• 식물병연구
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• 제26권1호
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• pp.29-37
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• 2020

2016년 콩을 재배하는 포장에서 마름 증상에 의한 콩의 피해가 심하게 발생하였다. 유묘기 때에는 잘록 증상과 자엽에 갈색 또는 검은 색의 반점이 나타나기 시작하다가, 8월 이후 개화기에는 지상부 잎이 황화되기 시작하면서 부분적으로 갈변되었다. 이 시기에 채집한 콩의 뿌리는 생육이 많이 억제된 상태이며, 표피가 벗겨지면서 균핵이 형성되기 시작하였다. 9월 이후부터는 지상부의 마름 증상이 더 뚜렷해졌으며 고사하기 시작하였고, 수침상 병징을 보이던 줄기에도 균핵이 형성되었다. 수확기인 10월 중순 이후에는 줄기의 표피가 벗겨지면서 피층 부위에 소립균핵이 다량으로 형성되었다. 이런 병징으로부터 분리한 병원균은 32-35℃에서 균사 생육이 가장 양호하였고, 소립균핵의 형성은 20-28℃에서 가장 많았다. 병원균의 균학적인 형태 관찰과 internal transcribed spacer 영역 유전자의 염기서열 분석을 실시한 결과, 병원균은 Macrophomina phaseolina로 동정되었다. 또한 이쑤시개를 이용한 인공접종에서도 포장에서와 같은 병징을 보였을 뿐만 아니라, 재분리에서도 동일한 병원균이 분리·동정되었다. 그 결과 이 병을 콩 균핵마름병(가칭)으로 보고하는 바이다.

• Parasites, Hosts and Diseases
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• 제53권1호
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• pp.135-139
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• 2015

A total of 1,708 small mammals (1,617 rodents and 91 soricomorphs), including Apodemus agrarius (n = 1,400), Microtus fortis (167), Crocidura lasiura (91), Mus musculus (32), Myodes (= Eothenomys) regulus (9), Micromys minutus (6), and Tscherskia (= Cricetulus) triton (3), were live-trapped at US/Republic of Korea (ROK) military training sites near the demilitarized zone (DMZ) of Paju, Pocheon, and Yeoncheon, Gyeonggi Province from December 2004 to December 2009. Small mammals were examined for their intestinal nematodes by necropsy. A total of 1,617 rodents (100%) and 91 (100%) soricomorphs were infected with at least 1 nematode species, including Nippostrongylus brasiliensis, Heligmosomoides polygyrus, Syphacia obvelata, Heterakis spumosa, Protospirura muris, Capillaria spp., Trichuris muris, Rictularia affinis, and an unidentified species. N. brasiliensis was the most common species infecting small mammals (1,060; 62.1%) followed by H. polygyrus (617; 36.1%), S. obvelata (370; 21.7%), H. spumosa (314; 18.4%), P. muris (123; 7.2%), and Capillaria spp. (59; 3.5%). Low infection rates (0.1-0.8%) were observed for T. muris, R. affinis, and an unidentified species. The number of recovered worms was highest for N. brasiliensis (21,623 worms; mean 20.4 worms/infected specimen) followed by S. obvelata (9,235; 25.0 worms), H. polygyrus (4,122; 6.7 worms), and H. spumosa (1,160; 3.7 worms). A. agrarius demonstrated the highest prevalence for N. brasiliensis (70.9%), followed by M. minutus (50.0%), T. triton (33.3%), M. fortis (28.1%), M. musculus (15.6%), C. lasiura (13.2%), and M. regulus (0%). This is the first report of nematode infections in small mammals captured near the DMZ in ROK.

• 자원환경지질
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• 제15권4호
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• pp.177-188
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• 1982

The Chungju and Seosan Groups have been known usually as Precambrian formations in Korea. But their relative and absolute ages have been controvericial problem in relation with other geologic system such as so-called Ogcheon and Yeoncheon Systems in Korea. This study has mainly focused on the corelation of the Chungju Group with the Seosan Group in their stratigraphy, structure, metamorphism, and iron ore deposits. In the process of study, the auther surveyed and reclassified the Chungju and Seosan Groups and corelated with Gyeonggi and Ogch cheon metamorphic belts and got some new data. The Chungju iron-bearing formations showing transtitional relation with the Gyeonggi Gneiss Complex and the Jangamri Formation consisting mainly of pebble bearing calcarious phyllite, should be seperated from the Gyemyeongsan formation which is mainly composed of metavolcanic rocks. The Jangamri Formation and the coaly phyllite, which can be corelated respectively with the Hwaggangri Formation and Changri Formation in Ogcheon Group, are repeated in the Gyemyeonsan and Munjuri Formations with the overturned anticlinal folding(F1). So the Chungju Group which was defined as an indipendant geologic unit from the Ogcheon Group should be limited only on the Chungju iron Formation. The Seosan Group can be classified stratigraphically such as Seosan Formation consisting of iron-bearing quartzite and mica schist, Daesan Formation overlying unconformably on the Seosan Formation and Gyeonggi Gneiss Complex. Taean Formation overlying unconformably on the Daesan Formation should be seperated from Seosan Group. There are many similarity in the stratigrphy, structure, and metamorphic facies between Chungju and Seosan Groups exept the metavolcanic rocks in the Gyemyeongsan and Munjuri Formations and the pebble bearing calcareous phyllite in the Jangamri Formation. The two Groups were deformed with two kinds of differant stages, the first shows $N30^{\circ}-40^{\circ}E$ trend of fold axis, the second $N70^{\circ}-80^{\circ}W$ respectively. The Seosan Formation, which is the lowest formation in Seosan Group and bearing the iron formation, was metamorphosed at 2500 m. y. before. These age is similar with the metamorphic age of Gyeonggi metamorphic belt and with the age of Algoman and Kenoran Orogenies which devide the Precambrian into Archean and Proterozoic Era. So the Seosan Formation, which is included in some migmatitic rocks of Gyeonggi Gneiss Complex, is the oldest formation in Korea and can be corelated with the Anshan Group which bears the oldest iron formation in China. The metamorphic facies of the Precambrian metamorphism in Seosan area is simillar with that of Chungju area, showing high temperature-low pressure amphibolite facies which is corelated with the Gyeonggi metamorphic belt, the oldest metamorphic belt in Korea ($650^{\circ}-680^{\circ}C$, 3.2-4.4 Kb). The high temperature intermediate pressure amphibolite facies in Seosan area with the low temperature-intermediate presure greenschist facies of Taean formation is corelated with that of Ogcheon Group ($590^{\circ}-640^{\circ}$ C, 5.2-6.3 Kb). The Chungju and Seosan iron formations were deposited in Archean, showing geochemical composition of Precambrian iron formations. The Chungju iron formation was mainly formed by the chemical precipitation, on the other hand, the Seosan iron formation was formed by alternated action of chemical and detrital depositions.

• 자원환경지질
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• 제20권2호
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• pp.85-95
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• 1987

The host rocks of titaniferous magnetite deposits in Gonamsan are alkaline gabbros, which are typical of undersaturated alkaline rocks in terms of the lack of normative quartz. According to field occurrences and petrographic features, these alkaline gabbros are divided into 3 rock types: coarse-grained and pegmatitic rock, medium-grained rock with equigranular texture, and layered cumulate rock. All these rocks mainly contain clinopyroxene(salite), plagioclase(An 43-66), pargasite, and ilmenite. The accessory minerals are apatite, sphene, quartz, and sometimes titaniferous magnetite. Pargasite, sphene, and quartz are considered to be secondary minerals formed by the reaction among clinopyroxene, plagioclase and Fe-Ti oxide at deuteric stage. Fe-Ti oxides generally occur as ilmenite in the alkaline rocks, and titaniferous magnetite in the ore deposits. Layered cumulate rocks are characterized by a recurrence of discontinuous thin mesolayer of clinopyroxene-pargasite within leucolayer mainly composed of plagioclase. Clinopyroxene is cumulus mineral whereas plagioclase, ilmenite and apatite occur as intercumulus minerals. According to the variation diagrams of oxide and trace element contents against the differentiation index, incompatible elements, such as Na, Ba and Sr, show positive correlations whereas compatible elements, such as Mg and Cr, show negative correlations. However some compatible elements, such as Co, Ni and V show irregular variations, reflecting relative cumulate status of cumulus and intercumulus minerals. On the de la Roche multicationic diagram, these alkaline gabbros are distributed along the differentiation curve of undersaturated alkaline series from alkaline basaltic composition through basanitic composition to tephritic composition. Layered cumulate rocks, which are distributed between basanitic composition and tephritic composition, reflect their cumulate character, slightly scattering away from the curve. The medium-grained rock shows higher contents in Ba, Sr and light rare earch elements than the coarse-grained and pegmatitic rock. The former shows two times higher contents of total rare earth elements than the latter, $while(La/Lu)_{cn}$ ratios maintain fairly constant values of 5.08~5.06 in these two rocks. This means that coarse-grained and pegmatitic rock, as compared with the medium-grained rock, was formed by the earlier differentiated magma but rare-earth element distribution pattern remained almost parallel during differentiation. From the data the above mentioned, these alkaline gabbros are considered to be comagmatic and to be formed by intrusions of differentiated magmas in its reservoir.

• 식물분류학회지
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• 제45권4호
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• pp.362-368
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• 2015

꼬리고사리속의 두 개의 신교잡종과 한 개의 미기록교잡종이 발견되었다. 이들 종들의 형태적 형질에 있어 부모종들의 중간형태를 보였다. 거미사철고사리($A.{\times}uiryeongse$)는 서울 북한산 우이령길에서 발견되었고 거미고사리와 사철고사리의 교잡에 의해 분화되었다. 다른 교잡종, 산꼬리고사리($A.{\times}montanus$)는 경기도 연천군, 성산에서 발견되었고, 거미고사리와 차꼬리고사리가 교잡에 의해 만들어지고 다시 꼬리고사리와의 중복교잡에 의해 형성되었다. 아울러 미기록 교잡종인 거미돌담고사리($A.{\times}kitazawae$)는 대구 도동에서 발견되었고, 거미고사리와 돌담고사리의 교잡에 의해 형성되었다. 이들 교잡종들은 부모종들과 같은 장소에서 자란다. 각 분류군의 형질을 분석해 교잡종임을 입증해 보였으며, 이들에 대한 기재, 도해 및 자생지의 서식 사진을 수록하였다.

• 암석학회지
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• 제24권1호
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• pp.1-10
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• 2015

본 연구에서는 경기도 포천시 관인면 중리 늘거리 유적지에서 출토된 일부 석기의 육안 및 현미경 관찰 그리고 모드분석 결과를 근거로 주변 지역에 대한 야외지질조사를 통해 석기의 산지를 추정하였다. 연구에 사용된 늘거리 석기 12점은 화산회 응회암, 화산력 응회암, 화강반암, 안산암, 섬록반암 등의 암석으로 동정되었으며, 석기의 용도와 암석의 종류를 살펴보면 격지는 다양한 암석으로, 돌날과 돌조각은 주로 응회암질 암석으로 제작되었다. 석기의 산지로 화산력 응회암은 철원분지에 분포하는 동막골 응회암, 화강반암은 옥산리 남동쪽, 연천 동쪽에 소규모 암주로 산출되는 백악기 관입암류인 화강반암, 안산암은 유적지 북쪽에 위치한 안산암체가 그 산지로 밝혀졌으며, 섬록반암은 유적지 남쪽에서 위치한 섬록암체가 산지로 추정된다. 산지해석 결과, 연구 대상 석기는 유적지로부터 최대 15 km 이내의 주변에서 산출되는 암석과 같거나 유사하다.

• 한국치위생학회지
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• 제5권2호
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• pp.171-184
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• 2005

In order to investigate correlation between mother's dental ca re for her children and their dental caries, this study was conducted wi th the dental examination record of 365 children who showed the same number of questionnaires with those examined for dental conditions and questionnaires written by mothers among children between three and six years of age and their mothers in Yeoncheon, Gyeonggi province in June 2004 to estimate frequency and percentage of general properties of subjects and mother's oral health care behaviors for her children by research items, to carry out cross-tabulation analysis and correlation analysis following Chi-square distribution for the presence of dental caries in deciduous teeth and oral health care behaviors, and to use decision tree analysis among data mining techniques for those factors associated with the presence of dental caries in deciduous teeth, and drew the following conclusions. 1. For mother's oral health care behaviors and attitudes for her children, 225 mothers(61.6%) confirmed their children's teeth-brushing; 278(76.2%) used no fluorine; and 286(78.6%) observed their children's teeth, 322 mothers(88.2%) instructed their children in teeth-brushing while 268 (73.4%) provided dental care, 232 mothers(63.7%) treated their children's cavity; 290(79.4%) believed that their children had good dental conditions; and 294(80.5%) answered that they began to provide their children with dental care in deciduous teeth. 2. As for the presence of dental caries in deciduous teeth and dental health care behaviors, there were statistically significant differences in employment, confirmation after teeth-brushing, teeth observation, instruction in time for teeth-brushing, use of fluorine, cavity treatment, time for dental care, and perception of dental conditions(p<0.05). 3. As for correlation between dental caries in deciduous teeth and oral health care behaviors, mothers who worked, who believed that their children didn't have good dental condition, and who thought that it was necessary to begin to provide dental care in permanent teeth were found to get their children to suffer from dental caries in deciduous teeth. Besides, those who failed to confirm teeth-brushing, who used no fluorine, and who failed to observe teeth and gave no instruction in time for teeth-brushing were shown to get their children to suffer from dental caries in deciduous teeth. 4. Variables to determine the presence of dental caries in deciduous teeth were classified by cavity treatment, mother's employment, time for dental care, and observation of children's teeth. The first node to determine the presence of dental caries in deciduous teeth was found to be cavity treatment; the next criteria for classification after cavity treatment were shown to be mother's employment and time for dental care. In case of children with no cavity, they were found to be mother's employment and teeth observation.

• Parasites, Hosts and Diseases
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• 제45권2호
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• pp.157-161
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• 2007

A total of 1,496 rodents and insectivores were live-trapped at Yeoncheon-gun (n = 351), Paju-shi (804), and Pocheon-gun (343), Gyeonggi-do (Province), and examined for intestinal helminths, including Neodiplostomum seoulense, seasonally from December 2004 to September 2005. Six species of rodents, including Apodemus agrarius (1,366), Mus musculus (32), Micronytus fortis (28), Eothenomys regulus (9), Micronys minutus (6), and Cricetulus triton (3), and 1 species of insectivores Crocidura lasiura (54) were collected. A total of 321 adult N. seoulense were collected from 19 (1.4%) A. agrarius. The worm burden ranged from 1 to 101 per A. agrarius (mean; 16.9). No N. seoulense was observed in other rodent or insectivore species examined. The infection rate during autumn (4.5%) was higher than those during spring (0.8%), summer (0.8%), and winter (0.5%). The average number of N. seoulense in infected A. agrarius was the highest in spring (66.0 specimens), followed by autumn (15.2), winter (4.5), and summer (3.3). This study first confirms that A. agrarius is a natural definitive host for N. seoulense, and demonstrates that the infection rates and intensities vary seasonally and geographically.

• 자원환경지질
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• 제52권5호
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• pp.347-356
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• 2019

경기육괴 서부에 분포하는 태안층의 독특한 쇄설성 저어콘 연대 분포가 알려진 이후 퇴적환경, 퇴적시기, 기원지, 변성사 등에 대한 다양한 연구가 이루어졌다. 이 논평에서는 그 동안 태안층에 대하여 이루어진 기존 연구들을 소개하고 퇴적시기 및 기원지에 대하여 고찰하고자 한다. 태안층은 전통적으로 선캠브리아시대의 지층으로 알려졌으나, 근래 다수의 전기-중기 고생대 저어콘들이 발견된 이후 중부 혹은 상부 고생대 퇴적층으로 해석되고 있다. 태안층은 주로 석영과 운모로 구성된 변성사암, 이질편암, 천매암으로 구성되었으며, 이들의 원암은 심해선상지의 로브 환경에서 쌓인 저탁암으로 해석되었다. 태안층이 퇴적된 시기는 쇄설성 저어콘 연령과 관입암의 연령 차이를 통해 데본기-트라이아스기 사이로 알려져 있는데, 퇴적시기가 데본기에 가깝다는 견해와 페름기에 가깝다는 견해로 나뉜다. 태안층의 기원지는 남중국지괴나 중국의 충돌대, 또는 경기육괴로 추정되고 있다. 태안층과 기타 한반도 (변성)퇴적층의 쇄설성 저어콘 연대를 다룬 기존 연구들의 자료를 비교한 결과, 태안층은 연천층군이나 옥천누층군의 피반령 단위와 주요 기원암을 공유하되 기원지가 완전히 일치하지는 않는 것으로 여겨진다. 이러한 결과를 바탕으로 태안층의 퇴적시기와 기원지에 대한 기존 가설들을 고려하면, 태안층을 페름기-전기 트라이아스기 사이에 퇴적된 것으로 해석한 모델이 비교적 합리적으로 보인다. 향후 태안층의 정의를 명확히 하고 기원지 규명을 위한 층서학 및 퇴적암석학적 추가연구가 필요하다.

• 아시안잔디학회지
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• 제20권2호
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• pp.237-251
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• 2006

본 연구는 국내 잔디생산 현황에 대한 설문조사 결과로 재배면적, 재배초종, 경영농가 현황,잔디유통 현황 등을 조사하였다. 설문 조사 기간은 2006년 4월부터 10월까지이며, 각시도별로 잔디재배를 많이 하고 있는 곳을 방문하여 15개 항목을 설문조사 하였다. 재배면적은 설문조사와 지역 재배농민의 추정치, 그리고 방문에서 제외된 지역은 2006년 산림청조사 자료를 종합하여 결정하였다. 기타 조사항목은 항목별 응답 인원에 대한 백분율로 나타내었다. 조사결과 국내 총 잔디 재배면적은 2,947ha로 나타났다. 지역별로는 전남 1,417ha(48%), 전북 442ha(14.9%), 경기 344ha(11.6%), 경남 248ha(8.4%), 충남 240ha(8.1%) 순으로 나타났다. 잔디 주 생산단지는 장성군, 함평군, 영광군, 고창군, 사천시, 익산시, 여주시, 연천군 등으로 조사되었다. 경영주 나이는 51세 이상이 72.4%로 노령화되어 있었으며, 재배경력은 10년 이상이 84.4%로 나타났다 전문경영의 형태를 보였다. 잔디재배 초종은 중지계통의 들잔디가 55.5%, 일반 들잔디가 37.4%로 높은 비율을 차지했으며, 켄터키블루그래스가 3.8%, 한국잔디 신품종이 0.1% 등으로 조사되었다. 한국잔디의 출하 규격은 다양했으며 $18{\times}18cm$ 규격으로 출하하는 경우가 43.6%로 가장 많았다. 출하형태는 위탁판매가 40.5%로 높게 나타났으며, 전남지역의 생산단가는 $2,160{\sim}2,730$원$/m^2$ 이었다.