• Journal of Chest Surgery
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• 제34권10호
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• pp.733-744
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• 2001

배경: 대동맥 축착증과 심실중격결손이 동반된 환아의 적절한 치료 방침에 대해서는 이견이 많다. 본 연구는 생후 6개월 이하의 환아에서 대동맥 축착증과 심실중격결손의 일타 완전교정 결과 및 수술방법에 따른 대동맥 축착증의 재발에 대해 알아보고자 하였다. 대상 및 방법: 1995년 1월부터 2000년 12월가지 본원에서 대동맥 축착증과 심실중격결손으로 일차 완전교정을 시행받은 생후 6개월 이하의 환아 33명을 대상으로 후향적으로 조사하였다. 환아의 평균 연령과 체중은 각각 54$\pm$37일(12일~171일)과 3.9$\pm$1.1kg(1.5~6kg)이었다. 대동맥 축착 고정은 연구 초기에는 저체온하 완전순환정지하에서 시행하였으며 최근에는 순환정지없이 무명동맥을 통한 국소 뇌관류 상태에서 시행하였다. 축착증 교정 방법은 초기에는 Extended cad-to-end anastomosis(EEEA;n=16)와 Extended side-to-side anastomosis(ESSA;n=2)를, 최근에는 Extended end-to-sidc anasto mosis(EESA;n=15)를 이용하였다 심실중격결손은 초기 16명에서는 Dacron을, 최근 17명에서는 자가 심낭편을 이용하여 폐쇄하였다. 대동맥궁 발육부전은 29명(88%)에서 있었으며 원위부 발육부전 18명, 완전형 5명, 그리고 복잡형은 6명이었다.

• Bulletin of the Korean Chemical Society
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• 제23권5호
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• pp.688-692
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• 2002

The aminomethylation of phenols with para-substituents by the Mannich reaction has successfully been accomplished to produce the Mannich bases 2-6. The compounds 7-8 have also been synthesized in order to identify the effect of the side arms and t he macrocycle in the complex formation. Protonation constants and stability constants of the double armed diaza-18-crown-6 ethers 2-7 with metal ions have been determined by potentiometric method at 25 $^{\circ}C$ in 95 % methanol solution. Under a basic condition (pH > 8.0), the double-armed crown ethers 2-6 revealed stronger interaction with divalent metal ions than the simple diazacrown ether 1. The stability constants with these metal ions were Co 2+ < Ni2+ < Cu2+ > Zn 2+ in increasing order, which are in accordance with the order of the Williams-Irving series. The stability constants with alkali earth metal ions were Ca 2+ < Sr 2+ < Ba 2+ in increasing order, which may be explained by the concept of size effect. It is noteworthy that the hosts 2-6, which have phenolic side arms and a macrocycle, bind stronger with metal ions than the hosts 1 and 7. On the other hand, the host 8, which has phenolic side arms with a pyperazine ring,provided comparable stability constants to those with the host 3. These facts demonstrate that phenolic side arms play a more important role than the azacrown ether ring in the process of making a complex with metal ions especially in a basic condition. In particular, the log KML values for complexation of divalent metal ions with the hosts 2-6 had the sequence, i.e., 2 (R=OCH3) < 3 (R=CH3) < 4 (R=H) < 5 (R=Cl) < 6 (R=CF3). The stability constants of the hosts 5 and 6 containing an electron-withdrawing group are larger than those of the hosts 2 and 3 containing an electron-donating group. This substituent effect is attributed to the solvent effect in which the aryl oxide with an electron-donating group has a tendency to be tied strongly with protic solvents.

• 한국물환경학회지
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• 제38권2호
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• pp.82-94
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• 2022

In this study, chemically modified biochar (NSBP500, KSBP500, OSBP500) derived from starfish was utilized to improve the adsorption ability of the SBP500 (Starfish Biochar Pyrolyzed at 500℃) in a solution contaminated with heavy metals. According to the biochar modification performance evaluation batch tests, the removal rate and adsorption amount of NSBP500 increased 1.4 times for Cu, 1.5 times for Cd, and 1.2 times for Zn as compared to the control sample SBP500. In addition, the removal rate and adsorption amount of KSBP500 increased 2 times for Cu, 1.8 times for Cd, and 1.2 times for Zn. The removal rate and adsorption amount of OSBP500 increased 5.8 times for Cu. The FT-IR analysis confirmed the changes in the generation and movement of new functional groups after adsorption. SEM analysis confirmed Cu in KSBP500 was in the form of Cu(OH)₂ and resembled the structure of nanowires. The Cd in KSBP500 was densely covered in cubic form of Cd(OH)₂. Lead(Pb) was in the form of Pb₃(OH)₂(CO₃)₂ in a hexagonal atomic layer structure in NSBP500. In addition, it was observed that Zn was randomly covered with Zn₅(CO₃)₂(OH)₆ pieces which resembled plates in KSBP500. Therefore, this study confirmed that biochar removal efficiency was improved through a chemical modification treatment. Accordingly, adsorption and precipitation were found to be the complex mechanisms behind the improved removal efficiency in the biochar. This was accomplished by electrostatic interactions between the biochar and heavy metals and ion exchange with Ca²⁺.

• 자원환경지질
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• 제42권4호
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• pp.315-333
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• 2009

이 연구에서는 대전지역 주요 도심하천인 갑천, 유등천, 대전천을 대상으로 하천수의 수리화학적 특성과 산소, 수소, 황, 탄소 동위원소 특성을 분석하였다. 하천수 시료는 풍수기와 갈수기 2차례 채취되었다. 하천의 수리화학적 특성은 상류에서는 Ca(Mg)-$HCO_3$ 유형을 보이다가 도심권을 통과하면서 Ca(Mg)-$SO_4(Cl)$유형으로 전이되고 하류에서는 Na(Ca)-$HCO_3$(Cl, $SO_4$) 유형으로 변하였다. 이와 같은 화학적 유형의 변화는 자연적 영향뿐만 아니라 하수처리장의 방류수와 인위적 오염물질의 유입에 의한 영향이 관여된 것으로 해석된다. 전반적으로 풍수기에 비해 갈수기에 하천수의 전기전도도 값이 높은 특성을 보여준다. 갑천하류는 하수종말처리장의 방류수가 합류되면서 수질이 급격하게 변화한다. 하천수의 pH는 상류에서 중성을 보이다가 도심권을 지나면서 최고 pH 9.8의 고알카리성을 보인다. 이는 현장조사결과 아파트의 우수관을 통한 세제 유입에 기인하는 것으로 보인다. 하천수의 산소-수소 동위원소 관계식은 ${\delta}D=6.45{\delta}^{18}O-7.4$으로 Craig의 순환수선보다 다소 하향 이동되어 도시된다. 이는 기단의 변화와 하천수의 표면 증발 효과에 의한 것으로 보인다. 뿐만 아니라, 상-하류사이에 고도효과를 반영하는 동위원소 조성 값의 차이를 보여준다. 하천수의 ${\delta}^{13}C$ 값은 $-19.5{\sim}-7.8%o$ 범위로 대기중 이산화탄소와 유기물 기원의 범위에 해당된다. 전반적으로 하천수의 상류에서 하류로 향할수록 ${\delta}^{13}C$값이 높아지므로 $CO_2$의 기원이 상류에서는 주로 유기물기원에서 도심권에서는 오염된 대기와 지하수의 기저유출로 인한 무기기원의 비율이 높아지기 때문으로 해석된다. ${\delta}^{34}S-SO_4$함량 관계도에서 하천수를 4개 그룹(갑천중 상류, 유등천, 대전천, 갑천하류)으로 구분하였다. 황산염의 농도는 갑천중상류<유등천<대전천<갑천하류의 순서로 높아지는 반면 ${\delta}^{34}S$값은 감소하는 경향을 보인다. 이는 하천별 황산염의 증가에 따른 공급원이 다르다는 것을 의미한다. 하천수내 황의 기원은 대기기원을 중심으로 황산염의 농도가 높아질수록 황철석의 영향이 큰 것으로 해석된다. 그러나 하천수에 유입되는 생활하수 등에 대한 황동위원소 자료가 없으므로 이에 대한 영향에 대해서는 향후 연구되어야할 과제이다.

• 자원환경지질
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• 제31권1호
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• pp.11-20
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• 1998

카올리나이트에 의한 세슘-137 및 스트론튬-90 흡착에 대한 지하수의 주요 양이온 ($Ca^{2+}$, $Mg^{2+}$, $K^+$, $Na^+$ 및 음이온 ($SO_4{^{2-}}$, $HCO_3{^-}$)의 영향을 그리고 pH의 영향을 뱃치실험을 통하여 알아보았다. 세슘 및 스트론튬 흡착에 대한 지하수 양이온들의 농도, 전하, 이온반경사이의 상대적인 영향을 알아보기 위하여 통계적 방법으로 디자인된 3차원적인 Kd 모델링 방법이 시도되었다. 모델링결과 흡착에 미치는 정도는 양이온의 수화반경이 가장 큰 영향을 미치며, 그다음 이온들의 전하, 농도의 순서임이 밝혀졌다. pH변화에 따른 카올리나이트의 제타전위를 측정하고 amphoteric 반응측면에서 Cs, Sr 흡착 특성을 설명하였다. 카올리나이트의 Cs 및 Sr 흡착에 대한 경쟁양이온들의 이온강도가 pH 보다는 더 큰 영향을 미친다. 탄산수소이온의 농도는 스트론튬의 흡착거동에 상당한 영향을 미친다. 이는 탄산수소이온 ($HCO_3{^-}$)의 농도변화에 다른 pH의 변화에 기인하는 것 뿐만아니라, WATWQ4F 프로그램을 이용한 열역학적 계산에 의하면 Strontianite ($SrCO_3$)의 침전에 의한 것으로 해석된다.

• 자원환경지질
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• 제32권6호
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• pp.611-631
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• 1999

Enviromental geochemisty and heary metal contamination at the Kongjueil mine creek were underaken on the basis of physicohemical properties and mineralogy for various kinds of water (surface, mine and ground water),soil, precipitate and sediment collected of April and December in 1998. Hydrgeochemical composition of the water samples are characterized by relatively significant enricant of Ca+Na, alkiali ions $NO_3$ and Cl inground and surfore water, wheras the mine waters are relatively eneripheral water of the mining creek have the characteristics of the (Ca+Mg)-$(HCO_3+SO_4)$type. The pH of the mine water is high acidity (3.24)and high EC (613$\mu$S/cm)compared with those of surface and ground water. The range of $\delta$D and $\delta^{18}O$ values (relative to SMOW) in the waters are shpwn in -50.2 to -61.6% and -7.0 to -8.6$\textperthousand$(d value=5.8 to 8.7). Using computer program, saturation index of albite, calcite, dolomite in mine water are nearly saturated. The gibbiste, kaolinite and smectite are superaturated in the surface and ground water, respectively. Calculated water-mineral reaction and stabilities suggest that weathing of silicate minerals may be stable kaolinite owing to the continuous water-rock reaction. Geochemical modeling showed that mostly toxic heavy metals may exist larfely in the from of metal-sulfate $(MSO_4\;^2)$and free metal $(M^{2+})$ in nmine water. These metals in the ground and surface water could be formed of $CO_3$ and OH complex ions. The average enrichment indices of water samples are 2.72 of the groundwater, 2.26 of the surface water and 14.15 of the acid mine water, normalizing by surface water composition at the non-mining creek, repectively. Characteristics of some major, minor and rate earth elements (Al/Na, K/Na, V/Ni, Cr/V, Ni/Co, La/Ce, Th/Yb, $La_N/Yb_N$, Co/Th, La/Sc and Sc/Th) in soil and sediment are revealed a narrow range and homogeneous compositions may be explained by acidic to intermediate igneous rocks. And these suggested that sediment source of host granitic gneiss colud be due to rocks of high grade metamorphism originated by sedimentary rocks. Maximum concentrations of environmentally toxic elements in sediment and soil are Fe=53.80 wt.% As=660, Cd=4, Cr=175, Cu=158, Mn=1010, Pb=2933, Sb=4 and Zn=3740 ppm, and extremely high concentrations are found are found in the subsurface soil near the ore dump and precipitates. Normalizing by composition of host granitic gneiss, the average enerichment indices are 3.72 of the sediments, 3.48 of the soils, 10.40 of the precipitates of acid mine drainage and 6.25 of the soils near the main adit. The level of enerichment was very severe in mining drainage sediments, while it was not so great in the soils. mineral composition of soil and sediment near the mining area were partly variable being composed of quartz, mica, feldspar, chlorite, vermiculite, bethierin and clay minerals. reddish variable being composed of quartz, mica, feldspar, chlorite, vermiculite, bethierin and clay minerals. Reddish brown precipitation mineral in the acid mine drainage identifies by schwertmanite. From the separated mineralgy, soil and sediment are composed of some pyrite, arsenopyite, chalcopyrite, sphalerite, galena, malachite, goethite and various kinds of hydroxied minerals.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2004년도 임시총회 및 추계학술발표회
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• pp.119-120
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• 2004

Urban groundwater has a unique hydrologic system because of the complex surface and subsurface infrastructures such as deep foundation of many high buildings, subway systems, and sewers and public water supply systems. It generally has been considered that increased surface impermeability reduces the amount of groundwater recharge. On the other hand, leaks from sewers and public water supply systems may generate the large amounts of recharges. All of these urban facilities also may change the groundwater quality by the recharge of a myriad of contaminants. This study was performed to determine the factors controlling the recharge of deep groundwater in an urban area, based on the hydrogeochemical characteristics. The term ‘contamination’ in this study means any kind of inflow of shallow groundwater regardless of clean or contaminated. For this study, urban groundwater samples were collected from a total of 310 preexisting wells with the depth over 100 m. Random sampling method was used to select the wells for this study. Major cations together with Si, Al, Fe, Pb, Hg and Mn were analyzed by ICP-AES, and Cl, N $O_3$, N $H_4$, F, Br, S $O_4$and P $O_4$ were analyzed by IC. There are two groups of groundwater, based on hydrochemical characteristics. The first group is distributed broadly from Ca-HC $O_3$ type to Ca-C1+N $O_3$ type; the other group is the Na+K-HC $O_3$ type. The latter group is considered to represent the baseline quality of deep groundwater in the study area. Using the major ions data for the Na+K-HC $O_3$ type water, we evaluated the extent of groundwater contamination, assuming that if subtract the baseline composition from acquired data for a specific water, the remaining concentrations may indicate the degree of contamination. The remainder of each solute for each sample was simply averaged. The results showed that both Ca and HC $O_3$ represent the typical solutes which are quite enriched in urban groundwater. In particular, the P$CO_2$ values calculated using PHREEQC (version 2.8) showed a correlation with the concentrations of maior inorganic components (Na, Mg, Ca, N $O_3$, S $O_4$, etc.). The p$CO_2$ values for the first group waters widely ranged between about 10$^{-3.0}$ atm to 10$^{-1.0}$ atm and differed from those of the background water samples belonging to the Na+K-HC $O_3$ type (<10$^{-3.5}$ atm). Considering that the p$CO_2$ of soil water (near 10$^{-1.5}$ atm), this indicates that inflow of shallow water is very significant in deep groundwaters in the study area. Furthermore, the P$CO_2$ values can be used as an effective parameter to estimate the relative recharge of shallow water and thus the contamination susceptibility. The results of our present study suggest that down to considerable depth, urban groundwater in crystalline aquifer may be considerably affected by the recharge of shallow water (and pollutants) from an adjacent area. We also suggest that for such evaluation, careful examination of systematically collected hydrochemical data is requisite as an effective tool, in addition to hydrologic and hydrogeologic interpretation.ion.ion.

• 한국축산식품학회지
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• 제38권5호
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• pp.1080-1091
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• 2018

The eggshell, which is a complex and highly ordered structure, is very important factor for food safety and egg marketing. This study investigated the changes in eggshell structure and shell components in relationship to hen age. For this study, we examined the histological change of the endometrium of the 30-, 60-, and 72-wk-old commercial layers, and analyzed the ultrastructure and ionic composition of their eggshells. The results showed that histological deformation, fibrosis, atrophy and elimination of micro-villi in the uterus endometrium were found through microscopic observation that was associated with increasing hen age. Concentration of blood-ion components such as $Ca^{2+}$, $Na^+$, $K^+$, and $Cl^-$ ions did not change with age. Along with the results from the ultrastructure analysis of the eggshell, the palisade layer ratio and the density of mammillary knobs were significantly decreased in older hens. In addition, the type B mammillary knobs were frequently observed with increasing hen age. In the mineral element assay from the eggshell, $Ca^{2+}$, $S^{2-}$, and $Co^{2+}$ significantly decreased with increasing hen age, whereas $Na^+$, $K^+$, and $V^{2+}$ significantly increased. Therefore, the damages of endometrial tissue inhibit the processes of ion transmission and the crystallization of eggshell formation, resulting in a large and non-uniform mammillary knob formation. This means the conditions of endometrial cells affect the formation of the eggshell structure. In conclusion, hen aging causes the weakness of the eggshell and degrades the eggshell quality.

• 대한화학회지
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• 제31권1호
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• pp.45-54
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• 1987

Calcon carboxylic acid[2-hydroxy-1-(2-hydroxy-4-sulfo-1-naphthylazo)-3-naphthoic acid;CCA)]를 이온교환시킨 Dowex 1-X8수지(CCA-Dowex 1-X8)와 2-methyl-8-hydroxyquinoline(MHQ)을 침윤시킨 Amberlite XAD-4 수지(MHQ-XAD-4)를 여러가지 매질중에 있는 철(Ⅲ)이온의 분리-농축에 사용하였다. 이들 수지의 안정성을 검토하고 철(Ⅲ)이온에 대한 흡착능을 측정하였다. 매트릭수의 주성분인 Al(Ⅲ), Ca(Ⅱ), 및 Fe(Ⅲ)들의 수지에 대한 흡착성을 pH를 변화시키며 조사하여 최적 pH범위를 결정하였다. 용리법으로 알루미늄호일과 초정약수중 미량의 철분을 매트릭스 이온으로부터 분리-농축하였다. 농축된 Fe(Ⅲ)는 소량의 강산으로 용리시켜 불꽃 원자흡광광도법으로 정량하였다. 초정약수중의 Fe(Ⅱ)와 Fe(Ⅲ) 이온들은 SP-Sephadex C-25컬럼으로 농축하고, ferrozine용액과 1% ascorbic acid-ferrozine용액으로 단계적 용리법에 의해 용리시킴으로써 각각을 분리할 수 있었다. 분리된 각 이온들은 Fe(Ⅲ)-ferrozine착물의 분석 파장인 562nm에서 분광 광도법으로 정량하였다.

• 한국수산과학회지
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• 제23권5호
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• pp.361-372
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• 1990

Processing conditions of whole sardine into modified fish sauce were investigated. Thawed and chopped sardine was homogenized and hydrolyzed using commercial proteolytic enzymes such as complex enzyme-2000($2.18{\cdot}10^4U/g solid$) and alcalase($1.94{\cdot}10^4\;U/g solid$) in a cylindrical vessel with 4 baffles and 6-bladed impeller. Optimal pH, enzyme concentration and temperature for the hydrolysis with complex enzyme-2000 were 7.0, $7\%$ (W/W) and $52^{\circ}C$, and-those with alcalase were 8.0, $6\%$ (W/W) and $60^{\circ}C$. In both cases, the reasonable amount of water for homogenization, agitation speed and hydrolyzing time were $100\%$ (W/W), 100 rpm and 210 minutes. Thermal treatment of the filtered hydrolysate at $90^{\circ}C$ for 2 hours with $6\%$ of invert sugar was adequated to inactivation of the enzymes and pasteurization of the hydrolysate. Flavor, taste and color of the hydrolysate were improved during the heating process in which the browning products might participate. The content of free amino nitrogen in the fish sauce seasoned with $15\%$ of table salt was ca. $1,640 mg\%$. Yield of the fish sauce based on the contents of proteinous and free amino nitrogen in the raw whole sardine was ca. $86\%$, and ca. $96\%$ of these compounds of the fish sauce was in the form of free amino nitrogen. The pH, salinity and histamine content of the fish sauce were $6.1\~6.3,\;14.2\~14.3\%$ and less than $10\;mg\%$.