• Journal of Microbiology and Biotechnology
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• 제31권2호
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• pp.317-326
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• 2021

Vanillyl alcohol (VA), which is abundant in Vanilla bean, has strong antioxidant activity. However, the use of VA in the food and cosmetics industries is limited, due to its low solubility in emulsion or organic solvents. Meanwhile, medium chain fatty acids and medium chain monoglycerides have antibacterial activity. We synthesized butyric acid vanillyl ester (BAVE) or caprylic acid vanillyl ester (CAVE) from VA with tributyrin or tricaprylin through transesterification reaction using immobilized lipases. BAVE and CAVE scavenged 2,2-diphenyl-1-picrylhydrazyl radicals in organic solvents. In addition, BAVE and CAVE decreased the production rate of conjugated diene and triene in the menhaden oil-in-water emulsion system. While BAVE showed no antibacterial activity, CAVE showed antibacterial activity against food spoilage bacteria, including Bacillus coagulans. In this study, the antibacterial activity of vanillyl ester with medium chain fatty acid was first revealed. Zeta potential measurements confirmed that BAVE and CAVE were inserted into B. coagulans membrane. In addition, the propidium iodide uptake assay and fluorescent microscopy showed that CAVE increased B. coagulans membrane permeability. Therefore, CAVE is expected to play an important role in the food and cosmetics industries as a bi-functional material with both antioxidant and antibacterial activities.

• 동굴
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• 제85호
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• pp.38-40
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• 2008

With regard to Jeju Special Self-governing Province's natural-spa tourist spot development project, this paper has investigated the natural environment of Sehwa-Songdang Lave Region. According to this study, the cave consists of many small caverns with poor cave formations. Due to unfavorable climate conditions in the cave, in addition, hydrological environment is also very poor. In terms of vegetation, the cave shows the general vegetation environment of Jeju.

• 동굴
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• 제7호
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• pp.9-10
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• 1998

This is but a brief description of a cave which, although well known to local inhabitants, appears to be unknown to the N.Z.S.S. It is reputed to be one of several caves in this region, but we have so far been unable to continue our prospecting here as fully as is needed. The cave is in no way unique nor of an outstanding nature; being within an isolated remnant of a much younger limestone which appears to have once extensively overlain the old Paleozoic basement rocks of the Aorere valley region. It seems probable that it is in the same limestone as the well-known Te Anaroa tourist cave, at Rockville near Collingwood, and that of the Brown River caves south of Bainham.(omitted)

• 동굴
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• 제7호
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• pp.11-14
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• 1998

1. Stafford's Cave, named by the miners because a former visitor, Mr. Stafford, broke his leg in it, is the most northern of the three caves. The entrance lies concealed in the undergrowth, but is otherwise wide and open. A steep conical shaft leads down for a depth of about 80 ft from the floor of the cave; at the bottom, rammed in between the two walls, lies a great block of limestone below which a rivulet streams forth, flowing through the cave, which runs from east; in the cave it is joined by a little tributary.(omitted)

• 동굴
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• 제73호
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• pp.45-47
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• 2006

The modern people spend more time with heir family on weekends, and this changed the perspective toward leisure and tourism. Along with this, the recognition toward tourism resources have underwent various modifications with the increasing number of family tourists. Caves are categorized as lava tube (formed by volcano activity), lime stone cave(formed by absorption of water into underground level), sea cave (formed by wave erosion) and artificial cave that were made for the fluent traffic activity of railways or roads. Caves manifest characteristics of tourism as a natural resources and tourism as a humanity study, so caves are valuable as a multipurpose tourism resource.

• 동굴
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• 제74호
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• pp.23-31
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• 2006

(1) Kaeusetgul Cave in Kimnyong-Ri, Jeju-Do, Korea. Kaeuset-gul Cave (KC) is situated in NNE area of the Manjang-gul cave (125m a.s.l.). Kaeuset-gul Cave lies at $126^{\circ}45'22"$ E in longitude and $33^{\circ}33'09"$ N in latitude. The coast belong Kimnyeong-Ri, Kujwa-eup, Jeju-Do. Altitude of the cave-entrance is 10m and length of the cave is 90m. Lava hand-specimens of KC are studied by X-ray fluorescence analysis (XRF). Average major chemical components of specimens from KC is as follows (wt.%); $SiO_2=47.03$, $TiO_2=3.16$, $Al_2O_3=18.41$, FeO*=13.53, MnO=0.14, MgO=5.05, CaO=8.66, $Na_2O=2.81$, $K_2O=0.67$, $P_2O_5=0.55$ in KC. Polarizing microscopic studyindicates that these specimens are described of alkali-basalt. (2) Tachibori Fuketsu (Cave) in Shizuoka Prefecture, Fuji Volcano, Japan Tachibori Fuketsu lies attoward the south in skirt of the Fuji volcano, $138^{\circ}42'04"$ east longitude and $35^{\circ}18'00"$ north latitude. The location of cave entrance is 2745, Awakura, Fujinomiya-shi, Shizuoka Prefecture. The above sea level and length of Tachibori Fuketsu are 1,170m and 82m. Average major chemical components of specimens from cave areas follows (Total 100 wt.%) ; ($SiO_2$=50.52, $TiO_2$=1.69, $Al_2O_3$=15.47, FeO*=13.13, MnO=0.20, MgO=5.97, CaO=9.17, $Na_2O$=2.52, $K_2O$=0.94 and $P_2O_5=0.40).$ Polarizing microscopic study indicates that these specimens may belong to tholeiite-basalt series. According to polarizing microscopic study, Au (Augite), P1 (Plagioclase), and O1 (Olivine) are contained as phenocryst minerals. (3) Gorely Cave in Kamchatka Peninsula, Russia Gorely caldera is located at the southeastern part of Kamchatka Peninsula, about 75km southwest of Petropavlovsk-Kamchatskiy.. Gorely lava caves are situated in NHE area of Mt. Gorely volcano (1829m a.s.1.). One of lava cave (Go-9612=K-1) lies at $158^{\circ}00'22"$ east longitude and $52^{\circ}36'18"$ north latitude. The elevation of cave entrance is about 990m a.s.1. and the main cave extends in the NNW direction for about 50m by 15m wide and 5m in depth. The cave of K-3is near the K-1 cave. "@Lava hand-specimens K-1 and K-3 caves are studied by X-ray fluorescence analysis and polarizing microscopic observation. Average major chemical components of specimens from these caves are as follows (wt.%) ;($SiO_2$=55.12, $TiO_2$=1.25, $Al_2O_3$=16.07, T-FeO* =9.41, MnO=0.16, MgO=5.01, CaO=7.21, $Na_2O$=3.39, $K_2O$=1.92, $P_2O_5$=0.45) and these values indicate that the Gorely basaltic andesite belong to high alumina basalt. Polarizing microscopic study indicates that these specimens are described of Augite andesite.

• 터널과지하공간
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• 제19권3호
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• pp.236-247
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• 2009

도심지에서의 인구 및 시설물 과밀화 현상으로 인해 지하 공간의 효율적 활용 문제가 대두되고 있으며, 이에 대한 해결책으로 저심도 지하공간의 개발이 증가되고 있다. 그러나 저심도 터널 굴착시 예상치 못한 붕락 문제도 함께 증가하고 있으므로, 터널 붕락으로 인한 인명과 재산의 피해를 줄이기 위해서는 굴착 개시전에 암반거동 유형을 파악하고 분류하는 것이 필요하다. 특히 붕락(cave-in)의 경우 낙반이나 소성변형보다 발생규모가 크고 빠르게 일어나는 특징이 있으므로 이에 대한 대비책이 마련되어야 한다. 본 연구에서는 7가지의 매개변수-일축압축강도, 암질지수, 절리면 상태, 응력 상태, 지하수, 지진 및 진동, 터널 폭을 이용하여 붕락 거동 유형을 파악하고자 하였다. 이러한 매개변수로부터 붕락 거동을 예측하기 위해서는 현장 사례로부터 충분한 자료를 확보하여야하나 현장자료의 부족 등의 현실적인 한계를 고려하여 7가지 매개변수들간의 상호영향성과 가중치를 산정하기위해 전문가 집단의 의견과 암반공학시스템의 원리를 이용하였다. 그 결과로 저심도 암반터널에서의 붕락 거동 지수를 서울 지하철 9호선 000구간에 적용하였다. 한편 288가지 경우의 불연속체 해석을 통해 붕락 발생 유무를 확인하였고 이를 붕락 거동 지수와 비교하였다. 또한 로지스틱 회귀분석을 통해 도출된 회귀식으로 지보패턴별 파괴확률을 산출하였고 이를 붕락 거동 지수와 비교하였다.

• 동굴
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• 제71호
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• pp.43-44
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• 2006

• 동굴
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• 제79호
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• pp.17-30
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• 2007

난고 김삿갓의 생애 :선생은 안동 김씨의 시조인 고건 개국공신 신평의 후예로 순조 7년(1807년) 3월 13일 경기도 양주군 회천면 회암리에서 부 안근과 모 함평 이씨 사이의 2남으로 출생하였고, 본명은 병연(炳淵)이고 자는 성심(性深) 호는 난고(蘭皐) 별호는 김삿갓 또는 김립(金笠)이다. 순조 11년(1811년) "홍경래의 난"이 일어났을 때 조부 김익순이 선천부사로 있으면서 홍경래에게 항복, 역적으로 몰려 폐족처분을 받아 가족이 영월로 옮겨와 은둔생활을 하였다. 이러한 생활 속에서도 모친은 자식에게 조부의 사연을 감추고 글을 가르쳤으며, 20세 되던 해 영월 동헌에서 백일장에 응시하여 조부를 비판하는 글로 장원이 되었다. 그 후에 조부라는 사실을 알고 자책과 통한을 이기지 못하여 22세에 집을 나서 방랑생활을 하면서 서민들의 애환을 시로 읊어 서민문학의 큰 틀을 마련하였다. 1863년 전라남도 화순군 동복에서 작고하여 그곳에 묘를 썼으며, 3년 후 둘째 아들 익균이 지금의 묘로 옮겨 모셨다. (난고선생 묘 옆에 서있는 안내문에서)

• 동굴
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• 제5호
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• pp.79-95
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• 1997

The main purpose of this article is to compare different mapping techniques, so that an appropriate one may be chosen for a particular cave. Ultra-accurate techniques such as using tripods are not discussed here, as their application is limited to a small minority of caves. Most modem mapping is carried out under time restraints, due to the shortness of an expedition or the difficulty of a cave; thus, rapid mapping techniques are emphasized here.(omitted)