• 제목/요약/키워드: semi-continuous

검색결과 424건 처리시간 0.02초

사막화방지(沙漠化防止) 및 방사기술개발(防沙技術開發)에 관한 연구(硏究)(I) - 중국(中國)의 사막화현황(沙漠化現況) 및 방지대책(防止對策) - (Studies on the Desertification Combating and Sand Industry Development(I) - Present Status and Countermeasures for the Combating Desertification in China -)

  • 우보명;이경준;전기성;김경훈;최형태;이승현;이병권;김소연;이상호;전정일
    • 한국환경복원기술학회지
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    • 제3권3호
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    • pp.45-76
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    • 2000
  • The purposes of this study were to investigate and understand the present status of various types of "deserts", such as sand desert, gravel desert, rock desert, earth desert, salt desert, desert, rocky desert, gobi desert, sandy desert, clay desert, etc., and the general countermeasures for the combating "desertification" "desertization", and to develop the technologies on the revegetation and restoration for the combating desertification in China. The methods of this study were mainly composed of field surveys on the several experimental sites and research institutes related to combating desertification in China, and examinations on the various technologies for the combating desertification at the Daxing Experimental Station of Beijing Forestry University. The conclusion from this study may be summarized as follows; 1. Status and tendency of desertification in China : China is one of the countries seriously threatened by desertification. Desertification affected areas in China are mainly distributed in arid, semi-arid and dry sub-humid areas in China, covering the most regions of the Northeast China (eastern region of Inner-Mongolia), the northern part of the North China (middle and western region of Inner-Mongolia, Shaanxi, Ningsha, Gansu) and the western part of the Northwest China (Xinzang, Qinghai, Xizang). The total area affected by desertification in China is approximately 2.622 million $km^2$. It covers 27.3% of the total territory of China. Until recently, it is estimated that the annual spreading ratio of desertification in China is 2,460 $km^2$. Therefore, desertification is mostly serious problems facing to the Chinese people. 2. The causes and environmental effect of desertification : The desertification in China is mainly caused by compound factors, including natural condition and human activities. In China, the desertification is started by the decrease of precipitation, continuous dry and drought, strong wind, wind and water erosion, land degradation and loss of natural vegetation caused by climate variation, and accelerated by the human activities, such as over-cultivating, over-grazing, over-cutting of woods, irrational use of water resources. Because desertification has affected the geographical features, soil nutrients contents, salinity, vegetation coverage and the functions of ecosystem, the environmental deteriorations in the desertification affected areas are very seriously. 3. The fundamental strategies of combating desertification in China are the increase of education and awareness of people through various mass media, the revision of laws to guarantee operation of Desertification Combating Law and to improve many relating laws and regulations, the application of advanced technologies and training of experts, the establishment of discriminative policies, and increasing arrangement of budget-investment, and so on. China, as a signed country in UNCCD, has made efforts for the combating desertification. Korea is also signed country in UNCCD, so we should play an important role in the desertification combating projects of China for the northest asia and global environmental conservation as well as environmental conservation of Korea.

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서울의 블랙카본 특성 연구 (The Characteristics of Black Carbon of Seoul)

  • 박종성;송인호;김현웅;임형배;박승명;신선아;신혜정;이상보;김정호
    • 환경영향평가
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    • 제28권2호
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    • pp.113-128
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    • 2019
  • 2018년 가을철(9월 5일~10일, 6일간) 수도권대기오염집중측정소에서 미세먼지와 함께 블랙카본(BC, black carbon)의 농도 및 코팅두께를 파악하였다. 가을철 $PM_{10}$$23{\pm}12.6{\mu}g/m^3$, $PM_{2.5}$$12{\pm}5.8{\mu}g/m^3$으로 다른 계절보다 낮은 수준이었다. Aethalometer로 측정한 BC는 $0.73{\pm}0.43{\mu}g/m^3$, SOCEC로 측정한 EC(elemental carbon)는 $0.34{\pm}0.18{\mu}g/m^3$, SP2로 측정한 rBC(refractory-BC)는 $0.32{\pm}0.18{\mu}g/m^3$으로 측정방법에 따른 농도차이를 보여주었으나, 시계열 분포와 일 변동은 동일한 경향을 나타내었다. 수도권대기오염집중측정소에서 측정된 블랙카본은 자동차와 같은 일차오염원의 영향을 강하게 받았고, 주간과 야간의 출퇴근으로 인한 교통 혼잡 시간대에 높은 특징을 보였다. SP2로 측정한 $PM_{1.0}$ 단일입자에 대한 블랙카본의 개수농도는 84 nm에서 최고치로 관측되었으며, 코팅두께는 43 nm로 산정되었다. 특히 블랙카본 입자의 직경이 작을수록 코팅두께는 증가하였고, 입자의 직경이 증가할수록 코팅두께는 작아지는 특성을 나타내었다.

3D 사진측량법을 이용한 여수 사도 공룡발자국 화석산지 조사 및 교육자료 활용방안 (A Survey of Yeosu Sado Dinosaur Tracksite and Utilization of Educational Materials using 3D Photogrammetry)

  • 조혜민;홍민선;손종주;이현영;박경범;정종윤;허민
    • 한국지구과학회지
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    • 제42권6호
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    • pp.662-676
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    • 2021
  • 여수 사도 공룡발자국 화석지는 많은 수의 공룡발자국 화석과 함께 공룡의 집단행동에 대한 연구로 잘 알려진 지역이다. 또한 다양한 종류의 지질유산 및 지형유산이 분포하고 있어 지질관광과 지질교육의 장으로 주목받고 있다. 그러나 지리적 위치에 따른 접근성, 조차에 의한 시간적 제약, 지속적인 풍화 및 훼손에 의해 학생들의 교육을 위한 야외조사는 매우 제한적으로만 이루어지고 있다. 따라서 이번 연구는 최근 다양한 분야에서 이용되고 있는 사진측량법을 이용하여 사도의 공룡발자국 화석들의 3D 모델과 이미지를 생성한 후 이를 통해 과거에 확인하지 못한 화석에 대한 세부적인 정보를 확인함과 동시에 이를 교육자료로 활용 할 수 있는 방안에 대하여 제안하고자 한다. 획득한 3D 이미지를 통해 확인한 결과 기존에 육안이나 사진으로 확인하지 못하였던 일부 발자국 화석들의 존재를 확인할 수 있었고 기존에 발견된 화석이라도 사진이나 해석 드로잉으로 표현하지 못하였던 세부를 이미지로 나타낼 수 있었다. 또한 발자국 화석의 3D 모델은 향후 반영구적인 데이터로 보존할 수 있어 여러 형태로의 활용과 보존이 가능하다. 이번 연구에서는 사진측량법으로 얻어진 3D 모델을 활용하여 3D 프린팅 및 가상야외조사에 활용할 모바일 증강현실 콘텐츠를 구현하였으며 향후 3D 모델이 필요한 다양한 교육 콘텐츠 분야에서 사진측량법을 활용할 수 있을 것으로 보인다.

한반도 권역별 대기 중 입자상 탄소 특성 연구 (Characteristics of Particulate Carbon in the Ambient Air in the Korean Peninsula)

  • 이영재;박미경;정선아;김선정;조미라;송인호;유영숙;임용재;김정훈;정해진;이상욱;최원준;안준영;이민희;강현정;박승명;서석준;정동희;현주경;박종성;황태경;홍유덕;홍지형;신혜정
    • 한국대기환경학회지
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    • 제31권4호
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    • pp.330-344
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    • 2015
  • Semi-continuous measurements of $PM_{2.5}$ mass, organic and elemental carbon were made for the period of January to October 2014, at six national air monitoring stations in Korea. OC and EC concentrations showed a clear seasonal variation with the highest in winter (January) and the lowest in summer (August). In winter, the high carbonaceous concentrations were likely influenced by increased fuel combustion from residential heating. OC and EC concentrations varied by monitoring stations with 5.9 and $1.7{\mu}g/m^3$ in Joongbu area, 4.2 and $1.2{\mu}g/m^3$ in Honam area, 4.0 and $1.3{\mu}g/m^3$ in Yeongnam area, 3.7 and $1.6{\mu}g/m^3$ in Seoul Metropolitan area, 3.0 and $0.8{\mu}g/m^3$ in Jeju Island, 2.9 and $0.7{\mu}g/m^3$ in Baengnyeong Island respectively. The concentrations of OC and EC comprised 9.6~ 15.5% and 2.4~ 4.7% of $PM_{2.5}$. Urban Joongbu area located adjacent to the intersection of several main roads showed the highest carbon concentration among six national air monitoring station. On the other hand, background Baengnyeong Island showed the lowest carbon concentration and the highest OC/EC ratio (4.5). During the haze episode, OC and EC were enhanced with increase in $PM_{2.5}$ about 1.3~ 3 and 1.3~ 4.0 times respectively. The concentrations of OC, EC in the Asian dust case are about 1~ 2.4 times greater than in the nondust case. The origins of air mass pathways arriving at Seoul, using the backward trajectory analysis, can be mostly classified into 6 groups (Sector I Northern Korea including the sea of Okhotsk, Sector II Northern China including Mongolia, Sector III Southern China, Sector IV South Pacific area, Sector V Japan, Sector VI Southern Korea area). When an air mass originating from northern China and Mongolia, the OC concentrations were the most elevated, with a higher OC/EC ratio (2.4~ 3.3), and accounting for 17% of $PM_{2.5}$ mass on average.