• Title/Summary/Keyword: 산소호흡률

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Current Use of Dexamethasone Rescue Therapy for Bronchopulmonary Dysplasia (기관지폐 이형성증에 대한 덱사메타손 구제 치료)

  • Jung, Eui-Seok;Ahn, Yo-Han;Lee, Ju-Young;Kim, Yoon-Joo;Son, Se-Hyung;Sohn, Jin-A;Lee, Eun-Hee;Choi, Eun-Jin;Kim, Eun-Sun;Lee, Hyun-Ju;Lee, Jin-A;Choi, Chang-Won;Kim, Ee-Kyung;Kim, Han-Suk;Kim, Beyong-Il;Choi, Jung-Hwan
    • Neonatal Medicine
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    • v.16 no.2
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    • pp.146-153
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    • 2009
  • Purpose: The aim of this study is to investigate the current use of dexamethasone rescue therapy (DRT) for bronchopulmonary dysplasia (BPD). Methods: This is a retrospective study of 251 BPD patients managed in the neonatal intensive care units at Seoul National University Childrens Hospital and Seoul National University Bundang Hospital between March 2004 and August 2008. The demographic data and clinical characteristics of the mothers and infants were analyzed. The infants were compared based on DRT responsiveness. The DRT complications were investigated. Results: Ninety-three patients (37.1%) were classified with severe BPD, DRT was only given to patients with severe BPD. Dexamethasone was administered to 24 patients (9.6%) whose respiratory status had precluded extubation, which indicated that conventional BPD management had failed. Fourteen patients (58.3%) who received DRT were responsive. DRT non-responders required more oxygenation and more complicated with pulmonary arterial hypertension (PAH). Responder had shorter length's of hospitalization and lower mortality rates. High dose dexamethasone was no more effective in weaning neonates from the ventilatior than low dose dexamethasone. Sepsis was the most common complication of DRT. Conclusion: DRT is a valuable treatment for severe BPD ahead of PAH development. DRT should not be performed in BPD patients with PAH due to the possibility of complications.

Determination of Total CO2 and Total Alkalinity of Seawater Based on Thermodynamic Carbonate Chemistry (해수중의 총이산화탄소와 총알칼리도 분석을 위한 탄산염 화학 이론 및 측정방법)

  • Mo, Ahra;Son, Juwon;Park, Yongchul
    • Journal of the Korean Society for Marine Environment & Energy
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    • v.18 no.1
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    • pp.1-8
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    • 2015
  • To evaluate accuracy and precision of determination of total alkalinity ($Alk_T$) and carbon dioxide ($TCO_2$) derived from present study, experiment was applied with $CO_2$ CRM (Batch 132, Scripps Institution of Oceanography; $Alk_T=2229.24{\pm}0.39{\mu}mol/kg$, $TCO_2=2032.65{\pm}0.45{\mu}mol/kg$). As the result, average concentration of $Alk_T$ and $TCO_2$ was $2354.09{\mu}mol/kg$ (~5.6% difference with $CO_2$ CRM) and $2089.60{\mu}mol/kg$ (~2.3% difference with $CO_2$ CRM), respectively. For previous method (Gran Titration) by addition $NaHCO_3$ to deionized water($Alk_T$ $2023.33{\mu}mol/kg$), average concentration was $2193.39{\mu}mol/kg$ (sd=57.15, n=7). Whereas, average concentration was $2017.02{\mu}mol/kg$ (sd=10.98, n=7) for the present study. Recovery yield experiments of total alkalinity in deionized water and seawater were implemented by addition of $NaHCO_3$. The recovery yield of deionized water in the range 0 to $4952.39{\mu}mol/kg$ was 100.8% ($R^2$=0.999), and seawater in the range 0 to $2041.32{\mu}mol/kg$ was 102.3% ($R^2$=0.999). Comparison of $pCO_2$ sensor (PSI $CO_2-Pro^{TM}$) with present method showed very meaningful correlation coefficient ($R^2$=0.977) in the range of 427 to $705{\mu}atm$ and 9.16 to $15.24{\mu}mol/kg$ throught elapsed time for two weeks. Field experiment of diurnal variation of total carbon dioxide was accomplished at Sachon harbor in the coastal waters of East Sea of Korea. Concentration of $Alk_T$ and $TCO_2$ was increased during night, and decreased during daylight hours. The results showed mirror type between $TCO_2$ and dissolved oxygen, which was attributable to photosynthesis and respiration of phytoplankton. Also, open ocean field study was performed to obtain vertical profile of $Alk_T$ and $TCO_2$ in C-C zone (Clarion-Clipperton Fracture Zone), Northeastern Pacific. Average concentrations of $Alk_T$ in the surface mixed layer (0~60 m) and deeper layer below 200 m were $2422.38{\mu}mol/kg$ (sd=78.73, n=20) and $2465.87{\mu}mol/kg$ (sd=57.68, n=103), respectively. And average concentrations of $TCO_2$ were $2134.47{\mu}mol/kg$ (sd=65.4, n=20) and $2431.87{\mu}mol/kg$ (sd=65.02, n=103) in the same depth ranges such as $Alk_T$. Vertical distributions of $Alk_T$ and $TCO_2$ concentrations tended to increase with depth, and analyzed concentrations showed slightly higher than those of previous studies in this area.