• 한국콘크리트학회:학술대회논문집
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• 한국콘크리트학회 1999년도 학회창립 10주년 기념 1999년도 가을 학술발표회 논문집
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• pp.267-270
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• 1999

In this paper, the application of limestone powder, which produced by being gathered electrically in the process of manufacturing of cement, to high fluidity concrete are investigated. According to the experimental results, especially, high viscosity and the loss of air content are accomplished by applying limestone powder as the partial substitution of fine aggregates. In case of hardened concrete, high compressive strength can be achieved by using limestone powder.

• 한국환경과학회지
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• 제15권6호
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• pp.587-592
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• 2006

The advantage of CFBC(Circulating fluidized bed combustor) is that it can apply to various fuel sources including the lower rank fuel and remove SOx by means of direct supply of limestone to the combustor without additional desulfation facility. In this paper, we denote characteristics of fly and bed ash to reuse finer limestone usually abandoned(used spec[Coarse LS] 0.1mm under 25%, new spec[Fine LS] 0.1mm under 50%). According to the results, the chemical composition of fly ash was as follows; $SiO_2\;40.8%,\;Al_2O_3\;31.9%,\;CaO\;10.7%,\;K_2O\;4.46%$ in the case of coarse limestone and $SiO_2\;41.1%,\;Al_2O_3\;31.3%,\;CaO\;10.9%,\;K_2O\;4.66%$ in the case of fine limestone. The chemical composition of bed ash was as follows; $SiO_2\;54.2%,\;Al_2O_3\;33.1%,\;CaO\;1.56%,\;K_2O\;4.34%$ in the case of coarse limestone and $SiO_2\;53.8%,\;Al_2O_3\;32.6%,\;CaO\;2.21%,\;K_2O\;4.45%$ in the case of fine limestone. It showed that there was no significant change in chemical composition. And it is conformed that there was no significant change in particle size and shapes.

• 자원환경지질
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• 제10권1호
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• pp.19-35
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• 1977

The study area is located in between Hacheonri and Weolgulri, Jecheon-gun where the formations of Okcheon group and Chosun group come in contact and the stratigraphy and geological age of the Okcheon group have been debated among previous workers. The dolomitic limestone which distributed at Cheongam and Dumusil is clarified as the Hyangsanri dolomite formation and the quartzite distributed at Cheongam and Howeunri as Taehyangsan quartzite formation. The newly named Soorumsan schist interbedded in the Great Limestone Series was previously classified Seochangri formation. It is also classified that the formation formerly named as Seochangri was divided into newly named Manji schist which seems to be correlated to Kemyeongsan and Munjuri formation. The formation formerly named as Buknori is clarified as Hwanggangri formation. The Samtaesan formation has been clarified as the lower and upper limestone beds which belong to the Great Limestone Series. The area divided into two groups, that is, Okcheon system of Pre-cambrian age occupies western part and the Great Limestone Series of Chosun system of Cambro-Ordovician age eastern part of this area. Okcheon system consists in ascending order of Manji schist, Hyangsanri dolomite, Taehyangsan quartzite, Munjuri schist, and Hwanggangri formation of meta-tillite. The Great Limestone Series of Chosun group consists in ascending order of lower limestone, Soorumsan schist, Hoosanri quartzite and upper limestone formations. Busan augen gneiss seems to be igneous origin. Unmetamorphosed shale interbed can be traced in the Soorumsan schist. Previous study (Kims, 1974) reveals that meta-volcanic rocks are distributed from south to north along contact zone of the Okcheon and Chosun groups, and it has been confirmed that the meta-volcanics crop out continuously from the adjacent southern quardrangle into the southern part of the area studied, intruding along the fault zone between the Okcheon and Chosun groups which seems to be upthrust as in the area south. This evidence coincides with Kims' work (1974) which states that the Precambrian Okcheon group is largely overturned and thrusted over the Chosun group.

• 자원리싸이클링
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• 제24권5호
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• pp.3-14
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• 2015

청정석탄발전기술 중 하나인 순환유동층보일러(CFBC) 기술의 고도화에 따라 국내외 로내탈황 기술개발 현황과 국내외 유동층보일러용 석회석의 탈황특성 연구현황을 조사하였다. 석회석계 탈황제는 고온탈황특성이 우수한 원소 중 하나로 $850-950^{\circ}C$ 내외에서 최적의 탈황특성을 가지고 있다. 그리고, 탈황시험방법에 따라 흡수제 표면의 격막의 확산반응, 입자의 크기, 기공의 수량, 크기 및 구조에 의한 탈황공정의 효율성을 결정할 수 있다. 2015년 이후 대형 순환유동층형발전소의 본격적인 가동에 따라 석회석의 광상학적, 결정학적 특성 및 소성특성과 연계된 추가적인 연구가 필요한 것으로 사료된다.

• 자원리싸이클링
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• 제24권6호
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• pp.38-44
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• 2015

동해-삼척지역 석회석을 활용하여 습식배연탈황공정기술에 대한 적용성을 검토하기 위해 석회석의 물리화학적 특성이 탈황성능에 미치는 영향을 연구하였다. 실험은 ASTM 표준 시험방법인 염산적정법을 적용한 실험실 규모의 실험 장치를 이용하여 총중화능력을 측정하였다. 실험결과 총중화능력은 CaO 함량 등의 화학성분 보다 입자크기의 물리적 특성에 더 큰 영향이 있음을 알 수 있었으며, 입자크기가 미립화 될수록 총중화능력의 값은 높아지는 것으로 확인되었다.

• Journal of Forest and Environmental Science
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• 제32권3호
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• pp.237-252
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• 2016

Improved knowledge of the environmental factors affecting the natural regeneration of tree species in limestone forest is urgently required for species conservation. We examined the environmental factors and tree species characteristics that are important for colonization in diverse forest stands growing on a limestone hill in northern Thailand. Our analysis estimated the relative influence of forest structure and environmental factors on the regeneration traits of tree species. We established sixty-four $100-m^2$ plots in four forest stands on the limestone hill. We determined the species composition of canopy trees, regenerating seedlings, and saplings in relation to the physical environment. The relationships between environmental variables and tree species abundance were assessed by canonical correspondence analysis (CCA), and we used generalized linear mixed models to examine data on seedling/sapling abundances. The CCA ordination indicated that the abundance of tree species within the mixed deciduous forest was closely related to soil depth. The abundances of tree species growing within the sink-hole and hill-slope stands were positively related to the extent of rocky outcropping; light and soil moisture positively influenced the abundance of tree species in the hill-cliff stand. Physical factors had a greater effect on tree regeneration than did factors related to forest structure. Tree species, such as Ficus macleilandii, Dracaena cochinchinensis, and Phyllanthus mirabilis within the hill-cliff or sink-hole stand, colonized well on large rocky outcroppings that were well illuminated and had soft soils. These species regenerated well under conditions prevailing on the limestone hill. The colonization of several species in other stands was negatively influenced by environmental conditions at these sites. We found that natural regeneration of tree species on the limestone hill was difficult because of the prevailing combination of physical and biological factors. The influence of these factors was species dependent, and the magnitude of effects varied across forest stands.

• 자원환경지질
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• 제3권1호
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• pp.17-24
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• 1970

The purpose of this report is to prepare a data for the economic evaluation on the Goobong Limestone Mine which is located at the south-eastern corner of the Yongchun Quadrangle scaled in 1:50,000. The accessibility from the mine to railroad was considered in two ways. One is to Dodam Station on Central Railway Line and the other is to reach Songjung-ni village which is near Sangyong Station on Hamback Railway Line. The distance of the former way is 26.7km and the later is 24.2km. Geologically the mine is situated near the base of the Greast Limestone Series which strikes generally $N25^{\circ}{\sim}30^{\circ}E$. The series comprises six different formations from older to younger; Pungchon Limestone Formation and Whajol Formation of Cambrian age, and Dongjum Quartzite Formation, Dumudong Formation, Maggol Limestone Formation and Goseong Formation of lower to middle Ordovician age. 82 samples; 48 from Pungchon Limestone Formation, 11 from Dumudong Formation, 15 from Maggol Limestone Formation and 8 from Goseong Formation, were taken from the series in the crossed direction to the general trend of the series as shown in geological map. They were chemically analyzed on the components of CaO, MgO, $SiO_2$, $R_2O_3(Al_2O_3+Fe_2O_3)$ and ignition loss as shown in table 2, table 3, table 4, and table 5. As seen from the tables, among the formations of the series, middle to upper parts of the Pungchon Limestone Formation and middle and upper parts of the Dumudong Formation have chemical composition as available source for the raw material of cement industry, not only that but also the part of the Pungchon Formation was highly evaluated as source for the flux of iron smelting and the raw material of carbide manufacturing because of its high purity of calcium carbonate.

• 자원리싸이클링
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• 제3권3호
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• pp.27-31
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• 1994

포항제철소에서 발생되는 석회석슬러지의 유효이용의 일환으로 포틀랜드 시멘트 혼합재로서 첨가반응효과에 대한 연구를 행하였다. 즉 포틀랜드 시멘트-석회석슬러지계 경화체에 관하여 수화반응속도, 비증발 수분량, 압축강도등의 실험을 통해 포틀랜드 시멘트-석히석 슬러지계에서의 슬러지 미분말 첨가반응효과에 대하여 실험을 하였다. 석회석슬러지를 10% 첨가한 계에서는 포틀랜드 시멘트 단독의 경우와 별차이가 없으나 5% 첨가계에서는 수화 반응속도가 크게 나타났으며 이는 석회석슬러지의 미분말 효과의 영향으로 사료된다. 한편 경화 시멘트 페이스트의 압축강도는 석회석슬러지 5% 첨가한 계에서 약간 높게 나타났으며 물성도 좋게 나타났다. 수화반응물은 주로 $Ca(OH)_2$와 칼슘실리케이트 수화물이며 석회석슬러지를 첨가한 계의 28일 시료에서는 calcium carbonate hydrate가 생성되었다.

• 공업화학
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• 제32권2호
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• pp.190-196
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• 2021

저품질 석회석의 탈황 성능 개선을 알아보기 위해 초산, 젖산, 개미산 등 3종의 유기산 첨가제를 사용하여 기포형 반응기에서 탈황 반응을 수행하였다. 유기산이 첨가되지 않은 석회석 슬러리는 pH 5.2 이하에서 초기 탈황 효율의 저하가 일어났다. 반면, 유기산이 첨가된 석회석 슬러리는 pH 4.2~4.5에서 안정된 초기 탈황 효율을 나타내었다. 슬러리 pH 4 이하에서 유기산이 첨가된 석회석 슬러리의 탈황 성능은 유기산의 해리에 의해 생성된 음이온의 양과 연관될 수 있다. 슬러리 중 유기산의 음이온 양이 많으면 슬러리 pH의 완충 기능 저하가 급격히 일어나지 않았다. 이와 같은 결과들은 유기산의 산성도 및 해리도에 기인하였다. 3종의 유기산 첨가에 따른 저품질 석회석 슬러리의 탈황 성능 증가율은 초산(2.6%) < 젖산 (6.4%) < 개미산 (16.7%) 순으로 나타났다.

• International Journal of Concrete Structures and Materials
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• 제4권2호
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• pp.105-108
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• 2010

In order to determine the effect of the use of limestone sand on chloride ion ingress in mortar, specimens were cast with two different sands: siliceous sand (used as reference) and limestone crushed sand (used for this study). To compare and assess the resistance of this mortar to chloride penetration, two different diffusions tests were employed: slow migration and rapid migration (AASHTO test). In this study, calculation of the effective diffusion coefficient is proposed using a model based on Nernst. Planck equation. The diffusion coefficients from each sample were compared. The results for all tests show that the diffusion coefficients for siliceous sand mortar are larger than those obtained with limestone sand. It appears also that the diffusion coefficient varies as a function of the W/C ratio.