CO2 production of the chick embryo during the first day of post-laying development.

The carbon dioxide production of the chick embryo cultured in vitro has been determined during the first 24 h of post-laying development using a non-invasive conductometric microtechnique. The mean CO2 production of the whole blastoderm (1) increased from 16 nmol/h at laying to 231 nmol/h at early neurulation, (2) became dependent on exogenous glucose and (3) was closely linked to mechanical tension generated in the blastoderm (loosening from vitelline membrane resulted in a decrease of 56%). In our experimental conditions, no significant influence of carbonic anhydrase on the CO2 production has been detected. The value of the respiratory exchange ratio varied from about 3 at pregastrular stages to 1 at neurula stage and CO2 was produced transiently in presence of antimycin A. Such results indicate that the source of CO2 is not exclusively mitochondrial and that the relative proportions of mitochondrial and non-mitochondrial CO2 productions might vary significantly throughout the early development. Our findings confirm that the metabolism of the chick embryo becomes more and more oxidative from laying onwards and suggest that the modifications of metabolism observed during the studied period of development could be associated with functional differentiation.

Emissioni atmosferiche da discariche di rifiuti in Lombardia: stato attuale e scenari tecnologici di riduzione

Lo studio ha valutato le emissioni atmosferiche in Regione Lombardia dallo smaltimento di rifiuti solidi in discariche controllate nell'anno 2001, proiettandone i quantitativi attesi a medio e lungo termine sulla base degli scenari di evoluzione più attendibili per le caratteristiche qualitative dei fifiuti, le modalità di smaltimento e le tecnologie adottabili per il controllo delle emissioni stesse. La valutazione è stata condotta acquisendo i dati base degli impianti attualmente presenti sul territorio lombardo per quanto riguarda i rifiuti smaltiti e le modalità di captazione e di combustione del biogas. Sono stati quindi definiti alcuni scenari alternativi ragionevolmente ipotizzabili nel medio e lungo periodo per lo smaltimento dei rifiuti, sulla base dell'evoluzione imposta dalla normativa nazionale e dagli strumenti della pianificazione regionale. L'individuazione delle migliori tecnologie applicabili per la captazione ed il trattamento del gas prodotto e per il controllo delle corrispondenti emissioni atmosferiche ha permesso di stimare l'evoluzione temporale, in corrispondenza dei diversi scenari, della produzione di gas e delle emissioni dei principali inquinanti di interesse. I risultati mostrano la possibilità di ottenere una consistente riduzione delle emissioni di metano, tale da comportare a scala regionale una corrispondente diminuzione del 2% delle emissioni complessive di C02 equivalente. [Autore]

Carbon and oxygen isotope study of hydrothermal carbonates in the zinc-lead deposits of the San Vicente district, central Peru: A quantitative modeling on mixing processes and CO2 degassing

Carbon and oxygen isotope studies of the host and gangue carbonates of Mississippi Valley-type zinc-lead deposits in the San Vicente District hosted in the Upper Triassic to Lower Jurassic dolostones of the Pucara basin (central Peru) were used to constrain models of the ore formation. A mixing model between an incoming hot saline slightly acidic radiogenic (Pb, Sr) fluid and the native formation water explains the overall isotopic variation (delta(13)C = - 11.5 to + 2.5 parts per thousand relative to PDB and delta(18)O = + 18.0 to + 24.3 parts per thousand relative to SMOW) of the carbonate generations. The dolomites formed during the main ore stage show a narrower range (delta(13)C = - 0.1 to + 1.7 parts per thousand and delta(18)O = + 18.7 to + 23.4 parts per thousand) which is explained by exchange between the mineralizing fluids and the host carbonates combined with changes in temperature and pressure. This model of fluid-rock interaction explains the pervasive alteration of the host dolomite I and precipitation of sphalerite I. The open-space filling hydrothermal white sparry dolomite and the coexisting sphalerite II formed by prolonged fluid-host dolomite interaction and limited CO2 degassing. Late void-filling dolomite III (or calcite) and the associated sphalerite III formed as the consequence of CO2 degassing and concomitant pH increase of a slightly acidic ore fluid. Widespread brecciation is associated to CO2 outgassing. Consequently, pressure variability plays a major role in the ore precipitation during the late hydrothermal events in San Vicente. The presence of native sulfur associated with extremely carbon-light calcites replacing evaporitic sulfates (e.g., delta(13)C = - 11.5 parts per thousand), altered native organic matter and heavier hydrothermal bitumen (from - 27.0 to - 23.0 parts per thousand delta(13)C) points to thermochemical reduction of sulfate and/or thiosulfate. The delta(13)C- and delta(18)O-values of the altered host dolostone and hydrothermal carbonates, and the carbon isotope composition of the associated organic matter show a strong regional homogeneity. These results coupled with the strong mineralogical and petrographic similarities of the different MVT occurrences perhaps reflects the fact that the mineralizing processes were similar in the whole San Vicente belt, suggesting the existence of a common regional mineralizing hydrothermal system with interconnected plumbing.

Numerical analysis of wave-induced fluid flow effects on seismic data: Application to monitoring of CO2 storage at the Sleipner Field

In this work we analyze how patchy distributions of CO2 and brine within sand reservoirs may lead to significant attenuation and velocity dispersion effects, which in turn may have a profound impact on surface seismic data. The ultimate goal of this paper is to contribute to the understanding of these processes within the framework of the seismic monitoring of CO2 sequestration, a key strategy to mitigate global warming. We first carry out a Monte Carlo analysis to study the statistical behavior of attenuation and velocity dispersion of compressional waves traveling through rocks with properties similar to those at the Utsira Sand, Sleipner field, containing quasi-fractal patchy distributions of CO2 and brine. These results show that the mean patch size and CO2 saturation play key roles in the observed wave-induced fluid flow effects. The latter can be remarkably important when CO2 concentrations are low and mean patch sizes are relatively large. To analyze these effects on the corresponding surface seismic data, we perform numerical simulations of wave propagation considering reservoir models and CO2 accumulation patterns similar to the CO2 injection site in the Sleipner field. These numerical experiments suggest that wave-induced fluid flow effects may produce changes in the reservoir's seismic response, modifying significantly the main seismic attributes usually employed in the characterization of these environments. Consequently, the determination of the nature of the fluid distributions as well as the proper modeling of the seismic data constitute important aspects that should not be ignored in the seismic monitoring of CO2 sequestration problems.

Intérêt du monitorage du CO2 expiré pour évaluer la PaCO2 lors d'insuffisance respiratoire aiguë hypercapnique traitée par ventilation non invasive.

Introduction: L'efficacité d'une séance de VNI est habituellement évaluée selon la réponse clinique, l'amélioration de l'acidose respiratoire et de l'hypercapnie. Le but de cette étude était d'évaluer l'intérêt de la mesure du CO2 en fin d'expiration (PETCO2) pour estimer la PaCO2 et son évolution dans le temps. Patients et Méthodes: Des patients de réanimation souffrant d'une insuffisance respiratoire aiguë hypercapnique (PaCO2 >45 mmHg) ont été inclus dans cette étude prospective. La PETCO2était mesurée à l'aide d'un capteur nasobuccal (SmartLine®, Oridion) au cours d'une séance de VNI de 60 minutes. Une gazométrie artérielle et la valeur de PETCO2 étaient enregistrées au début de la séance puis chaque 15 minutes. Des manoeuvres d'expiration complète passives et actives étaient effectuées à 30 et 60 minutes. Le gradient de CO2 (PaCO2- PETCO2) a été calculé pour l'ensemble des mesures, spécifiquement pour chaque manoeuvre d'expiration complète, ainsi qu'individuellement pour chaque patient. Ces grandeurs sont exprimées en moyenne et écart-type pour évaluer le biais et la dispersion observés entre PaCO2 et PETCO2. La différence entre chaque valeurs consécutives de gradient de CO2 (delta gradient de CO2) a été calculées par patient. Cette mesure quantifie la variation au cours du temps du gradient de CO2 pour un patient donné. Résultats: 11 patients ont été inclus (7 BPCO, 1 restrictif et 1 syndrome d'apnée du sommeil). Sur l'ensemble des mesures, le gradient de CO2 était de 14.7 + 10.6 mmHg, lors des manoeuvres d'expiration complètes active il était de 8.1 + 13.0 mmHg, et de 8.8 + 11.9 mmHg lors des expirations passives. Conclusion: Chez les patients présentant une insuffisance respiratoire aiguë hypercanique traitée par VNI, la mesure de la PETCO2 par capteur nasobuccal ne permet de prédire ni la valeur de PaCO2, ni son évolution dans le temps. Les manoeuvres d'expiration complète n'apportent aucune plus value.