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이광춘,김세현,이승호,서용찬 대한자원환경지질학회 2003 자원환경지질 Vol.36 No.1
동명광산을 경유하는 수계의 pH는 5.9∼7.1의 변화를 보여 약산성 내지는 중성의 환경을 보인다. 하천수 중 중금속 원소함량의 분포는 자원소의 지구화학적 특성에 따라 다양한 분포 양상을 보이나 전반적으로 폐광산 주변에서 증가하는 경향을 보인다. 동명광산 지역의 광미, 폐석적치장토양, 농경지토양에 대한 성분분석 결과 농경지토양에는 중금속의 총 농토가 광미나 폐석적치장의 토양보다 훨씬 낮았을 뿐 아니라 총 중금속 농도 중 adsorbed, carbonate, reducible fraction들이 차지하는 비율이 낮아 이들이 농작물이나 주변 수계에 큰 영향을 미치지 못할 것으로 생각된다. 그러나 하천수중 중금속 원소함량 분포가 전반적으로 광산지역에서 증가하는 경향을 보이며, 광미나 폐석적치장 토양에서도 중금속의 총 농도가 매우 높았을 뿐 아니라 adsorbed, carbonate, reducible fractions들이 차지하는 비율이 농경지 보다 상대적으로 높았기 때문에 이들이 유실되거나 또는 산성우, 산성인 광산폐수의 유입 등으로 인해 화학적 환경변화가 발생할 경우 중금속 오염의 확산이 우려되므로 이에 대한 오염방지대책이 필요하다고 생각된다. Researches were carried out to investigate the characteristics and concentration of heavy metal elements of stream water through Dongmyoung abandoned metal mine and soil adjacent to the mine. The pH range of water was 5.9∼7.1 that implies the water environment was acidic to neutral. The contents and distribution aspects of heavy metals in water samples varied with geochemical characteristics of element, but the concentration of heavy metals has the tendency of increase closer to the mine in general. The results of soil analysis show that total heavy metal concentration of agricultural soil near mine was far lower than those of ore tailing and dumping site. Therefore, the effects of the abandoned mine on stream water and agricultural products were supposed to be insignificant, particularly because the portion of absorbed carbonates and reducible fractions among total heavy metal concentration was relatively lower than the other. Since, however total heavy metal concentrations of mining site were relatively higher than those of adjacent region, there is a possibility of heavy metal difussion when the chemical environment of the site changes due to migration of surface and underground water. It is suggested that the preventive measures for water and soil pollution by the heavy metals would be considered around the region.
이광춘,이지숙,김경환,박준석,신동운,김훈,박준민,김현종,신희준,전우찬 대한응급의학회 2017 大韓應急醫學會誌 Vol.28 No.4
Purpose: Falling is one of the most common causes of injury for preschool children. Here, we aim to identify the characteristics and risk factors of injuries by falling-down in preschool children. Methods: Between January 2010 and December 2011, we enrolled patients under the age of 7 years, who were injured by falling down and visited an urban regional emergency center. We retrospectively surveyed the medical record of these patients, including age, sex, place and height of fall, type of floor, guardian’s witness, traumatic brain injury (TBI), and fracture of extremities. Results: The odds ratios sex (male), age (under 2 years old), height of fall, type of floor (hard), and guardian’s witness (presence) that resulted in TBI were 1.35 (95% confidence interval [Cl], 0.72?2.55; p=0.352), 3.83 (95% Cl, 1.78?8.65; p<0.05), 6.38 (95% Cl, 3.27-12.44;p<0.05), 3.58 (95% Cl, 0.47-27.30; p=0.218), and 1.47 (95% Cl, 0.63-3.43; p=0.377), respectively. The odds ratios sex (male), age (over 2 years old), height of fall, type of floor (soft), and guardian’s witness (absence) that resulted in fractures were 1.19 (95% Cl, 0.78-1.81; p=0.433), 3.10 (95%Cl, 1.99-4.84; p<0.05), 1.98 (95%Cl, 1.19-3.29; p<0.05), 2.41 (95% Cl, 1.29-4.54; p<0.05), and 1.15 (95%Cl, 0.72-1.85, p=0.554), respectively. Conclusion: In preschool children who experienced an injury from falling down, TBI was increased with younger patients and higher height of fall, but it was not related with patient’s sex, type of floor, and guardian’s witness; conversely, fractures were increased with older patients, higher height of fall, and soft floor, but not related with patient’s sex and guardian’s witness.
의성소익지(義城小益地) 신동층군(新洞層群)의 퇴적암석학(堆積岩石學) 및 퇴적환경(堆積環境)
이광춘,Lee, Kwang-Choon 대한자원환경지질학회 1985 자원환경지질 Vol.18 No.3
Sedimentary petrology and depositional environments of the Sindong Group, consisting of in ascending order the Nagdong, Hasandong and Jinju Formations, in the Euiseong Subbasin are studied. For these, the Sindong sequence over 1,000m thick is measured at the scale of 1:200 and 36 thin sections of sandstones of the Hasandong Formation are studied under the polarizing microscope. In addition, published paleontologic data are incorporated in the sedimentologic interpretation. Most of the sandstones are classified as arkose. They are moderately sorted, near symmetrical to fine skewed and mesokurtic. Relationship between the textural parameters suggests a fluviatile environment of the Hasandong Formation. The Sindong fauna and flora also indicate non-marine depositional environments. Sedimentologic data of the measured sections show that the Sindong Group is made up of from the bottom an alluvial fan (lower part of the Nagdong Formation), a fluvial plain (upper part of the Nagdong Formation and the Hasandong Formation) and a fluvial/lacustrine (the Jinju Formation) deposits.