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See detailEvolution du profil en azote des sols agricoles du sud de la Belgique.
Tychon, Bernard ULg; Guiot, S.; Debbaut, Vincent ULg et al

Conference (1990, November)

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See detailL'évolution du programme du Parti Social Chrétien / Christelijke Volkspartij (Noël 1945 - 1968). Éléments pour une histoire des idées sociales-chrétiennes
Jadoulle, Jean-Louis ULg

in W. DEWACHTER, G.-H. DUMONT, M. DUMOULIN, E. GERARD, E. LAMBERTS, X. MABILLE et M. VAN DEN WIJNGAERT (Ed.) Un Parti dans l'histoire, 1945-1995. 50 ans d'action du Parti Social Chrétien (1995)

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See detailEvolution du relief au Niger occidental : rôle de la fracturation du socle précambrien et de la formation de pseudo-karsts au sein de la lithomarge et de la couverture sédimentaire
Willems, Luc ULg; Lenoir, François; Levecq, Jean-Marie et al

in Comptes-Rendus de l'Académie des Sciences de Paris (1993), 317(Série II), 97-102

The observation of several forms in the Precambrian formations, in Tertiary and Quaternary deposits brings us to propose a model of topographic evolution mainly generated by a pseudo-karst. This latter is ... [more ▼]

The observation of several forms in the Precambrian formations, in Tertiary and Quaternary deposits brings us to propose a model of topographic evolution mainly generated by a pseudo-karst. This latter is developed in sedimentary deposits and in the lithomargin, in relation with fracturation of the basement. [less ▲]

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See detailEvolution du risque lié aux inondations de la Meuse : Influences relatives du climat et de la croissance des zones résidentielles
Beckers, Arnaud ULg; Detrembleur, Sylvain; Dewals, Benjamin ULg et al

Scientific conference (2013, February 28)

Chaque année, les inondations par débordement des rivières provoquent des dommages significatifs en Wallonie. L’ampleur de ceux-ci est liée à l’importance des crues elles-mêmes, mais aussi à l’occupation ... [more ▼]

Chaque année, les inondations par débordement des rivières provoquent des dommages significatifs en Wallonie. L’ampleur de ceux-ci est liée à l’importance des crues elles-mêmes, mais aussi à l’occupation du sol des terrains inondés. Dans le contexte des changements climatiques, comment évolueront les débits des crues « extrêmes » ? Quelle pourrait être l’influence de l’évolution de l’occupation du sol sur les dommages ? La vallée de la Meuse a été choisie pour investiguer et concrétiser les réponses à ces questions. Les dommages liés à une crue centennale ont été calculés pour la situation actuelle ainsi que pour différentes situations potentielles en 2100, suivant un scénario d’évolution climatique et neuf scénarios d’urbanisation de la Wallonie. L'accent sera mis sur tant sur le développement de ces scénarios que sur les conclusions robustes tirées des résultats obtenus en termes d’influence relative du climat et de l’occupation du sol sur les dommages futurs. [less ▲]

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See detailEvolution du statut des parties au procès pénal. Du Code d'instruction criminelle au projet de Code de procédure pénale
Chichoyan, Daisy ULg; Jacobs, Ann ULg

in Revue de Droit Pénal et de Criminologie (2007)

Article rédigé pour les cent ans de publication de la revue de droit pénal et de criminologie - la contribution passe en revue l'évolution des droits de chacune des parties dans le procès pénal.

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See detailL'évolution du système défensif au château de Franchimont
Hoffsummer, Patrick ULg

in Histoire et archéologie spadoises (1980), (juin), 87-97

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See detailEvolution du taux de cortisol plasmatique chez le veau de la naissance à l'âge de 14 jours
Massip, Alban; Wouters-Ballman, Patricia; Beckers, Jean-François ULg et al

in Comptes Rendus de l'Académie des Sciences de Paris (1977), 285

Plasma cortisol was recorded in 15 calves from birth to 14 days of age by a radioimmunoassay technique. At birth mean cortisol value is 67.3 ng/ml; 6 hours later it decreases by 58.4% then it gradually ... [more ▼]

Plasma cortisol was recorded in 15 calves from birth to 14 days of age by a radioimmunoassay technique. At birth mean cortisol value is 67.3 ng/ml; 6 hours later it decreases by 58.4% then it gradually diminishes and about 14 days after, it reaches adult levels (5.1 ng/ml). [less ▲]

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See detailL'évolution du vivant... un enseignement à (re)construire.
Hindryckx, Marie-Noëlle ULg

in TRACeS de ChanGements (2009), 193

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See detailEvolution économique de l'agriculture en province de Hainaut et perspectives
Burny, Philippe ULg

Conference given outside the academic context (1996)

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See detailL'évolution économique de la province de Liège depuis 1960
Merenne-Schoumaker, Bernadette ULg

in La Géographie (1971), (91), 215-234

Analysis of changes in the economy of Liege between 1960 and 1970

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See detailÉvolution et fréquence des inondations de l'Ourthe inférieure.
Pauquet, A.; Petit, François ULg

in Bulletin de la Société Belge d'Etudes Géographiques = Tijdschrift van de Belgische Vereniging voor Aardrijkskundige Studies (1993)

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See detailEvolution et systématique du genre Pinus
Toussaint, André ULg

in Annales de la Société Belge de Dendrologie = Jaarboek van de Belgische Dendrologische Vereniging (2012), 2010

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See detailÉvolution géomorphologique du littoral occidental de la péninsule tingitane (Maroc)
El Abdellaoui, Jamal ULg

Doctoral thesis (2014)

This work traces the geomorphological evolution of the western coast of the tingitane Peninsula (Morocco) in two time scales: the current scale and the Quaternary scale. Geomorphological characteristics ... [more ▼]

This work traces the geomorphological evolution of the western coast of the tingitane Peninsula (Morocco) in two time scales: the current scale and the Quaternary scale. Geomorphological characteristics have been identified and placed into their morphotectonic and/or morphodynamic contexts. To make our work more interesting, fruitful and realistic, we adopted an empirical approach. Firstly, we based our research on collection of data and analysis of available documents. Secondly, we made measurements, using appropriate techniques to answer specific questions, or to argue the hypotheses. It appears from this study, that the organization of geological units in a NNW-SSE direction has created a rugged shore, mainly in rocky cliff and pocket beaches on the Strait of Gibraltar coast, and a low sandy coast on the Atlantic coast. The geological and geomorphological quaternary history of Gibraltar Strait coast is characterized by a series of marine abrasion stepped and raised surfaces. The history of the Atlantic coast is rather marked by tectonic subsidence. This tectonic subsidence is manifested on the surface by a system of closed depressions (daya) arranged in a NNW-SSE axis, almost parallel to the orientation of geological units. The evolution of the geomorphological depressions is also controlled by the fluvio-marine action and wind activity. The last interglacial period is marked by two transgressive pulsations of eustatic origin. They were recorded at the marine terraces on both coasts. The second pulsation is aged at least 119.6 ± 2.3 ky. After the last interglacial, the central area of the Strait of Gibraltar was raised by an average of 8.1mm/100year from 117ky. The Ouljien was raised to a height of 13 to 16m. The Atlantic coast was stable at 117ky. Marine terraces are 5-6m high. The analysis shows that the current morphodynamics of the Atlantic coast are characterized by a barred beach geomorphology with a high spatio-temporal variability. It appears that a land wind plays a key role in the morphosedimentary evolution of backshore and foreshore. Indeed, the backshore develops, by negative retroaction, a geomorphology with a dune system to slow transport operated by land winds from the east. The foreshore, meanwhile, develops, by a positive retroaction, a system of bar and rip channels to counter a change in slope generated by the wind. On the one hand, risk analysis shows that the succession of anthropic changes at Tangier Bay has brooked the internal sediment balance. Erosion has affected both the sandy and rugged beaches of the eastern sector. The Atlantic coast doesn’t show signs of erosion, but it has a high vulnerability, because it evolves in a closed sedimentary system. On the other hand, the characteristic of a low open ocean coast facilitates the penetration of marine waters within the continent, especially the lower areas. Finally, a barred beach geomorphology creates problems of harbor silting and access disruption. [less ▲]

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See detailL'évolution géomorphologique du plateau des Hautes Fagnes et de son versant septentrional
Demoulin, Alain ULg

in Bulletin de la Société Belge d'Etudes Géographiques = Tijdschrift van de Belgische Vereniging voor Aardrijkskundige Studies (1980)

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See detailEvolution in the Sample Preparation for the Measurement of POPs in Biological Matrices
Focant, Jean-François ULg

Scientific conference (2012, August)

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See detailUne évolution inéluctable
Reginster, Jean-Yves ULg

in Jeune Pratique (1991), 50

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See detailL'évolution jurisprudentielle sur la compétence relative aux projets à la fois privés et publics
Van Damme, Nathalie; Donnay, Luc ULg

in Leleu, Yves-Henri (Ed.) Chroniques notariales (2013)

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See detailL'évolution jurisprudentielle sur le statut du notaire
Donnay, Luc ULg

in Leleu, Yves-Henri (Ed.) Chroniques notariales (2013)

Detailed reference viewed: 8 (0 ULg)