• Journal of Environmental Science International
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• v.16 no.8
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• pp.929-939
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• 2007

Red mud is a waste generated by the aluminium industry, and its disposal is a major problem for this industry. Red mud has a reddish-brown color and superfine particle characteristics. So, it can be a promising pigment admixture for concrete industry. An experimental study was conducted to investigate the potential use of red mud in color concrete. The micro structures of red mud and iron oxide pigment such as porosity, pore size distribution, diameter of particle were analyzed with the aid of SEM, X-ray diffraction(XRD), and the infrared absorbance. Tests on physical properties of color concrete, such as strength, slump, early shrinkage crack patterns, and color characteristics were carried out and the results were reported in this paper.

• Proceedings of the Korean Society of Precision Engineering Conference
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• 2008.06a
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• pp.569-570
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• 2008

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.1 no.2
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• pp.59-72
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• 1996

The stratigraphy of the Gomso-Bay tidal flat consists of basement, preHolocene oxidized unit, and Holocene tidal sequence in ascending order. The oxidized unit is a yellowish brown stiff mud of the last stadial (or subglacial) stage before 12,000 yr B.P. This yellowish brown preHolocene unit does not contain any marine fossils, but contains plant roots, plant fragments, and also vertical and horizontal microfractures indicating soil-formation when exposed. It is regarded as interfluve deposits. The Holocene tidal sequence is composed of lower mud facies (upper-flat muds), upper sand and muddy sand facies (middle to lower-flat sands). This coarsening-upward and retrograding pattern of Holocene tidal deposits reflects a Holocene sea-level rise. The plots of $\^$14/C-age versus depth of dated samples (peats and shells) show that the sea level of 7,000 yr B.P. was located about 6.5 m below the present mean sea level, and the sea levels of 4,000 yr B.P. and 2,000 yr B.P. were also situated about 3 m and 2.5 m below the present mean sea level, respectively.

• Proceedings of the Korean Environmental Sciences Society Conference
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• 2008.11a
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• pp.482-487
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• 2008

성능이 우수한 다성분계 전극을 개발하기 위하여 Ru를 주 전극성분으로 Pt, Sn, Sb 및 Gd를 보조 전극성분으로 하여 3, 4성분계 전극의 성능과 산화제 생성량 및 전극 표면 분석을 행하여 다음의 결과를 얻었다. 1. 2분 동안 단위 W당 제거된 RhB 농토는 Ru:Sn:Sb=9:1:1 > Ru:Pt:Gd=5:5:1 > Ru:Sn=9:1 > Ru:Sn:Gd=9:1:1 > Ru:Sb:Gd=9:1:1로 나타났다. Ru:Sn:Sb=9:1.1 전극에서 발생하는 free Cl, ClO$_2$ 및 H$_2$O$_2$농도가 다른 전극보다 높은 것으로 나타나 산화제 생성경향과 RhB 분해율과는 상관관계가 있는 것으로 사료되었다. 4성분계 전극 중에서 Ru:Sn:Sb:Gd 전극의 성능이 가장 우수한 것으로 나타났으나 3성분계 전극인 Ru:Sn:Sb=9:1.1 전극보다 성능이 떨어지는 것으로 나타났다. Ru:Sn:Sb=9:1:1 전극에서 생성되는 산화제 농도가 다른 두 종류의 산화제 농도보다 높은 것으로 나타났고 4성분 전극의 경우 Ru:Sn:Sb:Gd 전극의 산화제 농도가 Ru:Sn:Sb:Gd 전극이 높거나 유사한 경우로 나타나 산화제 생성 경향과 RhB분해 능과는 상관관계가 있는 것으로 나타났다. 초기 RhB 분해 속도가 높은 전극의 COD 제거율도 높은 것으로 나타났다. OH 라디칼은 발생하지 않지만 염소계 산화제 농도가 높고 RhB제거율이 높아 Ru를 주 성분으로 한 전극의 RhB분해는 주로 간접 산화작용에 의한 것이며, 개발된 3, 4성분계 산화물 전극은 간접 산화용 전극임을 알 수 있었다. 에칭을 하기 전의 Ti판은 표면이 매끄러운 것으로 나타났으며, 35% 염산으로 에칭한 후의 Ti메쉬는 매우 거친 표면조직을 가지는 것을 관찰할 수 있었다. Ru:Sn:Sb=9:1:1 전극과 Ru:Sn:Sb:Gd 전극의 SEM 사진을 관찰한 결과 두 전극 모두 전극 물질이 균일하게 도포되어 있었으며, 두 전극 모두 열소성을 통해 전극 성분을 코팅할 때 발생하는 "mud crack"이 발생한 것이 관찰되었다 EDX 분석에서 Cl이 관찰되었는데, 전극 성분의 불완전 산화로 인한 비양론적 산화물 때문이며 이는 RhB 분해성능과 관련 있는 것으로 사료되었다.

• Journal of the Korean association of regional geographers
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• v.11 no.6
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• pp.517-529
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• 2005

Mt. Apsan is well known to be one of the most popular tourist sites around Daegu. Annually, more than 16 million persons visit Mt. Apsan. Although, in the mountain there are varieties of geomorphic and geological resources, there has been less concern to utilize the resources for geo-tourism. For example, there are about 10 valleys within Mt. Apsan and various landforms are scattered around the valleys. In this context, this study, based on field surveys centering around Gosangol valley, Anjiranggol valley and Dalbigol valley, focuses on exploring ways towards developing Mt. Apsan as an example geo-tourist site. The main findings are as follows: 1) The main landforms of Mt. Apsan include river cliff, cavern, free face, mud crack, ripple mark, fold, sheeting joint, talus, alluvial fan, pot hole, fault line, gnamma, columnar joint and metamorphic rock. 2) The guide notes on the landforms are developed. 3) In order to raise a learning effect of visitors on geomorphic resources, 9 nature trails are designed according to valleys and the length of visitor's stay.

• Explosives and Blasting
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• v.16 no.4
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• pp.29-39
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• 1998

A case study was made on in site vibration velocity data collected for two months in the construction area of the Daeduck cultural City Hall. Taegu The geology over the area shows distributions of weathered and some crack developed hornfels of mud-shale in the upper part, underlain by less weathered and hard compact quartzite. For the period of 2 months of blasting event, the vibration velocities were measured and these data were analysed for K and n for three different period the test period, first month and second month. The data for the test period show that K and n are 2464 and 1.621 with the cube root method, and 7154 and 1.791 with the sqare root one, respectively. The data for the first month collected mostly from blasting in the upper hornfels show that K and n are 1668 and 1,492 for the cube root and 1219 and 1,366 for the square root, respectively. Such a significant decrease in the K and n values from the test period through the first month for the weathered and comparatively well crack developed rocks hard and compact lower quartzite, may be due to difference in attenuation of waves propagating through physically different media. Therefore, for more effective safety design and blasting, it seems that it may be n to adopt appropriate K and n values, with getting lower step by step while proceeding the operation. In the meantime, the attenuation rate of K and n together with SD cross point for the cube and square root methods indicates that the cube root one appears to be more applicable than the square root for this area with limited distance(The maximum is 100m).

• The Korean Journal of Quaternary Research
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• v.16 no.2
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• pp.9-21
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• 2002

In Korea, many open-air upper palaeolithic sites are located at the river valley, particularly exposed in gently rotting terrain along the river course. They are situated at an altitude less trail 30 m above present river bottom, and covered with the blankets of slope deposits of several meters in thickness. The purpose of this research is to eluridate depositional and vegetational environment of the alluvial upper palaeolithic Jangheung-ri sites on the basis of analytical properties of grain size population, chronology, palynology, soil chemistry and clay mineralogy and magnetic susceptibility of the Jangheung-ri Quaternary formations. The lithostratograpy of Jangheung-ri sit is subdivided into 3 layers based on the depositional sequence and radiocarbon ages. From bottom to top, they are composed of slope deposits with lower paleosol layers, young fluvial sand and gravel with backswamp organic muds, and upper paleosol layers. The upper paleosol was formed under rather dry climatic condition between each flooding period. Dessication cracks were prevalent in the soil solum which was filled with secondarily minuted fragments due to pedogenetic process. The soil structure shows typical braided-typed cracks in the root part of cracking texture, and more diversified pattern of crackings downward. The young fluvial sand gravel were formed by rather perennial streams after LGM. The main part of organic muds was particularly formed after 15Ka. Local backswamp were flourished with organic muds and graded suspension materials in the flooding muds were intermittently accumulated in the organic muds until ca. 11Ka. This episode was associated with migration of Nam River toward present course. Organic muds were formed in backswamp or local pond. Abies/Picea-Betula with Ranunculaceae, Compositae, Cyperaceae were prevalent. This period is characterized with B$\Phi$lling, Older Dryas, Allerod, and Younger Dryas (MIS-1). Stone artefacts were found in the lower paleosol layers formed as old as 18Ka-22Ka. Based on the artefacts and landscape settings of the Jangheung-ri site, it is presumed that settlement grounds of old people were buried by frequent floodings of old Nam River, the river-beds of which were heavily fluctuated laterally and river-bed erosions were activated from south to north in Jangheung-ri site until the terminal of LGM9ca 17Ka).