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1.
Eur Rev Med Pharmacol Sci ; 27(14): 6876-6881, 2023 Jul.
Article in English | MEDLINE | ID: mdl-37522700

ABSTRACT

OBJECTIVE: This retrospective study aimed at ascertaining the clinical usefulness of nebulized myo-inositol in the management of patients affected by bronchiectasis. PATIENTS AND METHODS: 19 patients, aged between 63 and 73 years old, with bronchiectasis, were treated for 15 days with nebulized myo-inositol or placebo. Lung functionality [forced expiratory volume in the 1st second (FEV1)], solid content of expectorate, and surfactant tension were analyzed. RESULTS: All patients treated with nebulized myo-inositol had a significant decrease in the percentage of solid content in the expectorate (T0 7.9±2.8% vs. T1 5.2±2.7%; p<0.001) and surfactant tension (T0 81.5±6.9 mN/m vs. T1 77.4±7.2 mN/m; p<0.001). Among treated patients, these variations correlated with FEV1 (rs=- 0.79; p<0.01) and forced expiratory flow at 25-75% of FVC (FEF25-75%) (rs=-0.81; p<0.01) scores. Also, variation of surfactant tension correlated with FEV1 (rs= -0.74; p<0.05) score. CONCLUSIONS: Nebulized myo-inositol increases lung functionality and mucus clearance in patients affected by bronchiectasis.


Subject(s)
Bronchiectasis , Pulmonary Surfactants , Humans , Infant , Retrospective Studies , Bronchiectasis/drug therapy , Forced Expiratory Volume , Surface-Active Agents/pharmacology , Surface-Active Agents/therapeutic use , Inositol/therapeutic use , Lung , Vital Capacity
2.
Science ; 378(6618): 412-417, 2022 10 28.
Article in English | MEDLINE | ID: mdl-36302013

ABSTRACT

Two >130-meter-diameter impact craters formed on Mars during the later half of 2021. These are the two largest fresh impact craters discovered by the Mars Reconnaissance Orbiter since operations started 16 years ago. The impacts created two of the largest seismic events (magnitudes greater than 4) recorded by InSight during its 3-year mission. The combination of orbital imagery and seismic ground motion enables the investigation of subsurface and atmospheric energy partitioning of the impact process on a planet with a thin atmosphere and the first direct test of martian deep-interior seismic models with known event distances. The impact at 35°N excavated blocks of water ice, which is the lowest latitude at which ice has been directly observed on Mars.

3.
J Geophys Res Planets ; 127(5): e2022JE007190, 2022 May.
Article in English | MEDLINE | ID: mdl-35865505

ABSTRACT

Observations of the South Polar Residual Cap suggest a possible erosion of the cap, leading to an increase of the global mass of the atmosphere. We test this assumption by making the first comparison between Viking 1 and InSight surface pressure data, which were recorded 40 years apart. Such a comparison also allows us to determine changes in the dynamics of the seasonal ice caps between these two periods. To do so, we first had to recalibrate the InSight pressure data because of their unexpected sensitivity to the sensor temperature. Then, we had to design a procedure to compare distant pressure measurements. We propose two surface pressure interpolation methods at the local and global scale to do the comparison. The comparison of Viking and InSight seasonal surface pressure variations does not show changes larger than ±8 Pa in the CO2 cycle. Such conclusions are supported by an analysis of Mars Science Laboratory (MSL) pressure data. Further comparisons with images of the south seasonal cap taken by the Viking 2 orbiter and MARCI camera do not display significant changes in the dynamics of this cap over a 40 year period. Only a possible larger extension of the North Cap after the global storm of MY 34 is observed, but the physical mechanisms behind this anomaly are not well determined. Finally, the first comparison of MSL and InSight pressure data suggests a pressure deficit at Gale crater during southern summer, possibly resulting from a large presence of dust suspended within the crater.

4.
Space Sci Rev ; 217(1): 20, 2021.
Article in English | MEDLINE | ID: mdl-33583960

ABSTRACT

Nine simulations are used to predict the meteorology and aeolian activity of the Mars 2020 landing site region. Predicted seasonal variations of pressure and surface and atmospheric temperature generally agree. Minimum and maximum pressure is predicted at Ls ∼ 145 ∘ and 250 ∘ , respectively. Maximum and minimum surface and atmospheric temperature are predicted at Ls ∼ 180 ∘ and 270 ∘ , respectively; i.e., are warmest at northern fall equinox not summer solstice. Daily pressure cycles vary more between simulations, possibly due to differences in atmospheric dust distributions. Jezero crater sits inside and close to the NW rim of the huge Isidis basin, whose daytime upslope (∼east-southeasterly) and nighttime downslope (∼northwesterly) winds are predicted to dominate except around summer solstice, when the global circulation produces more southerly wind directions. Wind predictions vary hugely, with annual maximum speeds varying from 11 to 19 ms - 1 and daily mean wind speeds peaking in the first half of summer for most simulations but in the second half of the year for two. Most simulations predict net annual sand transport toward the WNW, which is generally consistent with aeolian observations, and peak sand fluxes in the first half of summer, with the weakest fluxes around winter solstice due to opposition between the global circulation and daytime upslope winds. However, one simulation predicts transport toward the NW, while another predicts fluxes peaking later and transport toward the WSW. Vortex activity is predicted to peak in summer and dip around winter solstice, and to be greater than at InSight and much greater than in Gale crater. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1007/s11214-020-00788-2.

5.
Eur Rev Med Pharmacol Sci ; 24(15): 8187-8193, 2020 08.
Article in English | MEDLINE | ID: mdl-32767348

ABSTRACT

The ongoing worldwide pandemic of Coronavirus disease 2019 (COVID-19), raised the urgency to address knowledge gaps and to establish evidence for improving management and control of this viral infection. Throughout a keen analysis of the World Health Organization (WHO) most updated data, a gender-specific difference in the occurrence of infection was determined, which seems to correlate with patient's vitamin D status. Therefore, our purpose is to provide insights into the nutritional importance of vitamin D for its immunomodulatory effect, in order to help counteracting the COVID-19 pandemic. Novel interesting findings suggest that vitamin D, by inducing progesterone-induced blocking factor (PIBF), might regulate the immune response and also modulate cytokine IL-6, which appears to be increased in COVID-19 infections. Therefore, in addition to the standard recommendations to prevent the infection, supplementation of vitamin D might be considered an approach to help counteracting this global epidemic.


Subject(s)
Coronavirus Infections/immunology , Interleukin-6/immunology , Pneumonia, Viral/immunology , Pregnancy Proteins/immunology , Suppressor Factors, Immunologic/immunology , Vitamin D Deficiency/drug therapy , Vitamin D/immunology , Vitamin D/therapeutic use , Vitamins/therapeutic use , Betacoronavirus , COVID-19 , Coronavirus Infections/drug therapy , Coronavirus Infections/epidemiology , Coronavirus Infections/prevention & control , Geography , Humans , Inflammation , Italy/epidemiology , Pandemics/prevention & control , Pneumonia, Viral/epidemiology , Pneumonia, Viral/prevention & control , SARS-CoV-2 , Ultraviolet Rays , Vitamin D Deficiency/immunology , COVID-19 Drug Treatment
6.
Nat Commun ; 11(1): 1014, 2020 02 24.
Article in English | MEDLINE | ID: mdl-32094337

ABSTRACT

The Interior Exploration using Seismic Investigations, Geodesy and Heat Transport (InSight) spacecraft landed successfully on Mars and imaged the surface to characterize the surficial geology. Here we report on the geology and subsurface structure of the landing site to aid in situ geophysical investigations. InSight landed in a degraded impact crater in Elysium Planitia on a smooth sandy, granule- and pebble-rich surface with few rocks. Superposed impact craters are common and eolian bedforms are sparse. During landing, pulsed retrorockets modified the surface to reveal a near surface stratigraphy of surficial dust, over thin unconsolidated sand, underlain by a variable thickness duricrust, with poorly sorted, unconsolidated sand with rocks beneath. Impact, eolian, and mass wasting processes have dominantly modified the surface. Surface observations are consistent with expectations made from remote sensing data prior to landing indicating a surface composed of an impact-fragmented regolith overlying basaltic lava flows.

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