• 한국식품과학회지
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• 제30권2호
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• pp.253-259
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• 1998

전남지역 약수의 수질특성을 파악하고자 오랫동안 음용되어온 전남 도내 47개 약수터를 대상으로 약수 중에 함유되어 있는 성분 중 가장 함유량이 많은 미네랄 성분을 분석하였으며 아울러 건강하고 맛있는 물에 대한 지표를 설정하기 위한 기본자료를 제공하고자 하였다. 17종의 미네랄 성분을 분석한 결과, 최대분포율을 보이는 주요 미네랄 성분의 평균농도(mg/L)는 Ca 3.9, K 0.78, Na 7.4, Mg 0.7, Si 9.4, Ba 0.004, Ni 0.007, F 0.16, Cl 4.9, $SO_4$ 1.5, Fe 0.001, Zn 0.002이었으며 항목별 상관성 분석결과 Na, K, Ca, Mg, $SO_4$, Cl, Ba, Ni은 통계적으로 유의한 상관성(p<0.05)을 보였다. 건강한 물의 지표인 K index와 맛있는 물의 지표인 O index를 적용한 결과 도내 약수의 98%는 건강에 도움이 되거나 맛있는 물로 확인되었고 이 중 건강에 유익하고 맛있는 그룹에 속하는 약수의 K와 O index값은 각각 6.3과 5.2로 나타났다.

• 한국지하수토양환경학회지:지하수토양환경
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• 제23권6호
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• pp.9-27
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• 2018

In recent years, the sales of bottled spring water (BSW) have been drastically increasing in Korea and other countries, which accompanied great interests in conservation and reclamation of natural mineral water (NMW). In this study, management and research activities on NMW in Europe, USA, and Codex Alimentarius were reviewed. In each region, NMW is regulated with its own quality standards that differ from ordinary drinking water, and management actions are strictly implemented to protect water resources and to secure quality of NMW. Many studies on NMW were carried out for monitoring inorganic constituents including major and trace elements in national levels for bottled NMW, groundwater, and tap water in other countries. In Korea, NMW became commercialized in 1995 when BSW was legally approved as a drinking water. To further promote utilization of various types of NMW in Korea, regulations and policies for NMW need to be revised in accordance with international NMW management trends. Further, studies of NMW that compile a comprehensive set of physical and chemical parameters of NMW are also needed to properly understand occurrences, hydrogeological and geochemical processes of NMW, as well as to evaluate its potential use as a natural resource.

• 대한한방소아과학회지
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• 제25권3호
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• pp.77-84
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• 2011

Objectives: This study was performed to investigate the effect of hot spring therapy on children weight, body composition and heart rate variability. Methods: The study was carried out from 30 children who visited the spa from August 1, 2011 to August 31, 2011. We measured the change of weight, body composition, and heart rate variability after hot spring therapy for an hour per day. Results: The subject was consisted of 13 boys and 17 girls. This study revealed that their weight got lost from a hot spring therapy, which was statistically significant. Their body mass index(BMI) was decreased in from a hot spring therapy, which was not statistically significant. Total body water, muscle, protein, and mineral were decreased from a hot spring therapy, which was statistically significant. We measured HRV(heart rate variability) before and after the hot spring therapy. The mean HRT was increased, which was statistically insignificant. SDNN(standard deviation of the NN interval) and RMSSD(square root of the mean of the sum of the square of differences) were not different before and after the hot spring therapy. ln TP was decreased insignificantly. ln VLF was not affected before and after hot spring therapy. ln LF and ln HF was decreased, LF norm was increased, and HF norm was decreased, which were not statistically significant. Also, LF/HF ratio was increased insignificantly. Conclusions: From these results, we concluded that the weight, total body water, muscle, protein, and mineral got lost from the hot spring therapy. However, the HRV was not affected from the hot spring therapy.

• 한국지하수토양환경학회지:지하수토양환경
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• 제23권6호
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• pp.37-45
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• 2018

The source of Chusan Spring water in the Ulleungdo is the precipitation in the Nari caldera basin, which permeates in the Trachitic pumice and tuff area and moves downward, outflowing at the lithologic boundary between the trachyte and Nari tuff. It is known that the discharge rate of the Chusan Spring is large enough to be used for the small hydroelectric power generation, but the exact discharge rate and hydrogeologic characteristics have not been known. The discharge rates of the Spring were measured 11 times, which ranged from $15,220m^3/d$ to $36,278m^3/d$. The discharge rates, measured by the automatic level recorder, for two-year period, were $20,000{\sim}38,000m^3/d$. The variation of discharge rates did not coincide with rainfall event, but showed daily increases of $3,000{\sim}5,000m^3/d$. The annual discharge rate excluding the evapotranspiration and the surrounding stream discharge corresponded to 70.6% of the annual precipitation of the recharge area. Therefore, meteorological observations at the Nari basin, rather than the Ulleung-do meteorological station, are more appropriate to properly interpret the discharge characteristics of the Chusam Spring and the recharge rate of the basin.

• 지질공학
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• 제34권2호
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• pp.207-216
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• 2024

이 연구는 울릉도 나리분지 추산용천수의 유동 경로를 파악하는 것이다. 칼데라 내부 가장자리를 따라 발달하는 단층과 단열구조들의 발달 방향이 추산용천수 유동 경로에 영향을 주는 요소로 파악되었다. 추산용천수는 함양된 지하수가 동서 방향과 남북 방향의 단열대를 따라 추산용출소 방향으로 흐른다. 이와 더불어 북북동 방향으로 경사진 칼데라의 부등함몰의 영향으로 북동 내지 북북동 방향으로 흐르는 것으로 파악되었다. 장내세균과인 Entrobacteriaceae을 이용하여 나리지하수 쪽의 물이 추산용출소 방향으로 유동하는 것으로 파악되었다. 다만, 분석에 사용된 시료수가 매우 적어 성인계곡수로부터 나리분지와 추산용출소까지의 유동경로를 전체적으로 파악할 수 없다는 제한성이 있다.

• 자원환경지질
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• 제32권5호
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• pp.455-468
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• 1999

Carbonated mineral waters fo $Ca(Mg)-HCO_3$ type spring out fissure of Jurassic granite in the valley floor of the Chungsong area. The water has been long as a Dalki medicinal water because of its unique therapeutic effect against clacium deficit, stomach and skin troubles, ect. The water has a high $CO_2$ concentration ($P_{CO_2}$=0.51~1.12atm) and exhibits strong pH buffering (5.9~6.26) by $H_2CO_3/HCO_3$ couple. Electrical conductivity ranges from 1,900 to 3100 $\mu$S/cm. Environmental isotopic data $(^{2}H/^{1}H, ^{18}O/^{16}O \;and \;^3H)$ indicates that the water is of meteoric origin recharged in the Cretaceous sedimetary strata distributed in upper part of the catchment area at least before 1950s, The high $P_{co_2}$ and carbon isotope data (${\delta}^{13}C=-3\sim-0.2\textperthousand$) suggest that the potential source of carbonated mineral water was originated in deep-seated $CO_2$ as wel as aboundant carbonate minerals of sedimentary desimetary rocks. The major source minerals of the dissoved species in the carbonated mineral water appear to be carbonate minerals, albite and K-feld-spar in sedimentrary rocks.

• 지질공학
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• 제30권3호
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• pp.379-397
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• 2020

본 연구에서는 1922년부터 2019년까지 동래온천수의 장기적인 온천수 수질 변화 특성을 살펴보았다. Mann-Kendall 분석과 Sen의 기울기에 의해서 동래온천수의 장기적인 수질 특성 변화를 분석하면, 온도, Ca, SiO₂, HCO₃는 증가 추세를 보이는 반면에 EC, Na, K, Mg, Cl, SO₄은 감소 추세를 보이거나 또는 거의 추세 변화를 보이지 않는다. 동래온천수의 수질유형은 시간경과에도 변하지 않고 Na-Cl형에 안정적으로 속하고 있다. 2004년, 2009년, 2014년, 2019년의 수질 자료를 이용한 공간 분포도에 의하면, 시기별로 변동을 보이며, 시료 채취 지점에 따라 값의 변화를 보인다. 이는 장기적인 온천수 개발에도 불구하고 동래온천수의 공간적인 수질 특성은 거의 일정하다는 것을 지시한다.

• Environmental Analysis Health and Toxicology
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• 제24권4호
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• pp.293-301
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• 2009

This study was conducted to investigate the distribution of the concentrations of selected trace metals and inorganic anions in five types of drinking water samples (mineral spring water, well water, small community water, municipal tap water, and commercial mineral water) collected from Chuncheon, Gangwon-do in 2007. Forty four samples were analyzed for five metals and five anions using an atomic absorption spectrometer and an ion chromatograph, respectively. Arsenic (As) and nitrate (${NO_3}^-$) concentrations in some groundwater samples did not meet the future (10 ${\mu}g/L$) and current (44 mg/L) Korean drinking water standards, respectively. On the other hand, any municipal tap water samples, the sources of which were lake surface water, satisfied the Korean standards. Human health risk assessment results showed that arsenic in all types of water, especially groundwater including commercial mineral water, may pose both noncarcinogenic and carcinogenic effects on the residents. It is concluded that groundwater is not safe drinking water any longer and that a national survey and follow-up measures need to be taken.

• 한국환경보건학회지
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• 제17권2호
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• pp.27-34
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• 1991

This study was carried out to investigate the use habit of drinking water. The survey data were collected from 1,282 of students and 175 of officers from September 1990 to June 1991 in Pusan city and the South of Kyung sang-do. The use rate of tap water among respondents was 33.5%, and the reasons that the others avoid using tap water were having the risk of heavy metals contamination and unsanitary. The 80% of respondents have drunk spring water or bottled water within two or three years. The keeping method of them were 53% in the refrigerator, and 33% in the indoor. The use rate of water vessels what were equipped in mineral springs was 85%. It's advisable that the picking of mineral water be cautious within two or three days after rain. The holding rate of water purifier in respondents was about 20%, and it was purchased within one or two years and the reliance degree of that in users was below 50%.

• 지질공학
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• 제34권1호
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• pp.13-24
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• 2024

이연구는 울릉도 나리분지의 추산용출소에서 20,000~40,000 m³/day의 많은 수량이 용출될 수 있는 지배요소를 파악하기 위하여 나리분지의 지형 및 수리지질학적인 특성을 밝히는 것이다. 용천수가 용출되는 추산용출소 인근에는 층리가 잘 발달되어 있는 부석질 응회암과 라필리 응회암이 분포하고 있다. 추산용천수는 응회암의 엽층리나 부석질 응회암이 차별적으로 침식된 특별한 층준에서 렌즈상의 침식동굴처럼 발달한 곳을 따라 용출하는 구조를 보이고 있다. 추산용출소가 위치하고 있는 지점은 나리분지의 평탄면이 끝나고 급경사가 시작되는 곳으로, 모든 방향의 사면이 닫혀 있고, 추산용출소가 위치한 북쪽만 열려 있는 형태이다. 이러한 지형적인 특성으로 추산용출소는 나리분지 집수유역의 최종적인 유출구로 작용하고 있다.