Estimation of zero-sequence impedance of undergrounds cables for single-phase fault location in distribution systems with electric arc

This paper focus on the problem of locating single-phase faults in mixed distribution electric systems, with overhead lines and underground cables, using voltage and current measurements at the sending-end and sequence model of the network. Since calculating series impedance for underground cables is not as simple as in the case of overhead lines, the paper proposes a methodology to obtain an estimation of zero-sequence impedance of underground cables starting from previous single-faults occurred in the system, in which an electric arc occurred at the fault location. For this reason, the signal is previously pretreated to eliminate its peaks voltage and the analysis can be done working with a signal as close as a sinus wave as possible

Un Possible encaix de l’Euroregió Pirineus-Mediterrània en la figura de l’Agrupació Europea de Cooperació Territorial

Avui dia parlar de l’Euroregió i de les seves capacitats per optimitzar el nivell de cooperació no és estrany al mon del dret, però no sempre ha estat així. Ha calgut l’experiència positiva de diverses entitats regionals i locals d’arreu d’Europa per començar a reconèixer la importància d’aquest fenomen. Les regions europees havien iniciat diverses actuacions, algunes d'elles als inicis dels seixanta, amb l'objectiu de desenvolupar interessos comuns tractant que les fronteres estatals no suposessin una barrera insuperable. Estructures tal com l'Associació de Regions Frontereres Europees (ARFE), creada el 1969, o les accions dutes a terme per entitats territorials del denominat Arc Alpí (ARGE-ALP, ALPE-ADRIA i COTRAO) van constituir uns dels primers exemples de col·laboració permanent en el continent europeu. Així doncs, si bé a partir dels anys setanta (per posar una data orientativa) s’estengué la col·laboració d’entitats regionals i locals europees no va ser fins a la dècada dels noranta quan aquesta es va consolidar, sobretot pel llançament de les iniciatives comunitàries INTERREG que suposaren un recolzament econòmic a les actuacions empreses des dels seus organismes de cooperació

Cénotaphe [monument élevé à la mémoire des morts de la grande guerre près de l'Arc de Triomphe] : [photographie de presse] / [Agence Rol]

Référence bibliographique : Rol, 55023

[Installation du cénotaphe sous l'Arc de triomphe à l'occasion de la fête de la Victoire] : [photographie de presse] / [Agence Rol]

Référence bibliographique : Rol, 54816

[Installation du cénotaphe sous l'Arc de Triomphe dans le cadre de la fête de la Victoire] : [photographie de presse] / [Agence Rol]

Référence bibliographique : Rol, 54825

[Installation du cénotaphe sous l'Arc de triomphe à l'occasion de la fête de la Victoire] : [photographie de presse] / [Agence Rol]

Référence bibliographique : Rol, 54822

[Installation du cénotaphe sous l'Arc de triomphe à l'occasion de la fête de la Victoire] : [photographie de presse] / [Agence Rol]

Référence bibliographique : Rol, 54819

[Installation du cénotaphe sous l'Arc de triomphe à l'occasion de la fête de la Victoire] : [photographie de presse] / [Agence Rol]

Référence bibliographique : Rol, 54814

Structural and metamorphic evolution of the northern Himachal Himalaya, NW India - (Spiti-eastern Lahul-Parvati valley traverse)

The Himalayan orogen is the result of the collision between the Indian and Asian continents that began 55-50 Ma ago, causing intracontinental thrusting and nappe formation. Detailed mapping as well as structural and microfabric analyses on a traverse from the Tethyan Himalaya southwestward through the High Himalayan Crystalline and the Main Central Thrust zone (MCT zone) to the Lesser Himalayan Sequence in the Spiti-eastern Lahul-Parvati valley area reveal eight main phases of deformation, a series of late stage phases and five stages of metamorphic crystallization. This sequence of events is integrated into a reconstruction of the tectonometamorphic evolution of the Himalayan orogen in northern Himachal Pradesh. The oldest phase D-1 is preserved as relies in the High Himalayan Crystalline. Its deformational conditions are poorly known, but the metamorphic evolution is well documented by a prograde metamorphism reaching peak conditions within the upper amphibolite facies. This indicates that D-1 was an important tectonometamorphic event including considerable crustal thickening. The structural, metamorphic and sedimentary record suggest that D-1 most probably represents an early stage of continental collision. The first event clearly attributed to the collision between India and Asia is documented by two converging nappe systems, the NE-verging Shikar Beh Nappe and the SW-verging north Himalayan nappes. The D-2 Shikar Beh Nappe is characterized by isoclinal folding and top-to-the NE shearing, representing the main deformation in the High Himalayan Crystalline. D-2 also caused the main metamorphism in the High Himalayan Crystalline that was of a Barrovian-type, reaching upper amphibolite facies peak conditions. The Shikar Beh Nappe is interpreted to have formed within the Indian crust SW of the subduction zone. Simultaneously with NE-directed nappe formation, incipient subduction of India below Asia caused stacking of the SW-verging north Himalayan Nappes, that were thrust from the northern edge of the subducted continent toward the front of the Shikar Beh Nappe. As a result, the SW-verging folds of the D-3 Main Fold Zone formed in the Tethyan Himalaya below the front of the north Himalayan nappes. D-3 represents the main deformation in the Tethyan Himalaya, associated with a greenschist facies metamorphism. Folding within the Main Fold Zone subsequently propagated toward SW into the High Himalayan Crystalline, where it overprinted the preexisting D-2 structures. After subduction at the base of the north Himalayan nappes, the subduction zone stepped to the base of the High Himalayan Crystalline, where D-3 folds were crosscut by SW-directed D-4 thrusting. During D-4, the Crystalline Nappe, comprising the Main Fold Zone and relies of the Shikar Beh Nappe was thrust toward SW over the Lesser Himalayan Sequence along the 4 to 5 kms thick Main Central Thrust zone. Thrusting was related to a retrograde greenschist facies overprint at the base of the Crystalline Nappe and to pro-grade greenschist facies conditions in the Lesser Himalayan Sequence. Simultaneously with thrusting at the base of the Crystalline Nappe, higher crustal levels were affected by NE-directed D-5 normal extensional shearing and by dextral strike-slip motion, indicating that the high-grade metamorphic Crystalline Nappe was extruded between the low-grade metamorphic Lesser Himalayan Sequence at the base and the north Himalayan nappes at the top. The upper boundary of the Crystalline Nappe is not clearly delimited and passes gradually into the low-grade rocks at the front of the north Himalayan nappes. Extrusion of the Crystalline Nappe was followed by the phase D-6, characterized by large-scale, upright to steeply inclined, NE-verging folds and by another series of normal and extensional structures D-7+D-8 that may be related to ongoing extrusion of the Crystalline Nappe. The late stage evolution is represented by the phases D-A and D-B that indicate shortening parallel to the axis of the mountain chain and by D-C that is interpreted to account for the formation of large-scale domes with NNW-SSE-trending axes, an example of which is exposed in the Larji-Kullu-Rampur tectonic window.

[Préparatifs en vue du 14 juillet 1919, construction du cénotaphe sous l'arc de triomphe de l'Etoile] : [photographie de presse] / [Agence Rol]

Référence bibliographique : Rol, 54853