• 제목/요약/키워드: environmental geochemistry

검색결과 216건 처리시간 0.02초

Environmental geochemistry of persistent organic pollutants in the Pearl River Delta

  • Peng Ping'an;Fu Jiamo;Sheng Guoying;Xiao Xianming;zhang Gan;Wang Xinming;Mai Bixian;Ran Rong;Cheng Fanzhong
    • 대한자원환경지질학회:학술대회논문집
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    • 대한자원환경지질학회 2002년도 춘계 공동학술발표회
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    • pp.8-10
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    • 2002

  • POPs in sediments and soil in the PRD are comparable to or much higher than those reported in other regions. Some sites may be classified as POPs- polluted with high ecological risks. Large-scale land transform in the process of regional urbanization may facilitate the transfer of POPs in the soil to the sedimentary system by enhancing the soil run-off. Urban atmospheric PCBs in PRD are found to be less than some of the North American or European urbans, but PAHs are significantly higher. The center of the PRD has been the major source area of PAHs and organochlorine pesticides in the PRD. The northern part of the PRD serves as a regional sink for the air particulates and affiliated POPs.

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The Mineralogy and Geochemistry of the Uppermost Sediments of the Lake Hovsgol, North Mongolia : It's Implication to the Paleoenvironmental Changes

  • Tumurhuu, D.;Narantsetseg, Ts.;Ouynchimeg, Ts.
    • 한국제4기학회지
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    • 제18권2호통권23호
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    • pp.3-3
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    • 2004

  • One short core with length of 146cm(HB-107, at coordinates of $N51^{\circ}$11'37.5";$E100^{\circ}$24'45.6", from 229m water depth was subject of the present study. The sub-samples of the core were analyzed for the water contents (WC%), biogenic silica, identification of the main phases, grain size distribution, geochemistry and some physical properties of sediment(Wet density and Magnetic susceptibility) with aims of recording palaeo-environmental changes in Northem Mongolia. The evaluation of the geochemical and mineralogical proxies on palaeo-climated and palaeo-environmental changes are based on comparison to the behvior of biogenic silica through core, as later one had been showed itself, as good indicator of the climate and environmental fluctuation. Age model of the investigating core based on previously C 14 dated core HB105 taken from the central part of the Hobsgol Lake and the result had been published elsewhere. The core consists of two litological varieties : upper diatomaceous silt, lower clay. According to the age model the upper diatomaceous silt formed during the Holocene, lower caly-during the late Pleistocene glacial period. The geochemistry and phase identification analysis on the core samples are resulted in determining main minerals that form the bottom sediments and their geochemistry. The main include quartz, felspar, muscovite, clinochlore, amphibole and carbonate phase(dolomite and calcite). Through the core not only occur the relative quantitative changes of the main phases, but also happen that the carbonate phase completely disappear in diatomaceous silt. This is believed to be related to the lake water salinity changes, which occurred during the trassition period from Pleistocene glacial-to the Holocene interglacial. These abrupt changes of the mineralogy have been clearly traced in geochemistry of sediments, specially in calcium concentration, which is high in lower clay and low in upper diatomaceous silt. That means, geochemistry and mineralogy of the bottom sediments can be used as proxy data on palaeo-climate and palaeo-environmental changes.

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중부소백산육괴 선캠브리아 변성암류의 지구화학적 연구 (Geochemistry of the Precambrian metamorphic rocks from the central Sobaegsan Massif, Korea)

  • 송용선
    • 자원환경지질
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    • 제22권3호
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    • pp.293-300
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    • 1989

  • The basal metamorphic complex of the central Sobaegsan Massif consists of pelitic & psammitic paragneisses, various kinds of granitic gneisses and lesser amounts of amphibolite. The granitic gneisses could be clearly distinguished from the pelitic and psammitic paragneisses on the basis of major-element geochemistry. A number of geochemical plots reveals that granitic gneisses were derived from calc - alkaline igneous rocks.

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중석의 광물학적, 지화학적 고찰 (Some Aspects of Tungsten Mineralogy and Geochemistry)

  • 김상엽
    • 자원환경지질
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    • 제12권3호
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    • pp.127-146
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    • 1979

  • 중석은 우리나라에서 40여년간 개발되어 1951년 이후 세계 굴지의 중석 생산국의 하나로 등장 했으나 중석에 대한 광물학적및 지화학적인 지식은 이들을 다루고 있는 전문가에게도 극히 제한되어 이해되고 있다. 중석에 대한 광물학, 지구화학적인 활동특성, 중석광상의 특정과 광화작용의 지질적인 환경등에 관한 연구논문이 세계적으로 상당량 발표되어 있다. 일반적으로 잘 알려진 중석광물중 회중석과 흑중석은 일차광물로 회중석계열 및 흑중석계열 광물중의 하나에 불과하며 이외 이차광물은 극히 드물게 산출되나 이들은 중석광물을 탐사하는데 중요한 자료가 되기도 한다. 반면 중석에 대한 지구화학지식은 아직도 불완전하게 알려져 있고 지질과정에 있어 중석의 활동 특성은 연구단계에 있다. 최근 중석의 기초 지구화학연구가 많이 진전되어 여러 학자들에 의하여 그 자료가 정리되어 발표되고 있다. 중석광상을 보다 더 이해하고 앞으로 효율적인 탐사를 위하여 현재까지 알려진 중석에 대한 지구화학적인 기초연구와 중석광상에 수반되는 원소들을 요약한다.

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