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이호왕(李鎬汪),이평우,성인화(成仁華),백락주(白樂柱),김용상(金容商) 대한바이러스학회 1981 Journal of Bacteriology and Virology Vol.11 No.1
The name reovirus is sigla, short for respiratory enteric orphan, because these viruses are found in both the respiratory and enteric tracts of man but in general are orphans in the sense that they have not been associated with human disease. However, in 1973 a new reovirus was discovered which is in fast the major etiologieal agent of infantile enteritis. The genus Reovirus contains 3 mammalian serotypes which share a cammon CF antigen but are distinguishable by neutralization or HI tests. Reovirus was isolated for the first time in Korea and summary of the results are as follows: 1. Four strains of unknown virus were isolated from spleen and lymphnodes of Apodemus agrarius coreae and Microlus fortis pelliceus collected in the endemic foci of Korean hemorrhagic fever. 2. Chemieo-biologie properties of the isolated virus were; a) hemagglutination was occurred with only human red blood cells b) optimum pH for hemagglutination was 7.6 c) the nucleic acid of the virus component was RNA and d) it was insensitive to chloroform. 3. The viruses were identified as Reovirus type 2 by hemagglutination inhibition and tissue culture neutralization test using standard antisera of Reovirus type 1, 2 and 3. It was concluded that Reovirus type 2 was isolateu from rodent tissues for the first time in Korea.
이호 회계사의 세금칼럼 - 출산.입양 시 연 200만 원 추가로 소득 공제
이호,Lee, Ho 한국주택협회 2008 주택과 사람들 Vol.224 No.-
해마다 연말이 되면 13번째 월급이라 불리는 연말 정산이 기다리고 있다. 연말 정산 관련 규정은 매년 약간의 개정 사항이 생긴다. 이에 따라 개정 사항을 일목요연하게 정리해 본인에게 해당 사항이 있는지 살펴봐야 혜택을 놓치지 않고 챙길 수 있다. 이번 호에서는 올해부터 바뀌는 연말 정산 관련 사항에 대해 알아보자.
이호 회계사의 세금 칼럼-1세대 1주택 양도세 비과세 충족 요건 제대로 알기
이호,Lee, Ho 한국주택협회 2007 주택과 사람들 Vol.210 No.-
친지 또는 이웃들과 양도소득세 관련 세금 상담을 하다 보면 재건축한 주택의 경우 1세대 1주택 비과세 요건을 충족했음에도 이를 잘 알지 못해 제때 집을 팔지 못하고 재건축일로부터 다시 3년을 채우느라 기다리는 경우를 종종 보게 된다. 1세대 1주택 비과세 요건 보유기간 3년은 다음과 같이 계산하므로 이를 잘 활용한다면 주택을 양도하기 위한 의사 결정을 하는 데 도움이 될 것이다.
우포늪의 홀로세 동안 퇴적환경 변화 및 돌말류 분포 특성
이호일,이상득,이진영,임재수,권대률,박미례,윤석민 한국하천호수학회 2020 생태와 환경 Vol.53 No.2
Upo Wetland is the largest riverine wetland in Korea which has been inscribed on the Ramsar List of Wetlands of International Importance in 1998. In this study, sedimentological study was carried out in order to understand the environmental changes in Upo Wetland during the Holocene. The drilling work for recovering the Quaternary sediments was conducted on the inner part (UPW17-01, UPW17-02, and UPW17-03) and the outer part (UPL17-01, UPL17-02) of the Upo Wetland. The recovered sediments are commonly characterized by gravel-dominated deposits in the lower part and silty clay-dominated deposits in the middle to upper parts respectively, which are seemed to be changed from fluvial to palustrine/lacustrine environments around 4,000 cal yr BP. In order to establish the Holocene diatoms distribution from Upo Wetland, we identified 63 diatom taxa. Of these, 14 species were new records for Korea: Gomphonema consector, Gomphonema jadwigiae, Hantzschia abundans, Luticola pseudomurrayi, Luticola spauldingiae, Neidium suboblongum, Ninastrelnikovia gibbosa, Oricymba rhynchocephala, Pinnularia borealis var. lanceolata, Pinnularia latarea, Pinnularia paliobducta, Pinnularia saprophila, Sellaphora laevissima, Stauroneis pseudoschimanskii. All identified diatom species are illustrated by high-quality scanning electron microscopic and light microscopic microphotographs. The ecological habitat for all taxa are presented.
이호일,백인성,강희철,천종화 한국지질과학협의회 2014 Geosciences Journal Vol.18 No.2
Soft-sediment deformation structures (SSDS) are examinedin the late Pleistocene marine terrace deposits of the southeasterncoast of the Korean Peninsula. The marine terrace deposits areexposed in thicknesses of more than 10 m, and consist of lagoon,foreshore to backshore, coastal dune, and foreshore to backshoredeposits in ascending order. The SSDS are restricted to the coastaldune deposits and the upper part of the underlying foreshore tobackshore deposits, and are grouped into ductile and brittle deformationstructures. The ductile deformation structures include irregularlaminations, compacted laminations in the hinge zone of folds,asymmetric folds of foreset laminae, and water escape structures. The brittle deformation structures include syndepositional faultsor deformation bands. The most probable triggering mechanismfor the SSDS is liquefaction by moderate-magnitude earthquakes(M = 5–5.5). Likely, the SSDS were generated over time in variousstress fields, including those of main shocks, aftershocks, and laterseismic events. The evolution of the SSDS-bearing deposits in thestudy area can be summarised as follows: 1) rising of the groundwatertable in the coastal dune deposits as a result of seismic shock,2) formation of SSDS by liquefaction in the lower part of the dunedeposits and upper part of the underlying foreshore to backshoredeposits, 3) descending of the groundwater table, and 4) depositionof foreshore to backshore deposits on the SSDS-bearing dune depositswith erosion of the top of the dune deposits.