• 자원환경지질
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• 제36권2호
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• pp.75-87
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• 2003

함안-군북 광화대는 한반도 남동부의 백악기 경상분지내에 위치해있다. 자철석, 회중석, 휘수연석, 황동석의 주광석 광물과 천금속 및 소량의 황염광물이 백악기 퇴적암, 화산암, 화강섬록암(118${\pm}$3.0 Ma)내에 발달된 열극을 충진한 전기석, 석영 및 탄산염맥내에서 산출된다. 광석 및 맥석광물들은 세 개의 광화시기로 구분될 수 있다: 광화 1기, 전기석+석영+철-동광석: 광화 2기, 석영+황화광물+황염광물+탄산염광물; 광화 3기, barren한 방해석. 광화 1기 및 2기의 초기 유체는 고염농도(35~70 equiv. wt.% NaCl+KCl)이며, 기상이 풍부하고 약 300$^{\circ}$~50$0^{\circ}C$의 온도에서 균질 되었다. 비록 황화물 광물이 상기유체에 의해 생성된 초기광물조합과 연관성이 없을지라도, 고염농도의 유체는 상당량의 나트륨, 칼륨, 철, 동, 황을 함유하는 염화물복합체 염수로 사료된다. 후기 용액은 새롭게 생성된 열극 및 맥을 따라 순환되었으며, 낮은 염농도($\leq$20 equiv. wt.% NaCl)이며 약200$^{\circ}$~40$0^{\circ}C$에서 균질화되었다. 할안-군북 열수계 유체의 산소-수소 동위원소조성은 광화초기에는 마그마성 열수의 특징을 보이다가 점차 광화후기로 가면서 순환수성 열수의 특징을 보여주고 있다. 함안-군복지역의 광체가 부존된 화강섬록암내에서 손환하고 있는 초기 열수성유체는 정출마그마에서 용리된후 고염농도의 액상을 함유한 유체와 $H_2O$-NaCl계의 기상으 함유한 유체로 불혼화되었다. 상기 마그마유체가 열극을 따라 이동하면서, 다른 황화광물과 황염광물의 침전없이 전기석 및 초기 철, 텅스텐, 몰리브데늄, 동 광화작용을 유발시켰다. 순환수기원의 후기광화용액은 동과 천금속 황화물, 황염광화작용을 촉발시켰다.

• 한국농림기상학회지
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• 제14권4호
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• pp.222-228
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• 2012

산불 발생 이후 대부분의 지역에서 소나무보다는 참나무류로 천연갱신되는 패턴을 보인다. 그러나 능선부나 암반지대 등 척박한 곳에서는 소나무가 일부 생존하며, 때에 따라서는 임분을 형성하기도 한다. 따라서 본 연구는 산불피해지에서 능선부를 중심으로 소나무의 생장과 개체수를 조사하여 산불피해지에서 소나무의 천연갱신에 관한 기초자료를 제공하고자 수행되었다. 산불피해지에서 소나무 개체수의 변화는 1회 지표화 피해지인 5번 조사구에서는 산불 발생 후 초기 5년간 증가하는 패턴을 보여주었다. 이는 지표화에 의해 하층식생이 제거되고 지표화 피해로부터 생존한 개체로부터 종자가 지속적으로 유입되었기 때문으로 판단된다. 2회 전소화 피해지인 1, 2, 3, 그리고 4번 조사구의 경우 산불 발생 5년 이후부터 소나무 치수의 발생이 증가하는 패턴을 보였는데 이는 능선 근처에 소나무 잔존목이 존재하지 않아 종자의 유입이 어려워 소나무의 이입이 더뎠으나 시간이 경과함에 따라 토양 환경이 안정되고 종자를 생산하는 개체가 늘어 소나무 치수의 이입이 증가했을 것으로 사료된다. 소나무 수고의 상대 생장율은 임분에 관계없이 시간 경과에 따라 급격히 감소하는 경향을 보여주었으며, 이는 모든 조사구에서 공통적으로 나타난 결과이다. 따라서 산불피해지에서 자연 복원된 소나무의 수고 상대 생장율은 산불의 발생빈도나 형태와는 무관한 것으로 판단된다. 따라서 향후 개체수와 수고 생장속도에 영향을 끼치는 토양의 성질과 유실량, 그리고 주변 임분에서 자라는 참나무류의 생장에 관한 조사가 추가적으로 이루어져야 할 것이며, 한편, 생존한 주변 소나무 임분의 유전학적 동정을 통해 소나무 치수의 이입에 관한 연구가 이루어져야 할 것으로 판단된다.

• Journal of Ecology and Environment
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• 제42권3호
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• pp.111-119
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• 2018

Background: Juniperus chinensis L. populations are distributed locally on several areas including coastal cliffs which are difficult to access in the central eastern Korea. Wild populations inhabit relatively barren environments such as rocky areas and cliffs, which are very sensitive to even minor environmental disturbances including artificial interventions and natural disturbances, and thus demonstrate great fluctuations in the population size and density. This study aims to analyze the genetic diversity, differentiation, and genetic structure of each population in order to provide useful data required to establish a substantial conservation strategy of J. chinensis. Results: The genetic diversity of J. chinensis at the population level (P = 78.7%, h = 0.282, S.I. = 0.420) was somewhat higher compared with those measured in the same genus, Juniperus. The genetic differentiation degree among nine populations established naturally in central eastern Korea was 11.50% and that among sub-populations within the same area was 5.52%. On the other hand, genetic variation of individuals within the populations was 82.93%. But frequency of the main allele was different among loci. In particular, fixation of allele frequency and occurrence of rare allele in the highly isolated population suggest a likelihood that genetic drift would occur in populations of this plant. As the result of analysis on the genetic structure of nine populations, nearby populations and isolated populations tended to form separate clusters from each other as the hypothetical number of clusters (K) increase. Conclusions: This result implies that if the population size of J. chinensis is reduced due to environmental change and artificial and/or natural disturbances in the future, it could affect negatively on the genetic diversity of the plant species. In order to maintain and conserve genetic diversity of J. chinensis, ecological network, which can help genetic exchange among the local populations, should be prepared, and conservation strategies in situ as well as ex situ are also required with continuous monitoring.

• 한국환경복원기술학회지
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• 제18권6호
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• pp.39-49
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• 2015

This study was to evaluate the growth and spatial distribution characteristics of Rhus javanica population. The study was conducted between 2015 January and July at the cut-slope revegetation site in Dae-Ji Mountain. Seeds of native species were sowed on the disturbed cut-slope in 2002. There were 119 vascular plant species 55 families and 94 genera on the cut-slope. Compositae, Rosaceae, and Leguminosae plants were dominant species, which are pioneer species in dry and barren site. Canopy of trees covered 44.1% total area, which was 8.3% increase from 2008. Rhus javanica, main species, dominated all DBH classes except DBH >24cm. Albizzia julibrissin showed high frequency in the 6~17cm DBH class and Salix koreensis was abundant at >12cm. Elaeagnus umbellata, Corylus heterophylla var. heterophylla, Alnus sibirica, and Acer pictum were not observed. Rhus javanica population was the most frequently observed on the south facing cut-slope. The average DBH of Rhus javanica was $7.3({\pm}3.7)cm$ and the average height of them was $5.2({\pm}1.7)m$. Annual average DBH growth was 7.9mm/yr and the maximum growth(12.0mm/yr) was the $3^{rd}$ year. It decreased after $6^{th}$ years. Although Rhus javanica population in the Dae-Ji Mountain was a seed originated plantation, the forest had reverse J shape diameter frequency distribution. It indicated that the forest is uneven-aged forest. The Rhus javanica population was expected to sustain.

• 대한원격탐사학회지
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• 제29권1호
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• pp.105-114
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• 2013

지구온난화와 인간의 무분별한 활동과 같은 인위적인 요인과 아열대고압대라는 자연적인 요인으로 인해 동아시아 지역의 사막화가 확산되고 있다. 사막화의 확산으로 인하여 우리나라에 영향을 주는 황사의 발원지가 변화하고 있다. 본 연구에서는 황폐한 지역의 토지 피복을 연구하기 위한 유용한 식생지수로 알려진 Normalized Difference Vegetation Index (NDVI)를 이용하여 동아시아 사막 주변의 토지 피복 변화를 관측하여 사막화의 시계열 변화와 패턴을 알아보고자 한다. SPOT위성의 VEGETATION 센서를 통해 동아시아 S10-DAY NDVI 데이터를 1999년부터 2011년까지 취득하였다. 데이터에 포함되어 있는 노이즈값을 제거하기 위해 NDVI Correction, WaterMask를 수행한 후 ISODATA 방법으로 무감독분류를 하였다. 무감독분류 된 클러스터에 대한 분석을 수행한 결과 사막 경계 부분에서 식생의 밀도가 활발하게 변화하고 있는 것을 확인하였으며 특히 고비 사막과 내몽골 고원 그리고 만주 지역을 중심으로 변화가 큰 것을 확인하였다. 2000년대 후반에 들어서 사막의 전체적인 크기는 감소하는 것으로 나타났지만 동쪽으로 사막화가 진행되는 것을 확인하였다.

• 자원환경지질
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• 제20권1호
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• pp.1-18
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• 1987

The Cheolam silver deposits are emplaced along the fractures in breccia dike and the Hongjesa granite. Breccia dike contains fragments of late Cretaceous acidic volcanic rocks and other fragments of various rocks distributed in the mine area. Therefore it is presumed that the mineralization was taken place in later than late Cretaceous time. Mineral paragenesis is complicated by multiple episodes of fracturing. Six distinct depositional stages can be recognized: stage I, deposition of base metal sulfides; stage II, deposition of base metal sulfides and silver minerals; stage III, deposition of carbonates; stage IV, deposition of silver minerals and base metal sulfides; stage V, deposition of silver minerals; stage VI, deposition of barren quartz. Silver minerals from the deposits are native silver, acanthite, pyrargyrite, argentian tetrahedrite, stephanite, polybasite, pearceite, allargentum, antimonial silver and electrum. Fluid inclusion studies ware carried out for stage I, II, IV and VI quartz and stage III calcite. Homogenization temperatures for each stage are as follows: stage I, from $225^{\circ}$ to $360^{\circ}C$; stage II, from $145^{\circ}$ to $220^{\circ}C$; stage III, from $175^{\circ}$ to $240^{\circ}C$; stage IV, from $130^{\circ}$ to $185^{\circ}C$; stage VI, from $120^{\circ}$ to $145^{\circ}C$. Salinities of ore fluids were in the range of 4 and 10 wt.% equivalent NaCl over stage I and stage VI. Ore mineralogical data of each stage indicate that temperatures are within the range of homogenization temperature of fluid inclusions and sulfur fugacities declined steadily from $10^{-9.7}atm$. to $10^{-18.7}atm$. through stage I into stage V.

• 한국초지조사료학회지
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• 제6권1호
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• pp.44-48
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• 1986

사일리지 옥수수의 적정(滴定) 질소시비(窒素施肥) 수준(水準)과 재식밀도(栽植密度)를 알아보고자 1981년(年) 부터 1982년(年) 까지 축산시험장(畜産試驗場) 사료포(飼料圃)에서 단교잡종(單交雜種) 수원(水原) 19호(號)를 가지고 시험(試驗)한 결과(結果)는 아래와 같다. 1. 질소(窒素)를 증시(增施)하면 웅수출현기(雄穗出現期)와 간장(稈長)은 뚜렷한 변화가 없었으나 착수고(着穗高)는 다소 낮아지고 경(莖)의 직경(直徑)은 굵어지며 엽면적지수(葉面積指數)와 도복율(倒伏率)은 높아졌다. 2. 밀식(密植)하면 웅수출현기(雄穗出現期)는 늦어지고 간장(稈長)은 짧아지나 착수고(着穗高)는 높아지며 경(莖)의 직경(直徑)은 가늘어지고 엽면적지수(葉面積指數)와 도복율(倒伏率)은 증가(增加)되었다. 3. 질소(窒素)를 증시(增施)하면 결주율(缺株率)이 높아지고 밀식(密植)하면 불임율(不姙率)이 높아져 종실수량(種實收量)은 10a당(當) 질소(窒素) 10kg, 재식본수(栽植本數) 5,550본(本)에서 많았다. 4. 전가소화(全可消化) 건물수량(乾物收量) 역시 10a당 질소(窒素) 10kg, 재식본수(栽植本數) 5,550 본(本)에서 많았다.

• 한국농공학회논문집
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• 제52권3호
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• pp.39-45
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• 2010

Quantification of carbon absorption and understanding the human induced land use changes (LUC) forms one of the major study with respect to global climatic changes. An attempt study has been made to quantify the carbon absorption by LUC through remote sensing technology. The Landsat imagery four time periods was classified with the hybrid classification method in order to quantify carbon absorption by LUC. Thereafter, for estimating the amount of carbon absorption, the stand biomass of forest was estimated with the total weight, which was the sum of individual tree weight. Individual tree volumes could be estimated with the crown width extracted from digital forest cover type map. In particular, the carbon conversion index and the ratio of the $CO_2$ molecular weight to the C atomic weight, reported in the IPCC guideline, was used to convert the stand biomass into the amount of carbon absorption. Total carbon absorption has been modeled by taking areal estimates of LUC of four time periods and carbon factors for land use type and standing biomass. Results of this study, through LUC suggests that over a period of construction, 7.10 % of forest and 9.43 % of barren were converted into urban. In the conversion process, there has been a loss of 6.66 t/ha/y (7.94 %) of carbon absorption from the study area.

• 환경영향평가
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• 제19권2호
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• pp.117-125
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• 2010

Korea's researchers have recently studied the prediction of forest change, but they have not considered landuse/cover change compared to distribution of forest vegetation. The purpose of our study is to predict forest vegetation based on landuse/cover change on the Korean Peninsula in the 2090's. The methods of this study were Multi-layer perceptrom neural network for Landuse/cover (water, urban, barren, wetland, grass, forest, agriculture) change and Multinomial Logit Model for distribution prediction for forest vegetation (Pinus densiflora, Quercus Spp., Alpine Plants, Evergreen Broad-Leaved Plants). The classification accuracy of landuse/cover change on the Korean Peninsula was 71.3%. Urban areas expanded with large cities as the central, but forest and agriculture area contracted by 6%. The distribution model of forest vegetation has 63.6% prediction accuracy. Pinus densiflora and evergreen broad-leaved plants increased but Quercus Spp. and alpine plants decreased from the model. Finally, the results of forest vegetation based on landuse/cover change increased Pinus densiflora to 38.9% and evergreen broad-leaved plants to 70% when it is compared to the current climate. But Quercus Spp. decreased 10.2% and alpine plants disappeared almost completely for most of the Korean Peninsula. These results were difficult to make a distinction between the increase of Pinus densiflora and the decrease of Quercus Spp. because of they both inhabit a similar environment on the Korean Peninsula.

• 한국환경복원기술학회지
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• 제11권1호
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• pp.72-84
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• 2008

Since enactment of the Baekdu-Mountain Range protection law in Dec. 31st 2003, great interest arose in recovery of the natural environment in the Baekdu-Mountain Range. Since the Baekdu-Mountain Range has formed boundaries between different regions and it is the mountain that crosses our country from East to West, there are so many roads that penetrate this area. Slopes made by the construction of roads have poor foundation for the growth of vegetation and it takes a long period to restore only with natural restoration force. For this reason, various methods of revegetation to restore the damages are implemented but until now, revegetation of domestic soil cutting slopes are mainly covered by foreign import grasses to stabilize and cover grounds early. As we depended upon foreign import grasses for slopes revegetation, the landscape did not match in harmony with surrounding vegetation and therefore, we could see that these foreign grasses are withered in 2~3 years after the revegetation works and slopes become barren again. However, currently, there are no applicable standards for designs of green hill, desirable revegetation methods for the hill areas, roads and recovery models. Therefore, in this study, we investigated the status of revegetation plants and revegetation methods for the hill areas of the Baekdu-Mountain Range (azimuth, degree of tilt, and tilted places). Based on this, we attempted to find the desirable recovery models for the hill areas of the Baekdu-Mountain Range.