유칼리나무의 수피로부터 분리한 항산화활성 물질

이인경,윤봉식,김종평,정성현,심규섭,유익동,Lee, In-Kyoung,Yun, Bong-Sik,Kim, Jong-Pyung,Chung, Sung-Hyun,Shim, Gyu-Seop,Yoo, Ick-Dong 한국생약학회 1998 생약학회지 Vol.29 No.3

Seven antioxidative compounds were isolated from chloroform and ethyl acetate extracts of the stem bark of Eucalyptus globulus (Myrtaceae). They were identified as rhamnazin (1), rhamnetin (2), naringenin (3), eriodictyol (4), quercetin (5), taxifolin (6) and dihydrokaempferol-3-rhamnoside (7) on the basis of various spectroscopic analyses. These compounds inhibited lipid peroxidation with $IC_{50}$ values of 0.08-30 ${\mu}g/ml$.

농축 블루베리 퓌레 열처리 시 pH 조절제의 품질 저하 억제 효과

이인경,민세철,김희선,한귀정,김명환,Lee, In Gyeong,Min, Seo Cheol,Kim, Hee Sun,Han, Gwi Jung,Kim, Myung Hwan 한국식품조리과학회 2016 한국식품조리과학회지 Vol.32 No.5

Purpose: In this study, we aimed to minimize quality degradation of concentrated blueberry puree by thermal treatment at $90^{\circ}C$ for 5 min, with citric acid (CA) and acidic sodium metaphosphate (ASM) as pH modifiers. Methods: The color values, redness a, anthocyanin contents, DPPH radical scavenging, elastase inhibition and tyrosinase inhibition activities were evaluated for quality parameters of concentrated blueberry puree. Results: The highest values of color value, redness a, anthocyanin contents, DPPH radical scavenging, elastase inhibition and tyrosinase inhibition activities were 1% CA+0.5% ASM followed by 1% CA and control. The quality parameters of concentrated blueberry puree were significantly different between control and 1% CA+0.5% ASM treatment (p<0.05). Conclusion: During thermal treatment, quality degradation of concentrated blueberry puree was reduced by 1% CA+0.5% ASM treatment, which is expected for new acidulants.

상아질 지각과민증 치료후 임상 및 주사전자현미경적 관찰

이인경,한수부,고재승,김현만,Lee, In-Kyeong,Han, Soo-Boo,Ko, Jea-Sung,Kim, Hyung-Man 대한치주과학회 1990 Journal of Periodontal & Implant Science Vol.20 No.2

생체요업재료와 차폐막의 복합사용후 골연하 결손부의 재생효과

이인경,이기영,한수부,고재승,조정식,Lee, In-Kyung,Lee, Ki-Young,Han, Soo-Boo,Ko, Jae-Sung,Cho, Jeong-Sik 대한치주과학회 1996 Journal of Periodontal & Implant Science Vol.26 No.1

The purpose of this study was to observe the effect of $Biocoral^R$ graft and bioglass 45S5 graft in combination with ePTFE membrane in periodontal osseous defects for new bone formation. Nine healthy dogs were used. Under general anesthesia, 3-wall defects were created on the mesial and distal surfaces of the maxillary right canines, the mesials of the maxillary right second premolars, the distals of the mandibular right canines and the mesials of the mandibular right third premolars. To induce periodontitis, a silicone rubber, $Provil^R$ light body, was injected under pressure into the defects. Ninety days later, $Provil^R$was removed and followed by thorough root planing. The followings were then applied in the mesial and distal defects of the maxillary right canines, the mesials of the maxillary right second premolars, the distals of the mandibular right canines and the mesials of the mandibular right third premolars by random selections : 1) ePTFE membrane only application, 2) $Biocoral^R$ graft, 3) $Biocoral^R$ graft and ePTFE membrane application, 4)Bioglass 45S5 graft, 5) Bioglass 45S5 graft and ePTFE membrane application. The membranes were removed 1 month later. The dogs were sacrified at 1, 2 and 3 months following the graft, and block sections were made, demineralized, embedded, stained and examined by light microscope and transmission electron microscope. On the sections from teeth treated with ePTFE membrane only, the defect demonstrated extensive connnective tissue and alveolar bone regeneration. The $Biocoral^R$ graft group demonstrated extensive bone regeneration compared with ePTFE membrane only group. In the $Biocoral^R$ graft plus ePTFE membrane group, regeneration of new alveolus and crest occurred within the defect. As the experimental period lengthened, bone regeneration was increased and bone bridge was formed among the graft particles. The but bioglass 45S5 graft group demonstrated extensive bone regeneration but the amount of new bone was less than that of the $Biocoral^R$ graft group. For the bioglass 45S5 graft plus ePTFE membrane group, the amount of new bone was also increased. As the experimental period lengthened, bone regeneration was increased. Multinucleated giant cells, fibroblasts and macrophages were observed. As the bone formation was increased, the number of such cells was decreased. In conclusion, the $Biocoral^R$ was found better than the bioglass 45S5 for new bone formation, and the use of ePTFE membrane alone or with $Biocoral^R$/bioglass 45S5 can be supported as potential methods of promoting bone formation.

하동-산청 회장암체 내 부존하는 하동 함 철-티탄 광체의 광화작용

이인경,전영식,최상훈,Lee, In-Gyeong,Jun, Youngshik,Choi, Sang-Hoon 대한자원환경지질학회 2017 자원환경지질 Vol.50 No.1

하동-산청 회장암체는 영남육괴의 남서부에 선캠브리아기 지리산 편마암 복합체의 변성암류를 기반암으로 차노카이트(charnockite)와 함께 분포하며, 주변에는 중생대 화성암류가 관입 산출한다. 하동-산청 회장암체는 중생대 쥬라기의 섬장암을 경계로 북서쪽의 산청 회장암체와 남쪽의 하동 회장암체로 구분된다. 광체는 하동 회장암체 내에 남북방향으로 약 14 km의 연장을 보이며 단속적으로 산출되는 하동 함 철-티탄 암맥상 광체이다. 하동 함 철-티탄 암맥상 광체 내에는 함-철 산화광물인 자철석(magnetite) 및 티탄철석(ilmenite) 과 함께 함 티탄 광물들(금홍석(rutile) 과 티타나이트(titanite))과 소량의 황화광물들(자류철석, 황철석, 황동석, 섬아연석 등)이 수반하여 산출된다. 하동 함 철-티탄광체의 광화작용은 초기 자철석-티탄철석의 공생 산출로 시작되어 자철석-티탄철석 ${\rightarrow}$ 자철석-티탄철석-자류철석 ${\rightarrow}$ 티탄철석-자류철석-금홍석-티타니이트(${\pm}$황철석) ${\rightarrow}$ 황화광물의 공생관계를 보이며 진행되었다. 광체 내 공생관계와 및 열역학적 연구를 통하여 확인된 하동 함 철-티탄 광체의 초기 함 철-티탄 광화작용은 약 $10^{-11.8}{\sim}10^{-17.2}$ atm의 산소 분압조건($700^{\circ}C$)에서 $Fe_3O_4-FeS$ 상평형을 이루는 황 분압조건 (약 $10^0$ atm) 까지 황 분압의 증가에 의하여 진행되었으며, 그 후 황화광물의 산출은 산소 분압은 감소(${\geq}10^{-20.2}$ atm)되면서 황 분압이 증가(${\geq}10^0$ atm) 하는 환경에서 진행되었다. The Hadong-Sancheong Proterozoic anorthosite complex occurs in the southwestern region of the Ryongnam massif. The geology of the area mainly consists of metamorphic rocks of the Jirisan metamorphic complex as basement rocks, charnockite, and the Hadong-Sancheong anorthosite, which are intruded by the Mesozoic igneous rocks. Hadong-Sancheong anorthosite complex is divided into the Sancheong anorthosite and the Hadong anorthosite which occur at north-southern and south area of the Jurassic syenite, respectively. The Hadong Fe-Ti-bearing dike-like ore bodies developed intermittently in the Hadong anorthosite with north-south direction and extend about 14 km. The Hadong Fe-Ti-bearing ore bodies consist mainly of magnetite and ilmenite with rutile, titanite, and minor amounts of sulfides(pyrrhotite, pyrite, chalcopyrite and sphalerite). The Hadong Fe-Ti-bearing ore bodies show a paragenetic sequence of magnetite-ilmenite ${\rightarrow}$ magnetite-ilmenite-pyrrhotite ${\rightarrow}$ ilmenite-pyrrhotite-rutile-titanite(and/or pyrite) ${\rightarrow}$ sulfides. Equilibrium thermodynamic interpretation of the mineral paragenesis and assemblages indicate that early Fe-Ti-bearing ore mineralization in the ore bodies occurs at about $700^{\circ}C$ which corresponds to oxygen fugacity of about $10^{-11.8}{\sim}10^{-17.2}$ atm with the decrease tendency of sulfur fugacity to about $10^0$ atm as equilibrium of $Fe_3O_4-FeS$. The change of ore mineral assemblages from Fe-Ti-bearing minerals to sulfides in late ore mineralization of the ore bodies indicates that oxygen fugacity would have slightly decreased to ${\geq}10^{-20.2}$ atm and increased sulfur fugacity to ${\geq}10^0$ atm.

충북 영동지역 지하수의 수리지화학적 특성 및 질산염 오염 특성

이인경,최상훈,Lee, In-Gyerong,Choi, Sang-Hoon 대한자원환경지질학회 2012 자원환경지질 Vol.45 No.1

농업지역인 충북 영동 지역 지하수의 지화학적 특성과 질산염의 기원을 규명하기 위하여 지화학 및 질소동위원소 연구가 수행되었다. 지하수의 pH는 평균 7.2 (6.0~8.2)로 약산성 내지 약알칼리성으로 나타났다. 지하수의 평균 전기전도도, 산화환원전위 및 용존산소량은 각각 369 ${\mu}S/cm$ (70~729 ${\mu}S/cm$), 165.6 mV (29-383.2 mV), 4.3 mg/L(1.8~8.0 mg/L)이다. 지하수 내 양이온을 함량이 높은 순으로 나열하면, $Ca^{2+}$>$Na^{2+}$>$Mg^{2+}$>$K^{2+}$이고, 음이온의 경우는 ${HCO_3}^-$>${NO_3}^-$>${SO_4}^{2-}$>$Cl^-$>$F^-$이다. 연구지역 지하수의 대부분은 물-암석과의 반응으로 기인된 Ca-$HCO_3$ 유형으로 나타났으며, Ca-Cl 유형 (2.5%) 과 Na-$HCO_3$ (2.5%) 유형은 농업활동 등의 영향으로 전이된 것으로 밝혀졌다. 지하수 내 질산성 질소의 함량은 10.2 mg/l~26.9 mg/l 범위로 검출되어 오염이 우려되는 것으로 밝혀졌다. 지하수 내 질산성 질소의 기원을 파악하기 위한 질소 동위원소 분석 결과, 질산성 질소의 동위원소비 (${\delta}^{15}N_{-}NO_3$)는 1.9‰~19.4‰ (평균 10.1‰)로 측정되었으며, 동위원소비에 따른 질산염의 기원은 축사의 동물 분뇨나 농지에 시비된 유기물 비료임을 나타낸다. Major ions and nitrogen isotopic analyses were performed to determine the geochemical characters and to identify the source of nitrate of the shallow groundwater around agricultural field in the Youngdong area. The pH value of groundwater ranges from 60. to 8.2 (pH 7.2, mean). The average of EC, Eh and DO is 369 ${\mu}S/cm$ (70~729 ${\mu}S/cm$), 165.6 mV (29~383.2 mV), 4.3 mg/L (1.8~8.0 mg/L) respectively. The ion concentraion of groundwater was in the order of $Ca^{2+}$>$Na^{2+}$>$Mg^{2+}$>$K^{2+}$ and ${HCO_3}^-$>${NO_3}^-$>${SO_4}^{2-}$>$Cl^-$>$F^-$. Most of groundwater is Ca-$HCO_3$ type. The groundwater was affected by water-rock interaction in the shallow depth. Some groundwater is Ca-Cl or Na-$HCO_3$ (2.5%) type that was due to agricultural activities. The $NO_3$_N concetration of grondwater range from 10.2 mg/l to 26.9 mg/l, which show that this area is under nitrate pollution. ${\delta}^{15}N-NO_3$ value of the groundwater is the origins of are a combination of animal wastes and man-made fertilizers.

울진 폐광산의 매립광미와 폐광석에 의한 주변 토양 및 수계의 오염특성

이인경,최상훈,Lee, In-Gyeong,Choi, Sang-Hoon 대한자원환경지질학회 2008 자원환경지질 Vol.41 No.1

울진광산 지역에 매립된 광미와 방치된 폐광석이 주변 하천에 미치는 영향을 평가하기 위해, 하천수, 침출수, 갱내수 및 지하수의 물리화학적인 특성을 파악하였다. 또한 폐광석 내 황화광물의 풍화 특징을 파악하기 위한 광물학적 연구와, 토양 내 미량원소의 분산 특성을 파악하기 위한 총함량 분석을 수행하였다. 매립된 광미에서 발생하는 침출수의 pH의 범위는 $2.9{\sim}6.0$이며, EC는 $99{\sim}3990{\mu}S/cm$로 주원소(최대 492 mg/l Ca; 83.8 mg/l Mg; 45.2 mg/l Na; 44.7 mg/l K; 50.8 mg/l Si) 및 미량원소(최대 $826,060{\mu}g/l$ Fe; $131,230{\mu}g/l$ Mn; $333,600{\mu}g/l$ Al; $61,340{\mu}g/l$ Zn; $2,530{\mu}g/l$ Cu; $573{\mu}g/l$ Cd; $476{\mu}g/l$ Pb)함량이 높게 나타났다. 하천수의 물리화학적 특성은 침출수와 지류의 유입에 따른 공간적 변화와 강수량에 따른 시기별 변화가 관찰되었다. 침출수의 유입으로 하천수의 용존 이온의 농도는 증가하지만 오염되지 않은 지류와의 혼합에 의한 희석작용으로 하류로 갈수록 감소한다. 건기인 2월에는 침출수 유입량이 줄어 하천수의 용존 이온 함량이 우기보다 낮다. 하지만 건기에는 지류 및 하천수의 유량 감소로 인하여 희석작용이 상대적으로 미약하여 우기에 비해 오염 확산 범위가 더 넓은 것으로 확인되었다. 배경치와 비교한 울진광산 주변의 토양시료의 중금속 농집 순서는 망간>철>납>구리>아연으로 나타났다. 울진광산에서 산출되는 황화광물은 자류철석과 섬아연석이 주를 이루며, 방연석과 황동석이 수반된다. 이 중 자류철석이 가장 풍화가 빠르게 진행되었으며, 광물 내부에 발달된 균열부와 입자 가장 자리를 따라 내부로 산화가 진행되어 철수산화광물이 생성되며, 소량의 Zn을 흡착하는 것으로 밝혀졌다. Physicochemical characteristics of stream water, leachate, mine water and groundwater were investigated to estimate the influences of the tailing and waste rock from the abandoned Uljin mine area. Total extraction analysis and mineralogical studies were carried out to understand sulfide weathering and to determine the distributions of trace elements in the soil affected by mine waste (tailing, waste rock and leachate). The pH and EC value of the leachate from the tailing disposal ranged 2.9-6.0, $99{\sim}3,990{\mu}S/cm$, respectively, and the concentrations of dissolved major (up to 492 mg/l Ca; 83.8 mg/l Mg; 45.2 mg/l Na; 44.7 mg/l K, 50.8 mg/l Si) and trace elements (up to $826,060{\mu}g/l$ Fe; $131,230{\mu}g/l$ Mn; $333,600{\mu}g/l$ Al; $61,340{\mu}g/l$ Zn; $2,530{\mu}g/l$ Cu; $573{\mu}g/l$ Cd; $476{\mu}g/l$ Pb) were relatively high. The stream water showed the variation of dissolved metal concentrations in seasonally and spatially. The dissolved metal contents of the stream water increased by influx the leachate from the tailing disposal, but these of the down stream have been considerably decreased by mixing of dilute tributaries. The dissolved metal concentrations of the stream water at dry season (as February) were lower than these at rainy season (as May and July). These represent that the amounts of the leachate varied with season. However, stream water could not be effectively diluted by confluence with uncontaminated tributaries, because the flux of tributaries and streams reduced at dry season. Thus attenuations by dilution had been dominantly happened in rainy seasons. The order of accumulations of trace element in soils compared with background values revealed Mn>Fe>Pb>Cu>Zn. Sulfide minerals were mainly pyrrhotite, sphalerite and galena and chalcopyrite. Pyrrhotite was rapidly weathered along the edge and fractures, and results in the formation of Fe-(oxy)hydroxides, which absorbed a little amount of Zn.

무궁화나무의 성분 및 생물활성에 관한 연구(I)

이인경,유인자,정동호,한규훈,윤봉식,유익동,Lee, In-Kyoung,Ryoo, In-Ja,Choung, Dong-Ho,Han, Kyou-Hoon,Yun, Bong-Sik,Yoo, Ick-Dong 한국생약학회 1997 생약학회지 Vol.28 No.3

Hibiscus syriacus L. (Malvaceae) is widely distributed over Korean, China, India and Siberia. The dried flower of Hibiscus syriacus is used as a folk medicine for curing of hematochezia, dysentery, obstruction due to wind-phlegm, regurgitation, and vomiting of food, and the dried root bark is used antipyretic, anthelmintic and antifungal agents. From a chloroform extract of root bark of this plant, compound I, II, and III were isolated and the structures were elucidated by various spectroscopic analyses. These compounds were identified as syringaresinol. E-N-feruloyltyramine, and Z-N-feruloyltyramine, respectively and were isolated from this plant for the first time. Compound II and III exhibited lipid peroxidation inhibitory activities with $IC_{50}$ of 15.5 and 28.6 ${\mu}g/ml$, respectively.

멜라닌 색소 침착의 치료

이인경,한수부,Lee, In-Kyeong,Han, Soo-Boo 대한치주과학회 2003 Journal of Periodontal & Implant Science Vol.33 No.2

Oral melanin pigmentation is common in some races and ethnic groups. The gingivae are the most frequently pigmented intra-oral tissues. Melanin pigmentation is the result of melanin granules, produced by melanoblasts intertwined between epithelial cells at the basal layer of the epithelium. We present one case of melanin pigmentation of the gingiva of 26-year old female. Melanin depigmentation method is applying a 90% phenol solution to deepithelize pigmented areas, gingivectomy, epithelial abrasion, bone denudation, and split thickess flap. We chose epithelial abrasion using round diamond bur. The patient satisfies the result and have almost no pain and discomfort. But repigmentation potential must be noticed to patient.

장풍 폐광산 주변 지질환경에서 중금속의 존재형태

이인경,이평구,최상훈,김지수,소칠섭,Lee In-Gyeong,Lee Pyeong-Koo,Choi Sang-Hoon,Kim Ji-Soo,So Chil-Sup 대한자원환경지질학회 2005 자원환경지질 Vol.38 No.6

In order to identify the speciation of As and trace elements which are contained weathered waste rocks on the abandoned Jangpoong Cu mine area, five fraction sequential extraction was carried out. Concentrations of the extraction solutions which were acquaired each fraction were mesured by ICP-AES. Mineral characters of weathered waste rocks were determinated by XRD. The weathered waste rocks could divide into two types (Type I and type II). Type land type II weathered waste rocks are mainly composed of a quartz and a calcite, respectively. The most dominant speciation of As, Co and Fe is residual phase. Most of the speciation of Cd, Mn and Zn is residual phase for type I and Fe-Mn oxide phase for type II. In case of Cu, residual phase is predominant in type I and sulfide is predominet in type II. The most dominant speciation of Pb for type I and type II is associated with the residual phase and Fe-Mn oxide phase, respectively. At pH 4-7 range, the order of relative mobility considers Zn>Cu>Cd>Pb>Co>AS in type I, and Cd>Cu>Zn>Pb>As>Co in type II. 폐광된 장풍광산의 풍화된 폐광석에 함유된 중금속의 존재형태를 규명하기 위해 5단계 연속추출법을 수행하였다. 각 단계에서 용출된 용액은 ICP-AES로 분석하였다. XRD로 풍화된 폐광석 시료들의 광물조성을 파악한 결과, 시료는 산성 환경에서 pH에 대한 완충작용을 할 수 있는 방해석의 유무에 따라 두 유형(type I and type II)으로 나눌 수 있었다. Type I 시료의 주 구성광물은 석영으로 방해석이 산출되지 않으며, type II 시료의 주 구성광물은 방해석이었다. 모든 시료에서 비소, 코발트, 철은 잔류형태로 존재하는 것이 가장 우세하였다. 카드뮴, 망간, 아연의 경우 type I 시료에서는 잔류형태가, type II 시료에서는 산화철망간형태가 우세하였다. 구리는 type I 시료의 경우 잔류형태가 가장 우세하였고, type II의 경우 황화광물형태가 우세하였다. 납은 type I시료에서는 잔류형태가 가장 우세하였고, type II시료에서 산화철망간 형태가 우세하였다. pH 4-7 사이에서 중금속의 상대적인 이동성은 type I시료의 경우 아연>구리>카드뮴>납>코발트>비소의 순서였으며, type II시료에서는 카드뮴>구리>아연>납>비소>코발트의 순서로 확인되었다.