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19 pages, 1385 KiB  
Article
Geological Influences on Wine Quality: Analyzing Nebbiolo Grapes from Northern Italy
by Laura Santagostini and Vittoria Guglielmi
Appl. Sci. 2025, 15(1), 258; https://doi.org/10.3390/app15010258 - 30 Dec 2024
Viewed by 447
Abstract
This study investigates the critical relationship between soil characteristics, trace element concentrations in Nebbiolo grapes, and the resulting wine quality, emphasizing the importance of terroir in winemaking. Italy, particularly the regions of Piedmont, Lombardy, and the Aosta Valley, is home to Nebbiolo, a [...] Read more.
This study investigates the critical relationship between soil characteristics, trace element concentrations in Nebbiolo grapes, and the resulting wine quality, emphasizing the importance of terroir in winemaking. Italy, particularly the regions of Piedmont, Lombardy, and the Aosta Valley, is home to Nebbiolo, a prestigious grape variety known for its depth and aging potential in wines like Barolo and Barbaresco. The research focuses on seventeen grape and wine samples, highlighting how soil mineral composition could affect grape composition and wine characteristics. The analysis employed ICP-AES (inductively coupled plasma atomic emission spectrometry) to measure trace elements such as Al, Ba, and Mn, linking their concentrations to the soil’s geological properties. Elements were categorized into three groups based on their origins—natural soil contributions (Al, Ba, Li, Mn, Mo, Sr, Ti), those influenced by production cycles (Ca, Mg, K, Cu, Zn, Fe), and artificial sources (Co, Cr, Ni, V)—asserting that the first group serves as the most reliable indicators for tracing wines back to their vineyard origins. By establishing a chemical fingerprint for Nebbiolo wines, this research aims to enhance their authenticity and market value while providing insights into the intricate interplay between soil, grape varietals, and winemaking practices and contemporary challenges like climate change and evolving market demands. Full article
(This article belongs to the Special Issue Analytical Chemistry: Techniques and Applications)
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<p>(<b>a</b>) Bar-plot of Mg concentration in analyzed soils, reported as mg Mg/Kg soil. (<b>b</b>) Bar-plot of Fe concentration in analyzed soils, reported as mg Fe/Kg soil.</p>
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<p>(<b>a</b>) PCA of the complete dataset of elements’ concentrations variance PC1 56.0%, PC2 22.3%. (<b>b</b>) PCA performed only on ‘<span class="html-italic">meso elements’</span> variance PC1 66.8%, PC2 9.19%.</p>
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<p>(<b>a</b>) PCA of the complete dataset of elements’ concentrations in grapes. (<b>b</b>) PCA performed only on ‘<span class="html-italic">meso elements</span>’. (Variance PC1 46.56%, PC2 27.35%, PC3 13.09%).</p>
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<p>PCA of must elemental concentrations (PC1 57.47%, PC2 31.09%).</p>
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<p>PCA of wine elemental concentrations (PC1 59.95%, PC2 25.56%). Wines are divided based on their provenance: Canavese (red oval), Langhe (green oval), Valtellina (blue oval), and Aosta Valley (orange).</p>
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33 pages, 15088 KiB  
Article
A Multi-Criteria GIS-Based Approach for Risk Assessment of Slope Instability Driven by Glacier Melting in the Alpine Area
by Giulia Castellazzi and Mattia Previtali
Appl. Sci. 2024, 14(24), 11524; https://doi.org/10.3390/app142411524 - 11 Dec 2024
Viewed by 780
Abstract
Climate change is resulting in significant transformations in mountain areas all over the world, causing the melting of glacier ice, reduction in snow accumulation, and permafrost loss. Changes in the mountain cryosphere are not only modifying flora and fauna distributions but also affecting [...] Read more.
Climate change is resulting in significant transformations in mountain areas all over the world, causing the melting of glacier ice, reduction in snow accumulation, and permafrost loss. Changes in the mountain cryosphere are not only modifying flora and fauna distributions but also affecting the stability of slopes in those regions. For all these reasons, and because of the risks these phenomena pose to the population, the dentification of dangerous areas is a crucial step in the development of risk reduction strategies. While several methods and examples exist that cover the assessment and computation of single sub-components, there is still a lack of application of risk assessment due to glacier melting over large areas in which the final result can be directly employed in the design of risk mitigation policies at regional and municipal levels. This research is focused on landslides and gravitational movements on slopes resulting from rapid glacier melting phenomena in the Valle d’Aosta region in Italy, with the aim of providing a tool that can support spatial planning in response to climate change in Alpine environments. Through the conceptualization and development of a GIS-based and multi-criteria approach, risk is then estimated by defining hazard indices that consider different aspects, combining the experience acquired from studies carried out in various disciplinary fields, to obtain a framework at the regional level. This first assessment is then deepened for the Lys River Valley, where the mapping of hazardous areas was implemented, obtaining a classification of buildings according to their hazard score to estimate the potential damage and total risk relating to possible slope instability events due to ice melt at the local scale. Full article
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<p>Map highlighting the location of the Valle d’Aosta region and its main characteristics: natural (glaciers, protected areas, and parks) and anthropic (roads, skiing facilities, and main cities). Data obtained from regional geoportals and databases of the Autonomous Region of Valle d’Aosta.</p>
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<p>Methodology used for processing data to obtain the landslide risk map due to the ice melting of the Valle d’Aosta region.</p>
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<p>Individual hazard layers obtained through GIS software processing. Data sources are listed in <a href="#applsci-14-11524-t001" class="html-table">Table 1</a>.</p>
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<p>Aggregated hazard value: glacier melting landslide susceptibility map. The map was created through QGIS (v. 3.26.0) software, employing the data outlined in <a href="#applsci-14-11524-t001" class="html-table">Table 1</a>.</p>
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<p>Geological and hydraulic hazard map included in Piano Territoriale Paesistico. Data from the Geoportale of Valle d’Aosta region.</p>
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<p>Aggregated worth exposed value in the Valle d’Aosta region. The map was created through GIS software, employing the data outlined in <a href="#applsci-14-11524-t002" class="html-table">Table 2</a>.</p>
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<p>Glacier melting related landslide risk map in Valle d’Aosta region. The map was created through GIS software, interpolating hazard and worth exposed maps (<a href="#applsci-14-11524-f004" class="html-fig">Figure 4</a> and <a href="#applsci-14-11524-f006" class="html-fig">Figure 6</a>).</p>
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<p>Risk score comparison in Valle d’Aosta municipalities.</p>
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<p>High-risk areas: landscape typologies involved.</p>
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<p>The Lys Valley: the risk map and its representation as a box-plot for the municipalities.</p>
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<p>Positions of the four case studies for the local scale analysis representing the landscapes of the Lys Valley. Data obtained from regional geoportals and databases of the Autonomous Region of Valle d’Aosta.</p>
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<p>The four sites analyzed: Alpenzu Grande (<b>a</b>), Noversch (<b>b</b>) Gressoney-La-Trinité (<b>c</b>), and Orsia (<b>d</b>). Photographs by the authors.</p>
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<p>Local-scale analysis workflow for the Alpenzu Grande (Area 01) site: improved hazard calculation with a more detailed DTM (2 × 2 m) and assessed vulnerability and worth exposed values for the area to compute potential damage and assess the final risk score.</p>
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<p>The local scale analysis results (improved hazard calculation, assessed vulnerability and worth exposed values, and final risk score) for Noversch (<b>a</b>), Gressoney-La-Trinitè (<b>b</b>), and Orsia (<b>c</b>). Analysis made with data collected in the field with the vulnerability scores listed in <a href="#applsci-14-11524-t003" class="html-table">Table 3</a>.</p>
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16 pages, 3690 KiB  
Article
CHIMBO Air Quality Modeling System: Verification and Processes Analysis
by Tony Christian Landi, Marco Paglione, Mauro Morichetti, Fabio Massimo Grasso, Fabrizio Roccato, Rita Cesari and Oxana Drofa
Atmosphere 2024, 15(11), 1386; https://doi.org/10.3390/atmos15111386 - 17 Nov 2024
Viewed by 843
Abstract
This study presents an evaluation of the CHIMBO modeling chain applied to the Italian domain, specifically focusing on the Po Valley subdomain over the one-year period of 2019. The comparison between simulated and observed data indicates that the performance of the CHIMBO model [...] Read more.
This study presents an evaluation of the CHIMBO modeling chain applied to the Italian domain, specifically focusing on the Po Valley subdomain over the one-year period of 2019. The comparison between simulated and observed data indicates that the performance of the CHIMBO model aligns well with existing literature on other state-of-the-art models. The results demonstrate that the CHIMBO chain is particularly effective for regional-scale quantitative assessments of pollutant distribution, comparable to that of CAMS ensemble models. The analysis of key chemical species in particulate matter reveals that the CHIMBO model accurately represents the average concentrations of organic and elemental carbon, as well as secondary inorganic compounds (sulfate, nitrate, and ammonium), particularly at background monitoring stations in the flat terrain of the Po Valley, with the exception of Aosta, a city located at about 500 m asl. However, seasonal discrepancies were identified, especially during winter months, when significant underestimations were observed for several species, including elemental and organic carbon, predominantly at background sites. These underestimations are likely attributed to various factors: (i) inadequate estimations of primary emissions, particularly from domestic heating; (ii) the limited effectiveness of secondary formation processes under winter conditions characterized by low photochemical activity and high humidity; and (iii) excessive dilution of pollutants during calm wind conditions due to overestimation of wind intensity. In conclusion, while the CHIMBO modeling chain serves as a robust tool for mesoscale atmospheric composition investigations, limitations persist related to emissions inventories and meteorological parameters, which remain critical drivers of atmospheric processes. Full article
(This article belongs to the Section Air Quality)
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<p>CHIMBO integration domains: Europe (<b>a</b>) and Italy (<b>b</b>) with horizontal cell grids of ca. 20 km and ca. 8 km, respectively. The different colors indicate the orography: the sea surface is depicted in blue, brown shades for higher altitudes and green shades for lower altitudes or flat terrains are used.</p>
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<p>Locations of SYNOP-Land station for Italian peninsula where wind speed (<b>left panel</b>) and 2 m temperature (<b>right panel</b>) are measured and considered for this work. Color bar indicates the altitude of sampling sites.</p>
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<p>Location and names of the sites for which the observations vs. CHIMBO comparison was done throughout 2019.</p>
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<p>Time series of 2 m air temperature (<b>left panel</b>) and wind speed (<b>right panel</b>) of daily mean values as calculated over 97 and 107 SYNOP measurement stations (showed in <a href="#atmosphere-15-01386-f002" class="html-fig">Figure 2</a>).</p>
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<p>The comparisons of observed monthly median concentrations of PM<sub>10</sub>, PM<sub>2.5</sub>, O<sub>3</sub> and NO<sub>2</sub> (box plot (black and gray colors) with median, 25th and 75th percentiles and outliers), calculated by the CHIMBO modeling chain (red line) and the CAMS ensemble (blue line) are reported. The stations considered for this comparison are all those available nationwide for the year 2019 and representative of rural background conditions. In general, CHIMBO seems to have similar performances to the CAMS ensemble.</p>
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<p>Comparison of predicted vs. observed PM<sub>10</sub> mass and PM<sub>10</sub>/PM<sub>2.5</sub> main chemical components concentrations (μgm<sup>−3</sup>) from 11 measurement stations in Northern Italy during 2019. Each point corresponds to a 1-day average value. Also shown are the 1:1, 2:1 and 1:2 lines. Observed data represent gravimetric and chemical measurements. Carried out by ARPAs on filter samples.</p>
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<p>Time series of daily concentrations of different PM<sub>10</sub>/PM<sub>2.5</sub> chemical components as measured and simulated by CHIMBO (“Observed” and “Predicted” in the legend, respectively) for the site of Bologna (BO) and Aosta (AO).</p>
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31 pages, 112289 KiB  
Article
Deep Electrical Resistivity Tomography for Detecting Gravitational Morpho-Structures in the Becca France Area (Aosta Valley, NW Italy)
by Maria Gabriella Forno, Marco Gattiglio, Franco Gianotti, Cesare Comina, Andrea Vergnano and Stefano Dolce
GeoHazards 2024, 5(3), 886-916; https://doi.org/10.3390/geohazards5030045 - 9 Sep 2024
Viewed by 1031
Abstract
Deep-seated gravitational slope deformations (DSGSDs) consist of gravity-induced, large-scale, gradual rock mass movements. In the Aosta Valley region (Valle d’Aosta NW Italy), DSGDs affect wide valley slopes and produce several interconnected morpho-structures that involve bedrock and Quaternary cover. Some DSGSD effects are not [...] Read more.
Deep-seated gravitational slope deformations (DSGSDs) consist of gravity-induced, large-scale, gradual rock mass movements. In the Aosta Valley region (Valle d’Aosta NW Italy), DSGDs affect wide valley slopes and produce several interconnected morpho-structures that involve bedrock and Quaternary cover. Some DSGSD effects are not visible at the surface because of subglacial abrasion or burial by sediments and, therefore, are difficult to map with standard geomorphological surveys. This is the case for the Pointe Leysser DSGSD in the Aosta Valley, which is heavily influenced by the historical movements of the Verrogne-Clusellaz Glacier and its tributaries. We conducted a new geological investigation, integrated with deep electrical resistivity tomography geophysical surveys (ERTs). The ERT results were initially compared with geological/geomorphological evidence at the surface to define the correlation between the values and spatial distributions of electrical resistivity and the sediments, rocks, or morpho-structures. The resistivity values at various depths were subsequently analysed, interpreted, and discussed in conjunction with geological hypotheses. The geological and geophysical survey revealed three wide buried glacial valleys filled with glacial sediments and mapped the locations of gravitational morpho-structures at depth. These new data allowed us to draw a relationship between glacialism and gravitational evolution, distinguishing between pre-singlacial movements and postglacial movements. Full article
(This article belongs to the Special Issue Landslide Research: State of the Art and Innovations)
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<p>Geological sketch of the Aosta Valley with the location of the Pointe Leysser DSGSD (white square) (from [<a href="#B12-geohazards-05-00045" class="html-bibr">12</a>]).</p>
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<p>General view of Clusellaz and Clapin Valleys, separated by the Tsa de Fourmière Relief (TFR) and investigated by the ERT1 and ERT2 profiles, and bordered by the ridges of Mont Fallère and Becca France (the distance from Mont Fallère and Becca France is approximately 3500 m).</p>
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<p>Simplified geological map of the Pointe Leysser DSGSD (white box in <a href="#geohazards-05-00045-f001" class="html-fig">Figure 1</a>) modified from [<a href="#B3-geohazards-05-00045" class="html-bibr">3</a>] (for the tectonic sketch) and from [<a href="#B5-geohazards-05-00045" class="html-bibr">5</a>] (for the Fallère Lake area). The red rectangle indicates the investigated area.</p>
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<p>Wide asymmetrical Clusellaz Valley between the Becca France ridge (BFR) and the Tsa de Fourmière Relief (TFR) (the distance between BFR and TFR shown in the figure is approximately 470 m).</p>
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<p>Original geological map of the high Clusellaz Valley, north of the Becca France ridge.</p>
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<p>Frontal moraines (light blue lines) in the upper Clusellaz Valley along the ERT2 profile (with a range of 450–550 m), which partly cover the gravitational structures GS<b>20</b> and GS<b>21</b>.</p>
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<p>The geoelectric profiles in the high Clusellaz Valley on a Google Earth image with the location of the photographs.</p>
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<p>ERT1- (<b>A</b>) and ERT2- (<b>B</b>) interpreted geophysical profiles seen from NW.</p>
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<p>Clast-rich sediments along the stretch <b>a</b> of ERT1 (with a range of 600–640 m) form a landslide body (lb) covering the subglacial sediments (in the foreground) (s).</p>
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<p>Torrential sediments forming the alluvial fan (af) of the T. Tsa de Fourmière along the stretch <b>d</b> of the ERT1 profile (with a range of 430–460 m). A wide body consisting of debris flow sediments (df) is also evident behind the person.</p>
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<p>The frontal moraine (light blue line) at the Clapin Valley head along the stretches <b>d</b> and <b>e</b> of ERT1 (with a range of 800–920 m), formed by ice-marginal sediments, which are partly covered by a landslide body (red dotted line).</p>
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<p>Trend in ERT2 (with a range of 80–210 m) along the Clapin Valley (partially filled by subglacial sediments) bordered by the Tsa de Fourmière Relief (TFR), shaped in the bedrock by subglacial erosion and cut by the gravitational structures <b>GS11</b> (scarp on ice-marginal sediments with rhododendrons) and <b>12</b> (trench filled by subglacial sediments). In the background, the Becca France ridge (BFR) can be seen.</p>
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<p>Tsa de Fourmière Relief (TFR) shaped in the bedrock by subglacial erosion and cut by the WNW–ESE gravitational minor scarp (<b>GS11</b>, with a height of 15–20 m) east of the ERT2 profile. In the background, the summit of the Becca France ridge is visible.</p>
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<p>Gravitational trenches (<b>GS13</b> and <b>GS14</b>) and minor scarps (<b>GS15</b>) along stretch <b>b</b> of the ERT2 profile (with a range of 275–375 m) cut the Tsa de Fourmière Relief (TFR) shaped in the bedrock by subglacial erosion.</p>
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<p>Persistent joints feature the high fractured rocks (calcschist) outcropping in the Tsa de Fourmière Relief (TFR) (approximately 20 m high).</p>
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<p>The 3D visualisation of the 3D inversion of the two ERT profiles seen from the NW. The Y axis indicates the north direction.</p>
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<p>The glacial Clapin Trough (approximately 40 m wide), east of the ERT2 profile, is partly filled by subglacial sediments, as evidenced by wide meadows.</p>
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<p>Trench west of the ERT2 profile: (<b>A</b>) stretch of this trench shaped in the bedrock and (<b>B</b>) stretch of this trench (approximately 3 m wide) involving the subglacial sediments.</p>
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18 pages, 1981 KiB  
Article
At What Price Are Farmers Willing to Reduce Water Usage? Insights from the Aosta Valley
by Francesca Moino, Francesco Caracciolo, Patrizia Borsotto, Stefano Trione, Denise Chabloz, Mauro Bassignana, Teresa del Giudice and Filiberto Altobelli
Water 2024, 16(17), 2412; https://doi.org/10.3390/w16172412 - 27 Aug 2024
Viewed by 985
Abstract
As climate change and decreasing precipitation worsen water scarcity, understanding farmers’ willingness to reduce water usage is crucial. This study examines this issue in the Aosta Valley, a region facing unique challenges due to its mountainous terrain and high water management costs. The [...] Read more.
As climate change and decreasing precipitation worsen water scarcity, understanding farmers’ willingness to reduce water usage is crucial. This study examines this issue in the Aosta Valley, a region facing unique challenges due to its mountainous terrain and high water management costs. The aim is to evaluate farmers’ willingness to reduce water usage and the economic incentives needed to encourage water-saving strategies. To gather the data, 100 farmers participated in a survey that included a discrete choice experiment. The findings revealed that 75% of farmers were unwilling to reduce their water usage even with proposed monetary compensation (EUR 100–120 per hectare per year). On average, the additional compensation farmers would accept for a 10% reduction in water usage was estimated at EUR 360 per hectare per year. This high compensation demand suggests a disconnect between individual desires and economic feasibility. The key reasons for their reluctance included the belief that their current water usage is already optimized, inadequate compensation for potential economic losses and concerns about water shortage. The study highlights the need to understand the socio-cultural context when designing water management policies. Combining economic incentives with social and educational initiatives is likely more effective for promoting sustainable water practices. Full article
(This article belongs to the Section Water, Agriculture and Aquaculture)
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<p>Aosta Valley region [<a href="#B31-water-16-02412" class="html-bibr">31</a>,<a href="#B32-water-16-02412" class="html-bibr">32</a>].</p>
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<p>Example choice set.</p>
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<p>Descriptive statistics of respondents’ characteristics.</p>
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<p>A findings–response model of farmers’ willingness to reduce their irrigation water use by 10% as the compensation increases.</p>
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14 pages, 3024 KiB  
Article
Regional-Scale Analysis of Antimicrobial Usage in Smallholder Cattle Herds (Aosta Valley, Italy): Why Surveillance Matters
by Federico Scali, Sandra Ganio, Claudio Roullet, Mauro Ruffier, Stefania Bergagna, Giulia Pagliasso, Claudia Romeo, Nicoletta Formenti, Antonio Marco Maisano, Giovanni Santucci, Matteo Tonni, Federica Guadagno, Francesca Mazza, Flavia Guarneri, Giorgio Bontempi, Loredana Candela and Giovanni Loris Alborali
Antibiotics 2024, 13(3), 204; https://doi.org/10.3390/antibiotics13030204 - 22 Feb 2024
Viewed by 1474
Abstract
Optimising antimicrobial usage (AMU) in livestock is pivotal to counteract the emergence of antimicrobial resistance. We analysed AMU in more than 1000 cattle herds over 11 years (2008–2018) in the Aosta Valley (Italy), a region where 80% of farms house less than 50 [...] Read more.
Optimising antimicrobial usage (AMU) in livestock is pivotal to counteract the emergence of antimicrobial resistance. We analysed AMU in more than 1000 cattle herds over 11 years (2008–2018) in the Aosta Valley (Italy), a region where 80% of farms house less than 50 cattle. Dairy cows accounted for over 95% of AMU. AMU was estimated using the defined daily dose animal for Italy (DDDAit) per biomass for the whole herd and a treatment incidence 100 (TI100) for cows. Average annual herd-level AMU was low, with 3.6 DDDAit/biomass (range: 3.2–4.0) and 1.2 TI100 in cows (range: 1.1–1.3). Third and fourth generation cephalosporins, which are critical for human medicine, represented almost 10% of usage, and intramammary antimicrobials accounted for over 60%. We detected significant downward temporal trends in total AMU, as well as a positive relationship with herd size. The magnitude of such effects was small, leaving scant room for further reduction. However, the frequent use of critical antimicrobials and intramammary products should be addressed, following the principles of prudent AMU. Our findings highlight the importance of monitoring AMU even in low-production, smallholding contexts where a low usage is expected, to identify any deficiencies and implement interventions for further AMU optimisation. Full article
(This article belongs to the Special Issue Antibiotics Use in Farms, 2nd Edition)
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<p>Frequency distribution of cattle herds (<span class="html-italic">n</span> = 1260) included in the study by number of housed cows.</p>
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<p>Temporal trend of the average annual antimicrobial usage (AMU) per herd in cattle reared in the Aosta Valley (Italy): total AMU (orange) and usage of critical classes (red) included in the WHO’s Highest Priority Critically Important Antimicrobials list (i.e., polymyxins, quinolones, macrolides, third- and fourth-generation cephalosporins). Means were weighted on standardised biomass, and error bars represent 95% Confidence Intervals.</p>
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<p>Median antimicrobial usage from 2008 to 2018 in cows housed in Aosta Valley cattle farms, expressed as treatment incidence 100 (TI100). Error bars represent the interquartile range.</p>
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<p>Location of bovine herds (<span class="html-italic">n</span> = 1260) within the Aosta Valley region (Northern Italy) for which at least one year of antimicrobial usage data between 2008 and 2018 was available. Dot size is proportional to herd size as defined in the map legend. Map created using QGIS 3.22 software.</p>
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26 pages, 9640 KiB  
Article
The Lac Fallère Area as an Example of the Interplay between Deep-Seated Gravitational Slope Deformation and Glacial Shaping (Aosta Valley, NW Italy)
by Stefano Dolce, Maria Gabriella Forno, Marco Gattiglio and Franco Gianotti
GeoHazards 2024, 5(1), 38-63; https://doi.org/10.3390/geohazards5010003 - 11 Jan 2024
Cited by 1 | Viewed by 2155
Abstract
The Lac Fallère area in the upper Clusellaz Valley (tributary of the middle Aosta Valley) is shaped in micaschist and gneiss (Mont Fort Unit, Middle Penninic) and in calcschist and marble (Aouilletta Unit, Combin Zone). Lac Fallère exhibits an elongated shape and is [...] Read more.
The Lac Fallère area in the upper Clusellaz Valley (tributary of the middle Aosta Valley) is shaped in micaschist and gneiss (Mont Fort Unit, Middle Penninic) and in calcschist and marble (Aouilletta Unit, Combin Zone). Lac Fallère exhibits an elongated shape and is hosted in a WSW–ENE-trending depression, according to the slope direction. This lake also shows a semi-submerged WSW–ENE rocky ridge that longitudinally divides the lake. This evidence, in addition to the extremely fractured rocks, indicates a wide, deep-seated gravitational slope deformation (DSGSD), even if this area is not yet included within the regional landslide inventory of the Aosta Valley Region. The Lac Fallère area also shows reliefs involved in glacial erosion (roches moutonnée), an extensive cover of subglacial sediments, and many moraines essentially referred to as Lateglacial. The DSGSD evolution in a glacial environment produced, as observed in other areas, effects on the facies of Quaternary sediments and the formation of a lot of wide moraines. Glacial slope sectors and lateral moraines displaced by minor scarps and counterscarps, and glaciers using trenches forming several arched moraines, suggest an interplay between glacial and gravitational processes, which share part of their evolution history. Full article
(This article belongs to the Special Issue Geomorphological Mapping Research for Landslide)
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<p>Location of the Lac Fallère area (yellow line) consisting of the upper Clusellaz Valley and its tributary valleys; The blue lines are the watercourses.</p>
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<p>Elongated shape of Lac Fallère, along WSW–ENE trenches, and also characterised by a rocky ridge that longitudinally divides the lake.</p>
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<p>The Mont Fallère area evolution during the LGM and Lateglacial period (modified from [<a href="#B60-geohazards-05-00003" class="html-bibr">60</a>]); ?: The question marks indicate the lack of knowledge on the morphology of the slope in the pre-LGM phase.</p>
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<p>Simplified geological map of the Lac Fallère area. The red boxes refer to the case studies.</p>
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<p>Schmidt diagram of fractures collected in the study area. The fractures are reported as plan poles (black dots). Poles are clustered according to highly inclined surfaces with ENE–WSW, NE–SW, and NW–SE trends and, at low-angle surfaces, NW–SE and E–W trends.</p>
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<p>Main gravitational morpho-structures. The squares refer to the case studies.</p>
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<p>Detailed geological map of Lac Fallère (case 1) characterised by evident trenches and a bulging relief downstream of the lake. Black lines indicate the orientation of the glacial striae towards the SSE that characterise the <span class="html-italic">roche moutonnée</span>.</p>
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<p>Schmidt diagrams reporting the S2 poles (black dots) for the bulging relief sector downward Lac Fallère (<b>A</b>) and in the remaining study area (<b>B</b>). The dispersion of the regional foliation S2 is very evident in the bulging relief compared with S2 outside of this.</p>
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<p>Detailed geological map of the Lac des Feuilles area (case 2) with a moraine displaced by a minor scarp immediately NE of the lake across the Feuilles T.</p>
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<p>Detailed geological map of the complex rocky relief approximately 700 m north of Fourmière involved in minor scarps and counterscarps that also dislocate a moraine in M<sub>1</sub> and M<sub>2</sub>. A–A<sup>1</sup> is the trace of the geological cross section.</p>
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<p>Detailed geological map of the right side of the upper Clusellaz Valley with subglacial sediments (G<sub>1</sub>, G<sub>2</sub>, and G<sub>3</sub>) involving minor scarps (S<sub>1</sub> and S<sub>2</sub>) that appear covered by a Lateglacial moraine (M<sub>1</sub>). The bedrock and this moraine were later affected by a composite morpho-structure (S<sub>3</sub>, T<sub>1</sub>, S<sub>4</sub>, and T<sub>2</sub>). The square refers to a detailed picture of the relationships among morpho-structures, bedrock and glacial deposits.</p>
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<p>Trench T<sub>1</sub>, which involves the glacial slope G<sub>1</sub> and the more recent moraine M<sub>1</sub>.</p>
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<p>Cross section of the articulated relief north of Fourmière (case 3). The section over the white band is in the background and represents the geological view of the slope. See the map of <a href="#geohazards-05-00003-f010" class="html-fig">Figure 10</a> for the legend and location of A–A<sup>1</sup> cross section.</p>
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<p>Elongated shape of Lac Fallère along evident trenches (T), bordered downstream by a rocky bulging relief (B) and characterised by a submerged ridge shaped in the bedrock (R).</p>
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<p>A Lateglacial lateral moraine of the Feuilles Glacier displaced in M<sub>1</sub> and M<sub>2</sub> by an E–W-trending minor scarp (red line), which exposes rocks from the Distulberg Formation.</p>
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<p>Scarps (S<sub>1</sub> and S<sub>2</sub>) and counterscarps (C<sub>1</sub> and C<sub>2</sub>) that dislocate both the rocky relief (with the formation of R<sub>1</sub> and R<sub>2</sub> reliefs) and the moraine (M<sub>1</sub> and M<sub>2</sub>). See the map of <a href="#geohazards-05-00003-f010" class="html-fig">Figure 10</a> for the legend.</p>
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<p>Morphological surfaces on the right side of the Clusellaz Valley, with subglacial sediments (G<sub>1</sub>, G<sub>2</sub>, and G<sub>3</sub>) involved in rocky, minor scarps (S<sub>1</sub> and S<sub>2</sub>). The subsequent moraine (blue line) formed by ice-marginal sediments (M<sub>1</sub>) covers these minor scarps and is displaced by a more recent minor scarp (S<sub>3</sub>). See the map of <a href="#geohazards-05-00003-f011" class="html-fig">Figure 11</a> for the legend.</p>
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20 pages, 3841 KiB  
Article
Earth Observation Data and Geospatial Deep Learning AI to Assign Contributions to European Municipalities Sen4MUN: An Empirical Application in Aosta Valley (NW Italy)
by Tommaso Orusa, Annalisa Viani and Enrico Borgogno-Mondino
Land 2024, 13(1), 80; https://doi.org/10.3390/land13010080 - 10 Jan 2024
Cited by 12 | Viewed by 2133
Abstract
Nowadays, European program Copernicus’ Sentinel missions have allowed the development of several application services. In this regard, to strengthen the use of free satellite data in ordinary administrative workflows, this work aims to evaluate the feasibility and prototypal development of a possible service [...] Read more.
Nowadays, European program Copernicus’ Sentinel missions have allowed the development of several application services. In this regard, to strengthen the use of free satellite data in ordinary administrative workflows, this work aims to evaluate the feasibility and prototypal development of a possible service called Sen4MUN for the distribution of contributions yearly allocated to local municipalities and scalable to all European regions. The analysis was focused on the Aosta Valley region, North West Italy. A comparison between the Ordinary Workflow (OW) and the suggested Sen4MUN approach was performed. OW is based on statistical survey and municipality declaration, while Sen4MUN is based on geospatial deep learning techniques on aerial imagery (to extract roads and buildings to get real estate units) and yearly Land Cover map components according to European EAGLE guidelines. Both methods are based on land cover components which represent the input on which the financial coefficients for assigning contributions are applied. In both approaches, buffers are applied onto urban class (LCb). This buffer was performed according to the EEA-ISPRA soil consumption guidelines to avoid underestimating some areas that are difficult to map. In the case of Sen4MUN, this is applied to overcome Sentinel sensor limits and spectral mixing issues, while in the case of OW, this is due to limits in the survey method itself. Finally, a validation was performed assuming as truth the approach defined by law as the standard, i.e., OW, although it has limitations. MAEs involving LCb, road lengths and real estate units demonstrate the effectiveness of Sen4MUN. The developed approach suggests a contribution system based on Geomatics and Remote sensing to the public administration. Full article
(This article belongs to the Special Issue Applying Earth Observation Data for Urban Land-Use Change Mapping)
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<p>Area of study, involving the Region Valle d’Aosta, NW Italy. False color Sentinel-2 imagery 2022 meteorological summer composite (NIR, Red, Green).</p>
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<p>Sen4MUN workflow.</p>
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<p>MAEs computed per each municipality in Aosta Valley Autonomous Region comparing Sen4MUN with OW considering (<b>A</b>) Urban and anthropic areas; (<b>B</b>) Road length; (<b>C</b>) Real estate units.</p>
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19 pages, 18794 KiB  
Article
Slope-Scale Evolution Categorization of Deep-Seated Slope Deformation Phenomena with Sentinel-1 Data
by Davide Cardone, Martina Cignetti, Davide Notti, Danilo Godone, Daniele Giordan, Fabiana Calò, Simona Verde, Diego Reale, Eugenio Sansosti and Gianfranco Fornaro
Remote Sens. 2023, 15(23), 5440; https://doi.org/10.3390/rs15235440 - 21 Nov 2023
Viewed by 1564
Abstract
Deep-seated gravitational slope deformations (DsGSDs) are slope-scale phenomena which are widespread in mountainous regions. Despite interacting with human infrastructures and settlements, only a few cases are monitored with ground-based systems. Remote sensing technologies have recently become a consolidated instrument for monitoring and studying [...] Read more.
Deep-seated gravitational slope deformations (DsGSDs) are slope-scale phenomena which are widespread in mountainous regions. Despite interacting with human infrastructures and settlements, only a few cases are monitored with ground-based systems. Remote sensing technologies have recently become a consolidated instrument for monitoring and studying such widespread and slow processes. This paper proposes a three-step novel methodology to analyze the morpho-structural domain of DsGSDs by exploiting the advanced Differential Synthetic Aperture Radar Interferometry (A-DInSAR) technique through (i) the analysis of A-DInSAR measurement point density and distribution defining a coverage threshold; (ii) the assessment of the actual ground deformation with respect to the orientation of phenomena based on slope, aspect, and C-index; and (iii) ground deformation mapping with previously ranked velocity interpolation. The methodology was tested on two differently oriented phenomena: the mainly north–south-oriented Croix de Fana and the mainly east–west-oriented Valtournenche DsGSD, located in the Aosta Valley Region, northern Italy. The results show a variation in the kinematic behavior between the morpho-structural domains, while also considering any other superimposed surficial deformations. This work provides the lines for the implementation of a rapid and low-cost tool based on the use of A-DInSAR measurements which are suitable for assessing the impact of any type of DsGSD on the anthropic facilities and infrastructures in mountainous areas. Full article
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<p>Flow diagram of the developed methodology.</p>
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<p>(<b>a</b>) Map of the DsGSDs and landslides catalogued in the IFFI project [<a href="#B34-remotesensing-15-05440" class="html-bibr">34</a>] for the regional territory of the Aosta Valley. (<b>b</b>) Map of the morpho-structural domains recognizable within the Croix the Fana DsGSD. (<b>c</b>) Map of the morpho-structural domains recognizable within the Valtournenche DsGSD. Surficial displaces (e.g., debris coverage, minor nested landslides) and main anthropic elements that interfered with DsGSD evolution are also reported in the maps.</p>
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<p>PS distribution maps for ascending and descending orbit. (<b>a</b>) Map of PSs along the ascending orbit for Croix de Fana. (<b>b</b>) Map of PSs along the descending orbit for Croix de Fana. (<b>c</b>) Map of PSs along the ascending orbit for Valtournenche. (<b>d</b>) Map of PSs along the descending orbit for Valtournenche.</p>
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<p>Conceptual scheme of the SAR data suitability analysis. (<b>a</b>) C-index distribution matrix based on aspect/slope combination for ascending orbit; (<b>b</b>) C-index distribution matrix based on aspect/slope combination for descending orbit; (<b>c</b>) DSR matrix classified in the four main classes on the basis of <a href="#remotesensing-15-05440-t001" class="html-table">Table 1</a>.</p>
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<p>Analysis of PS density and distribution performed on the V<sub>SLOPE</sub> dataset. (<b>a</b>) Map of PS density that shows the valid cells (PS density ≥ 30 PSs/km<sup>2</sup>) and discarded cells (PS density &lt; 30 PSs/km<sup>2</sup>) for the DsGSD of Croix de Fana. (<b>b</b>) Map of C<sub>PS</sub> values expressed as a percentage for each domain of the DsGSD of Croix de Fana. (<b>c</b>) Map of PS density for the DsGSD of Valtournenche. (<b>d</b>) Maps of C<sub>PS</sub> values expressed as a percentage for each domain of the DsGSD of Valtournenche.</p>
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<p>These maps show the mean of the aspect, the mean of the slope, and the DSR calculated for each domain of both the DsGSDs for the V<sub>SLOPE</sub> dataset. (<b>a</b>) Map of the slope computed for each domain of Croix de Fana. (<b>b</b>) Map of the aspect computed for each domain of Croix de Fana. (<b>c</b>) DSR computed for each domain of Croix de Fana. (<b>d</b>) Map of the slope computed for each domain of Valtournenche. (<b>e</b>) Map of the aspect computed for each domain of Valtournenche. (<b>f</b>) DSR computed for each domain of the Valtournenche.</p>
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<p>Ranked ground deformation maps of the Croix de Fana DsGSD: (<b>a</b>) map obtained via the V<sub>v</sub> value interpolation; (<b>b</b>) map obtained via the V<sub>SLOPE</sub> value interpolation.</p>
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<p>Ground deformation maps of the Valtournenche DsGSD: (<b>a</b>) map obtained via the V<sub>LOSa</sub> value interpolation, (<b>b</b>) via the V<sub>SLOPE</sub> value interpolation, (<b>c</b>) via the V<sub>v</sub> value interpolation, and (<b>d</b>) via the V<sub>ew</sub> value interpolation. It should be noted that the coverage of the V<sub>v</sub> and V<sub>ew</sub> datasets in domain A is below the 25% threshold (<a href="#app1-remotesensing-15-05440" class="html-app">Table S1</a>).</p>
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<p>Overall intersection between the DsGSD phenomena and the anthropic elements. (<b>a</b>) Map of the V<sub>ew</sub> velocities related to the DsGSD of Valtournenche, affecting the Paquier village mainly in correspondence of the domain C. (<b>b</b>) Map of the V<sub>SLOPE</sub> interpolated velocities related to the DsGSD of Croix de Fana merged with the facilities of the hydroelectric plant of Quart and settlements variably distributed along the slope.</p>
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19 pages, 30442 KiB  
Article
Analysis of the Recharge Area of the Perrot Spring (Aosta Valley) Using a Hydrochemical and Isotopic Approach
by Luis Miguel Santillán-Quiroga, Daniele Cocca, Manuela Lasagna, Chiara Marchina, Enrico Destefanis, Maria Gabriella Forno, Marco Gattiglio, Giacomo Vescovo and Domenico Antonio De Luca
Water 2023, 15(21), 3756; https://doi.org/10.3390/w15213756 - 27 Oct 2023
Cited by 1 | Viewed by 1539
Abstract
The Perrot Spring (1300 m a.s.l.), located to the right of the Chalamy valley in the Monte Avic Natural Park (Valle d’Aosta, Italy), is an important source of drinking water for the municipality of Champdepraz. This spring is located on a large slope [...] Read more.
The Perrot Spring (1300 m a.s.l.), located to the right of the Chalamy valley in the Monte Avic Natural Park (Valle d’Aosta, Italy), is an important source of drinking water for the municipality of Champdepraz. This spring is located on a large slope characterised by the presence of a Quaternary cover of various origins (glacial, glaciolacustrine, and landslide) above the bedrock (essentially serpentinite referred to the Zermatt–Saas Zone, Penninic Domain). Water emerges at the contact between the landslide bodies and impermeable or semi-permeable glaciolacustrine deposits. The aim of this study is to define the processes and recharge zones of this spring. The analysis of the data revealed the presence of two contributions to the Perrot Spring input: a spring thaw contribution defined by a small increase in flow and an autumn contribution from rainwater infiltration. The low average temperature and low variation of the annual temperature (4.8–6.5 °C) suggest a sufficiently deep flow circuit. Chemical analyses showed a groundwater chemistry consistent with the regional geology: the hydrochemical facies is calcium–magnesium bicarbonate and isotopic analyses (δ2H and δ18O) of rainfall and spring water suggested a recharge altitude of about 2100 m a.s.l. In conclusion, this study makes it possible to recognize the water inputs to the spring discharge and to delineate its recharge area, which can be proposed to implement strategies to protect the resource. Full article
(This article belongs to the Special Issue The Use of Environmental Isotopes in Hydrogeology)
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<p>(<b>A</b>) Location of Aosta Valley in Italy. (<b>B</b>) Location of the study area (asterisk) in Northwestern Italy. (<b>C</b>) Location of the investigated area in the Chalamy Basin.</p>
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<p>Geological map of the study area.</p>
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<p>Map of permeability degree.</p>
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<p>Water sampling points in the study area: rainfall collectors, streams, lakes, and the Perrot Spring. See <a href="#water-15-03756-t002" class="html-table">Table 2</a> for co-ordinates.</p>
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<p>Average annual temperatures and rainfall for the period 2003–2022 at the Chevrère Station.</p>
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<p>Average monthly temperature and rainfall for the period 2003–2022 at the Chevrère Station.</p>
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<p>Snow height (SH) at Champorcher Station (modified from [<a href="#B62-water-15-03756" class="html-bibr">62</a>]).</p>
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<p>Piper diagram of the samples taken in various sites in July 2022 and in the Perrot Spring in February 2022 and May 2021. (R = stream; L = lake).</p>
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<p>Isotopic composition of water samples in the study area. Global and local meteoric line for northern Italy (GMWL and LMWL) are also reported for the comparison [<a href="#B61-water-15-03756" class="html-bibr">61</a>].</p>
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<p>Correlation graph between the altitude of the sampling points and the value of δ<sup>18</sup>O.</p>
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<p>Potential recharge area.</p>
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16 pages, 5039 KiB  
Article
Characterization and Valorization of Maize Landraces from Aosta Valley
by Alessandra Lezzi, Lorenzo Stagnati, Francesca Madormo, Denise Chabloz, Alessandra Lanubile, Marilisa Letey, Adriano Marocco, Mauro Bassignana and Matteo Busconi
Plants 2023, 12(14), 2674; https://doi.org/10.3390/plants12142674 - 17 Jul 2023
Cited by 3 | Viewed by 1627
Abstract
While there is a rich collection of maize germplasm from Italy, it lacks genetic resources from the Aosta Valley, an isolated mountain region where landraces have been preserved in the absence of modern germplasm introductions. These local materials, which are still cultivated mainly [...] Read more.
While there is a rich collection of maize germplasm from Italy, it lacks genetic resources from the Aosta Valley, an isolated mountain region where landraces have been preserved in the absence of modern germplasm introductions. These local materials, which are still cultivated mainly at household level, can have high importance from a genetic and historical point of view. In the present study, five landraces named, after the collecting sites, Arnad, Arnad-Crest, Châtillon, Entrebin and Perloz, were sampled in Aosta Valley and subjected to historic, morphologic and genetic characterization. This study provided evidence for the landraces’ long presence in Aosta Valley, a significant genetic variability and differentiation among the investigated landraces. Globally, 67 different alleles were detected ranging from 4 for markers phi127 and p-bnlg176 to 10 for phi031, with a mean of 6.7 alleles per locus. Observed heterozygosity levels were comprised from 0.16 to 0.51 and are generalkly lower than expected heterozigosity supporting fixation at some loci. STRUCTURE analysis revealed clear separation between accessions revealing the presence of four ancestral populations. This may be explained by the long reproductive isolation experienced by these materials. Finally, morphological observations confirm the high diversity between landraces revealing that they generally have flint kernels, variable color from yellow to dark red (Châtillon) while Perloz showed kernels with an apical beak. The present work confirms the importance of mountain areas in conserving biodiversity and increases the rich Italian maize germplasm with materials well adapted to marginal areas. Such new genetic variability may be used to breed new materials for more resilient agriculture. Full article
(This article belongs to the Section Plant Genetics, Genomics and Biotechnology)
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<p>Sampling location ad ear morphology of the five maize landraces. (<b>a</b>) Entrebin; (<b>b</b>) Châtillon; (<b>c</b>) Arnad; (<b>d</b>) Arnad-Crest and (<b>e</b>) Perloz. On the map, the location of Entrebin is reported in blue, Châtillon is reported in red, Arnad and Arnad-Crest in yellow, finally Perloz is reported in pink.</p>
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<p>Historical (1952; Photographer Octave Bérard. Regione Autonoma Valle d’Aosta, BREL Archive—Collection Bérard) and present (2021; Archive IAR) traditional drying of ears at the family who preserved Entrebin maize landrace.</p>
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<p>Principal Coordinates Analysis (PCoA): coordinate 1 vs. coordinate 2 of the 92 samples characterized by the 10 SSR set.</p>
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<p>Phylogenetic tree of the 92 individuals of the five maize landraces from Aosta Valley.</p>
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<p>Population genetic structure at K = 4 of the 92 individuals of 5 maize accessions evaluated in the present study. Different colors correspond to different ancestral populations.</p>
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<p>Population genetic structure at K = 5 of the 92 individuals of 5 maize accessions evaluated in the present study. Different colors correspond to different ancestral populations.</p>
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31 pages, 2818 KiB  
Article
Risk Assessment of Rising Temperatures Using Landsat 4–9 LST Time Series and Meta® Population Dataset: An Application in Aosta Valley, NW Italy
by Tommaso Orusa, Annalisa Viani, Boineelo Moyo, Duke Cammareri and Enrico Borgogno-Mondino
Remote Sens. 2023, 15(9), 2348; https://doi.org/10.3390/rs15092348 - 29 Apr 2023
Cited by 30 | Viewed by 2794
Abstract
Earth observation data have assumed a key role in environmental monitoring, as well as in risk assessment. Rising temperatures and consequently heat waves due to ongoing climate change represent an important risk considering the population, as well as animals, exposed. This study was [...] Read more.
Earth observation data have assumed a key role in environmental monitoring, as well as in risk assessment. Rising temperatures and consequently heat waves due to ongoing climate change represent an important risk considering the population, as well as animals, exposed. This study was focused on the Aosta Valley Region in NW Italy. To assess population exposure to these patterns, the following datasets have been considered: (1) HDX Meta population dataset refined and updated in order to map population distribution and its features; (2) Landsat collection (missions 4 to 9) from 1984 to 2022 obtained and calibrated in Google Earth Engine to model LST trends. A pixel-based analysis was performed considering Aosta Valley settlements and relative population distribution according to the Meta population dataset. From Landsat data, LST trends were modelled. The LST gains computed were used to produce risk exposure maps considering the population distribution and structure (such as ages, gender, etc.). To check the consistency and quality of the HDX population dataset, MAE was computed considering the ISTAT population dataset at the municipality level. Exposure-risk maps were finally realized adopting two different approaches. The first one considers only LST gain maximum by performing an ISODATA unsupervised classification clustering in which the separability of each class obtained and was checked by computing the Jeffries–Matusita (J-M) distances. The second one was to map the rising temperature exposure by developing and performing a risk geo-analysis. In this last case the input parameters considered were defined after performing a multivariate regression in which LST maximum was correlated and tested considering (a) Fractional Vegetation Cover (FVC), (b) Quote, (c) Slope, (d) Aspect, (e) Potential Incoming Solar Radiation (mean sunlight duration in the meteorological summer season), and (f) LST gain mean. Results show a steeper increase in LST maximum trend, especially in the bottom valley municipalities, and especially in new built-up areas, where more than 60% of the Aosta Valley population and domestic animals live and where a high exposure has been detected and mapped with both approaches performed. Maps produced may help the local planners and the civil protection services to face global warming from a One Health perspective. Full article
(This article belongs to the Special Issue Integrating Remote Sensing and GIS in Environmental Health Assessment)
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<p>Study Area corresponding to the boundaries of the Aosta Valley francophone Autonomous Region (NW Italy).</p>
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<p>Multiple correlation testing involving LST Gain Maximum, LST Gain Mean, Quote, FVC (Fractional Vegetation Cover), Slope, Aspect, Sun Duration (DS). Positive correlation is in blue, negative in red. Rectangles represent statistically significant <span class="html-italic">p</span>-value &lt; 0.05.</p>
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<p>Exposure-Risk class assessment map (scale 1:3,300,000). EPSG: 23032.</p>
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<p>Exposure-Risk class assessment map (with some zooms in in the bottom valley from East to West with a scale of 1:50,000). EPSG: 23032.</p>
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<p>Risk population exposure to rising LST mapped according to Equation (9). EPSG: 23032.</p>
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<p>Risk population exposure to rising LST mapped according to Equation (9) (with zooms in given areas with a scale of 1:50,000), EPSG: 23032.</p>
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39 pages, 1301 KiB  
Article
An Operational Checklist of the Birds of Northwestern Italy (Piedmont and Aosta Valley)
by Giovanni Boano, Marco Pavia, Gianfranco Alessandria and Toni Mingozzi
Diversity 2023, 15(4), 550; https://doi.org/10.3390/d15040550 - 13 Apr 2023
Cited by 2 | Viewed by 3484
Abstract
This paper provides the fourth edition of the checklist of birds recorded in northwestern Italy (the Piedmont and Aosta Valley regions) and covers more than 300 years of ornithological data, including subspecies. This work updates the previous works published in 1981, 2003, and [...] Read more.
This paper provides the fourth edition of the checklist of birds recorded in northwestern Italy (the Piedmont and Aosta Valley regions) and covers more than 300 years of ornithological data, including subspecies. This work updates the previous works published in 1981, 2003, and 2009, with the revision of the AERC codes and the addition of special annotations for several species. We also provide some new settings to make the bird checklist a more useful tool for all users, particularly scholars and professionals interested in biodiversity assessment and conservation reports. To this end, (a) new coding concerning population estimates and trends, as well as risk categories (Red List), is introduced; (b) bird lists are structured for analysis at two temporal levels: the General Checklist (GCL), covering the period from 1685 to 2022, and the Operational Checklist (OCL), covering the decade 2010–2019, providing periods of reference for comparison and analysis; and (c) an electronic spreadsheet is provided as part of the online Supplementary Materials to allow for further data analysis by readers, if necessary. The list presently contains 408 species and 444 taxonomic units, which consist of both subspecies and monotypic species. Each of them has been allocated to one of the AERC categories A, B, C, or D, while category E has been excluded. Since the publication of the previous list (2009), 19 species have been added. The avifauna currently breeding in the Piedmont and Aosta Valley regions comprises 197 species, with an additional 9 species that were once breeders but are now considered regionally extinct. Full article
(This article belongs to the Special Issue Biodiversity in Italy: Past and Future Perspectives)
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<p>Map of northwestern Italy (Piedmont and Aosta Valley, PAV). The nine provinces (the capital cities and administrative areas) are indicated on the map; the most important geographical sectors, lakes, and rivers are also indicated.</p>
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<p>Risk level (percentage classes) expressed for each breeding species (n = 203) in PAV belonging to the Operational Checklist 2010–2019 (see <a href="#diversity-15-00550-t004" class="html-table">Table 4</a> for details).</p>
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14 pages, 1902 KiB  
Article
External Benefits of Irrigation in Mountain Areas: Stakeholder Perceptions and Water Policy Implications
by Silvia Novelli, Francesca Moino and Patrizia Borsotto
Land 2022, 11(9), 1395; https://doi.org/10.3390/land11091395 - 25 Aug 2022
Cited by 2 | Viewed by 2132 | Correction
Abstract
Irrigation contributes to land and ecosystem degradation, especially in intensive farming areas. However, in marginal areas, long-established irrigation systems also supply agroecosystem services. This study aimed to identify and prioritize the external benefits provided by irrigation in extensive grazing farms in an Italian [...] Read more.
Irrigation contributes to land and ecosystem degradation, especially in intensive farming areas. However, in marginal areas, long-established irrigation systems also supply agroecosystem services. This study aimed to identify and prioritize the external benefits provided by irrigation in extensive grazing farms in an Italian alpine region (Aosta Valley, NW Italy). Three local stakeholder groups (land irrigation consortia members, non-farmer users of the irrigation water service, and non-user citizens) engaged in focus group discussions. The transcriptions were analyzed with an integrated subjective and computer-assisted approach. The main result of the study showed that a convergence of stakeholder opinions led to prioritization of the same four benefits, i.e., hydro-geological and land maintenance, traditional agricultural landscape conservation, biodiversity conservation, and leisure recreational activities provision. Incorporating this information into decision-making processes is relevant in marginal mountain areas, especially in light of the implementation of the water pricing policy laid down in the EU Water Framework Directive. To this end, the economic value of the external benefits should be considered along with the recovery costs for water services. Such information is essential to balance the environmental costs of irrigation and to compare the resource cost of alternative water uses. Full article
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<p>Diagram of methodological approach.</p>
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<p>Benefits ranked based on question Q2.</p>
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<p>Discussion topics compared across different stakeholder types: (<b>a</b>) Spoken words on each topic (%); (<b>b</b>) participants involved in the discussion (n).</p>
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15 pages, 790 KiB  
Article
An Integrated, Tentative Remote-Sensing Approach Based on NDVI Entropy to Model Canine Distemper Virus in Wildlife and to Prompt Science-Based Management Policies
by Emanuele Carella, Tommaso Orusa, Annalisa Viani, Daniela Meloni, Enrico Borgogno-Mondino and Riccardo Orusa
Animals 2022, 12(8), 1049; https://doi.org/10.3390/ani12081049 - 18 Apr 2022
Cited by 40 | Viewed by 3988
Abstract
Changes in land use and land cover as well as feedback on the climate deeply affect the landscape worldwide. This phenomenon has also enlarged the human–wildlife interface and amplified the risk of potential new zoonoses. The expansion of the human settlement is supposed [...] Read more.
Changes in land use and land cover as well as feedback on the climate deeply affect the landscape worldwide. This phenomenon has also enlarged the human–wildlife interface and amplified the risk of potential new zoonoses. The expansion of the human settlement is supposed to affect the spread and distribution of wildlife diseases such as canine distemper virus (CDV), by shaping the distribution, density, and movements of wildlife. Nevertheless, there is very little evidence in the scientific literature on how remote sensing and GIS tools may help the veterinary sector to better monitor the spread of CDV in wildlife and to enforce ecological studies and new management policies in the near future. Thus, we perform a study in Northwestern Italy (Aosta Valley Autonomous Region), focusing on the relative epidemic waves of CDV that cause a virulent disease infecting different animal species with high host mortality. CDV has been detected in several mammalian from Canidae, Mustelidae, Procyonidae, Ursidae, and Viverridae families. In this study, the prevalence is determined at 60% in red fox (Vulpes vulpes, n = 296), 14% in wolf (Canis lupus, n = 157), 47% in badger (Meles meles, n = 103), and 51% in beech marten (Martes foina, n = 51). The detection of CDV is performed by means of real-time PCR. All the analyses are done using the TaqMan approach, targeting the chromosomal gene for phosphoprotein, gene P, that is involved in the transcription and replication of the virus. By adopting Earth Observation Data, we notice that CDV trends are strongly related to an altitude gradient and NDVI entropy changes through the years. A tentative model is developed concerning the ground data collected in the Aosta Valley region. According to our preliminary study, entropy computed from remote-sensing data can represent a valuable tool to monitor CDV spread as a proxy data predictor of the intensity of fragmentation of a given landscape and therefore also to monitor CDV. In conclusion, the evaluation from space of the landscape variations regarding the wildlife ecological corridors due to anthropic or natural disturbances may assist veterinarians and wildlife ecologists to enforce management health policies in a One Health perspective by pointing out the time and spatial conditions of interaction between wildlife. Surveillance and disease control actions are supposed to be carried out to strengthen the usage of geospatial analysis tools and techniques. These tools and techniques can deeply assist in better understanding and monitoring diseases affecting wildlife thanks to an integrated management approach. Full article
(This article belongs to the Collection Wildlife Disease Ecology and Management)
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<p>Study area. The Aosta Valley region in NW Italy. Reference system ED50-UTM 32 N.</p>
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<p>Surfaces not included in the computation of NDVIt Entropy and that are therefore masked. Reference system WGS84.</p>
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<p>CDV trends in Aosta Valley.</p>
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<p>CDV trends in Aosta Valley.</p>
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<p>GLM between anomalies in NDVI entropy and CDV spread (data were grouped annually considering the entire Aosta Valley territory).</p>
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<p>H<sub>NDVIt</sub> maps adopted and calculated at a pixel level, grouped into two classes, and finally merged into a final one. Reference system WGS84.</p>
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