spectral area
Recently Published Documents


TOTAL DOCUMENTS

54
(FIVE YEARS 14)

H-INDEX

11
(FIVE YEARS 0)

Geophysics ◽  
2021 ◽  
pp. 1-85
Author(s):  
Wanli Cheng ◽  
Shoudong Wang ◽  
Chen Zhou ◽  
Liuqing Yang

The Q factor is an essential parameter describing the characteristics of medium absorption within a material during wave propagation. When a seismic wave propagates within the attenuating media, its amplitude decreases and frequency band narrows, resulting in a variation in its logarithmic spectral area. Based on these effects, we calculate the logarithmic spectral area difference (LSAD) before and after attenuation and set a division point to divide the LSAD into two parts. We then compute the difference between the two LSADs to derive a new Q-estimation formula based on computation of the logarithmic spectral area double difference (LSADD). To improve the noise robustness of the Q estimation, we select multiple different division points to calculate the Q factors and consider their average value as our final estimate. We then compare and analyze the noise robustness and bandwidth sensitivity of our technique with other commonly used methods. These results demonstrate that our approach is the most accurate and robust, and least sensitive to the frequency band when processing noisy synthetic seismograms. Finally, we apply our methodology to field vertical seismic profile (VSP) and seismic reflection data, further illustrating the effectiveness of this method to estimate the Q factor.


Circulation ◽  
2021 ◽  
Vol 144 (Suppl_2) ◽  
Author(s):  
Salvatore Aiello ◽  
Jenna Mendelson ◽  
Alvin Baetiong ◽  
Jeejabai Radhakrishnan ◽  
Raul J Gazmuri

Introduction: VF accounts for ~30% of all sudden cardiac arrest episodes. VF signal analysis in the frequency domain - calculating the amplitude spectral area (AMSA) - can inform on the probability that an electrical shock could terminate VF followed by return of spontaneous circulation (ROSC). BLS guidelines require delivery of shocks every 2 min and epinephrine every 4 min. Yet, shocks often do not terminate VF and may injure the myocardium. We have previously reported that guiding the timing of shock delivery based on AMSA reduces myocardial injury and improves outcome. Epinephrine is given to increase the coronary perfusion pressure (CPP) and therefore myocardial blood flow but has detrimental effects on post-resuscitation myocardial function and possibly on neurological outcome. Hypothesis: Monitoring AMSA during CPR could be used not only to guide shock delivery but also to avoid administering epinephrine when AMSA predicts a high probability of shock success, reserving epinephrine when AMSA predicts a low probability of shock success and additional CPP increase might be helpful. Methods: In a swine model of electrically induced VF and mechanical chest compressions, two resuscitation protocols were compared in 8 pigs each: (1) A guidelines-driven (GD), delivering shocks and epinephrine guided by the current BLS protocol and (2) An AMSA-driven, delivering shocks and epinephrine guided by AMSA (ADSE). VF was untreated for 10 min and pigs that achieved ROSC were monitored for 240 min. Results: Compared to GD, ADSE was associated with a shorter time to ROSC (400±80 vs 569±16 sec, p=0.034) and higher survival rate at 240 minutes with borderline statistical significance (7/8 vs 3/8, p=0.059). ADSE required fewer shocks (3±2 vs 5±2, p=0.026) and received fewer doses of epinephrine (median [interquartile range], 1[1-1] vs 2[1.3-3], p=0.038). Conclusions: Resuscitation with the ADSE protocol was superior to the GD protocol resulting in a shorter time to ROSC with improved survival requiring fewer shocks and fewer epinephrine doses. The ADSE protocol represents a more tailored approach to resuscitation enabling delivery of resuscitation interventions with higher precision and consequently minimizing their associated adverse effects.


Author(s):  
Salvatore R. Aiello ◽  
Jenna B. Mendelson ◽  
Alvin Baetiong ◽  
Jeejabai Radhakrishnan ◽  
Raúl J. Gazmuri

Background We previously reported that resuscitation delivering electrical shocks guided by real‐time ventricular fibrillation amplitude spectral area (AMSA) enabled return of spontaneous circulation (ROSC) with fewer shocks, resulting in less myocardial dysfunction. We now hypothesized that AMSA could also guide delivery of epinephrine, expecting further outcome improvement consequent to less electrical and adrenergic burdens. Methods and Results A swine model of ventricular fibrillation was used to compare after 10 minutes of untreated ventricular fibrillation a guidelines‐driven (n=8) resuscitation protocol, delivering shocks every 2 minutes and epinephrine every 4 minutes, with an AMSA‐driven shocks (n=8) protocol, delivering epinephrine every 4 minutes, and with an AMSA‐driven shocks and epinephrine (ADSE; n=8) protocol. For guidelines‐driven, AMSA‐driven shocks, and ADSE protocols, the time to ROSC (mean±SD) was 569±164, 410±111, and 400±80 seconds ( P =0.045); the number of shocks (mean±SD) was 5±2, 3±1, and 3±2 ( P =0.024) with ADSE fewer than guidelines‐driven ( P =0.03); and the doses of epinephrine (median [interquartile range]) were 2.0 (1.3–3.0), 1.0 (1.0–2.8), and 1.0 (0.3–3.0) ( P =0.419). The ROSC rate was similar, yet survival after ROSC favored AMSA‐driven protocols (guidelines‐driven, 3/6; AMSA‐driven shocks, 6/6; and ADSE, 7/7; P =0.019 by log‐rank test). Left ventricular function and survival after ROSC correlated inversely with electrical burden (ie, cumulative unsuccessful shocks, J/kg; P =0.020 and P =0.046) and adrenergic burden (ie, total epinephrine doses, mg/kg; P =0.042 and P =0.002). Conclusions Despite similar ROSC rates achieved with all 3 protocols, AMSA‐driven shocks and ADSE resulted in less postresuscitation myocardial dysfunction and better survival, attributed to attaining ROSC with less electrical and adrenergic myocardial burdens.


2021 ◽  
Vol 42 (Supplement_1) ◽  
Author(s):  
F R Gentile ◽  
S Compagnoni ◽  
E Baldi ◽  
E Aramendi ◽  
R Primi ◽  
...  

Abstract Background Ventricular fibrillation is the most common cause of out-of-hospital cardiac arrest (OHCA) and the use of antiarrhythmic drug therapy is usually recommended in addition to defibrillation. The role of the amplitude spectral area (AMSA) of ventricular fibrillation as a predictor of defibrillation efficacy has been established, while the existing data in favour of the use of amiodarone has been assessed with poor evidence and controversy. Purpose The aim of our study is to evaluate whether the administration of amiodarone during resuscitation could affect AMSA values. Materials All the OHCAs with a shockable presenting rhythm and attempted resuscitation which occurred from January 2015 to June 2019 in the province of Pavia were considered. Both the end-tidal CO2 (ETCO2) and AMSA values were calculated by retrospectively analyzing the data collected by the Corpuls 3 monitors/defibrillators (Corpuls, Kaufering, Germany) used in the territory and by considering a pre-shock interval of 2 seconds. Results Among a total of 3413 OHCAs, resuscitation was attempted in 2195 cases (64%), 377 (17%) had a shockable presenting rhythm and in 112 cases (3.4%) it was possible to obtain the values of ETCO2 and AMSA for a total of 391 shocks. Among these, 301 shocks (77%) were delivered to patients who received amiodarone during resuscitation. The success rate of each single shock was similar in the two groups but with an unfavorable trend for amiodarone (amiodarone 43.5% vs no amiodarone 54.4%, p=0.07). AMSA was significantly lower in patients treated with amiodarone (7.9 mV·Hz, IQR 5.4–12.2 vs 10.6 mV·Hz, IQR 7.1–14.1; p<0.001). According to a multivariate analysis, the administration of amiodarone and the time to shock were independent predictors of AMSA values. Lastly, on a sample of 124 shocks, homogeneous for age, sex, ETCO2, outcome of resuscitation and randomly matched, the AMSA of patients who received amiodarone was significantly lower (7.2 mV·Hz, IQR 7.2–11.7 vs 9.7 mV·Hz, IQR 6.7–12.5; p=0.02). Conclusions Our results indicate that amiodarone administration is associated with lower values of AMSA. Since higher AMSA values are known to be associated with a higher probability of shock rate success, this could help to better clarify the controversial role of amiodarone administration in patients with OHCA. FUNDunding Acknowledgement Type of funding sources: None.


2021 ◽  
Vol 0 (2) ◽  
pp. 38-51
Author(s):  
Evgeniy Butyrskiy ◽  
N.V. Mercachev ◽  
Vitaliy Rahuba

The article discusses the problem of synthesis of complex broadband signals in the spectral area. It is shown that the formation of complex broadband signals in the spectral area allows to determine the classes of signals that have good resolution in range and speed. Mathematical models of uncertainty functions for polyharmonic and strip signals are presented.


Author(s):  
Tia T. Raymond ◽  
Sandeep V. Pandit ◽  
Heather Griffis ◽  
Xuemei Zhang ◽  
Richard Hanna ◽  
...  

Background Amplitude spectral area (AMSA) predicts termination of fibrillation (TOF) with return of spontaneous circulation (ROSC) and survival in adults but has not been studied in pediatric cardiac arrest. We characterized AMSA during pediatric cardiac arrest from a Pediatric Resuscitation Quality Collaborative and hypothesized that AMSA would be associated with TOF and ROSC. Methods and Results Children aged <18 years with cardiac arrest and ventricular fibrillation were studied. AMSA was calculated for 2 seconds before shock and averaged for each subject (AMSA‐avg). TOF was defined as termination of ventricular fibrillation 10 seconds after defibrillation to any non‐ventricular fibrillation rhythm. ROSC was defined as >20 minutes without chest compressions. Univariate and multivariable logistic regression analyses controlling for weight, current, and illness category were performed. Primary end points were TOF and ROSC. Secondary end points were 24‐hour survival and survival to discharge. Between 2015 and 2019, 50 children from 14 hospitals with 111 shocks were identified. In univariate analyses AMSA was not associated with TOF and AMS‐Aavg was not associated with ROSC. Multivariable logistic regression showed no association between AMSA and TOF but controlling for defibrillation average current and illness category, there was a trend to significant association between AMSA‐avg and ROSC (odds ratio, 1.10 [1.00‒1.22] P =0.058). There was no significant association between AMSA‐avg and 24‐hour survival or survival to hospital discharge. Conclusions In pediatric patients, AMSA was not associated with TOF, whereas AMSA‐avg had a trend to significance for association in ROSC, but not 24‐hour survival or survival to hospital discharge. Registration URL: https://www.clinicaltrials.gov ; Unique identifier: NCT02708134.


Circulation ◽  
2020 ◽  
Vol 142 (Suppl_4) ◽  
Author(s):  
Tia Raymond ◽  
Sandeep Pandit ◽  
Heather M Griffis ◽  
Xuemei Zhang ◽  
Richard Hanna ◽  
...  

Introduction: Amplitude spectral area (AMSA) predicts termination of fibrillation (TOF) with return of spontaneous circulation (ROSC) and hospital survival in adults, but has not been studied during pediatric cardiac arrest (pCA). Hypothesis: We characterized AMSA during pCA from a pediatric resuscitation quality (pediRES-Q) collaborative and hypothesized that AMSA would be associated with TOF and ROSC. Methods: Children <18 years of age with pCA and VF were studied. AMSA was measured for 2 seconds prior to each shock and also averaged for each subject (AMSA-avg). TOF was defined as termination of VF 10 secs after defibrillation (DF) to any rhythm other than VF. ROSC was defined as >20 mins without chest compressions. Univariate and multivariable logistic regression analyses controlling for weight, current, and illness category (cardiac vs non-cardiac) were performed. Primary endpoints were TOF and ROSC without ECMO. Secondary endpoints were 24-hr survival and survival to hospital discharge. Results: Between 2015-2019, 50 children from 14 hospitals (median age 3.7 years [IQR 0.6, 13.1]; median weight 16.3 kgs [IQR 6.9, 37.2]; 46% male; 73% cardiac illness category) were identified. IHCA occurred in 47 children and OHCA in 3 children. We analyzed 111 shocks with median number of DFs 1.0 [IQR 1.0, 3.0], median DF energy dose 3.27 J/kg [IQR 2.65,5.01], median DF current 0.64 A/kg [IQR 0.38,0.96], median AMSA 12.21 [IQR 7.17,17.03], and median AMSA-avg 14.6 [IQR 8.6,19.2]. TOF was achieved in 72 DFs (65%), ROSC without ECMO in 31 (62%), ROC with ECMO in 11 (22%), 24-hr survival in 40 (80%), and survival to hospital discharge in 26 (52%). Weight (OR 0.91 [0.84, 0.99] P=0.025) and DF current (OR 1.44 [0.97, 2.2] P=0.07), but not AMSA, were significantly associated with TOF for the first shock. Controlling for DF current and illness category, there was a significant association between AMSA-avg (OR 1.11 [1.0, 1.24] P=0.044) and ROSC without ECMO. There was no significant association between AMSA-avg and 24-hr survival or survival to hospital discharge. Conclusions: In pediatric patients, TOF was associated with weight and DF current, but not AMSA, whereas AMSA-avg was associated with ROSC without ECMO, but not 24-hr survival or survival to hospital discharge.


2020 ◽  
Vol 44 (5) ◽  
pp. 365-373
Author(s):  
Fei Zhang ◽  
Kui Wang ◽  
Yaru Dang ◽  
Guoyin Wu

The macro mechanical properties of soil-rock mixture are closely related to the meso-structure features of block stones, namely, content, size, and shape. To promote the engineering application of soil-rock mixture, it is important to explore the meso-structure of the mixture, and evaluate its constitutive properties. The previous studies have shown that the wave propagation in the mixture is highly sensitive to the rock content and compaction. To clarify the meso-structure features of soil-rock mixture, this paper establishes a discrete element model of the mixture based on Particle Flow Code (PFC), investigates the wave propagation features in the model with different meso-structure parameters, and analyzes how the meso-structure parameters affect the wave propagation. The results show that: With the growing rock content, the first wave amplitude increased, while the take-off time shortened; With the growing feature size of block stone, the first wave amplitude gradually decreased, while the take-off time gradually lengthened; The soil-rock mixture containing spherical block stones had the highest first wave amplitude and shortest take-off time, while the mixture containing rectangular block stones had the lowest first wave amplitude and longest take-off time. With the growing rock content, the maximum amplitude, dominant frequency, and spectral area all exhibited an increasing trend; With the growing feature size of block stone, the maximum amplitude, dominant frequency, and spectral area all exhibited a decreasing trend.


2020 ◽  
Vol 12 (1) ◽  
pp. 919-927
Author(s):  
Kangsheng Xu ◽  
Ying Li

AbstractAn Ms7.0 earthquake occurred in Jiuzhaigou, Sichuan Province, China, on August 8, 2017. In this study, we used the vertical component data from 31 seismic stations near the epicenter from May 1 to August 20, 2017, to calculate the amplitude spectrum hourly using the fast Fourier transform method. Furthermore, the spectral area of the low frequency band (0.02–1 Hz), which represents the energy of low frequency motion, was calculated. In this way, the temporal and spatial variations in the vertical ground motion in this region were determined. Four high-value processes occurred in mid-June, mid-July, late July, and early August (the last three are discussed in this article). Based on a comparison with the local meteorological data, the meteorological factors had no influence, local geological factors did not affect the results, and typhoon factors did not show obvious correlation. Combined with the results of previous studies, we believe that the increase in the spectral area reflects the intense movement of deep material in the region related to the Jiuzhaigou earthquake. The spatial distribution of the spectral area (energy) reveals that the deep material moved eastward rapidly, was obstructed by the Sichuan Basin, and expanded to the northwest in a U-shaped channel, which may be the main dynamic factor for the formation or triggering of the earthquake.


Sign in / Sign up

Export Citation Format

Share Document