http://chineseinput.net/에서 pinyin(병음)방식으로 중국어를 변환할 수 있습니다.
변환된 중국어를 복사하여 사용하시면 됩니다.
귀류법에 대한 교사 지식 분석 -"교과 내용 지식" 및 "학생의 이해에 대한 지식"을 중심으로-
황진연 ( Jin Yeon Hwang ),신보미 ( Bo Mi Shin ) 한국수학교육학회 2016 수학교육 Vol.55 No.1
The aim of this study was to analyze characteristics of teachers`` knowledge about reductio ad absurdum. In order to achieve the aim, this study conducted didactical analysis about reductio ad absurdum through examining previous researches and developed a questionnaire with reference to the results of the analysis. The questionnaire was given to 34 high school teachers and qualitative methods were used to analyze the data obtained from the written responses by the participants. This study also elaborated the framework descriptors for interpreting the teachers`` responses in the light of the didactical analysis and the data was elucidated in terms of this framework. The specific features of teachers`` knowledge about reductio ad absurdum were categorized into five types as a result. This study raised several implications for teachers`` professional development for effective mathematics instruction related to reductio ad absurdum.
황진연 ( Jin Yeon Hwang ),최진범 ( Jin Beom Choi ),정기영 ( Gi Young Jeong ),오지호 ( Ji Ho Oh ),최영훈 ( Young Hun Choi ),이진현 ( Jin Hyun Lee ) 한국광물학회 2013 광물과 암석 (J.Miner.Soc.Korea) Vol.26 No.2
국내 주요 백운석 광산에서 산출되는 백운석 광석과 수반광물에 대하여 X-선회절분석, 박편관찰, 주사전자현미경 관찰 등을 통하여 광물학적 및 조직 특성을 분석하고, 이들의 산출상태와 성인을 검토하였다. 연구 결과, 백운석 광석은 담회색에서 암회색을 띠며 입자도 세립에서 조립까지 다양하였으나, 주로 거의 순수한 돌로마이트로 이루어졌다. 일부 백운암에서는 소량의 방해석, 석영, 운모가 함유되었다. 세맥, 암맥, 변질부 등에서 국지적으로 방해석, 석영, 일라이트, 장석, 고령토광물, 녹니석등이 산출되며, 일부 광산 변질부에서 세피올라이트와 규회석이 확인되었다. 그러나 이번 조사에서 온석면과 투각섬석과 같은 석면광물은 확인되지 않았다. 광산내 적갈색 및 황색을 띠는 점토물질들은 주로 일라이트로 구성되며, 카올린광물과 스멕타이트가 수반되기도 한다. 이들은 암맥관입과 관련된 부분적 열수변질과 이후의 풍화작용에 의해 형성된 것으로 보인다. 백운암층의 구성광물, 조직, 산출 상태와 기존의 연구결과로 볼 때, 백운석 광상은 선캄브리아기와 고생대의 얕은 바다에서 퇴적된 선회질 퇴적물이 속성작용에 의해 백운석화 작용을 받아 형성된 것으로 보인다. The occurrence, mineralogical characteristics, and origin of the dolomite ores were inve-stigated from major dolomite mines in South Korea. Mineralogical and textural properties of the ores and associated minerals were analyzed using X-ray diffraction, thin section petrography, and scanning electron microscopy. Dolomite ores were light to dark gray in color and mainly composed of dolomite in varying particle size with minor amounts of calcite, quartz and micas. Calcite, quartz, illite, feldspar, kaolin minerals, and chlorite occurred in local veins, dikes and alteration zones. Sepiolite and wolla-stonite occurred in the altered part of some mine. Asbestos minerals such as chrysotile and tremolite, however, were not identified in the present study. Reddish brown to yellow clay materials were mainly compesed of illite, occasionally associated with kaolin minerals and smectite. These clay minerals might be a product of the local hydrothermal alteration related to the dyke intrusion and subsequent weathering. As well indicated in the previous studies, mineral composition, texture, and occurrence of the dolostone beds suggest their formation through the diagenesis of carbonate sediments deposited in the shallow sea during the Precambrian to Paleozoic period.
국내 건축자재에 함유된 석면의 함량에 대한 X-선회절분석 연구
황진연 ( Jin Yeon Hwang ),이효민 ( Hyo Min Lee ),오지호 ( Ji Ho Oh ),박기남 ( Gi Nam Park ) 한국광물학회 2011 광물과 암석 (J.Miner.Soc.Korea) Vol.24 No.2
대표적인 일부 건축자재의 석면 함량을 일본공업표준법(JIS)에 따른 X-선회절분석으로 측정하였고, 분석과정에서의 광물학적 성분변화와 문제점을 검토하였다. 국내의 슬레이트, 벽재, 천장재의 대표적인 건축자재에 대해 석면 함량을 정량한 결과, 슬레이트 시료가 6.87~6.93%의 온석면을 함유하여 가장 많은 석면을 함유하고 있는 것으로 분석되었다. 분석된 다른 건축자재들에서도 1.35~3.98%의 범위로 다양한 양의 온석면이 포함되어 있는 것으로 분석되었다. 이번 연구에서 국내에서 처음으로 일부 건축자재의 석면 함량에 대한 X-선회절방법에 의한 분석결과를 제시하였으며, 이런 방법을 통하여 국내에서 최근에 개정된 규정(노동부 산업안전보건법 제2007-26호)에서 규정한 석면의 허용기준량 0.1% 함량을 평가하는데 효과적인 것으로 나타났다. 일부 시료에서 온석면과 함께 투각섬석이 소량 수반되고 있음이 나타났으나, 이들의 결정형태와 그 함량과 지질학적 산출상태 등으로 보아, 석면 활용의 목적으로 첨가한 것이 아니고 온석면에 본래 수반되었던 불순광물로 나타난 것으로 생각된다. X-선회절분석으로 석면상과 비석면상의 구분이 어렵기 때문에 형태를 관찰할 수 있는 광학현미경과 전자현미경의 보조적인 관찰도 필요한 것으로 나타났다. 이번에 사용한 X-선회절분석 방법에서는 가열처리와 산처리에 의한 소실율이 많아 석면의 농집도가 높은 건축자재 시료에 가장 효과적인 것으로 나타났다. The asbestos contents in some representative building materials were analyzed using JIS (Japanese Industrial Standard) X-ray diffraction (XRD) method. The changes in mineral composition during analysis process and problems in JIS method were also examined. XRD analysis of some representative domestic building materials used for roof, wall, ceiling, and floor indicates that slate have the highest asbestos content having 6.87~6.93% of chrysotile. Other building materials analyzed in this study also have 1.35~3.98% of chrysotile contents. The XRD analysis results of asbestos contents in some domestic building materials are presented in this study. This method is very effective for the asbestos content evaluation of building materials according to newly modified asbestos content regulation (Law of Industrial Safety and Health, 2007-26) that limits asbestos content less than 0.1% by Ministry of Employment and Labor. Small amount of tremolite as well as chrysotile were also observed in some samples. With consideration of crystal shape, contents and geological occurrence, it is considered that tremolite is an associated mineral of chrysotile and is not intentionally added. Complemental analyses with optical microscope and SEM/EDS are also necessary because XRD method cannot distinguish asbestiform from non-asbestiform. The XRD method applied in this study is very effective in the asbestos content analysis of building materials, specially building materials showing high asbestos concentration in residues due to the high loss rate with ashing and acid dissolution procedure.
한우 사육에 이용한 황토 ( 풍화토 ) 의 입도분리에 따른 광물성분 및 화학적 특성
황진연(Jin Yeon Hwang),박현진(Hyun Jin Park),양경희(Kyung Hee Yang),이효민(Hyo Min Lee) 한국광물학회 2002 광물과 암석 (J.Miner.Soc.Korea) Vol.15 No.1
Mineral composition and chemical properties of Hwangto (reddish residual soil) that used in feeding of cattles at Iksan, Jeollabuk-do, Korea were examined according to particle size separation such as gravel, sand, silt, coarse clay and fine clay. Mineral composition analyses reveal that gravel and sand silt. Iron oxides are mainly included in fine clay. According to chemical analyses of major elements. Al, Fe and H_2O contents are increased with decreasing of particle size. This trend well agrees with increase of clay minerals in smaller particles. Chemical analyses of trace elements indicate that contents of Zn, Rb, Sr, Ba, Pb significantly differ with particle sizes. Ba and Sr are included in feldspars since these elements are abundant in sand containing abundant feldspars. Pb and Sm are abundant in sample before particle size separation. but the contents are significantly decreased after separation. Therefore, most of these elements appear to be existed as removable phase. Nb, La, Th, Ce are more abundant in silt. The contents of all the other trace elements tend to be increased in smaller particles containing more clay minerals. The contents of exchangeable cations and leachable elements in acid and alkali solutions are high in clay samples. All the above results indicate that using the portion of smaller particle of Hwangto for livestock feed rather than bulk Hwangto can improve cation exchangeable capacity, ion leaching capacity and sorption properties.
벤토나이트로부터 합성한 Al-충간가교점토의 특성과 인산이온의 흡착성
황진연 ( Jin Yeon Hwang ),김나영 ( Na Young Kim ),이효민 ( Hyo Min Lee ) 한국광물학회 2002 광물과 암석 (J.Miner.Soc.Korea) Vol.15 No.4
Al-pillared clay was synthesized by constructing pillars of aluminum oxides at the interlayer of montmorillonite in bentonite. XRD, DTA and chemical analyses of Al-pillared clay were performed to examine mineralogical properties. Batch adsorption experiments were also conducted to determine the adsorption properties of this synthesized clay for phosphate ions. XRD analyses showed that the interlayer space of Al-pillared clay expanded to 18.03 A°at room temperature and shifted to 17 A° after heating to 550℃. A small change in interlayer space after heating indicates high thermal stability. The interlayer expansion by glycerol was also very small. From DTA analyses, pillared clay showed the characteristic endothermic peaks at 270 and 420℃, which might be caused by dehydration in framework of pillars between interlayers. Adsorption experiment revealed that Al-pillared clay had an excellent adsorption capacity to the phosphate ions, whereas montmorillonite had very low adsorption capacity to phosphate ions. In phosphate solution concentration up to 300 mg/L, 2 g of pillared clay could uptake almost 100% of phosphate ions from 20 mL of solution. After heat treatment of the phosphate adsorbed pillared clay at 500℃ to remove phosphate, the calcined pillared clay could adsorb phosphate ions with a little decreased adsorption efficiency. This fact indicates that Al-pillared clay can be recycled for the adsorption of phosphate ions.