SPOŁECZNO-KULTUROWE UWARUNKOWANIA PRZĘPSTW PRZECIWKO WOLNOŚCI SEKSUALNEJ MAŁOLETNIEGO

Wykorzystanie seksualne dziecka jest związane z przestępstwami z art. 200 i z kilku artykułów pokrewnych polskiego Kodeksu karnego. Czynniki społeczno-kulturowe oddziaływają na to zjawisko poprzez dwa rodzaje socjalizacji. Socjalizacja wtórna zachodzi w populacji polskiej w sposób jednolity dla wszystkich sprawców, natomiast różnicuje ich socjalizacja pierwotna, w związku z czym to ona winna być przedmiotem badań. Najlepsze wyjaśnienia zjawiska oferują ujęcia zintegrowane, akcentujące, między innymi, rolę czynników rodzinnych w jego powstawaniu. W niniejszym artykule, jako teoretyczną podstawę badań, wykorzystano zintegrowaną teorię etiologii przestępstw seksualnych, która uznaje rodzinne doświadczenia sprawcy za główną przyczynę późniejszego seksualnego wykorzystywania dzieci. Zaproponowano cztery ścieżki rozwoju patologii wskazujące, w jaki sposób wczesne uwarunkowania psychologiczne (typ opieki i postawy rodziców) przyczyniają się do zostania sprawcą wykorzystania seksualnego dziecka w przyszłości, oraz zweryfikowano je w badaniach własnych. Wyniki przeprowadzonych badań częściowo potwierdzają zaprezentowany model teoretyczny i pozwalają wyznaczyć kierunki dalszych poszukiwań.

Nazwiska mieszkańców Poznania od XVI do XVIII wieku w świetle ksiąg metrykalnych Kolegiaty św. Marii Magdaleny. Studium onomastyczno-socjolingwistyczne

Wydział Filologii Polskiej i Klasycznej

Columbia revisited: Paleomagnetic results from the 1790 Ma colider volcanics (SW Amazonian Craton, Brazil)

In an attempt to improve our understanding of the Paleoproterozoic geodynamic evolution, a paleomagnetic study was performed on 10 sites of acid volcanic rocks of the Colider Suite, southwestern Amazonian Craton. These rocks have a well-dated zircon U-Pb mean age of 1789 +/- 7 Ma. Alternating field and thermal demagnetization revealed northern (southern) directions with moderate to high upward (downward) inclinations. Rock magnetism experiments and magnetic mineralogy show that this characteristic magnetization is carried by Ti-poor magnetite or by hematite that replaces magnetite by late-magmatic cleuteric alteration. Both magnetite and hematite carry the same characteristic component. The mean direction (Dm = 183.0 degrees, Im = 53.5 degrees, N = 10, alpha(95) = 9.8 degrees, K = 25.2) yielded a paleomagnetic pole located at 298.8 degrees E, 63.3 degrees S (alpha(95) = 10.2 degrees, K = 23.6), which is classified with a quality factor Q = 5. Paleogeographic reconstructions using this pole and other reliable Paleoproterozoic poles suggest that Laurentia, Baltica, North China Craton and Amazonian Craton were located in laterally contiguous positions forming a large continental mass at 1790 Ma ago. This is reinforced by geological evidence which support the existence of the supercontinent Columbia in Paleoproterozoic times. (C) 2008 Elsevier B.V. All rights reserved.

Impactos emocionais causados pela mudança de estilo de gestão em um hospital na cidade de São Luis-MA

The objective of this study is to identify how a health institution can minimize the emotional impacts caused by the change of a style of classic management for a participative administration, that the workers and controllers can see the institution as a dynamic organization, that must be faced as an alive system, mobile and adaptable, where they is beings that have the right to react and to answer to the stimulatons. For that, the institution can handle motivator¿s instruments that develop in the people the potential to react of adequate way to the changes proposals, as well as increasing the perspective of possible technological improvements and interpersonal relationship between the internal and external customers. To change the style to manage, to hear the staff of support and user, are not part of the routine of the heads that develop classic management. This decision demands adaptation and flexibility, study, update and psychological preparation, to face common feelings to the new. It fits to the new directors, to visualize these feelings and work to minimize, avoiding future upheavals and the confrontation of situations that can harm the production of the company, as well as the quality of the communication between the diverse dimensions of the organization people. In this study case, based in phenomenological methodology, was possible to verify, through half-open interviews and comments, how was faced the feelings caused at the old direction time, composed for military who withheld the power and determined the actions of the hospital in study, was replaced by health professionals, that saw in the work team the best option to solve the problems and the potential to carry through an administration based in adequate strategies the reality of the moment, with the objective of reaching the satisfaction of the customer. Through this work, is possible to prove the theory that the changes cause impacts that affect the behavior of the people involved and cause stress, as well as conclude that despite the new direction show themselves, during the change, much made use to make right and involve all the workers, didn¿t have traced strategies to minimize the emotional impacts caused by the changes, what made all face their feelings of doubts and anxiety without no special care. Many obtained, by themselves, to face and to adapt the new proposals, but some could not assimilate the new administrative methodology and had been moved away definitively from the institution.

Lixo hospitalar: na estrutura curricular de cursos superiores de saude na cidade de Imperatriz – MA

SILVA, Dany Geraldo Kramer Cavalcanti e et al. Lixo hospitalar: na estrutura curricular de cursos superiores de saude na cidade de Imperatriz-MA. Educação Ambiental em Ação, v. 27, p. 00-10, 2009.

Isotopic evidence for the late Brasiliano (500-550 Ma) ore-forming mineralization of the Araes gold deposit, Brazil

The Araes gold deposit, located in eastern Mato Grosso State, central Brazil, is hosted in Neoproterozoic volcanosedimentary rocks of the Paraguay belt, which formed during collision of the Amazonian craton and the Rio Apa block. Ar-40/Ar-39 geochronology and Pb and S isotopic analyses constrain the timing and sources of mineralization. Three biotite flakes from two samples of metavolcanic host rock yield Ar-40/Ar-39 plateau ages between 5941 and 531 Ma, interpreted as cooling ages following regional metamorphism. Clay minerals from a hydrothermal alteration zone yield an Ar-40/Ar-39 integrated age of 503 +/- 3 Ma. Galena grains from ore-bearing veins yield values of Pb-206/(204)pb from 17.952 to 18.383, Pb-207/Pb-204 from 15.156 to 15.811, and Pb-208/Pb-204 from 38.072 to 39.681. Pyrite grains from ore-bearing veins yield values of Pb-206/Pb-204 from 18.037 to 18.202, Pb-207/Pb-204 from 15.744 to 15.901., and Pb-208/(204)pb from 38.338 to 38.800. Pb isotope variations may be explained in terms of mixing a less radiogenic lead component (mu similar to 8.4) from mafic and ultramafic basement host-rocks (Nova Xavantina metavolcanosedimentary rocks) and a more radiogenic lead component (mu similar to 9.2) probably derived from supracrustal rocks (Cuiaba sedimentary groups). Sulfur isotope compositions are homogeneous, with delta S-34 values ranging from -1.1 parts per thousand to 0.9 parts per thousand (galena) and -0.7 parts per thousand to 0.9 parts per thousand (pyrite), suggesting a mantle-derived reservoir for the mineralizing solutions. Based on the Ar, Pb, and S isotope data, we suggest that the precious metals were remobilized from metavolcanic host rocks by hydrothermal solutions during Brasilide-Panafrican regional metamorphism. The Arabs gold deposit probably formed during a late stage of the orogeny, coeval with other mineralization events in the Paraguay Belt.

Crescimento e produção de bananeiras 'prata anã' e 'maçã' fertirrigadas com potássio

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Beneficiamento de uma argila tipo paligorskita da bacia de S. Luis-Grajaú, região de Alcântara, MA, e sua utilização como adsorvente de fósforo

Este trabalho utilizou uma amostra proveniente da bacia de S. Luis-Grajaú, MA, que consiste numa mistura na qual há predominantemente palygorskita e dolomita, abordando a existência desta nova ocorrência, sugerindo um método de beneficiamento e sua aplicação como adsorvente de fósforo para utilização na agricultura, já que a dolomita funciona como corretor de solos, enquanto a palygorskita tem a função de carreador de nutrientes. Primeiramente foi feita a caracterização química e mineralógica por meio de análise de difração de raios X, fluorescência de raios X, microscopia eletrônica de varredura, e separação das frações de areia, silte e argila. Foram ainda realizados ensaios de decantação e de adsorção de fósforo, com determinação da curva cinética. Após a análise de difração de raios X pode-se afirmar que a amostra é constituída principalmente de palygorskita e dolomita, apresentando também ilita, clorita e quartzo. Também foi possível verificar que os diferentes tipos de desagregação utilizados não apresentaram diferenças significativas nos difratogramas de raios X das amostras. Quanto à separação areia-silte-argila, apesar de se basear somente na granulometria, apresentou uma eficiência razoável na separação mineralógica, assim como os ensaios de decantação, onde se verificou que após 24 h a dolomita praticamente desaparece do sobrenadante. A determinação da curva cinética de adsorção mostrou que 2 h não é suficiente para que haja a adsorção do fósforo, sendo necessárias 24 h para atingir o equilíbrio da reação. Os ensaios de adsorção de fósforo mostraram eficiência acima de 91% do fósforo inicialmente presente na solução e o valor máximo adsorvido por grama da amostra foi de 0,607 mg. A correlação com os modelos de isotermas de adsorção estudados mostrou melhor resultado para a isoterma de Langmuir-Freundlich, com coeficiente de correlação 0,9993, o que pode ser atribuído ao fato da adsorção ocorrer em mais de uma camada.

G'day Gondwana - the final accretion of a supercontinent: U-Pb ages from the post-orogenic Sao Vicente Granite, northern Paraguay Belt, Brazil

The Paraguay Belt in central South America is part of a larger chain of orogenic belts, including the Araguaia Belt to the northeast and potentially the Pampean Belt to the south, which are believed to mark the suture zone of the Clymene Ocean - interpreted amongst the youngest of the Gondwana amalgamation orogens. The post-orogenic Sao Vicente Granite crops out in the northern Paraguay Belt and cuts the basal unit of the deformed and metamorphosed Cuiaba Group. The age of this granite therefore provides a long sort after minimum age for orogenesis within the belt. Dating crystallisation of this important intrusion is challenging due to the presence of considerable common-Pb. However, based on LA-ICPMS dating of more than 100 zircons from three separate samples we interpret a robust crystallisation age for the Sao Vicente batholith at 518 +/- 4 Ma. This age constrains the termination of deformation within the Paraguay Belt and the final accretion of the supercontinent Gondwana. (C) 2011 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.

The 1420 Ma Indiavai Mafic Intrusion (SW Amazonian Craton): Paleomagnetic results and implications for the Columbia supercontinent

The configuration and the timing of assembly and break-up of Columbia are still matter of debate. In order to improve our knowledge about the Mesoproterozoic evolution of Columbia, a paleomagnetic study was carried out on the 1420 Ma Indiavai mafic intrusive rocks that crosscut the polycyclic Proterozoic basement of the SW Amazonian Craton, in southwestern Mato Grosso State (Brazil). Alternating field and thermal demagnetization revealed south/southwest ChRM directions with downward inclinations for sixteen analyzed sites. These directions are probably carried by SD/PSD magnetite with high coercivities and high unblocking temperatures as indicated by additional rock magnetic tests, including thermomagnetic data, hysteresis data and the progressive acquisition of isothermal remanent magnetization. Different stable magnetization components isolated in host rocks from the basement 10 km NW away to the Indiavai intrusion, further support the primary origin of the ChRM. A mean of the site mean directions was calculated at Dm = 209.8 degrees, Im = 50.7 degrees (alpha(95) = 8.0 degrees, K = 22.1), which yielded a paleomagnetic pole located at 249.7 degrees E, 57.0 degrees S (A(95) = 8.6 degrees). The similarity of this pole with the recently published 1420 Ma pole from the Nova Guarita dykes in northern Mato Grosso State suggests a similar tectonic framework for these two sites located 600 km apart, implying the bulk rigidity of the Rondonian-San Ignacio crust at that time. Furthermore these data provide new insights on the tectonic significance of the 1100-1000 Ma Nova Brasilandia belt-a major EW feature that cuts across the basement rocks of this province, which can now be interpreted as intracratonic, in contrast to previous interpretation. From a global perspective, a new Mesoproterozoic paleogeography of Columbia has been proposed based on comparison of these 1420 Ma poles and a 1780 Ma pole from Amazonia with other paleomagnetic poles of similar age from Baltica and Laurentia, a reconstruction in agreement with geological correlations. (C) 2012 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.

Tectonic implications of the 1419 Ma Nova Guarita mafic intrusives paleomagnetic pole (Amazonian Craton) on the longevity of Nuna

The Nuna supercontinent was probably assembled in the Paleoproterozoic, but its paleogeography and the timing for its demise are stills matter of debate. A paleomagnetic and geochronological study carried out on the Mesoproterozoic Nova Guarita dyke swarm (northern Mato Grosso State, SW Amazonian Craton) provides additional constraints on the duration of this supercontinent. Paleomagnetic AF and thermal treatment revealed south/southwest (northeast) magnetic directions with downward (upward) inclinations for 19 analyzed sites. These directions are carried by PSD magnetite with high unblocking temperatures as indicated by additional magnetic tests, including thermomagnetic curves, hysteresis loops and the progressive acquisition of isothermal remanence in selected samples. A positive contact test with the host granite in one of the studied dykes further attests to the primary origin of the characteristic magnetic component. A mean site direction was calculated at D-m = 220.5 degrees, I-m = 45.9 degrees (alpha(95) = 6.5 degrees, K = 27.7), which yielded a paleomagnetic pole located at 245.9 degrees E, 47.9 degrees S (A(95) = 7.0 degrees). Ar-40/Ar-39 dating carried out on biotites from four analyzed dykes yielded well-defined plateau ages with a mean of 1418.5 +/- 3.5 Ma. The Nova Guarita pole precludes a long-lived Nuna configuration in which Laurentia, Baltica, North China, and Amazonia formed a long and continuous block as previously proposed for the Paleoproterozoic. It is nevertheless fully compatible with a SAMBA (Amazonia-Baltica) link at Mesoproterozoic times. (C) 2011 Elsevier B.V. All rights reserved.

Water management aeroportuale: Analisi sperimentale dell'accumulo di inquinanti in airside. Il caso dell'aeroporto G. Marconi di bologna.

Negli ultimi quindici anni il traffico aereo passeggeri in Italia è stato interessato da un cospicuo incremento: si è passati dai 91 milioni di passeggeri nel 2000 ai 150 milioni nel 2014. Le previsioni di crescita per il Paese indicano il possibile raddoppio del traffico entro il 2030, quando si dovrebbe raggiungere la soglia dei 300 milioni di passeggeri, con un aumento soprattutto della quota parte internazionale. Non vi può essere sviluppo economico di uno Stato senza crescita del traffico aereo, la quale si può realizzare solo con un adeguamento e un potenziamento delle capacità delle infrastrutture aeroportuali compatibile con le condizioni ambientali e un’efficace interconnessione degli scali con gli altri modi di trasporto. Infatti la pianificazione e la progettazione degli aeroporti non può prescindere da un’analisi approfondita sugli impatti ambientali prodotti dalle attività svolte all’interno degli scali. Inoltre l’incremento del numero medio di passeggeri per movimento (dal 75 pax/mov nel 2000 a 106 pax/mov nel 2011, dato riferito al traffico nazionale) rappresenta un dato positivo dal punto di vista ambientale: nei cieli vola un minor numero di aeromobili, ma in grado di trasportare un maggior numero di passeggeri, con conseguente diminuzione del numero dei movimenti, quindi del rumore, delle emissioni e dell’inquinamento ambientale provocato dalle operazioni necessarie a garantire l’operatività di ciascun volo. La salvaguardia dell’ambiente per un aeroporto è un compito difficile e oneroso, poiché può creare problemi ambientali come inquinamento acustico, dell’aria, delle acque fondiarie e trattamento dei rifiuti. In particolare, scopo di questo elaborato è studiare l’impatto che le operazioni svolte in air-side provocano sulla qualità delle acque di dilavamento, osservando e analizzando le attività che avvengono presso l’Aeroporto G. Marconi di Bologna. Si intende svolgere un censimento delle operazioni che influenzano la qualità delle acque (sia direttamente sia a seguito del dilavamento delle pavimentazioni aeroportuali), indagando quali siano i soggetti coinvolti, le procedure da eseguire, la frequenza e gli eventuali mezzi impiegati. Poi si vogliono eseguire analisi chimiche e granulometriche con un duplice obiettivo: conoscere la qualità delle acque raccolte dalle caditoie presenti nel piazzale e a bordo pista e verificare l’efficacia delle operazioni eseguite anche per ridurre il build up, cioè il tasso di accumulo in tempo secco e, di conseguenza, l’apporto di inquinanti riversato nelle acque di dilavamento. Infine si propongono interventi volti a incrementare la sostenibilità ambientale dell’infrastruttura aeroportuale, con particolare attenzione alla riduzione dell’inquinamento idrico.

Detrital Zircon Evidence for Non-Laurentian Provenance, Mesoproterozoic (ca. 1490-1450 Ma) Deposition and Orogenesis in a Reconstructed Orogenic Belt, Northern New Mexico, USA: Defining the Picuris Orogeny

Detrital zircon and igneous zircon U-Pb ages are reported from Proterozoic metamorphic rocks in northern New Mexico. These data give new insight into the provenance and depositional age of a >3-km-thick metasedimentary succession and help resolve the timing of orogenesis within an area of overlapping accretionary orogens and thermal events related to the Proterozoic tectonic evolution of southwest Laurentia. Three samples from the Paleoproterozoic Vadito Group yield narrow, unimodal detrital zircon age spectra with peak ages near 1710 Ma. Igneous rocks that intrude the Vadito Group include the Cerro Alto metadacite, the Picuris Pueblo granite, and the Penasco quartz monzonite and yield crystallization ages of 1710 +/- 10 Ma, 1699 +/- 3 Ma, and 1450 +/- 10 Ma, respectively. Within the overlying Hondo Group, a metamorphosed tuff layer from the Pilar Formation yields an age of 1488 +/- 6 Ma and represents the first direct depositional age constraint on any part of the Proterozoic metasedimentary succession in northern New Mexico. Detrital zircon from the overlying Piedra Lumbre Formation yield a minimum age peak of 1475 Ma, and similar to 60 grains (similar to 25%) yield ages between 1500 Ma and 1600 Ma, possibly representing non-Laurentian detritus originating from Australia and/or Antarctica. Detrital zircons from the basal metaconglomerate and the middle quartzite member of the Marquenas Formation yield minimum age peaks of 1472 Ma and 1471 Ma, consistent with earlier results. We interpret the onset of ca. 1490-1450 Ma deposition followed by tectonic burial, regional Al2SiO5 triple-point metamorphism, and ductile deformation at depths of 12-18 km to reflect a Mesoproterozoic contractional orogenic event, possibly related to the final suturing of the Mazatzal crustal province to the southern margin of Laurentia. We propose to call this event the Picuris orogeny.

Exemestane Versus Anastrozole in Postmenopausal Women With Early Breast Cancer: NCIC CTG MA.27—A Randomized Controlled Phase III Trial

PURPOSE In patients with hormone-dependent postmenopausal breast cancer, standard adjuvant therapy involves 5 years of the nonsteroidal aromatase inhibitors anastrozole and letrozole. The steroidal inhibitor exemestane is partially non-cross-resistant with nonsteroidal aromatase inhibitors and is a mild androgen and could prove superior to anastrozole regarding efficacy and toxicity, specifically with less bone loss. PATIENTS AND METHODS We designed an open-label, randomized, phase III trial of 5 years of exemestane versus anastrozole with a two-sided test of superiority to detect a 2.4% improvement with exemestane in 5-year event-free survival (EFS). Secondary objectives included assessment of overall survival, distant disease-free survival, incidence of contralateral new primary breast cancer, and safety. RESULTS In the study, 7,576 women (median age, 64.1 years) were enrolled. At median follow-up of 4.1 years, 4-year EFS was 91% for exemestane and 91.2% for anastrozole (stratified hazard ratio, 1.02; 95% CI, 0.87 to 1.18; P = .85). Overall, distant disease-free survival and disease-specific survival were also similar. In all, 31.6% of patients discontinued treatment as a result of adverse effects, concomitant disease, or study refusal. Osteoporosis/osteopenia, hypertriglyceridemia, vaginal bleeding, and hypercholesterolemia were less frequent on exemestane, whereas mild liver function abnormalities and rare episodes of atrial fibrillation were less frequent on anastrozole. Vasomotor and musculoskeletal symptoms were similar between arms. CONCLUSION This first comparison of steroidal and nonsteroidal classes of aromatase inhibitors showed neither to be superior in terms of breast cancer outcomes as 5-year initial adjuvant therapy for postmenopausal breast cancer by two-way test. Less toxicity on bone is compatible with one hypothesis behind MA.27 but requires confirmation. Exemestane should be considered another option as up-front adjuvant therapy for postmenopausal hormone receptor-positive breast cancer.

Or Meʾir : kolel reshimat sifre Yiśraʾel, kitve yad ṿe-nidpasim, ha-nimtsaʾim be-vet otsar sefarim ha-gadol shel ... Meʾir Zultsberger be-Filadelfya; ʿim heʿarot, maʾamarim ṿe-shirim mi-kitve yad shonim ...

me-et Efrayim Deinard