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The use of Light Detection and Ranging (LiDAR) is becoming more and more common in different landscape exploration domains such as archaeology or geomorphology. In order to allow the detection of features of interest, visualization filters have to be applied to the raw Digital Elevation Model (DEM), to enhance small relief variations. Several filters have been proposed for this purpose, such as Sky View Factor, Slope, negative and positive Openness, or Local Relief Model (LRM). The efficiency of each of these methods is strongly dependent on the input parameters chosen in regard of the topography of the investigated area. The LRM has proved to be one of the most efficient, but it has to be parameterized in order to be adapted to the natural slopes characterizing the investigated area. Generally, this setting has a single value, chosen as the best compromise between optimal values for each relief configuration. As LiDAR is mainly used in wide areas, a large distribution of natural slopes is often encountered. The aim of this paper is to propose a Self AdaptIve LOcal Relief Enhancer (SAILORE) based on the Local Relief Model approach. The filtering effect is adapted to the local slope, allowing the detection at the same time of low-frequency relief variation on flat areas, as well as the identification of high-frequency relief variation in the presence of steep slopes. First, the interest of this self-adaptive approach is presented, and the principle of the method, compared to the classical LRM method, is described. This new tool is then applied to a LiDAR dataset characterized by various terrain configurations in order to test its performance and compare it with the classical LRM. The results of this test show that SAILORE significantly increases the detection capability while simplifying it.

ALS-derived raster visualization techniques have become common in recent years, opening up new possibilities for subtle landform detection in earth sciences and archaeology, but they have also introduced confusion for users. As a consequence, the choice between these visualization techniques is still mostly supported by empirical knowledge. Some attempts have been made to compare these techniques, but there is still a lack of analytical data. This work proposes a new method, based on gradient modelling and spatial statistics, to analytically assess the efficacy of these visualization techniques. A selected panel of outstanding visualization techniques was assessed first by a classic non-analytical approach, and secondly by the proposed new analytical approach. The comparison of results showed that the latter provided more detailed and objective data, not always consistent with previous empirical knowledge. These data allowed us to characterize with precision the terrain for which each visualization technique performs best. A combination of visualization techniques based on DEM manipulation (Slope and Local Relief Model) appeared to be the best choice for normal terrain morphometry, occasionally supported by illumination techniques such as Sky-View Factor or Negative Openness as a function of terrain characteristics.

The French Flemish Coastal Plain, which extends from Denmark to France, is characterised by a topography close to sea level and protected by a system of coastal dunes. Quaternary sediments, comprised of marine, estuarine and continental deposits, accumulated by infilling and then prograding above a network of incised valleys. This study focusses on the Holocene infill of the Denna palaeoestuary, south‐west to Dunkerque. Surface geophysics (electrical conductivity and ground‐penetrating radar) and vibrocore data are used to reconstruct the landscape evolution during the last stages of sedimentation. The conductivity map highlights the last network of tidal channels, ditches and dikes of the eastern side of the palaeoestuary. Over the upper 4 m of the infill, the ground‐penetrating radar profiles show two superimposed units. The bottom unit is composed of meandering channel bars and the top unit of flat strata intersected by sparse channels, mostly infilled in place. The sediment analysis of the vibrocores shows a predominantly sandy filling of marine to estuarine origin, evidenced by sponge spicules and a fauna of bivalves and foraminifera adapted to brackish settings. The uppermost deposit exhibits an oxidation profile which marks the groundwater zone transition. Clayey sediments are also present, infilling the uppermost channels and ditches dug during reclamation, in increasing proportions towards the axis of the estuarine palaeovalley. The tidal signature of sedimentary dynamics is evidenced by heterolithic facies in some channel fills and tidal rhythmites infilling scour depressions linked to dike breaching. The abrupt decrease in channel dynamics across the unit boundary, although sedimentation remained sandy in the upper unit, coincides with the development of embankment of the estuarine border and is tentatively interpreted as a result of reclamation. The French part of the Flemish coastal plain, Southern North Sea, has estuaries that vanished in the Middle Age through progressive embankment. Surface geophysics and cores show increased sand/mud partitioning during land reclamation, with channels becoming mud‐filled while emerging flats remained sandy. This could be the result of ingression of sheet flows in the polders caused by catastrophic floods breaching the dikes.

The IGEAN (Innovative Geophysical Approaches for the study of Early Agricultural villages of Neolithic) Thessaly project focused on Early and Neolithic settlements in Thessaly, Central Greece. The aim of the project was to highlight in an extensive way differences in settlement layouts while investigating commonalities as a way to understand Neolithic use of space. To accomplish this, a suite of geophysical prospection techniques (geomagnetic, electromagnetic induction, and Ground Penetrating Radar (GPR)), aerial platforms (historic aerial imagery and Remotely Piloted Aerial Systems (RPAS)) as well as very high resolution spaceborne sensors were integrated to acquire comprehensive pictures of settlements. Results of the IGEAN project provide archaeological information on the dynamic character of enclosures, the structure of architectural features and open spaces within sites as an indication of economic or communal spaces. At the same time, they demonstrated the importance of employing a suite of different geophysical techniques to reveal different aspects of the hindered prehistoric settlements that could not be highlighted with a single geophysical approach.

A study was carried out in a waste sorting plant (WSP) located in France, treating dry recyclable household waste (DRHW) as well as dry recyclable commercial and industrial waste (DRCIW). Stationary and personal inhalable samples were collected in the WSP in order to investigate bioaerosols (sampling on a filter; 2 L/min and 10 L/min) and airborne dust (CIP; 10 L/min). The aim of the study was to assess the extent to which the measurement of concentration, species composition, and particle size distribution contributes to a better assessment of the biological risks associated with exposure. The results confirmed that waste and waste sorting activities are sources of airborne fungi. Indeed, ambient concentrations ranged from 7.3 × 103 to 8.5 × 105 colony-forming units (CFU)/m3 for culturable fungi and up to 4 mg/m3 for dust. Personal exposure to inhalable dust was found up to 3 mg/m3 for dust and ranged from 8.6 × 103 to 1.5 × 106 CFU/m3 for fungi. Airborne fungal communities were found to be dominated by the Penicillium genera in both bioaerosols and settled dust samples, followed by the Aspergillus, Cladosporium, Wallemia, Mucor, and Rhizopus genera. Fungi were carried by particles of aerodynamic diameters, mainly between around 2.0 and 10.0 µm. The findings dealing with size distribution and biodiversity of bioaerosols suggest that employees are exposed to complex bioaerosols during their work and help to make a finer diagnosis of the risks involved, which is often difficult in the absence of any occupational exposure limit (OEL) value for bioaerosols in general.

Continuous seawater disinfection by chlorine dioxide (ClO₂) was studied at residual concentrations of 0.2 and 0.4 mg ClO₂ L⁻¹ and compared with sodium hypochlorite (NaClO) disinfection at 1 mg L⁻¹ of free chlorine. The results revealed that both disinfectants decrease the biological activity and cell counts in seawater. When NaClO was used, both the cell counts and the adenosine triphosphate (ATP) level were diminished (1.8 log and 76 %, respectively); however, when ClO₂ was used, the ATP level decreased to the same level as with NaClO (78–84 %), but the cell counts were reduced only weakly (~0.1 log). The biofilm concentration in seawater without disinfectants reached 700 pg ATP cm⁻² after 40 days, whereas in the treated lines, the biofilms remained below 1 pg ATP cm⁻² irrespective of the disinfectant and dose used. ClO₂ generated much less trihalomethanes than NaClO (<1 vs. 154 μg L⁻¹). Bromoform (77–96 %) was the predominant chemical species found in disinfected seawater.

The systematic exploration of large archaeological sites in the Mediterranean has evolved considerably since the \"big dig\" excavations. Pedestrian field surveying and remote sensing applications, including satellite and airborne image analysis, are now practical and relatively cost-efficient methods of characterizing large and diachronically diverse landscapes on regional scales. However, the use of geophysical techniques as a means for exploring manifold archaeological contexts is still in its infancy. In this paper, we highlight the advantages of archaeological geophysics to conduct regional surveys in the Mediterranean. Through a multi-site geophysical fieldwork campaign to investigate the patterns and dynamics of ancient cities in Greece, we show how geophysics offer new opportunities for characterizing the spatial attributes and regional dynamics of urban landscapes, and, in doing so, we make an argument for its wider adoption on regional survey projects.

Through the process of globalization, food has experienced an intense territorial restructuring process. Local agric-food links have weakened at the same time as daily products arrived from distant lands. There is presently a wide international debate on the importance of transport in the configuration of the agric-food system and its contribution in terms of greenhouse gas (GHG). The direct environmental costs of the transport of imported food, that is the ‘external food miles’, have been estimated in kilometer (km), ton (t), ton-kilometer (t-km) and GHG in Spain between 1995 and 2011. The analysis is made by ten food groups including 136 products, with special attention to the most important ones (cereals and animal feed), as well as by means of transport (air, rail, road and water) and from 113 different countries belonging to six geographical areas. Two phases are identified during this period: an expansive phase (1995–2007), in which the t-km of imported food increased from 81.8 to 147.8 million t-km and environmental pressure rose from 3.1 to 5.4 million CO2-eq t, and a recession phase (2007–2011), in which environmental pressure subsided as a consequence of the reduction of imports, even though it still remained above the 1995 level. The article reveals a clear interrelation between amounts, distances and modal distribution when it comes to determining the environmental cost of transporting food imports in the two periods studied. It also reflects on the role of the external food miles in the Spanish agri-food system from a sustainability perspective.

In the present study, we examined seawater biofiltration in terms of adenosine triphosphate (ATP) and turbidity. A pilot biofilter continuously fed with fresh seawater reduced both turbidity and biological activity measured by ATP. Experiments operated with an empty bed contact time (EBCT) of between 2 and 14 min resulted in cellular ATP removals of 32 to 60 % and turbidity removals of 38 to 75 %. Analysis of the water from backwashing the biofilter revealed that the first half of the biofilter concentrated around 80 % of the active biomass and colloidal material that produces turbidity. By reducing the EBCT, the biological activity measured as cellular ATP concentration moved from the first part of the biofilter to the end. Balances of cellular ATP and turbidity between consecutive backwashings indicated that the biological activity generated in the biofilter represented more than 90 % of the detached cellular ATP. In contrast, the effectively trapped ATP was less than 10 % of the overall cellular ATP detached during the backwashing process. Furthermore, the biological activity measured as cellular ATP generated in the biofilter seemed to be more dependent on the elapsed time than the volume filtered. In contrast, the turbidity trapped in the biofilter was proportional to the volume filtered, although a slightly higher amount of turbidity was found in the backwashing water; this was probably due to attrition of the bed medium. Finally, no correlations were found between turbidity and ATP, indicating that the two parameters focus on different matter. This suggests that turbidity should not be used as an alternative to cellular concentration.

Dans le cadre de l’agrandissement du port de Dunkerque, plus de 170 hectares de la plaine maritime ont été explorés sur la future « Zone Grande Industrie », dans l’ancien estuaire de la Denna (ou Déna, ou L’Enna), sous-bassin du petite fleuve côtier Aa. Le diagnostic d’archéologie préventive classique par ouverture de tranchées a été accompagnée de recherches en archives, de prospections géophysiques, de levés géomorphologiques en sondages en puits (profonds de 3 m) et en coupes. L’intégration des études de nature différente permet d’aboutir à une compréhension du secteur meilleure que ne l’eût fait chaque discipline séparément. Les dépôts sont essentiellement des sables tidaux recoupés par des chenaux de marée. Les décimètres supérieurs sont parfois plus limoneux. Les mesures de conductivité apparente permettent de spatialiser les données lithostratigraphiques ponctuelles. Leur confrontation, ainsi que des indices venant du réseau parcellaire, permet la mise en évidence d’un bord ouest de l’estuaire, contemporain d’occupations humaines. De même, la confrontation des vestiges archéologiques levés lors du diagnostic avec une zonation basée sur la géophysique et la stratigraphie permet d’appréhender l’évolution du paysage, notamment l’expansion et la contraction de l’habitat du secteur, depuis les premières interventions aux environs des X e –XII e  siècles sur la bordure ouest de l’estuaire. Depuis ce dernier, l’habitat a progressé vers le nord-est, jusqu’à un bras de la Denna resté longtemps actif et dont l’axe correspond au système de drainage actuel. La cartographie de conductivité électrique permet également de mettre en évidence des anomalies qui se sont révélées être de larges et profondes structures anthropiques (jusqu’à environ 40 m de diamètre et plus de 5 m de profondeur, soit −2,5 m sous la cote zéro). Bien que nombreuses, ces structures peuvent passer facilement inaperçues lors des diagnostics archéologiques. Plusieurs ont été testées. Leur remplissage est variable mais présente comme point commun une étanchéification du fond et des parois par des mottes d’argile. Ces structures sont interprétées comme des mares endiguées dont quelques exemples subsistent sur la côte de la mer du Nord (en Frise, en Zélande et en Allemagne). Elles permettaient de recueillir l’eau douce et leur couronne de remblais en élévation s’élevaient au-dessus des plus fortes marées. As part of the expansion of the port of Dunkirk, more than 170 hectares of the maritime plain were explored on the future “Zone de Grande Industrie” (heavy industrie area) in the former estuary of the Denna (or Déna, or L’Enna) river, sub-catchment of the small coastal Aa river. The usual preventive archaeological diagnosis by trial trenches was accompanied by an archival research, a geophysical survey and geomorphological surveys (cross-sections and 3 m deep test pits). The integration of the different results leads to an understanding of the sector better than each discipline would have done separately. The first meters of deposits consist of tidal sands intersected by tidal channels. The upper decimeters are possibly siltier. The apparent conductivity survey allows spatializing the lithostratigraphic data. Their combination, as well as information from the ancien cadastre, highlight a state of the western edge of the estuary, contemporary with human occupations. In the same way, combination of archaeological remains collected during the survey with the geophysical/stratigraphical data allows to understand the evolution of that landscape, along with the expansion and contraction of dwellings, since the first remains around the X th –XII th century on the western edge of the estuary. From that, dwellings move to the northeast, to a long time active channel of the Denna which its axis corresponds to the current drainage system. The electrical conductivity survey also revealed anomalies that turned out to be broad and deep anthropogenic features (up to about 40 m in diameter and more than 5 m deep, i.e. −2.5 m below mean water level). Although abundant, these structures can easily be unnoticed by trial trenches. Three structures were tested. Their filling is variable but has a common point to be sealed on the bottom and to have walls made with clumps of clay. These features are interpreted as diked ponds, some examples remain on the coast of the North Sea (Friesland, Zeeland and Germany). They were used to collect fresh water while the surrounding shape embankment was used to protect it from the highest tides.