in all Red Oxisols and lower value of specific surface area compared to goethite, reflecting the higher values of the crystal medium dimension to hematite; h) the correlation coefficients significant and positive observed between the Ca total levels and of P extracted by Mehlich-1 (r = 0.96**) and mixed ion exchange resin (r = 0.97** ), confirm the strong presence of P-Ca in Red Oxisols developed tuffite in Alto Paranaíba region; and i) a single extraction with the Mehlich-1 or mixed ion exchange resin extractor, is not sufficient to estimate the amount factor of P both young soils and those highly weathered, for successive extractions with the same extractant continue removing phosphorus from soil. / Com o objetivo de quantificar a suscetibilidade magnética e os teores totais de elementos traço tanto na TFSA, como nas frações areia silte e argila, e avaliar a dessorção de P, pelos extratores Mehlich-1 e resina de troca iônica mista, foram coletados amostras de horizontes B de Latossolos Vermelhos férricos e perférricos desenvolvidos a partir de diferentes materiais de origem de Minas Gerais. As amostras foram caracterizadas física, química e mineralogicamente, com prioridade para as análises de suscetibilidade magnética e as extrações sequenciais com os extratores Mehlich-1 e resina de troca iônica mista. Os principais resultados foram: a) o valor 8 para a relação molar Fe2O3/TiO2, obtida a partir dos resultados da digestão sulfúrica, pode ser utilizado como limite para distinção de Latossolos Vermelhos desenvolvidos de itabirito daqueles derivados de tufito, basalto, diabásio, gabro e anfibolito; b) a constituição mineralógica da fração argila das amostras dos solos estudados é composta basicamente por caulinita, gibbsita, anatásio, goethita, hematita e maghemita; c) o coeficiente de correlação positiva a 1 % de significância (r = 0,94**) encontrado entre os valores de suscetibilidade magnética das frações areia e argila indicam que a maghemita nos solos estudados é formada a partir da oxidação da magnetita e o mesmo ocorre para suas formas titano-estruturais; d) os teores de Fe2O3 obtidos pelo ataque sulfúrico apresentaram correlação positiva a 1 % de probabilidade com os valores de suscetibilidade magnética, refletindo a importância do material de origem na manifestação das propriedades magnéticas dos solos estudados; e) os teores de Fe2O3 obtidos pela digestão sulfúrica e os valores de suscetibilidade magnética apresentaram tendências de correlação com o conteúdo de elementos traço, no entanto, não podem ser generalizadas para todos os materiais de origem; f) a substituição isomórfica de Fe3+ por Al3+ na estrutura da goethita foi superior à da hematita; g) a hematita apresentou morfologia predominantemente placóide em todos Latossolos Vermelhos e menor valor da área superficial específica em comparação a goethita, refletindo os maiores valores da dimensão média do cristal para a hematita; h) os coeficientes de correlação significativos e positivos observados entre os teores de Ca total e de P extraídos por Mehlich-1 (r = 0,96**) e por resina de troca iônica mista (r = 0,97**), confirmam a presença marcante de P-Ca em Latossolos Vermelhos desenvolvidos de tufito na região do Alto Paranaíba; e i) uma única extração com o extrator Mehlich-1 ou resina de troca iônica mista, não é suficiente para estimar o fator quantidade de P tanto em solos jovens quanto aqueles altamente intemperizados, pois extrações sucessivas com o mesmo extrator continuam retirando fósforo do solo.

O trabalho envolve o estudo de amostras de poli(o-metoxianilina) (POMA) , dopadas com ácido trifluoracético (TFA) através das técnicas de espectroscopia de Ressonância Paramagnética Eletrônica (RPE) de onda contínua e pulsada. O sinal de RPE observado é atribuído a elétrons desemparelhados na cadeia polimérica, denominados pólarons. Uma vez que estes pólarons possuem carga elétrica e spin eletrônico, os estudos de RPE podem fornecer informações a respeito de sua mobilidade e sobre as propriedades de transporte no material em escala microscópica. O efeito da presença de oxigênio molecular, O2, (S=1), sobre a forma da linha CW é estudado em função do grau de dopagem e do envelhecimento das amostras. O alargamento observado da linha de RPE deve-se a processos de colisão entre o pólaron móvel e os spins localizados do O2. Durante uma colisão, os dois spins interagem entre si através de interações de troca magnética, produzindo spin-flips simultâneos. Uma vez que os spins fixos estão fortemente acoplados com a rede, o processo de relaxação spin-rede do pólaron torna-se muito eficiente, produzindo o alargamento da linha. Como resultado deste processo de colisões, a dependência da largura de linha em função da temperatura mostra um máximo em torno de 190 K. Modelos teóricos serão apresentados, a partir dos quais serão estimados os valores para a mobilidade do pólaron, raio de ação da interação pólaron-oxigênio e constantes de acoplamento. Amostras sintetizadas na presença de oxigênio possuem tempos de relaxação muito curtos em toda a faixa de temperatura estudada (2-280 K), impossibilitando a observação da RPE pulsada. Amostras envelhecidas mostram um comportamento diferente, característico da substituição do oxigênio por água, que leva ao cancelamento do efeito de alargamento. Nestas amostras, assim como em amostras sintetizadas em atmosfera inerte, estudos adicionais de RPE pulsada permitem, através de técnicas associadas ao eco de spins eletrônicos, ESE, a obtenção dos tempos de relaxação spin-spin e spin-rede, assim como o estudo das interações hiperfinas entre pólaron e núcleos vizinhos, 1H, 13C e 14N, que não são resolvidas no espectro CW. A quantificação e qualificação de núcleos interagentes, os quais possuem desdobramentos hiperfinos fracos, podem ser realizadas através das técnicas uni e bidimensionais, como ESEEM, 2DESEEM e HYSCORE. / Continuous wave (CW) and pulsed Electron Paramagnetic Resonance (EPR) techniques are used to study structural and dynarnical properties of poly(o-metoxyaniline) (POMA) doped in trifluoroacetic (TFA) solution. The observed EPR spectrum is attributed to chain unpaired electron spins named polarons. Since polarons carry both charge and spin, EPR studies can provide information about charge transport properties of the material on a microscopic scale. The width of the EPR signal reflects the interaction of the polarons with their environments. In the present study, special attention is given to the EPR linewidth, which is usually broadened by the presence of molecular oxygen, O2, (S=1). The oxygen induced linewidth is explained by the mutual spin flips occurring during the collision of a mobile polaron with fixed paramagnetic O2. The temperature dependence of the linewidth shows a maximum around 190K associated with these collision processes. Such effects are studied as a function of doping concentration, sample aging and vacuum conditions. From a theoretical model proposed in the field, some parameters, associated with the polaron mobility and exchange interaction between polaron and oxygen, are estimated. All synthesized samples have very short spin relaxation times in all the studied temperature range (2-280K), making impossible their observation by the pulsed EPR techniques. Aged samples show a different behavior; their long relaxation times seem to indicate that the substitution of O2 by H2O has promoted the canceling of the broadening effect. Studies are under progress to establish a sample preparation procedure in which the resulting samples are free of molecular oxygen. Aged samples have been used to perform preliminary studies conducted by the pulsed EPR techniques. Spin-echo spectroscopy and relaxation time measurements were interpreted on the basis of the interaction of the polaron with neighboring nuclei, such as 1H, 13C e 14N, which are not resolved in the CW spectra. To better understand the nature of the CW and pulsed EPR spectroscopy, one special chapter will introduce the several techniques, which are commonly employed in our research.

High resolution dating of loess on the Chinese Loess Plateau (CLP) using Optically Stimulated Luminescence (OSL) has increased the understanding of past monsoon climate but also raised questions regarding dust mass accumulation rate (MAR), the presence of disturbances or gaps in the sediment record, a possible teleconnection between North Atlantic and East Asian monsoon climate, and whether these events are due to climate variability, local settings, or age model uncertainties. This study undertakes a detailed (<20cm sampling resolution) -OSL investigation of the Lingtai section to create an independent age model using linear regression, to reconstruct monsoon climate changes using magnetic susceptibility(MS) and grain size (GS) proxies, as well as to calculate MAR for the site. The data shows that between 44-15 ka climate changes from a period of strong summer monsoon to a strong winter monsoon. GS data show variable trends attributed to changes in dust storm activity and local environmental conditions. MAR data does not correlate with grain size and is different from other loess records on the CLP. Such differences are either due to local variations or age model uncertainties. No clear correlation with Heinrich events or teleconnection with North Atlantic climate is visible in the records over the Last Glacial period, and hiatuses or gaps are not obviously present at this site. It is suggested that using linear regression for continuous age model construction from the luminescence ages comes with uncertainties due to subjective bias when fitting the lines and determining shifts in the data, especially during MAR calculations. Further studies are needed to ascertain optimal methods for creating age models, and to constrain the reasons behind the variability between different sites and loess records on the CLP. / Högupplöst OSL-datering av loessjordar från CLP har ökat förståelsen av dåtida monsunklimat, men har även lyft frågan gällande MAR, närvaron av avbrott eller småskaliga event i jordsektionerna, möjligheten av en relation mellan de Nordatlantiska och Ostasiatiska monsunklimaten, och om dessa förändringar sker till följd av faktisk klimatvariation, lokala förutsättningar, eller osäkerheter i åldersmodellen. Studien genomförde en detaljerad (<20cm) OSL-undersökning av Lingtai-sektionen för att skapa en oberoende åldersmodell, återge monsunklimatförändringarna genom tillämpning av MS och GS proxies, samt beräkna MAR från platsen. Resultaten påvisar att mellan 44-15 ka förändrades klimatet från en period av stark sommar- till en stark vinter-monsun. Kornstorleks-resultaten påvisar stora variationer vilka kan kopplas till en förändring i sandstormsaktivitet samt de lokala förutsättningarna för deposition av sediment. MAR-resultaten överensstämmer inte med kornstorleksdatan och skiljer sig från den övriga empirin, detta kan bero på lokala variationer i regionen eller osäkerheter i åldermodellen. Det finns ingen klar korrelation mellan "Heinrich events" eller en "teleconnection" i sektionen, och avbrott samt störningar i sektionen är inte förekommande. Avsaknaden av korrelation antyder att användningen av regressionslinjer för att skapa kontinuerliga åldermodeller kommer innebära fortsatta osäkerheter i empirin, speciellt gällande beräking av MAR. Ytterligare studier krävs för att bestämma optimala metoder för att framställa åldersmodeller, samt att utröna orsaken till skillnaden mellan resultat från olika platser på plat

M. Sc. / The substitution series CeCu5−xAlx where x 2 {1.0, 1.5, 2.0, 2.1, 2.2, 2.3, 2.4} was synthesized and characterized via x-ray diffraction and scanning electron microscope analysis. All the compounds formed single phase in the P6/mmm hexagonal crystal structure, which pushed the solubility limit of Al within this structure from CeCu3Al2 to CeCu2.6Al2.4. The ascast samples were annealed, but the annealing process had no visible effect on the crystalline nature nor on the physical properties of the samples. The electric, magnetic and thermal properties were measured on Quantum Design’s Physical Properties Measurement System and Magnetic Properties Measurement System. The electrical resistivity showed single-ion Kondo scattering at intermediate temperatures with no signs of coherence for x 2 {1.0, 1.5, 2.0, 2.1, 2.2, 2.3} CeCu2.6Al2.4 on the other hand showed a weak maximum at 2 K, which was the onset of antiferromagnetic ordering confirmed by other measurements. The magnetoresistance was fitted by the Beth´e ansatz spin-1/2 model and the obtained Kondo temperatures had a maximum at CeCu3Al2, with linear dependencies on Al concentration on either side of this point. The Kondo moments followed an exponential dependence on the Al concentration, but these effective moments were far lower than the free-ion value, due to the Kondo interaction. The thermal conductivity in this series was phonon dominated with the magnitude of the electronic component being inversely proportional to the Kondo temperature, showing the effect that the Kondo scattering mechanism has on the availability of the conduction electrons to participate in heat transport. The magnitude of the peak in the thermoelectric power S(T) was strongly dependent on the Al concentration, having a maximum at CeCu2.8Al2.2. Below the peak there were two temperature dependencies: S(T) / T for x 2 {1.0, 1.5, 2.4} which is metallic and for x 2 {2.0, 2.1, 2.2, 2.3} S(T)/T /−ln(T) which is characteristic of a quantum critical point. The data were also fitted with a phenomenological model and the obtained Kondo temperatures were quantitatively similar to those obtained from the Beth´e ansatz. The heat capacity Cp(T) data confirmed these compounds to be heavy fermions and also showed Cp(T)/T /−ln(T) below 10 K, which is the hallmark for a magnetically tuned quantum critical point. The magnetic susceptibility showed a Curie-Weiss temperature dependence at temperatures above 100 K, with magnetic moments close to the free-ion value, indicating the presence of localized magnetic moments. The low temperature data found (T) /−ln(T) for Al concentrations near CeCu3Al2 and the ordering present in CeCu2.6Al2.4 was suppressed by 0.3 K in going from 0.01 T to 2 T, suggesting that the ground state is antiferromagnetic in this compound.

Orientador: Marco Antonio Bica de Moraes / Tese (doutorado) - Universidade Estadual de Campinas, Instituto de Fisica Gleb Wataghin / Made available in DSpace on 2018-08-18T19:35:50Z (GMT). No. of bitstreams: 1 Fischer_GiovanaZaniniGadioli_D.pdf: 32265979 bytes, checksum: f410dfb24adff86c43498027515957c8 (MD5) Previous issue date: 2011 / Resumo: Neste trabalho, a técnica de magnetron-sputtering foi empregada para fabricar filmes multicamadas de Gd/W e Gd/Cr, cujas propriedades magnéticas foram investigadas em função da espessura das camadas de Gd, dGd, e da temperatura do substrato, TS, durante a deposição. Espectroscopia de retroespalhamento Rutherford e espectroscopia fotoeletrônica de raios-x foram utilizadas, respectivamente, para detectar possível contaminação de oxigênio e para verificar a continuidade da camada de Gd sobre W e Cr. Difratometria de raios-X de baixo ângulo (GAXRD) e microscopia eletrônica de varredura (MEV) foram empregadas para investigar a estrutura cristalina e morfologia das amostras. As análises de GAXRD mostraram que nas amostras Gd/W as camadas de Gd são amorfas. Nas amostras Gd/Cr, entretanto, a cristalinidade do Gd aumenta com o aumento de dGd e TS. Pelas medidas de MEV foi visto que os filmes de Gd tanto sobre W quanto Cr são granulares. Para investigar as propriedades magnéticas utilizamos um magnetômetro SQUID e um PPMS. O primeiro foi utilizado para as medidas de momento magnético em função do campo estático, Hdc, e da temperatura, T. O PPMS foi utilizado nas investigações de susceptibilidade magnética ac em função de T, medidas em diferentes frequências de oscilação do campo e diferentes Hdc. A complexa natureza magnética dos filmes com dGd = 10 nm foi observada através das isotermas M x H, que não apresentaram saturação, para a maioria das amostras, nem mesmo em baixas temperaturas e altos campos. Pela análise dos dados magnéticos em função da temperatura, observamos que o caráter ferromagnético nas amostras se acentua à medida que TS e dGd aumentam. A temperatura de Curie, TC, também depende de TS e dGd, aumenta de 247 a 297 K com o aumento dos dois últimos parâmetros. A partir das isotermas M x H o momento magnético de saturação a 0 K foi calculado, e ele mostrou-se dependente de TS. A existência de vidros magnéticos nas amostras com dGd = 10 nm foi fortemente sugerida pelos resultados obtidos de magnetização e susceptibilidade ac, ambas em função de T. Para filmes com dGd = 10 nm, o efeito magnetocalórico foi investigado através da variação de entropia magnética, ?SM, em função da temperatura, para a remoção de um campo de 50 kOe. Curva de ?SM x T para as amostras Gd/Cr com TS = 300 e 500 ºC exibiram picos a alta temperatura denotando ferromagnetismo. Por outro lado, a amostra Gd/Cr depositada a 30ºC e todos os filme Gd/W não apresentaram nenhum pico em ?SM x T, indicando ausência ou baixa quantidade da fase ferromagnética. Todas as medidas são consistentes em indicar múltiplas fases magnéticas nas amostras e temperaturas de transição. Uma forte consistência entre as medidas magnéticas, GAXRD e MEV é verificada / Abstract: Direct current magnetron sputtering was used to synthetize Gd/W and Gd/Cr multilayer films, whose magnetic properties were investigated as a function of the Gd layer thickness, dGd, and the substrate temperature, TS, during deposition. Rutherford backscattering spectroscopy and x-ray photoelectron spectroscopy were employed, respectively, to detect possible oxygen contamination and to check the continuity of the coverage of the Gd layers on top of those of W and Cr. Grazing angle X-ray diffraction (GAXRD) and scanning electron microscopy (SEM) were used to investigate the crystalline structure and the morphology of the samples. The GAXRD analyses have shown that in the Gd/W samples the Gd layers are amorphous. In the Gd/Cr samples, however, Gd is crystalline. In these samples, the Gd crystalline order increases with increasing TS and dGd. From the SEM analysis, it was found that the Gd layers in either Gd/W or Gd/Cr samples were granular. To investigate the magnetic properties of the films, SQUID and PPMS magnetometries were used. With the former technique, the magnetic moments of the samples were measured as a function of a dc magnetic field, Hdc, and temperature, T. By PPMS, alternating magnetic fields, superimposed by different Hdc fields were used. The moments were measured as a function of T, Hdc and the frequency of the alternating field. The complex magnetic nature of the films with dGd = 10 nm was observed from the M x H isotherms, which did not show, for most of the samples, saturation even at high magnetic films and low temperatures. From the magnetic data as a function of temperature, it was observed that ferromagnetic character of the samples is enhanced as dGd and TS were increased. The Curie temperature, TC, also depends on TS and dGd as it increases from 247 to 297 K as the latter variables are increased. From the M x H isotherms the saturation magnetic moment at 0 K was determined, and it was observed that it depends on TS. The existence of magnetic glass states in samples with dGd = 10 nm was strongly suggested from both magnetization and ac susceptibility measurements as a function of T. For films with dGd = 10 nm, the magnetocaloric effect was investigated by the magnetic entropy change, ?SM, as a function of the temperature for the removal of a 50 kOe field. The ?SM x T plots for the Gd/Cr samples deposited at TS = 300 and 500 ºC exhibited high temperature peaks denoting ferromagnetism. On the other hand, for the Gd/Cr sample deposited at 30 ºC and for the all the Gd/W samples, such peaks were not seen, indicating the absence, or low-content, ferromagnetic phase. All magnetic measurements are consistent in indicating multiple magnetic phases in the samples and magnetic transition temperatures. A strong consistency among the magnetic and the GAXRD and SEM observations was also verified / Doutorado / Física da Matéria Condensada / Doutora em Ciências

A model study about the precise stratigraphy of the Kralodvorian Formation was made on the drill core from Ořech near Prague. The exposure at Levín was used as a reference section. Both sections were sedimentologicaly studied and described in detail. The study of thin sections was a supplemented for exact description of the rocks and lithotypes. Chemostratigraphic methods (?13C and TOC) and method of the rock magnetic susceptibility were used for detailed stratigraphic analyse. All the mentioned methods of both sections. Samples for the measurements of the magnetic susceptibility were taken by 0.5 m of thickness. The measurement of ?13C and TOC was taken from the non-wheathered 80 m of the drill core Ořech and from the upper 20 m Králův Dvůr Formation at Levín profile by 2 m. The available data show that Ořech represents low and middle part of the Kralodvorian strata and that all studied thickness (80 m) belongs to only positive excursion of ?13C. This excursion is interpreted to be the upper Katian. It gives an evidence that sedimentation of the Kralův Dvůr Formation was very fast. Identification and interpretation of this excursion makes possible the accurate interregional corelation of the strata. A precise regional stratigraphic subdivision is based on inhomogenities caused by different materials or...

ENGLISH ABSTRACT We present new results of structural and magnetic (AMS) analyses of selected dikes of melasyenite, quartz melasyenite to melagranite porphyries accompanied by lamprophyres (minettes). The studied dike from the locality Nihošovice were dated by U-Pb method on zircons at 338 Ma. The asymmetric structural pattern of the studied dikes gives an excellent evidence for their emplacement and orientation of magmatic flow. The studied dikes were emplaced into: (i) Prevailing parts of the Central Bohemian Plutonic Complex (locality Malčice) and (ii) host high-grade metamorphic rocks of western part of the Moldanubian Zone (locality Nihošovice). Despite of the extensive area of occurrence, compositional variations and age of emplacement of these dikes are relatively narrow. Their geochemical and petrological compositions broadly correspond to ultrapotassic plutonic rocks (durbachites). The dikes are steeply dipping in trend ~NNW-SSE to ~W-E, with range in width between ~20 and ~25 meters. In general, our results show: (i) A relatively low degree of magnetic anisotropy (P= 1.012 - 1.152); (ii) Mostly oblate (planar) fabric, especially in marginal parts of the intrusive bodies (T= -0.091 - 0.941); (iii) Evidence for subhorizontal magmatic flow trajectory defined for a newtonian magma with typical...

Systematic measurements of the magnetic moment in dependence on temperature and magnetic field of hexagonal 6H-BaTiO3 + 0.04 BaO + x/2 Fe 2 O 3 (0.005 x 0.05) ceramics were performed to study the influence of Fe ions on the magnetic properties. While the samples show Curie–Weiss paramagnetism for Fe concentrations 1.0 mol%, antiferromagnetic interactions become manifest for 2.0 and 5.0 mol% iron. With increasing Fe content the antiferromagnetic interaction, which is assumed to be caused by a superexchange mechanism Fe 3+ Ti(1) − O 2− O(2) − Fe3+ Ti(2) , becomes stronger. At external magnetic fields smaller than 1 T a further, ferromagnetic interaction between Fe 3+ ions is detected below 200 K. The interactions between Fe 3+ ions in the samples with 2.0 and 5.0 mol% iron are also manifest in the EPR spectra by numerous lines with low intensity. Q-band EPR investigations of 5.0 mol% Fe doped single crystals confirm the existence of only one type of Fe 3+ –V O associates in the samples.

<p> The magnetic properties of MnP2O7, CuP2O7, Co2P2O7 and Ni2P2O7 were studied. They were investigated using magnetic susceptibility and magnetic resonance techniques. They were all found to become magnetically ordered between 10°K and 30°K. In all the predominant exchange interaction was antiferromagnetic. Ni2P2O7 however did show a resultant moment at low temperatures which was attributed to weak ferrornagnetism. The experimental results were analysed in the molecular field approxmation which accounted for their behaviour except in the case of Cu2P2O7 where the High Temperature Series Expansion method was necessary to explain the temperature dependence of its paramagnetic susceptibility. </p> / Thesis / Doctor of Philosophy (PhD)

Mapping anomalies in the Earth’s magnetic field is one method used in applied geophysics, for exploring buried structures and objects. Magnetic surveys can be ground-based or made airborne, onboard airplanes, helicopters, or unmanned aerial vehicles (UAV), also known as drones. The measurements in this project were made as part of a mapping project by the Swedish Geological Survey (SGU) in the Enåsen area in Hälsingland, central Sweden. The magnetic data were collected by SGU in the field summer of 2021. The aim of this project is to model the data from UAV-borne surveys and validate them by checking the response with the measure ground-based data collected by SGU and compare several different profiles to investigate the different results from ground-based vs. UAV-borne surveys. Two models from two different UAV flight lines were made using the software Potent, to show anomalies in the magnetic field intensity. The modelling results show a relatively good correlation between the response from the model and ground-based data. However, there are detailed variations in the ground-based data that are not resolved by the UAV data. This is partly because of the height difference and partly different sampling. The magnetic anomalies in the project area were interpreted, with the help of the modelled profiles, as being caused mainly by geological units consisting of metasedimentary rock/migmatite. These units generally dip with 30-50°, some of them containing Cuand Au-mineralizations. The dip, rock type, and magnetic susceptbilities of these units match the field data from SGU relatively well and are also backed up by SGU models of electrical resistivity from the same area. / Kartläggning av avvikelser i jordens magnetfält är en metod som används inom tillämpad geofysik för att upptäcka underjordiska strukturer och objekt. Magnetiska undersökningar kan utföras på marken eller från luften, med hjälp av flygplan, helikopter eller drönare. De geofysiska mätningarna i detta projekt gjordes som en del av ett karteringsprojekt av Sveriges geologiska undersökning (SGU) i Enåsen, Hälsingland. Dessa magnetiska data insamlades av SGU under sommaren 2021. Syftet med projektet är att modellera magnetiska data insamlade med hjälp av drönare, för att sedan kontrollera modellerna med magnetiska markdata insamlade av SGU i samma område. Dessa profiler jämfördes för att undersöka hur insamlad data från drönare respektive markmätningar skiljer sig. Modellerna gjordes i programvaran Potent, där anomalierna i magnetfältets intensitet. Resultaten från modelleringen visar en relativt tydlig korrelation mellan hur modellen (från insamlade drönardata) svarar mot markdata. Det förekommer dock små variationer i profilerna från markdata, som inte syns i modellerna från drönardata. Detta beror delvis på att mätningarna gjordes på olika höjd, och delvis på att proverna skiljer sig åt i viss mån. De magnetiska anomalierna i projektområdet tolkades med hjälp av de modellerade profilerna, och förmodas vara orsakade av enheter av metasedimentär bergart/migmatit. Dessa enheter stupar mestadels med 30-50°, och på vissa platser förekommer Cu- och Au-mineraliseringar. Stupningen, bergarter och den magnetiska susceptibiliteten stämmer relativt väl överens med SGU:s information från fältundersökningar, och tolkningen styrks ytterligare av SGU:s modeller av den elektriska resistiviteten i samma område.