• 대한통합의학회지
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• 제11권4호
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• pp.189-198
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• 2023

Purpose: This study aims to investigate the preferences of hot spring users regarding the utilization of Asan's hot springs after the COVID-19 pandemic. Methods: A survey was conducted on 340 hot spring users visiting hot spring resorts in the Onyang, Dogo, and Asan hot spring districts. The survey was conducted twice from November 5th to November 7th, 2021, and from May 25th to 26th, 2022. The survey included general questions, such as the frequency of hot spring usage, the purpose of visits, and the intention for future visits. Specific questions were related to Asan hot springs, focusing on the reasons for choosing Asan, its perceived advantages, and improvement suggestions. Results: The survey revealed that the average number of visits to hot springs was less than five in the past five years, and the main reason for visiting was to recover from fatigue. A percentage of respondents said they would use hot springs more often when the COVID-19 pandemic ends. When asked about their reasons for visiting Asan hot springs, responses varied by age. However, across all groups, the majority considered "good water" as an advantage of Asan hot springs, while improvements to "hot spring facilities" was the highest response among all age groups. Thus, despite the decline in the number of customers due to COVID-19, the overall perception of hot springs remains positive. This suggests a promising future for the hot spring industry, with the potential for a return to pre-pandemic usage levels. Conclusion: These results provide valuable foundational data for informing policy development aimed at revitalizing the hot spring industry in the post-COVID-19 era.

• 농촌계획
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• 제13권1호
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• pp.85-95
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• 2007

Hot springs development will be more activated with the five-day work week system than before. Nevertheless, investment and development achievement of hot springs has not resulted in a successful performance to foster townships, and this calls upon locals to build a guideline to develop hot springs. This study intends to analyze laws on hot springs, which influence mostly on the hot spring development, to gather up the information on the present state of the development, and to suggest considerations for further development plans. Features of the hot spring development are as follows: One is that metropolitan cities will discover hot spring resources more than small cities. Therefore the development will be twofold : one for resort tour and the other for one-day rest and recreation. In addition, Korean laws on hot springs are more site development-oriented to support tourism and recreation than to protect environment and discover unused resources. This makes hot spring development easier and efficient being supported by hot spring law, law on territory development and use, and tourism promotion law. On the other side, planned landscape trimming can be uniformized and unharmonized in terms of local identity and environment-friendliness. This is why careful considerations such as goods and bads of the local resources, local history and culture are needed in hot spring development. A long-term development project should include remodeling based on local identity and development trends. The third point indicates that Korean hot springs development has recorded relatively low performance due to difficult private capital attraction, and a high fence on land purchase and development approval. It is essential to release restrictions on the hot spring development-especially on those whose development performance has not been successful so that best practice can be supported by the government in remodeling and marketing. New plans on hot spring development should be also examined based on developer's capacity and local authorities' volition on the plan. Last point shows that most hot springs development plans have been designed only based on territory utilizing plan and facilities arrangement, not considering much on fund-raising, operational plan or feasibility analysis. Therefore the tourism promotion law should reinforce guidelines on tourist site approval system by supplementing criteria. At the same time, an education on tourism development planning is necessary to deepen developers' understanding, since most developers are experts more on city development, landscape architecture, designing, constructing and engineering than tourism development.

• 농촌지도와개발
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• 제18권2호
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• pp.281-313
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• 2011

67.82% of domestic hot springs are in rural areas. (Ministry of Public Administration and Security statistics, 2010) Most of hot spring's facilities are aging and inability to accommodate the current changes of leisure patterns. So, a decrease of the number of visitor to the hot spring resulted in economic decline of rural areas. Hot spring has been studied, but Architecture of Hot Springs has never been interested in and research. Therefore, Nation architecture of Hot spring and foreign architecture was compared and analyzed. Then, Architectural characteristics of Hot spring in rural areas was identify. The architecture of Hot spring type of foreign and images are routinely burned, the organic form and old-fashioned adrift. However, our country found in Hot spring architecturally and daily life had any features. Thus, the country's hot springs spa area for construction of the architecture design should be characterized. And, through institutional guidelines and deliberations should be provided in the right direction.

• 헤리티지:역사와 과학
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• 제57권1호
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• pp.110-123
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• 2024

온양행궁은 <온천행궁도(溫泉行宮圖)>『온궁사실(溫宮事實)』(1795), 『영괴대기(靈槐臺記)』 및 <영괴대도> 등의 문헌자료와 영괴대(靈槐臺), 신정비(神井碑)로 왕의 온행을 확인가능한 문화유산이다. 특히 1906년 헤르만 산더(Hermann Sander)가 촬영한 사진을 통해, 조선시대 온양행궁의 온천(탕실)이 일제강점기 초기까지 유지되고 있음을 확인할 수 있다. 본 연구는 온양행궁 관련 문헌 및 <온천행궁도>(1795)에 기초하여, 온양행궁 탕실의 건축형식을 밝혀내는 것을 목적으로 하고 있다. 이를 위해 첫째 온양행궁 및 탕실의 변천을 살펴보고, 둘째 왕의 목욕문화 및 행태를 고찰한 후, 셋째 <온천행궁도> 온천(탕실) 건축을 「온궁수리」를 통해 정리하고, 넷째 일제강점 초기 헤르만 산더(Sander)의 사진과 비교하여 조선 후기 마지막 온양행궁 온천(탕실) 건축 형식을 고찰하였다. 이상의 연구결과 다음과 같은 결론을 얻을 수 있다. 첫째, 온양행궁 온천(탕실)은 현종 초 온정실(溫井室, 8칸), <온천행궁도> 온천(탕실)로 이어지면서 조선 후기 『호서읍지』(1871)까지 유지되고 있는데, 일제강점기 초기 헤르만 산더(1906) 및 <1912년 충남 아산시 온양온천>(한국저작권 위원회) 사진 건축물과 일치하고 있다. 둘째, 조선시대 국왕의 목욕법은 목욕평상(沐浴平床) 또는 교의(交倚)에 앉아 세두, 유두, 목두 등을 시행하거나, 온천수 증기를 직접 쐬는 훈세, 탕정 앞에 목판을 깔고 앉아 물에 발을 담그는 침족 또는 침세, 그리고 배꼽 아래만 물에 담그는 반신욕인 체욕, 좌탕 등의 다양한 목욕방법을 채택하였다. 셋째, 온양행궁 온천(탕실)은 온천수가 상탕 서북쪽에서 분출되어 동쪽으로 꺾여 중탕으로 들어가고 남쪽으로 꺾어지면서 바깥으로 나와 하탕이 되는 구조로서, 탕체 주변부는 태안에서 실어 온 바둑돌을 탕실 바닥에 깔았다. 이상의 고찰로부터, 어실로부터 왕의 접근동선, 왕의 목욕법과 목욕도구, 입대하는 의관과 목욕보조 인력 등 목욕행태와 「온궁수리」에서 언급된 각 실 등의 구성을 헤르만 산더의 사진과 비교하여, 온양행궁 온천(탕실) 건축물을 추정할 수 있다.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2003년도 Proceedings of ACRS 2003 ISRS
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• pp.28-30
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• 2003

Hot Spring Law of Taiwan was passed in legislative assembly on 3 June 2003. Hot springs would become one of the most important natural resources for recreation purposes. Both public and private sectors will invest large amount of capital in this area in the near future. The value of remote sensing technology is to give a critical tool for observing the landscape to find out mega-scaled geological structures, which may not be able to be found by conventional approaches. The occurrences of the hot springs in Taiwan are mostly in metamorphic and sedimentary rocks , other than in volcanic environments. Local geothermal anomaly or heat of springs transfer by liquid convection other than conduction or radiation. The deeply -seated fractures of hard rocks are the conduit of the convection of hot water, which could be as deep as 3000 meters in a hypothetical model of Taiwan. Clues to find outcrops of hot spring can be obtained by a structure-controlled model deduced by geological lineaments observed by satellite images and stereoscopic interpretation of aerial photographs. A case study conducted in Eastern Taiwan will be demonstrated.

• ALGAE
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• 제24권4호
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• pp.185-193
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• 2009

Geothermal springs in India, formed as a result of volcanic or tectonic activities, are characterized by high temperature and relatively abundant reduced compounds. These thermal springs are inhabited by characteristic thermophilic organisms including cyanobacteria. Cyanobacteria are among the few organisms that can occupy high temperature aquatic environments including hot springs. In alkaline and neutral hot springs and streams flowing from them cyanobacteria can form thick colourful mats that exhibit banding patterns. The present investigation involves study of mat forming cyanobacterial flora from hot springs located in Bakreswar, West Bengal, India. The important species found are Synechococcus bigranulatus, S. lividus, Gloeocapsa gelatinosa, G. muralis, Phormidium laminosum, P. frigidum, Oscillatoria princes, O. fragilis, Lyngbya lutea, Pseudanabaena sp., Calothrix thermalis, and Fischerella thermalis. Their distribution pattern in relation to physico-chemical parameters of spring water has also been studied. Three cyanobacterial strains of the above mentioned list were grown in culture and their pigment content and nitrogen fixing capacity were also studied. Nitrogen fixing capacities of Calothrix thermalis, Nostoc sp. (isolated in culture) and Fischerella thermalis are 5.14, 0.29, and 2.60 n mole $C_2H_4/{\mu}g$ of Chl-${\alpha}$/hr respectively. Carotenoid : Chlorophyll-${\alpha}$ ratio of four mat samples collected from Kharkunda, Suryakunda, Dudhkunda and bathing pool are 2.45, 1.60, 1.48, and 1.34, respectively. Higher value of Carotenoid : Chlorophyll-${\alpha}$ ratio coincided with higher temperature.

• 대한화학회지
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• 제14권1호
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• pp.75-83
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• 1970

忠南 溫陽邑內의 地下水中의 弗素含量을 1969年 8月 19日부터 同年 11月 5日까지 사이에 測定하였다. 溫泉에서부터0.9km 以內의 地域內에 있는 地下水 中에는 1.0mg/l以上의 $F^{-1}$이 含有되어 있으며,1.2km 以內의 地域內에 있는 것에는 0.3mg/l 以上의 $F^{-1}$이 含有되어 있어 이들 地下水를 齒牙 生長期에 飮料水로 常用時에는 班狀齒의 原因이 되므로 住意해야 되며, 溫泉에서 1.2km∼3.9km 以內의 地域內에 있는 地下水에는 0.04∼0.29mg/l의 $F^{-1}$을 含有하고 있어서 모두 치아우식억제효과를 얻을 것이다. 溫泉 附近에서는 溫泉水에 岩石中의 $F^{-1}$이 $Ca^{+2}$과 함께 溶出되어, 이들 溫泉水가 地下水에 混入된다고 보여진다. 溫泉에서 먼 距離의 地下水에는 有機物의 分解에 基因하는 $F^{-1}$도 含有되어 있다고 보여진다.

• 한국신재생에너지학회:학술대회논문집
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• 한국신재생에너지학회 2005년도 춘계학술대회
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• pp.674-677
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• 2005

The characteristics of geothermal resources in Korea was roughly estimated using hot springs, 580 geothermal gradients and 338 heat flow data. In the aspect of hot springs with geologic structure, location of hot springs coincide with fault zone, especially younger age of Cretaceous to Tertiary. In the aspect of geothermal gradients, Pohang area shows the highest geothermal gradient anomaly, which is covered with unconsol idated rock of low thermal conductivity preserving the residual heat from igneous activity or radioactivity elements decay. In the aspect of heat flow density, high anomaly can be found along the zone connecting Uljin-Pohang-Busan on the southeastern part of Korean peninsula at which big fault zone as Yangsan fault is well developed.

• 한국신재생에너지학회:학술대회논문집
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• 한국신재생에너지학회 2008년도 춘계학술대회 논문집
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• pp.621-625
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• 2008

There are nine hot spring wells at Icheon hot spring area, hot springs are pumped by submersible motor. Drilling depths of hot spring wells is about 166-294 m, piezometric heads of hot springs is about 50 m below the surface. The geothermal gradient of SB-2 is about $64.00^{\circ}C$/km from the surface to depth within 300 m which is the highest value, that of SB-1 is about $45^{\circ}C$/km which is the lowest value. In addition, the average geothermal gradient of the region is calculated at approximately $54.28^{\circ}C$/km. However, it is analysed that this area has highly irregular temperature distribution because the groundwater penetrated to the depth of 720 m through the fracture rise to the surface according to the results of the data after drilling well to the depth of 996 m.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2004년도 임시총회 및 추계학술발표회
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• pp.115-118
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• 2004

The purpose of this research is to investigate the noble gas isotope and the hydrochemical characteristics of hot springs in the Chungcheong area in Korea. This study was carried. out by the financial support of Korea-Japan joint research program of KOSEF, Noble gases are very useful tracers to investigate volatile elements circulation, because of their unique isotopic compositions in various reservoirs of the Earth. Isotopic ratios of noble gases has been carried out for If hot-spring samples from Daejon and its near areas in Korea last January 2004. Helium isotope ratio gave the evidence that helium gas of different origins(air-crust mixing origin, crust-origin and mantle-origin) is supplied into hot-spring waters in Korea. We found the distinct relationship between temperature of hot springs and helium gas origin.