• The Journal of Engineering Geology
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• v.21 no.1
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• pp.65-77
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• 2011

Hydrochemical and carbon isotopic (${\delta}^{13}C_{DIC}$) analyses of 11 water samples, and noble gas isotopic analyses of 8 water samples collected in the Kyeoungbuk and Kangwon areas of Korea were performed to determine their hydrochemical characteristics and to interpret the source of noble gases and $CO_2$ gas in the water. The carbonated mineral waters are weakly acidic (PH = 5.59-6.04), and electrical conductivity ranges from 302 to $864\;{\mu}S/cm$. The chemical composition of all the water samples is Ca-$HCO_3$ type. The high contents of Fe and Mn exceed the safe limits for drinking water. The ${\delta}^{13}C_{DIC}$ values of the samples range from -5.30‰ to -2.84‰, indicating that the carbon is supplied mainly from a deep-seated source and to a lesser degree from an inorganic carbonate source. The $^3He/^4He$ ratios of the samples range from $1.51{\times}10^{-6}$ to $6.45{\times}10^{-6}$. The samples plot into three groups on a $^3He/^4He$ versus $^4He/^{20}Ne$ diagram: the deep-seated field (e.g., a mantle source), the atmospheric field, and the air-mantle mixing field. A wide range of $^4He/^{20}Ne$ ratios is observed ($0.036{\times}10^{-6}$ to $1.76{\times}10^{-6}$), indicating that while radiogenic $^4He$ is dominant in these water samples, mantle-origin He is also present. The supply of $CO_2$ gas and noble gases from a deep-seated source to carbonated waters is inferred to be controlled by geological structures such as faults and geological boundaries.

• The Hankook-Saengyark Bo
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• no.238
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• pp.2-2
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• 2000

대구약령시 활성화 대곡동에 약초 식물원 - 한강변, 한의학 문화벨트 조성 - 내고장 특산물

• Journal of the Korean Chemical Society
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• v.44 no.4
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• pp.380-386
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• 2000

• Monthly Korean Chicken
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• v.18 no.2
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• pp.103-105
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• 2012

• Proceedings of the Korean Environmental Sciences Society Conference
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• 1999.04a
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• pp.259-261
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• 1999

• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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• 2003.09a
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• pp.540-542
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• 2003

산을 관통하는 터널은 기존의 지하수위를 낮추어 지하수량 및 수질 변화와 함께 주변 식생에 영향을 미칠 수 있다. 본 연구는 서울시 내부 순환도로 건설에 따라 관악산을 관통할 예정인 터널 건설로 인한 지하수 환경변화를 이해하고자 한다. 즉, 현재 산출되는 지하수, 약수 및 지하수 화학특성을 파악하고 지하수 수문 자료와 연계하여 향 후 수질변화 가능성을 예측하고자 한다. 조사 지역에 분포하는 지하수는 지하수위가 대체로 최대 2m 정도에서 최대 20m를 넘지 않으며 일부 관정은 계절에 따라 수온 변화를 보여 지표수와 연계성을 시사한다. 전반적으로 중성에서 약산성을 띄며 이는 화강암과 화강 편마암으로 이루어진 이 지역의 지질특성에 기인한 것으로 생각된다. piper diagram에 도시하였을 경우 지표수는 지하수에 비하여 Na, K 에 비하여 Ca, Mg, Cl, SO$_4$가 우세한 반면 지하수와 약수의 경우 뚜렷한 특성 차이를 보이지 않으며 넓은 영역에 걸친 분포를 보인다.

• Journal of Korean Society of Water and Wastewater
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• v.25 no.1
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• pp.7-14
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• 2011

This study was motivated by the purpose of improving the O-Index, currently used to quantify water tasty. The authors first develop the M-Index after normalizing Ca, K, and $SiO_{2}$ concentrations in the spring water, in that the concentrations are subject to their log-normal distributions. The M-Index is then compared with the O-Index based on the results of sensory tests, revealing that sensory tests are correlated with the M-Index much more than the O-Index. Furthermore, the developed index is applied to evaluate water sampled from 53 springs in Korea. It is concluded that water, sampled from five most famous springs, has high values in M-Index. In addition, water, collected from springs that are relatively accessible, contains low values, and thus is expected not to tasty good.

• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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• 2000.05a
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• pp.160-161
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• 2000

• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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• 1999.04a
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• pp.37-38
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• 1999

• The Korean Journal of Food And Nutrition
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• v.26 no.4
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• pp.706-712
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• 2013

This is the basic study on the extraction characteristics of Omija (Schizandra chinensis) for juices of Korean traditional foods. Extraction is being performed as 25 times of the solvent ratio at room temperature and at $65^{\circ}C$ with deionized water, tap water and Cheong-song mineral water which have high contents of Ca and Mg. The overall good results of the extraction conditions are calculated from the values of L (Lightness), redness (a), yellowness (b), soluble solids content, acidity, pH levels and the DPPH radical scavenging activity by using the electron donating ability (EDA). The results are as follows: 12 hours of room temperature and 6 hours at $65^{\circ}C$ were good extraction times. The Cheong-song mineral water at $65^{\circ}C$ is available for rapid extractions when compared to deionized water and tap water. A longer extraction time shows lower values of acidity but increasing values of soluble solids content and DPPH radical scavenging activity when using the electron donating ability. The best sequences for the extractions are Cheong-song mineral water followed by tap water and distilled water after overall consideration.