• 한국동물학회:학술대회논문집
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• 한국동물학회 1998년도 한국생물과학협회 학술발표대회
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• pp.197.1-197
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• 1998

No Abstract, See Full Text

• 한국정보기술응용학회:학술대회논문집
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• 한국정보기술응용학회 2007년도 추계 국제학술대회
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• pp.145-145
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• 2007

• 한국환경생물학회:학술대회논문집
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• 한국환경생물학회 2004년도 학술대회
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• pp.31-31
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• 2004

• 한국환경생태학회:학술대회논문집
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• 한국환경생태학회 1999년도 정기총회 및 학술논문 발표회
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• pp.105-107
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• 1999

• 한국주거학회논문집
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• 제10권3호
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• pp.181-186
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• 1999

• 한국동물학회:학술대회논문집
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• 한국동물학회 1999년도 한국생물과학협회 학술발표대회
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• pp.142.2-142
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• 1999

No Abstract, See Full Text

• 한국토양비료학회지
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• 제29권2호
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• pp.199-206
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• 1996

휴경논의 증가가 쌀 생산량 감소의 원인이 됨에 따라 휴경논의 합리적 재이용을 위한 생태환경 변화 양상을 구명하기 위하여 중서부 평야 기후권에 속하는 경기도(수원 외 9)지역을 대상으로 휴경년수별로 토양특성과 식생변화를 조사한 결과는 아래와 같다. 1. 휴경논 토양의 pH, Ca, Mg 변동(變動)은 휴경기간이 길수록 심토보다 표토부분이 증가(增加)하는 경향을 나타내었다. 2. 미생물상은 휴경기간이 길수록 세균은 감소하고, 방선균은 증가 하였으나, 사상균은 변화가 작은 경향을 나타내었다. 3. 휴경논의 식생에 대한 휴경기간별 분포비율을 평균(平均)해서 비교해보면 일년생은 1년: 89.5%, 2년: 30.7%, 3년: 33.1% 다년생은 1년: 10.5%, 2년: 69.3%, 3년: 66.9%로 일년생 초종에서 급격히 다년생 초종으로 변화하였고, 초종수(草種數)도 종합하면 1년: 38종(種), 2년: 37종(種), 3년: 25종(種)으로 감소하는 경향을 보였다. 4. 휴경논에서 자라는 버드나무는 휴경기간이 길수록 본수, 직경, 초장이 증가하였으며 휴경논의 재경작시 가장 큰 문제 식생으로 생각되었다.

• 한국환경생태학회지
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• 제21권4호
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• pp.356-365
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• 2007

본 연구는 상관에 의한 현존식생 및 종조성표 분류법과 배열법의 군집분류법을 적용하여 치악산국립공원 구역의 식생천이 경과에 따라 변화된 식물군락구조를 분석하였다. 현존식생은 신갈나무림(33.1%)이 가장 넓은 면적을 차지하였으며 다음으로 혼효림(16.2%), 일본잎갈나무림(15.6%), 낙연활엽수림(14.7%), 소나무림(11.1%), 잣나무림(2.3%), 리기다소나무림(0.1%)순이었다. 식생은 당단풍-신갈나무군락, 층층나무-까치박달군락, 졸참나무군락, 소나무군락 및 식재림으로 분류되었다. 당단풍-신갈나무군락은 하위단위 군락으로 서어나무-조릿대군락, 물푸레나무군락, 노린재나무-대사초군락이 구분되었다. 종조성표의 분류법과 배열법의 식물군락 분류는 유사하였다. 식생천이는 산중턱 이상에서 신갈나무(교목층)-당단풍(아교목층)-철쭉(관목층)이 결합하여 극상림을 이룰 것으로 예측되었다.

• Journal of Ecology and Environment
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• 제38권4호
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• pp.461-476
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• 2015

Global warming has accelerated glacial retreat in the high Arctic. The exposed glacier foreland is an ideal place to study chronosequential changes in ecosystems. Although vegetation succession in the glacier forelands has been studied intensively, little is known about the microbial community structure in these environments. Therefore, this study focused on how glacial retreat influences the bacterial community structure and its relationship with soil properties. This study was conducted in the foreland of the Midtre Lovénbreen glacier in Svalbard (78.9°N). Seven soil samples of different ages were collected and analyzed for moisture content, pH, soil organic carbon and total nitrogen contents, and soil organic matter fractionation. In addition, the structure of the bacterial community was determined via pyrosequencing analysis of 16S rRNA genes. The physical and chemical properties of soil varied significantly along the distance from the glacier; with increasing distance, more amounts of clay and soil organic carbon contents were observed. In addition, Cyanobacteria, Firmicutes, and Actinobacteria were dominant in soil samples taken close to the glacier, whereas Acidobacteria were abundant further away from the glacier. Diversity indices indicated that the bacterial community changed from homogeneous to heterogeneous structure along the glacier chronosequence/distance from the glacier. Although the bacterial community structure differed on basis of the presence or absence of plants, the soil properties varied depending on soil age. These findings suggest that bacterial succession occurs over time in glacier forelands but on a timescale that is different from that of soil development.

• 한국석유지질학회:학술대회논문집
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• 한국석유지질학회 1998년도 제5차 학술발표회 발표논문집
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• pp.29-37
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• 1998

The sedimentary succession on the northern coast of Jindo and the adjacent area comprises the thinly bedded, fine-grained deposits of an epiclastic sandstone, siltstone, black shale/mudstone, and cherty mudstone (ca. 200m in vertical thickness), which are interpreted as the finely stratified turbidites mainly by density underflow-induced currents. Most deposits can be divided into eight facies: thin-bedded, ash-rich massive sandstone layer (mS), graded and laminated mudstone layer (glM), graded mudstone layer with ripple lamination (rM), laminated and graded siltstone layer (lgZ), finely laminated black shale layer (IBS), structureless mudstone layer (mM), thin-bedded cherty mudstone layer (lCM), and contorted and laminated mudstone layer (dlM), The thin-bedded, ash-rich sandstone facies is interpreted to be deposited from high-density turbid underflows during a relatively large flooding. Most thinly bedded mudstone facies would be deposited from low-density turbid underflows (turbidity currents) with some different hydrodynamic condition and sediment concentration during the high discharge of river water. Whereas the structureless mudstone facies may result from raining down of suspended sediment intermittently supplied by overflows and interflows. From the entire succession, graded and laminated mudstone layers interbedded with thin-bedded, ash-rich massive sandstone are dominant in the lower part of the succession, and graded mudstone layers with ripple lamination ripple lamination occur mainly in the middle part of it. On the other hand, iaminated/raded siltstone and contorted/laminated mudstone layers prevail in the upper part. The transition of facies association is suggestive of the continuous change of main depositional setting from basin plain to lower slope, which could be due to the movement of depocenter by the increase of sediment supply (volcanic activity).