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Evaluation of water quality in open channels flowing through Beni-Mellal City (Morocco) / Ocena jakości wody w otwartych kanałach płynących przez miasto Beni-Mellal (Maroko)

Earth Sciences. Vol. 63 p. 839-846. EATON F.M. 1950.Significance of carbonates in irrigation waters. Soil Science. Vol. 69 p. 123-133. EL BAGHDADI M., BARAKAT A., SAJIEDDINE M., NADEM S. 2012. Heavy metal pollution and soil magnetic susceptibility in urban soil of BeniMellal City (Morocco). Environmental Earth Sciences. Vol. 66. Iss. 1 p. 141-155. EL HASSEN A., DRISS B., MOHAMED B., HAMID E., EBY F.M., MOHAMADOU O. 2011. Physicochemical typology of water of a middle atlas river (Morocco) where the common trout (Salmo

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High resolution airborne radiometric and magnetic studies of ilesha and its environs, southwestern Nigeria

wavenumber methods, Society of Exploration Geophysics Annual General Meeting, Calgary, Alberta, Expanded Abstracts. [44] Olowofela, J.A., Badmus, B.S., Ganiyu, S.A., Olurin, O.T., Babatunde, P. (2011): Source location and depth estimation from digitised aeromagnetic data acquired from the basement complex formation. Earth Science India , 4, pp. 136–142. [45] Geosoft INC. (2010). Geosoft INC. 85 Richmond Street, 8 th Floor, Toronto, Ontario, Canada. [46] Frantisek, H., Jiri, P., Jazek, J. Chadina, M. (2009): Out – of-Phase Magnetic Susceptibility of

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High temperature EPR study of the M3Fe4V6O24 (M = Cu, Zn, Mg and Mn)

methods [ 1 , 3 , 10 , 11 ]. The structure contains three sublattices associated with metal ions including two sublattices with iron ions. The M ion site may be occupied by magnetic or diamagnetic ions and in case of the former one a more complex magnetic system is achieved. Measurements of DC magnetic susceptibility χ as a function of temperature showed that the Curie-Weiss behavior, χ = C/(T – ), dominates at high temperatures with a negative Curie-Weiss temperature (the largest value of was found for the compound M = Mn and the smallest for M = Cu) [ 5 , 7

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Ammonites and magnetostratigraphy of the Berriasian–Valanginian boundary deposits from eastern Crimea

2012. Elsevier, 1-1144. Grishchenko V.A. & Bagayeva M.I. 2014: Anisotropy of magnetic susceptibility of the boundary Berriasian-Valanginian interval near village South (East Crimea) as an indicator of the relative age of the last deformation of clays and their degree of plasticity. Geophysical Bulletin. 6, 23-26 (in Russian). Guzhikov A.Yu. 2013: Solving unsolvable problems in stratigraphy (Comments to the paper “New data on the magnetostratigraphy of the Jurassic-Cretaceous boundary interval, Nordvik Peninsula (northern East Siberia

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The Development of Freshwater Deltas and their Environmental and Economic Significance / Rozwój I Znaczenie Środowiskowo-Użytkowe Delt W Zbiornikach Śródlądowych

limnicznych w warunkach zróżnicowanej antropopresji na przykładzie regionu górnośląskiego. Katowice: Wyd Uniwersytetu Śląskiego; 2008 (in Polish). [29] Kabata-Pendias A, Pendias H. Biogeochemia pierwiastków śladowych. Warszawa: Wyd Nauk PWN; 1999 (in Polish). [30] Magiera T, Strzyszcz Z, Kostecki M. Seasonal changes of magnetic susceptibility in sediments from Lake Zywiec (south Poland). Water Air Soil Pollut. 2002;141:55-71. DOI: 10.1023/A:1021309301714. [31] Büttner O, Becker A, Keliner S, Kuehn K, Wendt-Potthoff K, Zachmann

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Middle Devonian palynomorphs from southern Moravia: an evidence of rapid change from terrestrial deltaic plain to carbonate platform conditions

Polyedrixium Deunff. Révision et observation. In: Jardiné S. (Ed.): Microfossiles Organiques du Paléozoique. CIMP , Paris, 7-48. Dvořák J. 1998: Lower Devonian basal clastics Old Red Formation, Southern Moravia, Czech Republic. Czech Geol. Surv. Bull. 73, 4, 271-279. Geršl M. & Hladil J. 2004: Gamma-ray and magnetic susceptibility correlation across a Frasnian carbonate platform and the search for "punctata" equivalents in stromatoporoid-coral limestone facies of Moravia. Geol. Quart. 48, 3, 283

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Pleistocene Stratigraphy of Poland and Its Correlation with Stratotype Sections in the Volhynian Upland (Ukraine)

Paleogeographic Interpretation of Analysis Results of Magnetic Susceptibility of Loesses in Bojanice (NW Ukraine). Annales Universitatis Mariae Curie-Skłodowska B 50: 51-64. Boguckyj A and Łanczont M, 2002. Loess stratigraphy in the Halyc Prydnistrov'ja region. Studia Geologica Polonica 119: 315-327. Butrym J and Zuchiewicz W, 1985. Results of thermoluminescent datings of Quaternary sediments from the Nowy Sącz Basin (West Carpathians). Przegląd Geologiczny 33(3): 126-136. Dolecki L, 2002. Main

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Time-Efficient Perfusion Imaging Using DCE- and DSC-MRI

in Medicine , 30(6), 764–768. [36] Pedersen, M., Klarhöfer, M., Christensen, S. r., Ouallet, J.-C., Østergaard, L., Dousset, V., Moonen, C. (2004). Quantitative cerebral perfusion using the PRESTO acquisition scheme. Journal of Magnetic Resonance Imaging , 20(6), 930–940. [37] Boxerman, J.L., Hamberg, L.M., Rosen, B.R., Weisskoff, R.M. (1995). MR contrast due to intravascular magnetic susceptibility perturbations. Magnetic Resonance in Medicine , 34(4), 555–566. [38] Kjølby, B.F., Østergaard, L., Kiselev, V.G. (2006). Theoretical model of

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New exposure of loess deposits in Boyanychi (Ukraine) — Results of thermoluminescence analyses

Lublinie: 246–249 (in Polish). [17] Bogucki AB, Maruszczak H and Nawrocki J, 1995. Stratigraphic and Paleogeographic Interpretation of Analysis Results of Magnetic Susceptibility of Loesses in Bojanice (NW Ukraine). Annales UMCS 50, sec. B: 51–64. [18] Bogucki (Bogutsky) AB, Łanczont M and Wojtanowicz J, 2000a. The Korshov (=Lublinian) interglacial and oxygene isotope stage 7 in the loess profiles of Poland and Ukraine. Ukraina ta globalni procesi, geografičnii simir. Kiev-Luck 2: 185

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Magnetic studies of 0.7(Fe2O3)/0.3(ZnO) nanocomposites in nanopowder form and dispersed in polymer matrix

magnetic susceptibility χ (defined as χ = M/H) in zero field cooled (ZFC) and field cooled (FC) modes of the 0.7(Fe 2 O 3 )/0.3(ZnO) nanopowder ( Fig. 2a ) and the 0.7(Fe 2 O 3 )/0.3(ZnO) dispersed in polymer ( Fig. 2b ) measured in two different magnetic fields (H = 100 Oe and 1000 Oe) is presented. In ZFC mode all magnetic moments in each single domain particle point along the nanoparticle easy axis when the nanoparticles are cooled down to very low temperature and magnetic anisotropy prevents switching of magnetization from the easy axis. As a result, the average

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