• Title/Summary/Keyword: 추가령

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포장과 법률 - 제품의 포장재질·포장방법에 관한 기준 등에 관한 규칙

  • (사)한국포장협회
    • The monthly packaging world
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    • s.342
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    • pp.104-107
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    • 2021
  • 환경부는 '제품의 포장재질·포장방법에 관한 기준 등에 관한 규칙'(약칭 : 제품포장규칙) 일부개정령을 9월 10일 공포했다. 이번 개정령은 제품의 포장재질·포장방법에 관한 기준 등을 지켜야 하는 제조자 등이 이를 위반한 것으로 인정되는 경우, 제품의 포장방법과 포장재의 재질에 관한 검사를 신속하게 받을 수 있도록 해당 검사를 수행하는 전문기관에 한국환경산업기술원을 추가하는 것을 주요 내용으로 하고 있다. 다음에 그 상세내용을 살펴보도록 한다.

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서울.경기 지역의 지질 및 지반특성

  • 김명모
    • Proceedings of the Korean Geotechical Society Conference
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    • 2004.03a
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    • pp.176-187
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    • 2004
  • 서울ㆍ경기지역은 한반도의 서부중앙지역으로 동경 126$^{\circ}$와 127$^{\circ}$, 북위 36$^{\circ}$와 38$^{\circ}$ 사이에 위치해 있으며, 면적은 서울 605$\textrm{km}^2$, 경기도 10,184$\textrm{km}^2$를 차지한다. 북쪽으로는 휴전선, 서쪽으로는 서해, 동쪽으로는 강원도, 남쪽으로는 충청도와 접하고 있으며 한강에 의해 남북지역으로 나뉘어져 한 수 이북은 산간지역이 한 수 이남지역에는 평야지대가 발달하고 있다. 지형은 대체로 추가령 구조곡을 경계로 북부산지와 남부산지로 나누어지는데, 북부는 중국 요동방향의 마식령산맥, 남부는 중국방향의 광주산맥과 차령산맥이 각각 그 골간을 이루고 있으며, 서쪽해안에 가까워질수록 고도가 낮아져 평야나 구릉성 산지로 바뀐다.(중략)

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우리 나라 동굴의 지질과 환경 보전

  • 정창희
    • Proceedings of the Speleological Society Conference
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    • 1996.09a
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    • pp.64-64
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    • 1996
  • 석회동굴은 카르스트 지형 지역에서 지하 형성물로 나타나는 공동지역으로, 이 공동화된 공간에 2차적으로 석순, 석주, 종유석 등이 침전되어 생긴 동굴이다. 이런 카르스트 지형은 석회암 지층에서 용식작용으로 생겨나는데, 우리나라에서는 북쪽은 평안남도 동반지역과 함경남도의 남부서경지역, 황해도 서남부, 그리고 강원도 남부지역, 추가령 구조곡의 일부들이 해당한다. 그리고 남쪽은 문경 - 단양 - 제천 - 영월 - 평창 - 정선 - 삼척 - 강릉에 걸친 지역들이다. 따라서 우리나라의 석회암동굴들은 그 대부분이 조선계 대석회암통의 막동 석회암 층에 분포되고 있다.(중략)

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새로운 전자파장해관련 기준 제.개정 EMI기준강화 및 EMS기준 추가

  • Gang, Deok-Geun
    • 정보화사회
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    • s.108
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    • pp.16-20
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    • 1996
  • 우리나라의 전자파장해검정제도는 국내의 전자파 환경보호를 위해 '89.12.30 법률 제 3686호로 전파법을 개정하고, 그 이듬해인 '90.9.3 전자파장해(EMI: Electro Magnetic Interference)기준과 장해검정의 대상기기.방법 및 절차 등을 규정한 전자파장해검정규칙을 체신부령 제825호로 제정하고, '90. 11월 모뎀 및 팩시밀리 등 9개의 유선통신단말기기에 대한 장해검정을 시작으로 최초 도입되었다.

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Drainage Derangement and Revision by the Formation of Cheolwon-Pyeonggang Lava Plateau in Chugaryeong Rift Valley, Central Korea (추가령 열곡의 철원-평강 용암대지 형성에 따른 하계망 혼란과 재편성)

  • Lee Min-Boo;Lee Gwang-Ryul;Kim Nam-Shin
    • Journal of the Korean Geographical Society
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    • v.39 no.6 s.105
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    • pp.833-844
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    • 2004
  • In Chugaryeong rift valley, lava plateau formation by the fissure eruption had vanished original landforms and effected on drainage derangement and revision. 4 rivers including Namdae-cheon, Bukhan-gang, Imjin-gang and Hantan-gang watersheds have shared Cheolwon-Pyeonggang lava plateau, that is, ownerless watershed. Main agency of the dividing process are central-eruption volcanic peaks such as Orisan(453m) and 680 Peak. Especially, Orisan has played the role of divide point for 4 watersheds. In the lower-relief plateau zone, complex drainage system have caused continually river capture between neighboring watersheds. In more elevated range slope, river capture have proceeded to headward erosion. Hydrogeomorphologically, lava-filled valley has initiated decrease of the original size of flood plain, maybe, causing higher capability of inundation by heavy rains, and then more active dissection of lava plateau layer.

Stratigraphic Analysis on Paleofluvial Outcrop underJeongok Basalt Layer in the Chugaryeong Rift Valley, Central Korea (추가령 열곡 내 전곡 현무암층 하부 고하성층 노두 층서 분석)

  • Lee, Min-Boo;Lee, Gwang-Ryul
    • Journal of The Geomorphological Association of Korea
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    • v.20 no.3
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    • pp.55-63
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    • 2013
  • The study deals with the geochemical analyses on the stratigraphy and sedimentation of the paleofluvial outcrop under Jeongok basalt layer in Chugaryeong Rift Valley. The results of field survey and analysis show that the paleofluvial sand and gravel layers had been constructed before the arrival of basaltic lava in Jeongok area of Hantan River valley in central Korea. XRF, for the main elements analysis, results present that JG2-3, a test sample from basalt weathering layer, has different characteristics from 5 other samples in the aspects of chemical weathering levels. ICP-MS, for analysis of the rare earth elements analysis, estimates that gravel layer, in the lowest part of the outcrop, had been originated from pre-lava bedrocks near the upper reach of the Hantan River, so the layer is almost not related to basalt layers. Finally, the OSL dating results in paleofluvial sedimentation had been in process until nearly 40,000 BP, before formation of lava plateau in the Jeongok area.

Reports on bionomical characteristics of Mellicta ambigua (여름어리표범나비(Mellicta ambigua (Menetries))의 생태적 특성에 관한 보고)

  • Kim, Se-Gwon;Nam, Gyoung-Pil;Kim, Nam-Ee;Bae, Kyoung-Sin;Choi, Young-Cheol;Lee, Sang-Hyun
    • Journal of Sericultural and Entomological Science
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    • v.52 no.2
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    • pp.110-116
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    • 2014
  • Recently the number of the butterflies, Mellicta ambigua, had been decreasing rapidly, and already disappeared at many habitat. In this studies, we investigated ecological environment of Mellicta ambigua for preparing of primary research data recovering habitat, and studied on bionomical characteristics. Two different habitat, Jindo and Inje, were selected for investigation of ecological environment. We investigated four times during 3-month, from June to August in 2012. In Jindo, we observed more than 100 butterflies and a lot of host plants, Melampyrum roseum var. japonicum. But only 5 butterflies and only a few host plants, Veronicastrum sibiricum were observed in Inje. We could not observe the eggs, the larva and pupa on the host plants at all. For finding of bionomical characteritics, we reared butterflies at natural conditions. Collected 3-female butterflies from Jindo laid 465 eggs on the leaves of 3-host plants, Veronicastrum sibiricum. 120 ~ 186 eggs per each female were laid in the shape of cluster. An egg was globular shape, 0.6 mm diameter and 0.7 mm height. The egg periods were $9.96{\pm}0.4days$ after ovipositioning, and the hatchability was 95.% at natural condition. The larval periods were $4.1{\pm}0.6days$ (1st instar), $2.1{\pm}1.0days$ (2nd), $8.1{\pm}0.7days$ (3rd), $239.2{\pm}10.9days$ (4th), $12.3{\pm}1.3days$ (5th), $17.1{\pm}1.1days$ (6th), $10.5{\pm}1.0days$ (7th) each other. The larva of 4th instar overwintered in the nest that had been made into the leaf of host plant with secreted thread as a group until early March next year. In the early March next year, overwintered larva went around their nest in search of host plants, and went to other host plants, Veronica persica and Plantago asiatica, sometimes. The overwintered larva of Mellicta ambigua could grow up on two other host plants normally. In the following experiment, the butterflies of Mellicta ambigua laid eggs on the leaves of Plantago asiatica, but the 1st instar larva from eggs died all. The headwidth of each developmental larval stage were $0.28{\pm}0.02mm$ (1st), $0.45{\pm}0.02mm$ (2nd), $0.58{\pm}0.02mm$ (3rd), $0.75{\pm}0.03mm$ (4th), $0.89{\pm}0.05mm$ (5th), $1.23{\pm}0.06mm$ (6th), $2.13{\pm}0.11mm$ (7th). The pupal ratio was 92.0%. The pupal period were $9.1{\pm}1.6days$, and the emergence rate was 88.6%. As a result we determined that Mellicta ambigua can rear at natural conditions. But indoor-rearing is considered to be difficult and not useful industrially, because they have long term larval stage and only one life cycle per an year.