568 research outputs found

    Il Pooling-score (P-score): Variabilit\ue0 inter- e intra-individuale nella valutazione endoscopica della gravit\ue0 della disfagia

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    This study evaluated the intra- and inter-rater reliability of the Pooling score (P-score) in clinical endoscopic evaluation of severity of swal- lowing disorder, considering excess residue in the pharynx and larynx. The score (minimum 4 - maximum 11) is obtained by the sum of the scores given to the site of the bolus, the amount and ability to control residue/bolus pooling, the latter assessed on the basis of cough, raclage, number of dry voluntary or re ex swallowing acts ( 5). Four judges evaluated 30 short lms of pharyngeal transit of 10 solid (1/4 of a cracker), 11 creamy (1 tablespoon of jam) and 9 liquid (1 tablespoon of 5 cc of water coloured with methlyene blue, 1 ml in 100 ml) boluses in 23 subjects (10 M/13 F, age from 31 to 76 yrs, mean age 58.56\ub111.76 years) with different pathologies. The lms were randomly distributed on two CDs, which differed in terms of the sequence of the lms, and were given to judges (after an explanatory ses- sion) at time 0, 24 hours later (time 1) and after 7 days (time 2). The inter- and intra-rater reliability of the P-score was calculated using the intra-class correlation coef cient (ICC; 3,k). The possibility that consistency of boluses could affect the scoring of the lms was considered. The ICC for site, amount, management and the P-score total was found to be, respectively, 0.999, 0.997, 1.00 and 0.999. Clinical evaluation of a criterion of severity of a swallowing disorder remains a crucial point in the management of patients with pathologies that predispose to complications. The P-score, derived from static and dynamic parameters, yielded a very high correlation among the scores attributed by the four judges during observations carried out at different times. Bolus consistencies did not affect the outcome of the test: the analysis of variance, performed to verify if the scores attributed by the four judges to the parameters selected, might be in uenced by the different consistencies of the boluses, was not signi cant. These initial data validate the clinical use of the P-score in the management of patients with deglutition disorders by a multidisciplinary team

    Sensitivity of the Atlantic meridional overturning circulation to South Atlantic freshwater anomalies

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    The sensitivity of the Atlantic Meridional Overturning Circulation (AMOC) to changes in basin integrated net evaporation is highly dependent on the zonal salinity contrast at the southern border of the Atlantic. Biases in the freshwater budget strongly affect the stability of the AMOC in numerical models. The impact of these biases is investigated, by adding local anomaly patterns in the South Atlantic to the freshwater fluxes at the surface. These anomalies impact the freshwater and salt transport by the different components of the ocean circulation, in particular the basin-scale salt-advection feedback, completely changing the response of the AMOC to arbitrary perturbations. It is found that an appropriate dipole anomaly pattern at the southern border of the Atlantic Ocean can collapse the AMOC entirely even without a further hosing. The results suggest a new view on the stability of the AMOC, controlled by processes in the South Atlantic. <br/

    On Pacific Subtropical Cell Variability over the Second Half of the Twentieth Century

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    Abstract The evolution of the Pacific subtropical cells (STC) is presented for the period 1948–2007. Using ocean models of different resolutions forced with interannually varying atmospheric forcing datasets, the mechanisms responsible for the observed STC weakening and late recovery during the period of study are analyzed. As a result of the STC weakening (strengthening), warming (cooling) trends are found in the equatorial Pacific sea surface temperatures (SSTs). Model results agree well with observed estimates of STC transport, STC convergence, and equatorial SST anomalies. It is shown that subtropical atmospheric variability is the primary driver of the STC and equatorial SST low-frequency evolution and is responsible for both the slowdown during the second half of the twentieth century and the rebound at the end of the century. Subtropically forced STC variability is identified as a major player in the generation of equatorial Pacific decadal SST anomalies, pacing tropical Pacific natural climate variability on interdecadal time scales, as observed in historical records. The natural mode of variability has implications for the evolution of equatorial SST in the coming decades under the concomitant effects of climate change

    Ester content of blueberry fruit can be ruled by tailored controlled atmosphere storage management

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    This study examines the effects of controlled atmosphere (CA) storage with high CO2 concentration (16 KPa) on the volatile organic compound (VOC) profile of blueberries (Vaccinium spp.), considering their genetic variability. The research focuses on the denovo production of esters and their association with fermentation related VOCs, employing complementary analytical techniques for comprehensive VOC profiling: direct injection mass spectrometry using Proton Transfer Reaction - Time of Flight - Mass Spectrometry (PTR-ToF-MS) and gas chromatography utilizing Solid-phase microextraction coupled to gas chromatography-mass spectrometry (SPME/GC-MS). In the first experiment, PTR-ToF-MS and SPME/GC-MS were applied to analyze the volatilome of seven blueberry cultivars under regular (RA) and controlled (CA) atmosphere storage conditions for 42 days. In the second experiment, 39 cultivars were tested to evaluate genetic variability in response to CA storage using PTR-ToF-MS. The third experiment focused on the effect of different oxygen concentrations during storage (1, 7, and 12 kPa O2), studying four cultivars using PTR-ToF-MS. Results of the three experiments revealed high variability among Vaccinium genotypes for all quality traits, which was amplified during storage, particularly under modified atmosphere conditions. CA storage generally enhanced the positive effects of cold storage by reducing texture decay and water loss and improving VOC profiles. Several ester compounds were synthesized de novo under low oxygen conditions, possibly as a response to hypoxic stress. The study concludes that CA storage offers potential to enhance postharvest fruit quality beyond shelf-life extension. The increase in fruity ester compounds during storage may improve blueberries' organoleptic properties. However, the variability in responses among cultivars needs tailored storage protocols. This research provides valuable insights for market segmentation and breeding programs aimed at enhancing blueberry quality and storability, while also validating PTR-ToF-MS as a rapid phenotyping tool for blueberry assessmen

    High-throughput analysis of food volatilome by direct injection mass spectrometry

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    Rapid, non-invasive and real-time analysis of food volatilome by direct injection mass spectrometry (DIMS) techniques contributes to the evaluation of food quality. Among DIMS application, we report three case studies show the potential of the PTR-ToF-MS technique in product characterization and process monitorin

    Role of the Seasonal Cycle in the Subduction Rates of Upper–Southern Ocean Waters

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    Abstract A kinematic approach is used to diagnose the subduction rates of upper–Southern Ocean waters across seasonally migrating density outcrops at the base of the mixed layer. From an Eulerian viewpoint, the term representing the temporal change in the mixed layer depth (which is labeled as the temporal induction in this study; i.e., Stemp = ∂h/∂t where h is the mixed layer thickness, and t is time) vanishes over several annual cycles. Following seasonally migrating density outcrops, however, the temporal induction is attributed partly to the temporal change in the mixed layer thickness averaged over a density outcrop following its seasonally varying position and partly to the lateral movement of the outcrop position intersecting the sloping mixed layer base. Neither the temporal induction following an outcrop nor its integral over the outcrop area vanishes over several annual cycles. Instead, the seasonal eddy subduction, which arises primarily because of the subannual correlations between the seasonal cycles of the mixed layer depth and the outcrop area, explains the key mechanism by which mode waters are transferred from the mixed layer to the underlying pycnocline. The time-mean exchange rate of waters across the base of the mixed layer is substantially different from the exchange rate of waters across the fixed winter mixed layer base in mode water density classes. Nearly 40% of the newly formed Southern Ocean mode waters appear to be diapycnally transformed within the seasonal pycnocline before either being subducted into the main pycnocline or entrained back to the mixed layer through lighter density classes
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