Monitoring Transcutaneously Measured Partial Pressure of CO2 During Intubation in Critically Ill Subjects

2021 ◽  
pp. respcare.08009
Author(s):  
Aurélien Frérou ◽  
Adel Maamar ◽  
Sonia Rafi ◽  
Claire Lhommet ◽  
Pierre Phelouzat ◽  
...  
Keyword(s):  
Partial Pressure ◽  
Critically Ill ◽  
Partial Pressure Of Co2

scholarly journals A Simple and Accurate Approach for Determining the VFA Concentration in Anaerobic Digestion Liquors, Relying on Two Titration Points and an External Inorganic Carbon Analysis

2021 ◽  
Vol 5 (2) ◽  
pp. 15
Author(s):  
Paz Nativ ◽  
Yonatan Gräber ◽  
Yaron Aviezer ◽  
Ori Lahav
Keyword(s):  
Partial Pressure ◽  
Volatile Fatty Acids ◽  
Inorganic Carbon ◽  
Strong Acid ◽  
Direct Analysis ◽  
Anaerobic Digesters ◽  
Acid Titration ◽  
Partial Pressure Of Co2 ◽  
Ph Range

A new analytic approach is presented for determining the total volatile fatty acids (VFAT) concentration in anaerobic digesters. The approach relies on external determination of the inorganic carbon concentration (CT) in the analyzed solution, along with two strong-acid titration points. The CT concentration can be determined by either a direct analysis (e.g., by using a TOC device) or by estimating it from the recorded partial pressure of CO2(g) in the biogas (often a routine analysis in anaerobic digesters). The titration is carried out to pH 5.25 and then to pH 4.25. The two titration results are plugged into an alkalinity-mass-based equation and then the two terms are subtracted from each other to yield an equation in which VFAT is the sole unknown (since CT is known and the effect of the total orthophosphate and ammonia concentrations is shown to be small at this pH range). The development of the algorithm and its verification on four anaerobic reactor liquors is presented, on both the raw water and on acetic acid-spiked samples. The results show the method to be both accurate (up to 2.5% of the expected value for VFAT/Alkalinity >0.2) and repetitive when the total orthophosphate and ammonia concentrations are known, and fairly accurate (±5% for VFAT >5 mM) when these are completely neglected. PHREEQC-assisted computation of CT from the knowledge of the partial pressure of CO2(g) in the biogas (and pH, EC and temperature in the liquor) resulted in a very good estimation of the CT value (±3%), indicating that this technique is adequate for the purpose of determining VFAT for alarming operators in case of process deterioration and imminent failure.

scholarly journals Hurricane Arthur and its effect on the short-term variability of pCO<sub>2</sub> on the Scotian Shelf, NW Atlantic

2017 ◽  
Author(s):  
Jonathan Lemay ◽  
Helmuth Thomas ◽  
Susanne E. Craig ◽  
William J. Burt ◽  
Katja Fennel ◽  
...  
Keyword(s):  
Partial Pressure ◽  
Carbon Cycling ◽  
Dissolved Inorganic Carbon ◽  
High Temporal Resolution ◽  
Co2 Uptake ◽  
Surface Mixed Layer ◽  
Scotian Shelf ◽  
Short Term ◽  
Partial Pressure Of Co2 ◽  
Short Term Variability

Abstract. The understanding of seasonal variability of carbon cycling on the Scotian Shelf, NW Atlantic Ocean, has improved in recent years, however, very little information is available regarding its short-term variability. In order to shed light on this aspect of carbon cycling on the Scotian Shelf we investigate the effects of Hurricane Arthur, which passed the region on July 5th 2014. The hurricane caused a substantial decline in the surface water partial pressure of CO2 (pCO2), even though the Scotian Shelf possesses CO2 rich deep waters. High temporal resolution data of moored autonomous instruments demonstrate that there is a distinct layer of relatively cold water with low dissolved inorganic carbon (DIC) slightly above the thermocline, presumably due to a sustained population of phytoplankton. Strong storm-related wind mixing caused this cold intermediate layer with high phytoplankton biomass to be entrained into the surface mixed layer. At the surface, phytoplankton begin to grow more rapidly due to increased light. The combination of growth and mixing of low DIC water led to a short-term reduction in partial pressure of CO2 until wind speeds relaxed and allowed for the restratification of the upper water column. These Hurricane-related processes caused a (net-) CO2 uptake by the Scotian Shelf region that is comparable to the spring bloom, thus exerting a major impact on the annual CO2 flux budget.

Inhibition of CO2 Assimilation by Supraoptimal CO2: Effect of Light and Temperature

1983 ◽  
Vol 10 (1) ◽  
pp. 75 ◽  
Author(s):  
KC Woo ◽  
SC Wong
Keyword(s):  
Partial Pressure ◽  
Co2 Concentration ◽  
Co2 Assimilation ◽  
Quantum Yields ◽  
Co2 Partial Pressure ◽  
Low Co2 ◽  
O2 Partial Pressure ◽  
Partial Pressures ◽  
High Partial Pressure ◽  
Partial Pressure Of Co2

In cotton the rate of CO2 assimilation, at O2 partial pressures up to 200 mbar, increased to a maximum and then declined as the intercellular partial pressure of CO2 was increased. The specific intercellular partial pressure of CO2 at which rate of assimilation began to decline depended on the environmental conditions. At 19 mbar partial pressure of O2 the decline occurred at CO2 partial pressure >390 �bar. At 200 mbar partial pressure of O2 it occurred at CO2 partial pressure > 534 �bar. O2 increased the CO2 partial pressure required for inhibition but it did not appear to affect the steepness of the decline of rate of assimilation with further increase in partial pressure of CO2 once the decline became apparent. The decline was more readily observed at low temperature and low O2 partial pressure, and in plants grown at low light and NO3- levels. It was also observed in cowpea and sunflower. Changes in quantum efficiency in cotton at high and low CO2 concentrations were observed. At ambient CO2 concentration (300 �bar), the quantum yields measured at 19 and 200 mbar partial pressure of O2 were 0.072 � 0.0003 and 0.053 � 0.0060 mol CO2 per mol absorbed quanta, respectively. In contrast, at 900 �bar CO2 partial pressure the respective values were 0.050 � 0.0023 and 0.070 � 0.0006 mol CO2 per mol absorbed quanta. The nature of the inhibition of CO2 assimilation by high partial pressure of CO2 is discussed.

Changes in longitudinal distribution of the partial pressure of CO2(pCO2) in the central and western equatorial Pacific, west of 160°W

1996 ◽  
Vol 23 (14) ◽  
pp. 1781-1784 ◽  
Author(s):  
Hisayuki Y. Inoue ◽  
Masao Ishii ◽  
Hidekadzu Matsueda ◽  
Michio Ahoyama ◽  
Ichio Asanuma
Keyword(s):  
Partial Pressure ◽  
Equatorial Pacific ◽  
Longitudinal Distribution ◽  
Partial Pressure Of Co2 ◽  
Western Equatorial Pacific

Physiological Determinants of Inspiratory Effort Sensation during CO2 Rebreathing in Normal Subjects

1993 ◽  
Vol 85 (5) ◽  
pp. 637-642 ◽  
Author(s):  
J. E. Clague ◽  
J. Carter ◽  
M. G. Pearson ◽  
P. M. A. Calverley
Keyword(s):  
Partial Pressure ◽  
Muscle Fatigue ◽  
Breathing Pattern ◽  
Normal Subjects ◽  
Inspiratory Effort ◽  
Inspiratory Muscle ◽  
Time Index ◽  
Partial Pressure Of Co2 ◽  
Tension Time ◽  
Inspiratory Muscle Fatigue

1. The physiological basis of inspiratory effort sensation remains uncertain. Previous studies have suggested that pleural pressure, rather than inspiratory muscle fatigue, is the principal determinant of inspiratory effort sensation. However, only a limited range of inspiratory flows and breathing patterns have been examined. We suspected that inspiratory effort sensation was related to the inspiratory muscle tension-time index developed whatever the breathing pattern or load, and that this might explain the additional rise in sensation seen with hypercapnia. 2. To investigate this we measured hypercapnic re-breathing responses in seven normal subjects (six males, age range 21–38 years) with and without an inspiratory resistive load of 10 cm H2O. Pleural and transdiaphragmatic pressures, mouth occlusion pressure and breathing pattern were measured. Diaphragmatic and ribcage tension-time indices were calculated from these data. Inspiratory effort sensation was recorded using a Borg scale at 30s intervals during each rebreathing run. 3. Breathing pattern and inspiratory pressure partitioning were unrelated to changes in inspiratory effort sensation during hypercapnia. Tension-time indices reached pre-fatiguing levels during both free breathing and inspiratory resistive loading. 4. Stepwise multiple regression analysis using pooled mechanical, chemical and breathing pattern variables showed that pleural pressure was more closely related to inspiratory effort sensation than was transdiaphragmatic pressure. When converted to tension-time indices, ribcage tension-time index was the major determinant of inspiratory effort sensation during loaded rebreathing, but partial pressure of CO2 was an important independent variable, whereas during unloaded rebreathing partial pressure of CO2 was the most important determinant of inspiratory effort sensation. 5. These results suggest that the pattern of inspiratory pressure partitioning and inspiratory flow rate have little influence on inspiratory effort sensation during CO2 stimulated breathing. The close association between inspiratory effort sensation and ribcage tension-time index, an index of inspiratory muscle work, suggests that inspiratory effort sensation may forewarn of potential inspiratory muscle fatigue. Changes in PaCO2 have a small independent effect on respiratory perception.

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