• Title/Summary/Keyword: Expedition of CM

Search Result 3, Processing Time 0.018 seconds

Policy Plans for promoting the Construction Management in Korea (${\cdot}$${\cdot}$학 측면에서의 CM 활성화 정책과제)

  • Lee Pil-Won;Choi Jae-Ho
    • Proceedings of the Korean Institute Of Construction Engineering and Management
    • /
    • autumn
    • /
    • pp.563-566
    • /
    • 2002
  • This paper proposes the methods to promote the Construction Management (CM) in Korea from the perspectives of government, academia, and industry. Recent seminar reports and research documents were referred to provide important sources for this work added by years of author's own experience in construction industry. First, the expected trend of various CM forms over time was identified by referencing the needs assessment results accomplished by the other researchers to provide a general sense of the way the CM is expected to evolve. Then, the 16 detailed ways of promoting the CM in Korea was proposed and explained.

  • PDF

New Record of Karoowia saxeti (Stizenb.) Hale in South Korea

  • Lim, Kwang-Mi;Yamamoto, Yoshikazu;Harada, Hiroshi;Lee, You-Mi;Koh, Young-Jin;Hur, Jae-Seoun
    • Mycobiology
    • /
    • v.34 no.3
    • /
    • pp.148-150
    • /
    • 2006
  • Karoowia saxeti was recorded during the lichen field expedition in southern part of Korea in 2006. The lichen was found on the rock surface along coastal line. This species was easily recognized by chemistry (K+ yellow) and the presence of isidia. Thallus was saxicolous, subcrustose, more or less lobate at the center with clearly lobed margins, $2{\sim}6\;cm$ broad and pale yellowish green. Thalli lobes were irregular, variable, up to 1.0mm wide, not branched, flat to more or less convex and contiguous to subimbricate. Upper surface of the thalli was continuous, emaculate, moderately isidiate. The isidia was subglobose to cynlindrical, darkening at the tips and unbranched. Low surface of the thalii was black with a spongy rhizoidal and lamellar layer. HPLC analysis proved the presence of stictic acid (K+ yellow), norstictic acid and usnic acid. This is the first record of the species in South Korea.

Variations in Morphological and Geochemical Characteristics in Manganese Nodules from the East Siberian Arctic Shelf with Varying Water Depths (동시베리아해 대륙붕에서 산출되는 망가니즈단괴의 수심에 따른 형태학적·지화학적 특성 변화)

  • Hyo-Jin Koo;Hyen-Goo Cho;Sangmi Lee;Gi-Teak Lim;Hyo-Im Kim
    • Economic and Environmental Geology
    • /
    • v.56 no.1
    • /
    • pp.1-11
    • /
    • 2023
  • In this study, we explore the morphological and geochemical characteristics for 440 manganese nodules collected from two different water depths [ARA12B-St52 (150 m, n = 239) and ARA12B-St58i (73 m, n = 201)] on the continental shelf of the East Siberian Sea from the ARA12B expedition in 2021. We also discussed the variations in the characteristics of manganese nodules with varying water depths in the Arctic Sea. The sizes of the nodules are generally greater than 3 cm at both sites. However, there is an obvious difference in the morphology with water depths. For the nodules collected at 150 m, brown-black colored tabular, tube, and ellipsoidal shapes with a rough surface texture are dominant. On the other hand, yellow-brown tabular shapes with a smooth surface texture are common for the nodules collected at 73 m. Furthermore, the slope of trend line between size and weight is significantly different at both sites: particularly, the slopes of nodules at 150 and 73 m are 1.60 and 0.84, respectively. This indicates the difference in the internal structure, porosity, and constituting elements between both nodules. Micro X-ray Flourescence (µ-XRF) results clearly demonstrate that the internal textures and chemical compositions are different with water depths. The nodules at 150 m are composed of a thick Mn-layer and a thin Fe-layer centered on the nucleus, while the nodules at 73 m are alternately grown with thin Mn- and Fe- layers around the nucleus. The average chemical compositions obtained by µ-XRF are 40.6 wt% Mn, 5.2 wt% Fe, and 7.9 Mn/Fe ratio at 150 m, and 10.3 wt% Mn, 19.0 wt% Fe, and 0.6 Mn/Fe ratio at 73 m. The chemical compositions of the nodules at 150 m are similar to those of nodules from the Peru Basin in the Pacific Ocean, while the compositions of the nodules at 73 m are similar to those of nodules from the Cook Islands or the Baltic Sea. The observed morphological and geochemical characteristics of the nodules show a clear difference at the two sites, which indicates that the aqueous conditions and formation processes of the nodules in the Arctic Sea vary with the water depths.