• Journal of Oral Medicine and Pain
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• v.26 no.1
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• pp.11-16
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• 2001

타액은 그 양과 조성 등에 있어 많은 인자들의 영향을 받는다. 타액분비 감소는 구강의 자정작용, 완충능, 치아우식저항성 등 타액의 고유한 기능을 변화시켜서 구강건조감, 구강작열감, 다발성 치아우식증 등의 소인이 된다. 이에 저자는 심리적 요인이 구강내 환경에 미치는 영향을 평가하고자 타액선질환을 포함한 전신질환이 없는 전북대학교 치과대학생 20명을 대상으로 일상생활시와 시험 직전의 비자극성 전타액을 5분간 추출하여, 그 유출량과 수소이온농도를 측정, 비교, 평가하였다. 타액유출량은 $25m{\ell}$의 메스실린더를 사용하였고, 수소이온농도는 pH/SEmeter(ORION, 720A model)를 이용하여 측정하였다. 평가 결과 남성의 비자극성 타액유출량과 수소이온농도는 $3.68{\pm}1.31m{\ell}/5min$와 $7.63{\pm}0.17$이었고, 여성에서는 각각 $4.93{\pm}1.47m{\ell}/5min$와 $7.43{\pm}0.29$로서 성별간 유의한 차이가 없었다. 그리고 일상생활시의 성인의 5분간 수집된 비자극성 타액유출량은 $4.18{\pm}1.48m{\ell}/5min$였고, 스트레스하에서의 양은 $2.20{\pm}0.95m{\ell}/5min$로 나타나 스트레스시 타액유출량이 감소하는 것으로 나타났다(p<0.01). 또한 일상생활시의 성인의 비자극성 타액의 수소이온농도는 $7.55{\pm}0.24$였고, 스트레스하에서의 수소이온농도는 $7.22{\pm}0.20$으로 나타나 스트레스시 수소이온농도가 감소하는 것으로 나타났다(p<0.01). 이상의 결과로 보아 스트레스는 타액유출량을 감소시키고 구강내를 보다 산성화시킨다고 사료된다.

• Korean Journal of Environment and Ecology
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• v.29 no.6
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• pp.917-922
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• 2015

This study was carried out to investigate solutes concentration change with respect to discharge change in coniferous forest experiment watershed in Gyeonggi-do, Korea. From 2005 to 2008. Precipitation, discharge, solutes has been analyzed from 23 precipitation events. The results showed that low API induced low discharge. $NH_4{^+}$, $K^+$, and $Ca^{2+}$ were indicated by clockwise and $Cl^-$ and $NO_3{^-}$ were represented by counterclockwise hysteresis loop. ${SO_4}^{2-}$, $Na^+$, $Mg^{2+}$ showed no hysteresis loop pattern. $Cl^-$, $Na^+$, $NH_4{^+}$ was relatively constant due to groundwater during precipitation, $NO_3{^-}$ was increased due to soil water compared to early precipitation. $Cl^-$, ${SO_4}^{2-}$, $Na^+$, $Mg^{2+}$, $Ca^{2+}$ was diluted with respect to increased discharge and $NO_3{^-}$ was diluted in early precipitation and then increased in the end. $NO_3{^-}$ and $Ca^{2+}$ eluviated in early precipitation. This characteristics was presumed by the effect of API, discharge and ground water.

• Proceedings of the KAIS Fall Conference
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• 2002.05a
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• pp.140-143
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• 2002

연속 이온교환 평형 모델을 개발하여 원자력발전소 탈염기의 성능을 평가한 결과 특정이온의 누출 현상과 유입수 및 유출수중 이온농도 비율이 운전조건에 따라서 달라짐을 확인하였다. 본 모델은 국부 불완전 평형을 고려할 수 없으나 다성분 존재하의 경쟁적 이온교환을 묘사할 수 있는 장점을 가지고 있다.

• Journal of Korean Society of Forest Science
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• v.89 no.3
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• pp.342-355
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• 2000

This study was carried out to reveal the influence of discharge change on matters and stream water quality between pH, EC and dissolved matters obtained by observation of long-term and short-term on stream water quality and separated runoff components from stream water by using HYCYMODEL. From January in 1998 to September in 1999, it was estimated by relationships of character of water quality and discharge for the experimental watershed in Mt. Palgong. The results were summarized as follows : 1. Annual average pH values of stream water in 1998 and in 1999 were 6.48(6.22~6.89) and 6.52(5.75~7.18), respectively. The observed annual average pH values were maintaining identical values in general, but pH values decreased continuously during the four months after thinning in the experimental watershed. So thinning is suspected of the major cause for the decrease. 2. Annual average EC values of stream water in 1998 and in 1999 were $26.69(17.95{\sim}33.5){\mu}S/cm$ and $25.19(17.5{\sim}33.8){\mu}S/cm$, respectively. The observed annual average EC values were maintaining identical values in general. 3. As a result of the comparison of average dissolved ions of rainfall and stream water, $Na^+$, $Mg^{2+}$, $Ca^{2+}$, $Cl^-$, $NO_3{^-}$, and $SO_4{^{2-}}$ showed minus values between incomings and outgoings. $Na^+$ and $NO_3{^-}$ among the dissolved ions of stream water showed the highest concentration out of cations and anions respectively. 4. By the change of pH value in stream water due to rainfall events, pH value decreased with increasing runoff as pH value increased before and after peak flow. 5. By the change of EC value in stream water due to rainfall events, EC value decreased with increasing runoff of first rainfall as EC value changed with runoff before and after peak flow. 6. As the runoff increased, the concentration of $Na^+$, $Ca^{2+}$, $K^+$, total cation, $Cl^-$, and $SO_4{^{2-}}$ in stream water lowered. On the other hand, the runoff decreased, their concentration in stream water tended to get high. But in terms of $NO_3{^-}$ and total anion, they turned out vice versa. $Mg^{2+}$ produced no reaction. 7. The base flow among runoff components separated by using HYCYMODEL influenced greatly on pH, EC, concentration of cation and anion.

• Proceedings of the Korean Environmental Sciences Society Conference
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• 2001.05a
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• pp.211-216
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• 2001

수용액상에서 게 껍질에 의한 납 이온 제거시 납 이온 메카니즘을 규명하기 위하여 납이온 제거에 미치는 pH의 영향에 대해 조사하였다. 게 껍질에 의한 납 이온의 제거는 게껍질 내에 함유되어 있는 CaC $O_{3(S)}$의 용해에 따른 미세침전에 의한 제거가 대부분인 것으로 나타났다. pH가 증가하면 납 이온 제거량도 증가하였고 이온교환에 의해 발생되는 칼슘 이온의 유출은 납 이온 제거를 더욱 증가시키고 게 껍질 내의 $CO_{3}^{2-}$는 납 이온의 침투로 게 껍질 내부에 $PbCO_{3(S)}$ 형태의 복합체를 형성하는 것으로 판단되었다. 납 이온의 제거는 대부분 게 껍질 내 $PbCO_{3(S)}$의 용해로 인해 발생되는 $Pb_{3}(CO_{3}){2}(OH)_{2(S)}$와 $PbCO_{3(S)}$의 침전으로 이루어졌다. 수용액 중의 납 이온은 게 껍질 내 CaC $O_{3(S)}$의 용해를 가속화시키며 게 껍질 내부에서도 납 이온의 침전물이 발생하는 것으로 관찰되었다.

• Journal of Korean Society of Environmental Engineers
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• v.34 no.3
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• pp.162-167
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• 2012

The removal of orthophosphate ions from aqueous solutions by the anion exchange resin in the form of $Cl^-$ ion was investigated to elucidate the ion exchange mechanism which depends on the forms of orhthophoshate ions. In addition, the effects of alkalinity and other common anions were studied. The results showed that the orhthophosphate ions with the oxidation state of 2 and 3 ($HPO{_4}^{2-}$ and $PO{_4}^{3-}$) were effectively removed by the anion exchange resin, whereas the part of the $H_2PO_4{^-}$ ion passed through the ion exchange column. This suggested that the affinity of $H_2PO_4{^-}$ to the ion exchange resin was comparable with that of $Cl^-$ ion. In all cases, the effluent pHs have shown to be much lower than the calculated values, indicating that more $Cl^-$ ions than the orthophosphate equivalents in the influent were eluded. As the alkalinity increases, the decrease in pH was minimized. When the alkalinity was 100 mg/L ($CaCO_3$) or greater, 100 mg/L orthophosphate ions including $H_2PO_4{^-}$ were completely removed. The common anions such as $SO{_4}^{2-}$ and $NO_3{^-}$ were also removed by the anion exchange resin, and thus decreased the ion exchange capacity for the removal of orthophosphate.

• FLOWER RESEARCH JOURNAL
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• v.17 no.4
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• pp.237-241
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• 2009

This study was conducted to determine injury symptoms of orchids by sulfur dioxide gases, three orchid plants (Phalaenopsis, Cymbidium, Oncidium) were exposed to sulfur dioxide gas in an enclosed growth chambers. Sulfur dioxide gases treatments consist of five different concentrations (0, 5, 10 25, and 50 ppm) and plant exposure of 18 hours with $25{\pm}5^{\circ}C$ air temperature and $50{\pm}5%$ relative humidity. SPAD values for chlorophyll content and percent leaf injury as well as leaf ion exudation were measured before and after the gas treatments. Phalaenopsis leaves showed 23.3% leaf injury at 10 ppm sulfur dioxide gas, whereas Cymbidium and Oncidium showed 4.0 and 4.4% leaf injury under 25 ppm or less, respectively. Major leaf injury symptoms appeared as initial water-soaking under side of the leaf, followed by rapidly progressed complete leaf discolorization or chlorosis. As the gas concentration increased, the SPAD value decreased while ion exudation increased. Cymbidium and Oncidium were resistant to sulfur dioxide gas than Phalaenopsis.

• Journal of Forest and Environmental Science
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• v.13 no.1
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• pp.90-95
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• 1997

This study examined the effect of forest road construction on electronic conductivity(EC) and ion concentrations under different precipitation. They were torrential streams within three different watersheds with various forest road densities (watershed A : 8.82m/ha, watershed B: 2.32m/ha, and watershed C: control) in the Experimental Forest of Kangwon National University. The results were as follows: 1. EC of three watersheds did not show on difference in precipitation, but it was high in case of long interval rainfall time period. EC of watershed A and B were higher than that of watershed C. 2. Concentrations of cation was about 2 times higher than those of anion. Average concentrations of $N^+$ and $Ca^{2+}$ showed maximum and minimum respectively, and $SO_4{^{2-}}$ was 3.7 times higher than $Cl^-$. 3. Precipitation and discharge had no effect on ion concentrations, but watershed A and B were higher in concentrations of cation than watershed C.

• Journal of the Korean Chemical Society
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• v.33 no.2
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• pp.232-237
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• 1989

The elution mechanism of rare earth elements in cation exchange resin which was substituted with $NH_4^+,\;Zn^{2+}\;or\;Al^{3+}$ as a retaining ion had been investigated. Rare earths or rare earths-EDTA complex solution was loaded on the top of resin bed and eluted with 0.0269M EDTA solution. When the rare earth-EDTA complex was adsorbed on the $Zn^{2+}\;or\;Al^{3+}$ resin form, retaining ion was complexed with EDTA and liberated rare earths was adsorbed in the resin again. Adsorbed rare earths in resin phase could be eluted by the complexation reaction with EDTA eluent. On $NH_4^+$ resin form, the rare earth-EDTA complex which had negative charge could not adsorbed on the cation exchange resin because the complexation reaction between $NH_4^+$ and EDTA was impossible. So the elution time was much shorter than in $Zn^{2+}\;or\;Al^{3+}$ resin form. When the rare earths solution was loaded on the $Zn^{2+},\;Al^{3+}$ resin form bed, rare earths was adsorbed in the resin and the retaining ion was liberated. Adsorbed rare earths in resin bed was exchanged by EDTA eluent forming rare earths-EDTA complex, and eluted through these processes. On $NH_4^+$ resin form, rare earths loaded was adsorbed by exchange reaction with $NH_4^+$. As the EDTA eluent was added, rare earths was liberated from resin forming negatively charged rare earth-EDTA complex and eluted without any exchange reaction. So the elution time was greatly shortened and there was no metallic ion except rare earths in effluent. When the $Zn^{2+}\;and\;Al^{3+}$ was used as retaining ion, the pH of efflent was decreased seriousely because the $H^+$ liberated from EDTA molecule.

• Journal of the Korea Academia-Industrial cooperation Society
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• v.3 no.2
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• pp.141-145
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• 2002

Successive ion Exchange Column model was developed with the combination of mass action law and mole balance equation. consuming that ions entering the ion exchange bed pass the resin layer via consecutive ion exchange equilibrium. The application of the model to condensate polishing demineralizer in nuclear power plants indicates that the leakage of $Na^+$ and $Cl^-$ depends upon the degree of resin regeneration and that the ratio of specific ion concentration in Influent to in effluent is subject to the characteristics of resin and solution. The model can account for the local in-equilibrium with the correction of resin concentration and also can be applicable to a competitive ion exchange.