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Peer Reviewed
See detailGrossesses prolongées et risques psycho-médicaux
Halin, Stéphanie; Emonts, Patrick ULg; Fohn, Bruno et al

Poster (2014, December)

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See detailGrote en kleine geschiedenis van de infectieziekten en micro-organismen
Mainil, Jacques ULg; De Graef, Evelyne

in Vlaams Diergeneeskundig Tijdschrift (2005), 74

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See detailGrote scheppen zoete broodpap : de receptie van Hendrik Conscience in Frankrijk
Andringa, Kim ULg

in Verslagen en Mededelingen van de Koninklijke Academie voor Nederlandse Taal- en Letterkunde (2013), 123(2/3),

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See detailEen groteske revolutie. Over Van Ostaijens 'film met jazzbegeleiding' De bankroet jazz
Spinoy, Erik ULg

in Poëziekrant (2010), 34(2), 50-57

This article reads De bankroet jazz, a satiric film script by the Flemish expressionist Paul van Ostaijen, within the context of his ideological and literary development.

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See detailGrotesque et ironie dans le théâtre de Jean-Marie Piemme
Delhalle, Nancy ULg

in Textyles : Revue des Lettres Belges de Langue Française (2006), 29

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See detailThe Grotesque
Delville, Michel ULg

Learning material (2008)

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See detailGrotesques, concrétions et paysages
Havelange, Carl ULg; Christiaens, Alexandre

Book published by Les Brasseurs/art contemporain (2007)

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See detailLa grotte d'Öküzini: chronologie et mode de fonctionnement d'un remplissage (analyse radiométrique, rythme sédimentaire et cycles climatiques)
López Bayón, Ignacio; Léotard, Jean-Marc; Kartal, Metin et al

in Yalçinkaya, Isin; Otte, Marcel; Kozlowski, Janusz (Eds.) et al La grotte d'Öküzini. Évolution du Paléolithique final du sud-ouest de l'Anatolie (2002)

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See detailLa grotte de Remouchamps
Ek, Camille ULg; Dewez, Michel; Denoël, René et al

Book published by Lesire (1972)

The first inhabitants of the cave. Explorations history. Geology. Cave genesis. Speleothems genesis. The cave climate. Fauna. The swallowhole Dale.

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See detailLa grotte de Remouchamps: compte rendu de l'excursion de la Société Géographiqe de Liège le 28 mai 1969
Ek, Camille ULg

in Bulletin de la Société Géographique de Liège (1970), 6

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See detailLa grotte de Spy (Jemeppe-sur-Sambre ; prov. Namur)
Semal, Patrick; Jungels, Cécile; Di Modica, Kevin et al

in Toussaint, Michel; Di Modica, Kevin; Pirson, Stéphane (Eds.) Le Paléolithique moyen en Belgique. Mélanges Marguerite Ulrix-Closset (2011)

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See detailLa Grotte du Bois Laiterie, du Magdalénien au Mésolithique: différences comportementales
López Bayón, Ignacio; Straus, Lawrence; Otte, Marcel ULg et al

in Notae Praehistoricae (1996), 16

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See detailLa Grotte et l'Abîme de Comblain-au-Pont
Ek, Camille ULg; Godissart, Jean

Book published by Découverte de Comblain-au-Pont et environs, ASBL (2007)

Summary: Historical review; Geology; Cave genesis; Climate; Fauna; Paleontology

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See detailLes grottes d'Azé (Saône-et-Loire, France): de la roche altérée aux sédiments
Barriquand, Lionel; Barriquand, Johan; Baele, Jean-Marc et al

in Karstologia (2012), 59

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See detailLes Grottes d'Azé: contexte géologique et encaissant calcaire jurassique
Dechamps, Sylvain ULg; Boulvain, Frédéric ULg; Barriquand, Lionel et al

Book published by Département de Saône-et-Loire (2015)

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See detailLes grottes de la Serra d’Itaqueri, exemple de karsts dans les grès, Brésil
Willems, Luc ULg; Hardt, Rubens; Rodet, Joël

Conference (2012)

Dans l’état de Sao Paulo, au Brésil, de nombreuses cavités sont trouvées dans des grès continentaux du Jurassique affleurant dans le front de la cuesta d’Itaqueri. Ces grottes se développent ... [more ▼]

Dans l’état de Sao Paulo, au Brésil, de nombreuses cavités sont trouvées dans des grès continentaux du Jurassique affleurant dans le front de la cuesta d’Itaqueri. Ces grottes se développent subhorizontalement dans une lithologie compacte et non carbonatée. Elles peuvent s’enfoncer d’une centaine de mètres à dans le massif. Précédemment, plusieurs auteurs ont donné aux différentes failles parcourant les roches un rôle prépondérant dans la genèse des cavités. Deux hypothèses ont été proposées pour leur formation: une dissolution en profondeur, aux nœuds de fracturation et/ou une évacuation mécanique postérieure des résidus d’altération par des écoulements percolant à travers le massif et résurgeant dans le front de cuesta. Pourtant, plusieurs observations telles que l’absence de circulation d'eau à l’intérieur des grottes ou la dislocation de morphologies anciennes par les différentes fractures contredisent ces deux propositions. Les accidents répertoriés au sein des cavités sont datés de 126 Ma et viennent démanteler plus qu’accompagner le développement des systèmes souterrains préexistants. Ces failles permettent de déterminer une karstification initiale des grès antérieure, vraisemblablement en milieu noyé. [less ▲]

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See detailGrottes et rivières des régions calcaires
Ek, Camille ULg

in Demoulin, Alain (Ed.) L'Ardenne, Essai de Géographie physique. Hommage à A. Pissart (1995)

Location of soluble rocks and karstic areas. Morphology of closed depressions. Valleys of limestone regions; dry valleys; blind valleys. Caves. Present-day processes.

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See detailGround and Excited State Dissociation Dynamics of Ionized 1,1-Difluoroethene
Gridelet, Evelyne; Dehareng, Dominique ULg; Locht, Robert ULg et al

in Journal of Physical Chemistry A (2005), 109(37), 8225-8235

The kinetic energy release distributions (KERDs) for the fluorine atom loss from the 1,1-difluoroethene cation have been recorded with two spectrometers in two different energy ranges. A first experiment ... [more ▼]

The kinetic energy release distributions (KERDs) for the fluorine atom loss from the 1,1-difluoroethene cation have been recorded with two spectrometers in two different energy ranges. A first experiment uses dissociative photoionization with the He(I) and Ne(I) resonance lines, providing the ions with a broad internal energy range, up to 7 eV above the dissociation threshold. The second experiment samples the metastable range, and the average ion internal energy is limited to about 0.2 eV above the threshold. In both energy domains, KERDs are found to be bimodal. Each component has been analyzed by the maximum entropy method. The narrow, low kinetic energy components display for both experiments the characteristics of a statistical, simple bond cleavage reaction: constraint equal to the square root of the fragment kinetic energy and ergodicity index higher than 90%. Furthermore, this component is satisfactorily accounted for in the metastable time scale by the orbiting transition state theory. Potential energy surfaces corresponding to the five lowest electronic states of the dissociating 1,1-C2H2F2+ ion have been investigated by ab initio calculations at various levels. The equilibrium geometry of these states, their dissociation energies, and their vibrational wavenumbers have been calculated, and a few conical intersections between these surfaces have been identified. It comes out that the ionic ground state (X) over tilde B-2(1) is adiabatically correlated with the lowest dissociation asymptote. Its potential energy curve increases in a monotonic way along the reaction coordinate, giving rise to the narrow KERD component. Two states embedded in the third photoelectron band ( (B) over tilde (2)A(1), at 15.95 eV and (C) over tilde B-2(2) at 16.17 eV) also correlate with the lowest asymptote at 14.24 eV. We suggest that their repulsive behavior along the reaction coordinate be responsible for the KERD high kinetic energy contribution. [less ▲]

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See detailGround beetle habitat templets and riverbank integrity
van Looy, K.; Vanacker, S.; Jochems, H. et al

in River Research & Applications (2005), 21(10), 1133-1146

The habitat templet approach was used in a scale-sensitive bioindicator assessment for the ecological integrity of riverbanks and for specific responses to river management. Ground beetle habitat templets ... [more ▼]

The habitat templet approach was used in a scale-sensitive bioindicator assessment for the ecological integrity of riverbanks and for specific responses to river management. Ground beetle habitat templets were derived from a catchment-scale sampling, integrating the overall variety of bank types. This coarse-filter analysis was integrated in the reach-scale fine-filtering approaches of community responses to habitat integrity and river management impacts. Higher species diversity was associated with the higher heterogeneity in bank habitats of the un-navigable river reaches. The abundant presence of habitat specialists in the riverbank zone allows a habitat integrity assessment based on the habitat templet indicator species. Significant responses were detected for channel morphology in the width-to-depth ratio and for hydrological regime in peak frequency and peak velocity, enabling the development of evaluation methods for the impact assessment of river management and flood protection strategies. Copyright © 2005 John Wiley & Sons, Ltd. [less ▲]

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