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  • Authors: Ould Mohamed, S.; Bruand, Ary;

    Abstract Ould Mohamed, S. and Bruand, A., 1994. Morphology and origin of secondary calcite in soils from Beauce France. In: A.J. Ringrose-Voase and G.S. Humphreys (Editors), Soil Micromorphology: Studies in Management and Genesis. Proc. IX Int. Working Meeting on Soil Micromorphology, Townsville, Australia, July 1992. Developments in Soil Science 22, Elsevier, Amsterdam, pp. 27–36.

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    Authors: Lassin, Arnault; Mercury, Lionel; Azaroual, Mohamed;

    International audience; In arid environments, porous media are unsaturated with water which is submitted to capillary constraints. The present chapter focuses on the geochemical impacts of such physical constraints and how theoretical analysis can help interpreting field or laboratory observations. The basic principles of capillary geochemistry suggest that the fate of contaminants, either organic or inorganic, can be significantly impacted in terms of reactive mass transfer in addition to flow and transport processes. All these mechanisms are closely interconnected, what makes the description of the behavior of such systems very complicated. An important work still has to be done in order to achieve such a goal: a number of mechanisms are not taken into account in the current state of development of the capillary geochemistry, namely mechanisms that occur in the thinnest confining geometries, like disjoining pressures, surface forces, etc.

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ https://hal-insu.arc...arrow_drop_down
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    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    https://doi.org/10.1007/978-94...
    Part of book or chapter of book . 2013 . Peer-reviewed
    License: Springer Nature TDM
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    Part of book or chapter of book . 2013
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ https://hal-insu.arc...arrow_drop_down
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
      https://doi.org/10.1007/978-94...
      Part of book or chapter of book . 2013 . Peer-reviewed
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      Part of book or chapter of book . 2013
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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: Yahyaoui, Zouhour; Sabatier, François; Rebai, Noamen; Abdeljaouad, Sâadi;

    Conference: 1st International Conference on Mapping and Spatial Analysis of Socio-Economic and Environmental Indicators for the Local and Regional Sustainable Development (SEE GEOMATICS)Location: Tataouine, TUNISIADate: MAR 25-26, 2015; International audience; For mapping the three-dimensional shape of the submarine bars, studying their dynamics and assessing the spatiotemporal evolution of sedimentary balances, the coastal prism of Korba (emerged and submerged beach) has benefitted from topo-bathymetric monitoring. This monitoring was carried out on an annual basis between July 2006 and July 2009. Numerical Terrain Models (N.T.M.) and transverse profiles were then analyzed. The main results show, firstly, that the shoreface of Korba is characterized by a homogeneous evolution across all profiles of its two-bar system. Moreover, the extent of changes in the sand volume of the beach suggests that the evolution takes place without significant sedimentary loss and that the beach is in a dynamic equilibrium. Accretion of the bars and migration towards the shore are found in periods of small waves (between July 2006 and July 2007). However, following a period of minor agitations, a filling of the outer trough is observed. It is proceeded by the migration of the outer bar towards the coast (between July 2007 and July 2009). These results confirm the traditional model of self-organization of a barred beach. These data and results, then, allow us to establish conceptual models and simulations of the evolution of the microtidal, barred beach of Korba.

    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao https://doi.org/10.1...arrow_drop_down
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    https://doi.org/10.1007/978-3-...
    Part of book or chapter of book . 2019 . Peer-reviewed
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      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao https://doi.org/10.1...arrow_drop_down
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      https://doi.org/10.1007/978-3-...
      Part of book or chapter of book . 2019 . Peer-reviewed
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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: Barbière, Franck; Marivaux, Laurent;

    Introduction The modern Afro-Asian porcupines, the African cane-, mole- and dassie-rats, as well as the South American guinea pigs, chinchillas, capybaras, pacas, agoutis, etc., make up the natural group of the hystricognathous rodents (infra-order Hystricognathi Tullberg, 1899). The phylogenetic relationships between the hystricognaths from South America (caviomorphs (Caviomorpha Wood, 1955)) and Africa (phiomorphs (Phiomorpha sensu Lavocat, 1967; Thryonomyoidea sensu Wood, 1955)) are today well-supported by a body of anatomical (e.g. Wood, 1974; Lavocat, 1976; Bugge, 1985; George, 1985; Meng, 1990; Luckett and Hartenberger, 1993; Martin, 1994) and molecular (e.g. Nedbal et al ., 1996; Huchon and Douzery, 2001; Huchon et al ., 2002, 2007; Poux et al ., 2006; Montgelard et al ., 2008; Blanga-Kanfi et al ., 2009; Churakov et al ., 2010) evidence, and also by endoparasite studies (e.g. Hugot, 1999). In contrast, the phylogenetic and geographic origins of hystricognaths have been the subject of considerable controversy over the past several decades (e.g. Wood and Patterson, 1959; Hoffstetter, 1972; Wood, 1972, 1973, 1974, 1985; Lavocat, 1973, 1974, 1976; Hussain et al ., 1978; Flynn et al ., 1986; Jaeger, 19; Huchon and Douzery, 2001, 2002; Marivaux et al ., 2002, 2004; Jaeger et al ., 2010a), and critical issues about their historical biogeography, notably their arrival in South America, are still a matter of on-going debate (e.g. Poux et al ., 2006; Bandoni de Oliveira et al ., 2009; Sallam et al ., 2009, 2011; Coster et al ., 2010; Antoine et al ., 2012). Although hystricognaths are absent from the earliest Tertiary fossil record at a global scale, their earliest known fossil occurrences date back to the late middle Eocene from both Africa and South America. This either suggests that hystricognaths have rapidly achieved a widespread distribution throughout the Old and New Worlds just after their emergence, or points out the existence of a significant Eocene gap in their fossil record. During the late Eocene and early Oligocene, the group exhibited a high diversity and morphological disparity on both landmasses, thereby suggesting a considerable amount of undocumented diversity in their early evolutionary history.

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    https://doi.org/10.1017/cbo978...
    Part of book or chapter of book . 2015 . Peer-reviewed
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      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao https://doi.org/10.1...arrow_drop_down
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      https://doi.org/10.1017/cbo978...
      Part of book or chapter of book . 2015 . Peer-reviewed
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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: Piégay, Hervé;

    The fluvial system is a complex adaptive process‐response system with two main physical components, the morphological system and the cascading system. The fluvial system changes progressively through geological time, as a result of normal erosional and depositional processes. The hydrosystem integrity depends on the dynamic interactions of hydrological, geomorphological and biological processes acting in these three dimensions over a range of time‐scales. The fluvial anthroposystem theory, with human pressures ubiquitous for many centuries, rivers are reacting to multiple human pressures acting at different time‐scales and different locations within the basin. Similarity analysis and connectivity analysis are ways to study the fluvial system in a comparative manner, one focusing on single temporal and spatial‐scale components, the other on the links between components of different scales. This chapter talks about research on the Drome, the Roubion, the Eygues and the Bega river to understand the system evolution and to inform management decisions. International audience deuxième édition

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    https://doi.org/10.1002/978111...
    Other literature type . 2016
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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: Damase Mouralis; Erkan Aydar; Ahmet Türkecan; Catherine Kuzucuoğlu;

    The southern Cappadocia shows a large variety of Quaternary volcanic landscapes, offering the opportunity to observe beautiful and generally fresh morphologies. These landscapes include two rhyolitic complexes (Golludag and Acigol), a huge composite volcano (Hasandag) and numerous monogenic vents, with scoria cones, domes and maars. Natural and anthropogenic sections show a large variety of lava flows and tephra layers. The precise study of this volcanic material allows reconstructing the volcanic and geomorphologic evolution of this area during the Quaternary, including modes of emplacements, chronology of the volcanic successions, morphological impacts on the landscapes. In addition, archaeological excavations in southern Cappadocia testify for the presence of ancient populations since the Middle to Upper Palaeolithic. During the Neolithic and Chalcolithic periods, the southern Cappadocia has been intensively occupied with permanent sites (Asikli Hoyuk, Musular, Tepecik Ciftlik, Kosk Hoyuk, etc.) as well as non-permanent sites devoted to mining and chopping of obsidian associated with some of the volcanoes.

    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao https://doi.org/10.1...arrow_drop_down
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    https://doi.org/10.1007/978-3-...
    Part of book or chapter of book . 2019 . Peer-reviewed
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    Authors: Khuntia, J; Proust, Sébastien; Khatua, K;

    International audience; We report here a laboratory study on the effects of bed roughness and emergent rigid veg-etation on the unsteady flows associated with flash floods and extreme flood events. The flow structure of unsteady open-channel flows over rough bed with and without emergent rigid vegetation has been investigated in an 18m long and 3m wide laboratory flume. Steady uniform flows were also studied and served as reference flows. For both steady and unsteady flows, two geometries are tested: (1) uniform bed roughness (uniform dense synthetic grass modelling meadow) along the flume and (2) a uniform staggered distribu-tion of emergent wooden circular cylinders (model of rigid vegetation) set on the bed roughness. Transient flow depths are simultaneously measured at six longitudinal positions using ultra-sonic sensors. Transient velocities are measured at one longitudinal position over the water column using a side looking ADV probe to estimate depth-averaged veloci-ty. In order to compute ensemble averages of the flow parameters, 109 runs of the same hydrograph are carried out repeatedly at the flume entrance. Two consecutive runs are separated by a base flow. The ensemble averages of the measured discharge, flow depths and velocity are found to be converged after 72 runs. For the two geometries: at the peak flow of the hydrograph, the vertical profiles of mean streamwise velocity and horizontal Reynolds shear stress are comparable to the profiles obtained for steady uniform cases of same flow depth; and accelerated and decelerated velocity profiles are obtained during the rising limb and falling limb of the hydrograph, respectively. Reynolds shear stresses are also found to be higher during the rising limb than during the falling limb for a fixed flow depth. The hysteresis in the depth-averaged velocity / flow depth relationships is compa-rable in shape and size for the two geometries highlighting the weak effect of the rigid vegetation compared to the effects of un-stationarity.

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    Other literature type . 2020
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    https://doi.org/10.1201/b22619...
    Part of book or chapter of book . 2020 . Peer-reviewed
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      Other literature type . 2020
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      https://doi.org/10.1201/b22619...
      Part of book or chapter of book . 2020 . Peer-reviewed
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    Lunar minerals and impact glasses, convert the polyatomic beam of solar wind (SW) ions into a flux of small molecules ( e.g. , H 2 , N 2 , H 2 O, CO, CO 2 , CH 4 , C 2 H 4 , C 2 H 6 , HCN, metal carbides and deuterides, etc.). They thus behave as “Solid State Molecular Reactors”. Moreover, ~100–200 μ m size micrometeoroids ( μ Ms) have also been exposed to the SW in the zodiacal cloud, before being captured by the Earth and recovered as Antarctic micrometeorites. They are mostly composed of a PAH-rich hydrous-carbonaceous material, which amplifies their power as molecular reactors. In particular, during the first ~200 Myr of the post-lunar period, about 75% of the μ Ms have been melted and/or volatilized upon atmospheric entry. The release of their volatile species triggered a cosmic volcanism around the mesopause that ruled the formation of the early Earth’s atmosphere and climate. Furthermore, a fraction of the μ Ms that survive unmelted upon atmospheric entry did settle on the proto-oceans floors. Upon further burial in sediments their constituent PAH-rich kerogen was cracked into abiotic oil, which generated giant oil slicks that fed prebiotic chemistry. Many stars, of all ages and types, are embedded into a secondary debris-disk loaded with ion implanted μ Ms. Some of them are expelled to the interstellar medium (ISM) where they behave first as “dormant-invisible” molecular reactors, until they became reactivated by various processes to synthesize interstellar molecules. This short paper only focus on some highlights of this research dealing with the synthesis of important interstellar molecules, including the most abundant ones (H 2 and CO) and H 2 O, HCN and PAHs, all involved in prebiotic chemistry.

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    https://doi.org/10.1051/978-2-...
    Part of book or chapter of book . 2020 . Peer-reviewed
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    https://www.degruyter.com/docu...
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    https://doi.org/10.1051/978-2-...
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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: Petrolo, Riccardo; Loscrì, Valeria; Mitton, Nathalie;

    The continuous growth of the urban population has generated a drastic expansion of our cities. Nowadays, indeed, more than 50 % of the world’s population is urban, and they forecast that it will reach 70 % by 2050. Therefore, cities need to be ready to accommodate this huge amount of citizens and to face new challenges (e.g., traffic congestion, air pollution, waste management, etc.). The concept of cyber-physical systems, as integration of computation and physical processes, can help toward the realization of real smart cities capable to ensure sustainability and efficiency. To this purpose, this chapter investigates the cyber-physical system (CPS) and their cyber-physical object (CPO) as key units, in the context of a smart city concept. We survey the smart city vision, providing information on the main requirements, the open challenges, and highlighting the benefits; we also browse the European Commission initiatives for smart cities and some pilot projects that are in development.

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    https://doi.org/10.1007/978-3-...
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      https://doi.org/10.1007/978-3-...
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  • Authors: Deng, D.; Nguyen Minh, D.; Constantinescu, A.;

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  • Authors: Ould Mohamed, S.; Bruand, Ary;

    Abstract Ould Mohamed, S. and Bruand, A., 1994. Morphology and origin of secondary calcite in soils from Beauce France. In: A.J. Ringrose-Voase and G.S. Humphreys (Editors), Soil Micromorphology: Studies in Management and Genesis. Proc. IX Int. Working Meeting on Soil Micromorphology, Townsville, Australia, July 1992. Developments in Soil Science 22, Elsevier, Amsterdam, pp. 27–36.

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    Authors: Lassin, Arnault; Mercury, Lionel; Azaroual, Mohamed;

    International audience; In arid environments, porous media are unsaturated with water which is submitted to capillary constraints. The present chapter focuses on the geochemical impacts of such physical constraints and how theoretical analysis can help interpreting field or laboratory observations. The basic principles of capillary geochemistry suggest that the fate of contaminants, either organic or inorganic, can be significantly impacted in terms of reactive mass transfer in addition to flow and transport processes. All these mechanisms are closely interconnected, what makes the description of the behavior of such systems very complicated. An important work still has to be done in order to achieve such a goal: a number of mechanisms are not taken into account in the current state of development of the capillary geochemistry, namely mechanisms that occur in the thinnest confining geometries, like disjoining pressures, surface forces, etc.

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    https://doi.org/10.1007/978-94...
    Part of book or chapter of book . 2013 . Peer-reviewed
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      https://doi.org/10.1007/978-94...
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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: Yahyaoui, Zouhour; Sabatier, François; Rebai, Noamen; Abdeljaouad, Sâadi;

    Conference: 1st International Conference on Mapping and Spatial Analysis of Socio-Economic and Environmental Indicators for the Local and Regional Sustainable Development (SEE GEOMATICS)Location: Tataouine, TUNISIADate: MAR 25-26, 2015; International audience; For mapping the three-dimensional shape of the submarine bars, studying their dynamics and assessing the spatiotemporal evolution of sedimentary balances, the coastal prism of Korba (emerged and submerged beach) has benefitted from topo-bathymetric monitoring. This monitoring was carried out on an annual basis between July 2006 and July 2009. Numerical Terrain Models (N.T.M.) and transverse profiles were then analyzed. The main results show, firstly, that the shoreface of Korba is characterized by a homogeneous evolution across all profiles of its two-bar system. Moreover, the extent of changes in the sand volume of the beach suggests that the evolution takes place without significant sedimentary loss and that the beach is in a dynamic equilibrium. Accretion of the bars and migration towards the shore are found in periods of small waves (between July 2006 and July 2007). However, following a period of minor agitations, a filling of the outer trough is observed. It is proceeded by the migration of the outer bar towards the coast (between July 2007 and July 2009). These results confirm the traditional model of self-organization of a barred beach. These data and results, then, allow us to establish conceptual models and simulations of the evolution of the microtidal, barred beach of Korba.

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    https://doi.org/10.1007/978-3-...
    Part of book or chapter of book . 2019 . Peer-reviewed
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      https://doi.org/10.1007/978-3-...
      Part of book or chapter of book . 2019 . Peer-reviewed
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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: Barbière, Franck; Marivaux, Laurent;

    Introduction The modern Afro-Asian porcupines, the African cane-, mole- and dassie-rats, as well as the South American guinea pigs, chinchillas, capybaras, pacas, agoutis, etc., make up the natural group of the hystricognathous rodents (infra-order Hystricognathi Tullberg, 1899). The phylogenetic relationships between the hystricognaths from South America (caviomorphs (Caviomorpha Wood, 1955)) and Africa (phiomorphs (Phiomorpha sensu Lavocat, 1967; Thryonomyoidea sensu Wood, 1955)) are today well-supported by a body of anatomical (e.g. Wood, 1974; Lavocat, 1976; Bugge, 1985; George, 1985; Meng, 1990; Luckett and Hartenberger, 1993; Martin, 1994) and molecular (e.g. Nedbal et al ., 1996; Huchon and Douzery, 2001; Huchon et al ., 2002, 2007; Poux et al ., 2006; Montgelard et al ., 2008; Blanga-Kanfi et al ., 2009; Churakov et al ., 2010) evidence, and also by endoparasite studies (e.g. Hugot, 1999). In contrast, the phylogenetic and geographic origins of hystricognaths have been the subject of considerable controversy over the past several decades (e.g. Wood and Patterson, 1959; Hoffstetter, 1972; Wood, 1972, 1973, 1974, 1985; Lavocat, 1973, 1974, 1976; Hussain et al ., 1978; Flynn et al ., 1986; Jaeger, 19; Huchon and Douzery, 2001, 2002; Marivaux et al ., 2002, 2004; Jaeger et al ., 2010a), and critical issues about their historical biogeography, notably their arrival in South America, are still a matter of on-going debate (e.g. Poux et al ., 2006; Bandoni de Oliveira et al ., 2009; Sallam et al ., 2009, 2011; Coster et al ., 2010; Antoine et al ., 2012). Although hystricognaths are absent from the earliest Tertiary fossil record at a global scale, their earliest known fossil occurrences date back to the late middle Eocene from both Africa and South America. This either suggests that hystricognaths have rapidly achieved a widespread distribution throughout the Old and New Worlds just after their emergence, or points out the existence of a significant Eocene gap in their fossil record. During the late Eocene and early Oligocene, the group exhibited a high diversity and morphological disparity on both landmasses, thereby suggesting a considerable amount of undocumented diversity in their early evolutionary history.

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    https://doi.org/10.1017/cbo978...
    Part of book or chapter of book . 2015 . Peer-reviewed
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      https://doi.org/10.1017/cbo978...
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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: Piégay, Hervé;

    The fluvial system is a complex adaptive process‐response system with two main physical components, the morphological system and the cascading system. The fluvial system changes progressively through geological time, as a result of normal erosional and depositional processes. The hydrosystem integrity depends on the dynamic interactions of hydrological, geomorphological and biological processes acting in these three dimensions over a range of time‐scales. The fluvial anthroposystem theory, with human pressures ubiquitous for many centuries, rivers are reacting to multiple human pressures acting at different time‐scales and different locations within the basin. Similarity analysis and connectivity analysis are ways to study the fluvial system in a comparative manner, one focusing on single temporal and spatial‐scale components, the other on the links between components of different scales. This chapter talks about research on the Drome, the Roubion, the Eygues and the Bega river to understand the system evolution and to inform management decisions. International audience deuxième édition

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    https://doi.org/10.1002/978111...
    Other literature type . 2016
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    Authors: Damase Mouralis; Erkan Aydar; Ahmet Türkecan; Catherine Kuzucuoğlu;

    The southern Cappadocia shows a large variety of Quaternary volcanic landscapes, offering the opportunity to observe beautiful and generally fresh morphologies. These landscapes include two rhyolitic complexes (Golludag and Acigol), a huge composite volcano (Hasandag) and numerous monogenic vents, with scoria cones, domes and maars. Natural and anthropogenic sections show a large variety of lava flows and tephra layers. The precise study of this volcanic material allows reconstructing the volcanic and geomorphologic evolution of this area during the Quaternary, including modes of emplacements, chronology of the volcanic successions, morphological impacts on the landscapes. In addition, archaeological excavations in southern Cappadocia testify for the presence of ancient populations since the Middle to Upper Palaeolithic. During the Neolithic and Chalcolithic periods, the southern Cappadocia has been intensively occupied with permanent sites (Asikli Hoyuk, Musular, Tepecik Ciftlik, Kosk Hoyuk, etc.) as well as non-permanent sites devoted to mining and chopping of obsidian associated with some of the volcanoes.

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    https://doi.org/10.1007/978-3-...
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    Authors: Khuntia, J; Proust, Sébastien; Khatua, K;

    International audience; We report here a laboratory study on the effects of bed roughness and emergent rigid veg-etation on the unsteady flows associated with flash floods and extreme flood events. The flow structure of unsteady open-channel flows over rough bed with and without emergent rigid vegetation has been investigated in an 18m long and 3m wide laboratory flume. Steady uniform flows were also studied and served as reference flows. For both steady and unsteady flows, two geometries are tested: (1) uniform bed roughness (uniform dense synthetic grass modelling meadow) along the flume and (2) a uniform staggered distribu-tion of emergent wooden circular cylinders (model of rigid vegetation) set on the bed roughness. Transient flow depths are simultaneously measured at six longitudinal positions using ultra-sonic sensors. Transient velocities are measured at one longitudinal position over the water column using a side looking ADV probe to estimate depth-averaged veloci-ty. In order to compute ensemble averages of the flow parameters, 109 runs of the same hydrograph are carried out repeatedly at the flume entrance. Two consecutive runs are separated by a base flow. The ensemble averages of the measured discharge, flow depths and velocity are found to be converged after 72 runs. For the two geometries: at the peak flow of the hydrograph, the vertical profiles of mean streamwise velocity and horizontal Reynolds shear stress are comparable to the profiles obtained for steady uniform cases of same flow depth; and accelerated and decelerated velocity profiles are obtained during the rising limb and falling limb of the hydrograph, respectively. Reynolds shear stresses are also found to be higher during the rising limb than during the falling limb for a fixed flow depth. The hysteresis in the depth-averaged velocity / flow depth relationships is compa-rable in shape and size for the two geometries highlighting the weak effect of the rigid vegetation compared to the effects of un-stationarity.

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    https://doi.org/10.1201/b22619...
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    Lunar minerals and impact glasses, convert the polyatomic beam of solar wind (SW) ions into a flux of small molecules ( e.g. , H 2 , N 2 , H 2 O, CO, CO 2 , CH 4 , C 2 H 4 , C 2 H 6 , HCN, metal carbides and deuterides, etc.). They thus behave as “Solid State Molecular Reactors”. Moreover, ~100–200 μ m size micrometeoroids ( μ Ms) have also been exposed to the SW in the zodiacal cloud, before being captured by the Earth and recovered as Antarctic micrometeorites. They are mostly composed of a PAH-rich hydrous-carbonaceous material, which amplifies their power as molecular reactors. In particular, during the first ~200 Myr of the post-lunar period, about 75% of the μ Ms have been melted and/or volatilized upon atmospheric entry. The release of their volatile species triggered a cosmic volcanism around the mesopause that ruled the formation of the early Earth’s atmosphere and climate. Furthermore, a fraction of the μ Ms that survive unmelted upon atmospheric entry did settle on the proto-oceans floors. Upon further burial in sediments their constituent PAH-rich kerogen was cracked into abiotic oil, which generated giant oil slicks that fed prebiotic chemistry. Many stars, of all ages and types, are embedded into a secondary debris-disk loaded with ion implanted μ Ms. Some of them are expelled to the interstellar medium (ISM) where they behave first as “dormant-invisible” molecular reactors, until they became reactivated by various processes to synthesize interstellar molecules. This short paper only focus on some highlights of this research dealing with the synthesis of important interstellar molecules, including the most abundant ones (H 2 and CO) and H 2 O, HCN and PAHs, all involved in prebiotic chemistry.

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    https://doi.org/10.1051/978-2-...
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    https://doi.org/10.1051/978-2-...
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    Authors: Petrolo, Riccardo; Loscrì, Valeria; Mitton, Nathalie;

    The continuous growth of the urban population has generated a drastic expansion of our cities. Nowadays, indeed, more than 50 % of the world’s population is urban, and they forecast that it will reach 70 % by 2050. Therefore, cities need to be ready to accommodate this huge amount of citizens and to face new challenges (e.g., traffic congestion, air pollution, waste management, etc.). The concept of cyber-physical systems, as integration of computation and physical processes, can help toward the realization of real smart cities capable to ensure sustainability and efficiency. To this purpose, this chapter investigates the cyber-physical system (CPS) and their cyber-physical object (CPO) as key units, in the context of a smart city concept. We survey the smart city vision, providing information on the main requirements, the open challenges, and highlighting the benefits; we also browse the European Commission initiatives for smart cities and some pilot projects that are in development.

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    https://doi.org/10.1007/978-3-...
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      https://doi.org/10.1007/978-3-...
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  • Authors: Deng, D.; Nguyen Minh, D.; Constantinescu, A.;

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