• 한국토양동물학회지
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• 제2권2호
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• pp.104-114
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• 1997

Herein, 29 species of the ground beetles are reported from the Cheju Island (=Quelpart Is.). Of these, 18 species are new to Cheju Island.

• 한국토양동물학회지
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• 제3권2호
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• pp.106-110
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• 1998

제주도의 한라산에서 채집된 날개응애 55과 88속 112종의 목록을 작성하여 보고한다. 그 중에 76종은 제주도의 날개응애로 처음 보고되는 종이다.

• 농약과학회지
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• 제4권1호
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• pp.19-25
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• 2000

제주도 토양에서 EPN(O-ethyl-O-4 -nitrophenyl phenylphosphonothioate) 유기인계 농약의 이동을 예측하기 위해서, 제주도의 흑색 화산회토인 남원토양, 농암갈색 화산회토인 애월토양 및 암갈색 비화산회토인 무릉토양에서 EPN의 흡착과 토양칼럼에서 용탈을 검토하였으며, 또한 연안해수와 저니토에서의 EPN 잔류를 조사하였다. 남원토양, 애월토양, 무릉토양의 유기물함량은 각각 19.8%, 6.2%, 2.4%였고, 양이온 치환용량은 각각 24.8 meq/100g, 13.0 meq/100g, 9.5 meq/100g이었다. Freundlich 상수 k는 남원토양, 애월토양, 무릉토양에서 각각 89.4, 26.9, 9.2로 남원토양>애월토양>무릉토양의 순으로 감소하였다. 즉 유기물 함량 및 양이온 치환용량이 매우 높은 토양인 남원토양에서 흡착능이 높았다. Freundlich 상수 1/n은 유기물 함량이 많은 남원토양에서 0.82로 1보다 낮게 나타났으며, 유기물함량이 적은 무릉토양에서는 1.07로 1보다 높았다. EPN의 토양 중 용탈은 거의 일어나지 않았다. 토성별 용탈 경향은 농약의 흡착능이 큰 남원토양이 가장 침출이 적었고, 흡착능이 작은 무릉토양은 상대적으로 크게 일어났다. 한편 EPN은 도두와 위미에서의 해수와 저니토에서 모두 검출되지 않았다.

• 한국자기학회:학술대회 개요집
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• 한국자기학회 2000년도 International Symposium on Magnetics The 2000 Fall Conference
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• pp.413-420
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• 2000

Cheju Island has nature of typical trass through volcanic activities in many times. The soil in Cheju Island has principally sprung from basalt and partially made up of trachyte, trachyte's nature and site. Also ancient relics, plain coarse pottery's kilns and pantiles kilns are homogeneously distributed all over the Cheju Island. In this study, as a result of X-ray fluorescence spectrometer and Mossbauer spectroscopy of a sample are from plain coarse pottery and pantiles in 5 regions of Cheju Island. It is thought that these samples are partially formed from neutral volcanic rock like trachyte and Atomicity state of iron is almost Fe$\^$3+/. Also the magnetic hyperfine field length of goethite, contained these samples is less than synthetic goethite magnetic hyperfine field length and this result shows that disintegration of inner magnetic order, created by partial substitution of diamagnetic positive ion containing Fe$\^$3+/ and Al$\^$3+/ in goethite lattice.

• Journal of Magnetics
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• 제6권1호
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• pp.5-8
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• 2001

Cheju island is composed of volcanic tuff. The soil in Cheju island has principally sprung from basalt and partially made up of trachyte, and andesite. Also ancient relics, plain coarse pottery kilns and pantiles kilns are homogeneously distributed all over the Cheju island. In this study samples of plain coarse pottery and pantiles from five regions of Cheju island have been examined through X-ray fluorescence spectrometer and Mossbauer spectroscopy. It is thought that these samples be partially formed from neutral volcanic rock like trachyte and the valence state of iron is almost $Fe^{3+}$. Also the magnetic hyperfine field of goethite contained in these samples is less than synthetic goethite. This result shows the degradation of magnetic order caused by the partial substitution of diamagnetic positive ion $Fe^{3+}$ by $Al^{3+}$ in the goethite lattice.

• 한국환경과학회지
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• 제8권3호
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• pp.379-386
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• 1999

The adsorption and leaching of organophosphorus pesticides (phenthoate, diazinon, methidathion) were investigated in Namwon soli(black volcanic soil), Aewol soil(very dark brown volcanic soil) and Mureung soil(dark brown nonvolcanic soil) sampled in Cheju Island. The Freundlich constant, K value, was 52.4, 31.3 and 27.7 for phenthoate, diazinon and methidathion in Namwonsoil, respectively and decreased in the order of phenthoate, diazinon and methidathion among the pesticides. The K value of phenthoate was 52.4, 15.9 and 5.9 for Namwon, Aewol and Mureung soil, respectively and was the highest for Namwon soil with very high organic matter content and cation exchange capacity(CEC). The Freundlich constant, 1/n, showed a high correlation with organic matter content, i.e., its value was less than unity for organic matter rich soil(Namwon soil) and greater than unity for organic matter poor soil(Mureung soil). Total recoveries of pesticides in soil and leachate with leaching in soil column, were in the range of about 74~86%. The leaching of pesticides was less for phenthate with high K values, and more for methidathion with low K values among the pesticides. It was slower for Namwon soil with high K values, and more for methidathion with low K values among the pesticides. It was slower for Namwon soil with high K values, and faster for Mureung soil with low K values among the soils.

• 한국토양동물학회지
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• 제1권1호
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• pp.48-55
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• 1996

This study was carried out to investigate the arthropod fauna at tangerine orchards in Cheju-do island. To fulfil this purpose, samples were taken at 21 areas from the Cheju-do island 1985 to 1989. During this period, 33 species were identified, thus making 217 species, 99 genera, 31 families of spiders recorded from this island, In tangerine orchards alone, 26 species of spiders were found.

• 한국균학회지
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• 제26권1호통권84호
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• pp.97-102
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• 1998

제주도 일원 14개소의 감귤원에서 감귤 뿌리를 포함한 토양 시료를 95년 10월에 수집하여 VA균의 포자를 분리하여 관찰 동정하였다. 분리된 공생균근균은 3속 5종으로서 Acaulospora bireticulata, Glomus deserticola, G. geosporum, G. vesiculiferum, Sclerocystis pachycaulis였으며, Acaulospora sp.로 사료되는 두 가지는 아직 종동정이 되지 않았다. 이중에서 G. deserticola와 미동정된 Acaulospora sp.는 모든 시료토양에서 빈도가 매우 높게 관찰되어 우점종으로 사료되었으나, 다른 종에 속하는 포자들은 이들 종에 비하여 관찰 빈도가 매우 낮았다.

• 한국미생물·생명공학회지
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• 제24권4호
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• pp.399-403
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• 1996

Total 938 actinomycete strains were isolated from 59 soil samples collected at Cheju island. All of these isolates were identified to the genus level based on morphological and physiological characteristics. As the result, 62.6% of those isolates were Streptomyces, 16.4% were Micromonospora, 8.6% were Nocardioform group, 2.2% were Actinomadura, 1.7% were Microbispora, 1.6% were Nocardiopsis, 1.0% were Streptosporangium, and 5.9% were the others. As the sources of soil, Streptomyces and Microbispora were abundant in grassland soil, Streptomyces and Micromonospora were abundant in field soil, and Micromonospora were abundant in forest soil. Especially, Nocardioform strains were abundant in natural caves.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 1997년도 추계 국제학술심포지움 논문집
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• pp.97-142
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• 1997

The Seoguipo Formation occurs only in a small exposure along the coast of the Seoguipo City, but in the subsurface, underlies tile western part of the Bugcheon-Pyoseon Line in the northeastern part of tile island. The Bugcheon-Pyoseon Line is presumed to be a facies boundary that reflects tile distribution of hyaloclastites resulted from submarine volcanic activity. The Seoguipo Formation is distributed in the subsurface along the part which is lower than 400m in average altitude, and occurs at El. -5.76∼-46.63m in tile southern area, El. -41.89∼-57.97m in the western area, El. -13.15∼-50.59m in the northern area. Therefore, the southern area was uplifted after the deposition of the Seoguipo Formation. In the subsurface, the vertical depth of the volcanic rocks of the Cheju Volcanic Edifice is El. -40.6m in the southern area, El. -111.3m in the western area, El. -81.5m in the northern area and El. -134.7m in the eastern area. The unconsolidated U Formation, which is, overlying the basement and about 70∼250m thickness underlies the whole island. There is a positive correlation between tile groundwater level and the depth of the subsurface distribution of the Seoguipo Formation. Consequently, it is conformed that the subsurface distribution of the Seoguipo Formation plays important role for controlling the characteristics of the reservoir of tile groundwater in Cheju Island.