Relevant bibliographies by topics / Pinerolo (Italy)

Academic literature on the topic 'Pinerolo (Italy)'

Author: Grafiati
Published: 27 July 2024
Last updated: 28 July 2024

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Journal articles on the topic "Pinerolo (Italy)"

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Ilgren, Edward B., Carlo Sartorio, and John Hoskins. "Analysis of an Authentic Historical Italian Cosmetic Talc Sample – Further Evidence for the Lack of Cancer Risk." Environment and Pollution 6, no. 2 (September 29, 2017): 6. http://dx.doi.org/10.5539/ep.v6n2p6.

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Italian talc from the Pinerolo Mines in North West Italy is known for its extreme purity. Several historical investigations of these mines have demonstrated very small amounts of tremolite in the host rock that occasionally found their way into the mined ore. However, more than sixty years of epidemiological studies of the Pinerolo miners and millers have failed to demonstrate any attendant cancer risk and show that this trace tremolite contamination is of no biological significance.Claims made that the Pinerolo Italian cosmetic talc produced prior to 1975 were contaminated with asbestos, principally tremolite, have been difficult to refute given the lack of authentic historical samples of commercial products. We now describe the analytical findings of a recently discovered authentic historical sample.Sample analyses of this material showed only a few non-asbestiform tremolite fibres - a finding discussed in the light of the historical (pre-1975) studies of this talc deposit: no serpentine (chrysotile) or amphibole fibres were detected.The numerical concentration of tremolite fibres in the talc sample was 3.687 x 106 fibres/gram, corresponding to a mass concentration of 0.722 parts per million.
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Wójcik, Zbigniew. "Italian Horse Riding School." Physical education, sport and health culture in modern society, no. 1 (49) (March 31, 2020): 60–63. http://dx.doi.org/10.29038/2220-7481-2020-01-60-63.

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The system solutions in the field of horse riding technique appeared for the first time in Italy in the 16th century, but at the same time equestrian academies also functioned in other countries, e.g. Austria, France, Germany and Russia. They formed the horse riding system which was based on such movements that horse never performs in its natural habitat. Therefore, according to the methodology research, applicable in historical and pedagogical sciences, an attempt was made to determine stages of the Art of Horsemanship on the European continent. In the research process, it was established that the horse riding style that had been being practiced for several centuries, was not changed until the late 19th century. The revolutionary changes, based on years of observation and experience, were made by Captain Federico Caprilli of the Military Equestrian School in Pinerolo (Italy). The result of his observations accepeted in 1906 was an innovative horse riding system called natural. A great numer of officers from 22 countries were coming to Italy at that time to learn the new system. As it was very practical, it became quickly adapted by equestrian sport.
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3

Pratesi, M., A. Lazzero, P. Ribet, M. Ribet, A. Marciello, P. Rolando, G. Falcone, et al. "Flood Disaster in Northern Italy: The Experience of the Azienda Sanita Locale (ASL) 10 in Pinerolo (Torino)." Prehospital and Disaster Medicine 16, S1 (June 2001): S56. http://dx.doi.org/10.1017/s1049023x00036165.

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Tamietti, G. "First Report of Phytophthora cinnamomi on High-Bush Blueberry in Italy." Plant Disease 87, no. 4 (April 2003): 451. http://dx.doi.org/10.1094/pdis.2003.87.4.451c.

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Beginning in the summer of 1996, a disease of high-bush blueberry (Vaccinium corymbosum L.) appeared on cvs. Sparta and Berkeley in commercial plantings near Cuneo and in a nursery in Pinerolo (northwest Italy). In the field, the disease became evident 5 to 8 months after planting. Symptoms included stunting, pale green-to-reddish leaves, premature defoliation, and root and crown rot. The root system was reduced, with few feeder roots and a dark discoloration of the root cortex. Root, crown, and basal stem rot led to death of the plants. Pieces of the discolored organs were surface-sterilized in sodium hypochlorite (2%) for 5 min, rinsed in sterile water, dried on sterile filter paper, and plated on acidified malt extract agar (pH 4.6) (MEA) and a selective medium for oomycetes (2). Slow-growing colonies developed on MEA, whereas colonies characteristic of Phytophthora spp. grew on the selective medium for oomycetes. Six isolates from plants collected from the field and the nursery were inoculated as V8 juice culture homogenate on the roots of blueberry cv. Berkeley, azalea, and 1-year-old chestnut plants in pots. All six isolates reproduced the symptoms in blueberry and caused root and foot rot in the other hosts. The original fungus was reisolated from all inoculated hosts. The isolates were examined and compared with strain 0229 of P. cinnamomi Rands from the International Mycological Institute. They were identified as P. cinnamomi on the basis of morphological characteristics and total mycelial soluble protein patterns on sodium dodecyl sulfate-polyacrylamide gel electrophoresis. In Italy, blueberry is a new host for this pathogen that was previously observed in rhododendron (1), and recently in chestnut (3) and other forest species. Because of the high risk of spreading the pathogen to areas where susceptible plants are grown, it is recommended that high-bush blueberry nursery stock be tested for the pathogen. References: (1) G. Gullino and A. Garibaldi. La difesa delle piante 10:273, 1987; (2) H. Masago et al. Phytopathology 67:425, 1977. (3) A. M. Vettraino et al. Plant Pathol. 50:90, 2001.
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5

Nosenzo, Francesco, Paola Manzotti, Mikaela Krona, Michel Ballèvre, and Marc Poujol. "Tectonic architecture of the northern Dora-Maira Massif (Western Alps, Italy): field and geochronological data." Swiss Journal of Geosciences 117, no. 1 (April 22, 2024). http://dx.doi.org/10.1186/s00015-024-00459-2.

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AbstractHigh-pressure and ultra-high-pressure metamorphic terrains display an internal architecture consisting of a pile (or stack) of several coherent tectonic thrust sheets or units. Their identification is fundamental for understanding the scale and mechanisms active during subduction and exhumation of these crustal slices. This study investigates the geometry of the northern Dora-Maira Massif and the kinematics of the major tectonic boundaries, combining field and geochronological data. The tectonic stack of the northern Dora-Maira Massif comprises the following units. The lowermost unit (the Pinerolo Unit) is mainly characterized by Upper Carboniferous fluvio-lacustrine (meta-)sediments. The Pinerolo unit is overthrust by a pre-Carboniferous basement. The latter is subdivided in two tectonic units (the Chasteiran and Muret Units) with different Alpine metamorphism (ultra-high-pressure and high-pressure, respectively). The pre-Carboniferous basement of the Muret Unit is thicker than previously thought for two main reasons. Firstly, some paragneisses, traditionally assumed to be Carboniferous and/or Permian in age, display detrital zircon ages indicating a main source at about 600 Ma. Secondly, three samples of the Granero Orthogneiss, previously assumed to be a Permian intrusive body, have provided zircon U–Pb ages of 447 ± 1 Ma, 456 ± 2 Ma and 440 ± 2 Ma, indicating a late Ordovician or early Silurian age for the protoliths. The uppermost unit (the Serre Unit) comprises porphyritic (meta-) volcanic and volcaniclastic rocks dated to the Permian (271 ± 2 Ma), on top of which remnants of the Mesozoic cover is preserved. Detailed mapping of an area about 140 km2 shows that (i) the ultra-high pressure Chasteiran Unit is localized at the boundary between the Pinerolo and Muret Units, (ii) the Granero Orthogneiss may be considered as the mylonitic sole of the Muret Unit, characterized by a top-to-W sense of shear, and (iii) the contact between the Muret and Serre Units displays ductile-to brittle structures (La Fracho Shear Zone), indicating a top-to-the-NW displacement of the hangingwall with respect to the footwall. A final episode of brittle faulting, cutting across the nappe stack (the Trossieri Fault), indicates an extensional stage in the core of the Alpine belt, as previously documented in more external zones. This work provides a necessary and robust basis before an accurate discussion of processes acting during continental subduction of the Dora-Maira Massif may be understood.
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Dissertations / Theses on the topic "Pinerolo (Italy)"

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Povero, Chiara. "Missioni in terra di frontiera : la Controriforma nelle valli del Pinerolese, secoli XVI - XVIII /." Roma : Istituto Storico dei Cappuccini, 2006. http://www.loc.gov/catdir/toc/casalini03/06920600.pdf.

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Books on the topic "Pinerolo (Italy)"

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Avondo, Gian Vittorio. Il Gibuti: Storia della tramvia Pinerolo- Perosa Argentina. Torino: Kosmos, 1995.

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2

Gontier, Mario. Pinerolo: Città della cavalleria : il fascino dell'uniforme a cavallo di due secoli. Pinerolo: Alzani, 1999.

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3

Pucciarelli, Mauro. Esercito e tradizioni a Roma, Torino e Pinerolo: Un viaggio negli storici musei militari d'Italia = The Italian Army and its traditions : a journey through the military historical museums of Rome, Turin, Pinerolo. [Milano]: F. Motta, 1990.

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4

Collezione civica d'arte di Palazzo Vittone (Pinerolo, Italy). Pinerolo: La Collezione civica d'arte di Palazzo Vittone. Pinerolo [Italy]: Tipolitografia Giuseppini, in collaborazione con la Collezione civica d'arte di Palazzo Vittone, 1994.

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5

Alexandrou, Charalampos K. Merarchia Pinerolo: Chroniko tēs antistasēs kai tou martyriou tēs, Septemvios 1943-Dekemvrios 1944. Athēna: Ekdoseis Gruppo D' Arte, 2008.

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6

G, Bahn Paul, and Fossati Angelo 1958-, eds. Rock art studies: News of the world I : recent developments in rock art research (acts of symposium 14D at the NEWS95 World Rock Art Congress, Turin and Pinerolo, Italy). Oxford: Oxbow Books, 1996.

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Avondo, Gian Vittorio. Il Gibuti: Storia della tramvia Pinerolo- Perosa Argentina. Kosmos, 1995.

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Book chapters on the topic "Pinerolo (Italy)"

1

Pede, Elena, Mattia Scalas, and Luca Staricco. "Analysis of Hydrogeological Risks Related to Climate Change: Testing the ClimeApp Assessment Tool on the Torino Nord Homogenous Zone." In The Urban Book Series, 111–21. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-33894-6_9.

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AbstractThe current changes in temperatures and precipitations can lead to increased frequency and magnitude of natural hazards such as floods, resulting in forthcoming losses of life and damages to private and public properties. This paper presents an applied hydrogeological risk assessment methodology developed as part of an interdisciplinary European project between France and Italy (Interreg Alcotra ARTACLIM). A practical framework is proposed to assess the risk for urban settlements and infrastructural assets at a sub-regional level, within one of the 11 homogeneous zones of the Turin Metropolitan City, the “Torino Nord” Homogeneous Area of Pinerolo (ZOP). Based on the most reliable guidelines of institutions and organizations such as IPCC, United Nations, Covenant of Mayors for Climate & Energy EUROPE, the methodology here presented identifies risks related to climate change as a function of hazard (H), exposure (E) and vulnerability (V) factors, the latter one being in turn a function of sensitivity (S) and adaptive capacity (AC). Each factor is operationalized through specific indicators. The results of the analysis generate a geo-localized risk score that can be used to support urban planners and local policymakers to prioritize the adaptation measures required for reducing hydrogeological damages related to climate change.
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