• 한국콘크리트학회:학술대회논문집
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• 한국콘크리트학회 2004년도 추계 학술발표회 제16권2호
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• pp.759-764
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• 2004

In this study, the experiment was carried out to investigate and analyze the ready-mixed concrete production of ultra-high strength concrete with mixing strength of $100N/mm^2$ according to types of mineral admixtures. The main experimental variables were water/binder ratio $25.0\%$, water content $160kg/m^3$ and mineral admixtures such as fly ash, silica fume and meta kaolin. According to the test results, the principle conclusions are summarized as follows. 1) even if it secures similar slump, the viscosity appear to difference by mixing condition relatively. 2) The autogeneous shrinkage of ultra-high strength concrete is profitable that use admixture, and heat of hydration is desirable that apply considering countermeasure enough in the advance. 3) The concrete that use SF10+MK10 on 56days could confirm that it is possible that achieve compressive strength more than $100N/mm^2$ under mixing conditions that is appearing by compressive strength $102.7N/mm^2$.

• 한국세라믹학회지
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• 제20권2호
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• pp.153-160
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• 1983

This study was carried out to research the change of mineral phases and the characteristics(apparent specific gra-vity water absorption firing shrinkage modulus of rupture thermal expansion and specific dielectric constant) of the sintered bodies manufactured by kaolin and limestone. Samples were composed of the same theoretical composition as it of anorthite and fired up to 145$0^{\circ}C$ Investigated the change and micro-structure of the mineral phases by XRD and SEM the characterisdtics of the sintered bodies by TMA Automatic Capacitance Bridge and etc. The results were as follow. 1. Reactions of sintering are occurred between 860-95$0^{\circ}C$ and 1200-138$0^{\circ}C$ and state of bloating is occurred at 1410-145$0^{\circ}C$ 2. For the inclusion of feldspar and its fine particles of materials the temperature of producing and collapsing is decreased. 3. Pseudo-wollastonite and gehlenite are formed about 95$0^{\circ}C$ 4. At 114$0^{\circ}C$ anorthite are begin to forming and increase continuously to 138$0^{\circ}C$. Above 141$0^{\circ}C$ content of anorthite are decreased. 5. The variations of bending strength with sintering temperature reflect similar trend of sintered contraction and in-crease continuously from 120$0^{\circ}C$. At 145$0^{\circ}C$ reached about 680kg/cm2. 6. Specific dielectric constant$($\varepsilon$_s)$ of specimen sintered at 141$0^{\circ}C$ is 7.12 and that value is most favorable.

• 콘크리트학회논문집
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• 제16권3호
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• pp.319-326
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• 2004

본 연구는 콘크리트의 시공성 및 역학적 특성을 향상시키기 위하여 사용되는 혼화재료(플라이애쉬, 고로슬래그미분말, 실리카퓸 및 메타카올린)를 해양환경에 노출되는 콘크리트에 적용할 경우, 혼화재료가 콘크리트의 내염성능 향상에 미치는 영향을 검토하기 위하여 비교적 단기간에 평가할 수 있는 전기적 촉진시험방법을 사용하여 혼화재 종류 및 치환율, 물-결합재비, 재령에 따른 염화물 확산계수를 비교$\cdot$평가하였다. 혼화재 종류 및 치환율에 따른 염화물 확산계수 평가결과 물-결합재비 수준에 따라 성능의 차이는 있지만 각 혼화재별로 염화물 침투저항성이 우수한 치환율 수준이 있는 것을 알 수 있었다. 또한, 염화물확산계수는 물-결합재비 수준에 따른 영향과 더불어 적정의 치환율을 적용한 혼화재의 사용에 의해서도 현저하게 저감시킬 수 있는 것으로 나타났으며, 시간의 경과와 함께 염화물 확산계수도 감소되는 시간의존적인 특성은 혼화재 종류 및 치환율에 의해 영향을 받는 것으로 사료된다. 압축강도와 염화물 확산계수는 반비례의 관계를 보이고 있으며, 본 연구의 범위에서 보면 50MPa 이하영역에서는 염화물 확산계수는 압축강도 발현특성과 더불어 혼화재 사용 및 치환율에 따른 영향도 크게 나타나고 있어, 향후 염해 환경하에서 내구성을 고려한 구조물 설계시 보다 정확한 내구성능 평가를 위해서는 압축강도 발현특성 검토와 더불어 염화물 확산계수의 평가가 이루어져야 할 것으로 사료된다.

• 자원환경지질
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• 제19권spc호
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• pp.43-52
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• 1986

Kaolin-pyrophyllite are locally abundant in the three hydrothermal areas at Yangsan-Tongnae area, Hadong-Sancheong area and Haenam area, deposits are originally composed of acidic volcanic rocks and anorthositic rocks in Hadong-Sancheong area. The clay deposits are formed in the near shallow depths environment through acid hydrothermal alteration. Hadong-Sancheong halloysite deposits are formed by alteration of anorthosite. These differences are mainly on the various country rocks, geological structure and properties of hydrothermal solutions. Country rock is mostly underlain by rhyolitic tuffaceous and anorthositic rocks and a large number of clay deposits were formed during volcanic activity through upper Cretaceous-lower Tertiary. Intrusive rocks is broadly distributed in this area and clay deposits are variable in shapelayer and funnel typed. Zonal pattern of mineral assemblage is as follows, Yangsan-Tongnae deposits-kaolinite, pyrophyllite, dumortierite, andalusite and sericite, Hadong-Sancheong-mostly halloysite, and Haenam-dickite, pyrophyllite, alunite and diaspore. The difference in the zonal pattern of altered rock is considered to depend on differences in the initial acidity of related hydrothermal solution, initial acidity was controlled by the oxygen fugacity.

• 산업기술연구
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• 제10권
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• pp.83-88
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• 1990

The samples used for this work were low grade c1ay($Fe_2O_3$ : 2.90%, $TiO_2$ : 1.65%) produced from Youngsan-po district, and for the iron-bearing impurities removal having a bad influence on Kaoline sample was carried out column floatatoin using Oleic acid, Potassium oleat, Aero 840 promotor, Aero 870 promotor and Keroseneas collectors. For removal of the iron-vearing impurities from the kaoline, investigated first chemical composition size distribution of Kaoline sample, also performanced a basic study on pulp density, collector and pH change on a sort of frother. The flotation separation of impurities from kaoline can be achieved by using both oleic acid and Aero 840 promotor as collectors within narrow acid limits(pH 2-3). Pine oil was more effective frother than MIBC with olelic acid as aa collector.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 1999년도 가을 학술발표회 논문집
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• pp.241-246
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• 1999

In this research, electrokinetic remediation test was experimented with contaminated kaoline specimen at below, above the cation-exchange capacity of the mineral. The changes of the flow in electro-osmosis with open electrodes and current were presented, and lead removal results were evaluated through the extraction test. As a result, it was showed that removal efficiency was 20-30%, 67-87% In the anode As lead transport continues, the lead precipitation within a narrow zone very close to the cathode can go significantly high. This high lead precipitation near the cathode could block the flow path, decrease the conductivity, and thus the electroosmotic flow. The net effect will cause a decrease in the efficiency of electrokinetic processing. Therefore, in this study, citric acid and surfactant solution was used at the cathode as enhancement techniques.

• 한국광물학회지
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• 제11권2호
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• pp.97-105
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• 1998

Weathering of biotite in Palgonsan granite was studied by using X-ray diffraction, optical microscopy, scanning electron microscopy, and electron probe micro analysis. Biotite altered to biotite/vermiculite regular mixed layer mineral (B/V) in the early stage of weathering. Although partially replaced by kaolinite with the progress of weathering. B/V is the major weathering product of biotite throughout the profile. During the formation of B/V, Mg, Fe and K are removed from a biotite layer to form a vermiculite layer by about 28%, 44% and 88%, respectively, whereas the Ti content is not changed. Considerable volume increase after the kaolinitization of B/V suggests that Al and Si are largely introduced from the external weathering solution. The silicate lattice templet of a weathering biotite facilitated the nucleation and growth of kaolinite. In the Palgongsan granite weathering profile, plagioclase weathered mostly into halloysite whereas biotite greatly contributes to the kaolinite crystallization though its small content in fresh rock.

• 한국광물학회지
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• 제14권1호
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• pp.58-72
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• 2001

The Cretaceous granite, andesite and sedimentary rocks are widely distributed in the northern Pusan area. The present study investigates mineralogical and geochemical charateristics of residual and cultivated soils derived from these rocks. The soils of granite area contain a large amount of quartz relative to clay minerals, whereas the soils of the andesite area contain more clay minerals than quartz. Clay minerals consist mainly of kaolin minerals illite hydroxy interlayered vermiculite interstratified mica/vermiculite and chlorite. Kaolin minerals are abundant in paddy soils while illite is abundant in less weathered soils. Si and K are major elements in the soils of granite area while Fe and Al in the soils of andesite area. In all the soils Ca, Mg and Na were generally depleted in comparison to those in parent rocks. Analysis data of trace element show that the enrichment pattern in soils depends on parent rock type with high oncentration of some elements over 100 ppm: Ba and Rb in granite area Zn, Bn, and V in andesite area, and Ba and V in sedimentary rock. In granite area, Rb and Th were greatly enriched in soil than in parent rocks. However, Cr, Ni and Sr commonly decrease, whereas Pb increases in all the soils. Exchangeable cation capacity(CEC) is relatively high in the soils of andesite are including abundant clay minerals. Collective evidences prove that the mineralogical and chemical compositions of soils are strongly dependent on the parent rock type. The mineralogy and chemistry of long cultivated soils are not significantly different from those of residual soils.

• 한국구조물진단유지관리공학회 논문집
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• 제15권1호
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• pp.215-225
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• 2011

메타카올린은 고령토나 카올린으로 알려진 카올린 광물의 풍화물로, 도자기 산업에 주로 사용되는 원료로, 일반적으로 메타카올린의 입자 크기는 시멘트보다는 작지만, 마이크로 실리카퓸보다는 크다. 본 연구에서는 콘크리트용 혼화재로 메타카올린을 사용한 콘크리트의 압축강도와 염소이온 투과저항 특성에 관한 영향에 관해 조사하였다. 메타카올린과 실리카퓸의 혼입률이 압축강도와 염소이온 투과저항에 주는 영향을 비교하기 위해 물-결합재비를 30%로 고정하고 각각 0, 5, 10, 15, 20%인 배합수준을 설정하여 비교하였다. 연구결과 메타카올린을 혼입한 콘크리트는 실리카퓸을 혼입한 콘크리트와 유사한 강도특성을 보였지만, 염소이온 투과저항성은 다소 불리한 것으로 나타났다. 따라서, 강도와 염소이온 투과저항 성능을 동시에 만족하기 위한 메타카올린의 혼입률은 10% 정도인 것으로 나타났다.

• 한국광물학회지
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• 제24권4호
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• pp.265-278
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• 2011

전남지역의 점토광상은 그 구성광물이 단사정계형 엽납석(pyrophyllite), 1T형 고령석(kaolinite)을 주로 하고 부구성 광물로서 견운모, 석영 및 장석류를 포함한다. 이들 점토광상은 유사한 시기에 유사한 성분을 가진 화산암류로부터 생성되었으며, 각 광상은 광물학적으로 엽납석과 고령석 중의 하나를 우세하게 포함하는 경향이다. 고령토 광상은 주로 다이아스포나 강옥을 포함하지 않지만, 광체 상부에 명반석을 흔히 포함한다. 반면에 강옥이나 다이아스포는 납석 광상에서 흔히 수반된다. 점토광체 상부의 규화응회암류와 응회암류 등 지질시대가 젊어짐에 따라 엽납석 및 고령석의 양은 감소하는 경향이며, 마침내는 나타나지 않게 된다. 반면에 견운모, 석영 및 사장석류는 미약한 상부층에서 흔히 나타난다. 대부분의 점토광체는 상단부에 저색 응회암층이 오고, 그 상부로는 규화대층, 응회암층, 그리고 최상부에 각력 응회암층이 온다. 화학성분 분석에 의하면, $Al_2O_3$는 중-저급의 점토광체뿐 아니라 응회암류에서도 다소 높게 나타내며, 그 이유는 응회암류의 주요 구성광물인 사장석 때문이다. 광체와 모암에서 $Na_2O$와 CaO는 비교적 낮은 함량을 나타내나, $K_2O$는 광체에서 좀더 낮게 나타난다. 점토의 작열 감량은 명반석이나 다이아스포를 포함하는 부분에서는 특히 높게 나타나는 것은 이들이 포함하는 $Al_2O_3$ 및 $SO_4$ 성분에 의한다. 희토류함량분석에 의하면, 경희토류가 중희토류보다 많이 포함되는 경향이며, 다소 미약하지만 부의 유러피움(Eu)이상대를 나타낸다. 대부분의 점토광체는 주로 유백-담회색의 미립이며 층리가 양호하여 야외에서 구분이 어렵지 않은 경우가 많지만, 괴상광체 등이 나타나는 곳에서의 효과적인 탐사를 위해서는 광체 상부 지층 중에서 확인되는 특징적 지층을 선정하는 것이 바람직하다. 전남지역에서 광체를 배태하는 층의 상단부에 연속성이 양호한 저색점토/응회암과 함께 그 상부로 층리와 연장성이 지극히 좋은 규화대가 확인되며, 광물조성 상으로도 광체 및 인근 지층과의 구분이 확실하므로 효과적인 점토광체 탐사를 위한 건층(key bed나 mark horizon)으로서의 역할이 가능하다.