증편 제조시 콩물과 반죽 내의 $\alpha$-amylase활성 및 특성에 관한 연구

나한나,윤선,김정수,김보영,Na, Han-Na,Yoon, Sun,Kim, Jung-Soo,Kim, Bo-Young 한국식품조리과학회 1998 한국식품조리과학회지 Vol.14 No.3

증편의 발효시 일어나는 이.화학적 성질의 변화는 발효 중 생성되는 $\alpha$-amylase의 활성과 밀접한 관계를 가지고 있을 것이다. 이에 본 연구에서는 콩물과 발효시간에 따른 증편 반죽 내의 $\alpha$-amylase 활성과 특성을 측정하였다. 콩물과 증편 반죽에는 생전분과 호화전분을 기질로 하는 $\alpha$-amylase가 존재함이 밝혀졌다. 콩물 $\alpha$-amylase 의 호화전분과 생전분에 대한 $\alpha$-amylase의 비활성도는 각각 0.79 units/mg protein, 0.036 units/mg protein 이었다. 콩물의 $\alpha$-amylase는 호화전분과 생전분에 대해 pH 5.92, 6.87과 6$0^{\circ}C$에서 최대 활성을 나타내었다. 증편 반죽의 호화전분과 생전분에 대한 $\alpha$-amylase의 최적 pH는 5.25였고 최적 온도는 5$0^{\circ}C$였다. 증편 반죽내의 $\alpha$-amylase의 활성은발효 시간에 대해 일정한 경향을 가지고 있지 않았다. 콩물을 첨가한 반죽의 호화전분에 대한 $\alpha$-amylase의 비활성도는 평균 25.59 units/mg protein이었고 생전분에 대한 $\alpha$-amylase의 비활성도의 평균은 1.37 units/mg protein이었다. 콩물을 첨가하지 않은 반죽에서의 호화전분과 생전분에 대한 $\alpha$-amylase의 비활성도는 각각 3.37 units/mg protein, 0.49 units/mg protein이었다. $\alpha$-amylase의 활성은 기질에 상관없이 콩물 첨가한 군이 그렇지 않은 군보다 유의적으로 높았다(p<.05). The activity and characteristics of ${\alpha}$-amylase in soy milk as well as in Jeungpyun batters were determined to investigate the enzyme system related to Jeungpyun preparation. ${\alpha}$-Amylase activity was detected in soy milk as well as in Jeungpyun batters. Soy milk had ${\alpha}$-amylase activity of 0.79 units/mg protein for gelatinized starch and 0.036 units/mg protein for raw starch. ${\alpha}$-Amylase in soy milk showed maximum activities at pH 5.92∼6.87 and at 60$^{\circ}C$ for both gelatinized starch and raw starch. ${\alpha}$-Amylase activities of Jeungpyun batters containing soy milk were 25.59 units/mg protein for gelatinized starch and 1.37 units/mg protein for raw starch. Jeungpyun batters without soy milk demonstrated ${\alpha}$-amylase activities of 3.37 units/mg protein for gelatinized starch and 0.49 units/mg protein for raw starch. ${\alpha}$-Amylase of Jeungpyun batters showed an optimal activity at pH 5.25 and at 60$^{\circ}C$ for both gelatinized and raw starch. The results demonstrated that Jeungpyun batters with soy milk showed significantly higher ${\alpha}$-amylase activity than the ones without soy milk.

지하수 모델의 주요 경계조건에 대한 민감도 분석 사례

나한나,구민호,차장환,김용제,Na, Han-Na,Koo, Min-Ho,Cha, Jang-Hawn,Kim, Yong-Je 한국지하수토양환경학회 2007 지하수토양환경 Vol.12 No.3

Appropriate representation of hydrologic boundaries in groundwater models is critical to the development of a reliable model. This paper examines how the model predictions are affected by the uncertainty in the conceptualization of the hydrologic boundaries including groundwater divides, streams, and the lower boundaries of the flow system. The problem is analyzed for a study area where a number of field data for model inputs were available. First, a groundwater flow model is constructed and calibrated for the area using the Visual Modflow code. Recharge rate is used for the unknown variable determined through the calibration process. Secondly, a series of sensitivity analyses are conducted to evaluate the effects of model uncertainties embedded in specifying boundary conditions for streams and groundwater divides and specifying lower boundary of the bedrock. Finally, this paper provides some guidelines and discussions on how to deal with such hydrologic boundaries in view of developing a reliable conceptual model for the groundwater flow system of Korea. 지하수 모델 개발 시 수문 경계를 실제 지하수계에 부합되도록 개념화하는 것은 모델의 신뢰도를 결정하는데 매우 중요하다. 본 논문에서는 지하수 분수령, 하천, 대수층의 하부 경계면 등의 수문 경계를 모델에서 개념화할 때 수반되는 불확실성이 모델 결과에 미치는 영향을 고찰하였다. 첫째, 연구지역을 대상으로 현장시험을 수행하여 모델 입력 자료를 확보하였으며, Visual Modflow 프로그램을 이용하여 연구지역에 대한 지하수 흐름 모델을 개발하였다. 지하수 함양량을 모델 보정 인자로 설정하였으며, 현장에서 관측된 지하수위 자료를 이용하여 모델을 보정하였다. 둘째, 민감도 분석을 통하여 지하수 분수령의 위치, 하천 지류들의 경계조건 설정 여부, 암반의 하부 경계면의 위치 등이 모델 결과에 미치는 영향을 정량적으로 분석하였다. 셋째, 민감도 분석 결과에 근거하여, 국내 지하수계를 대상으로 신뢰성 있는 개념 모델을 개발하고자 할 때 요구되는 주요 내용들을 토의하였으며, 현장조사 단계에서 부지특성화를 위해 필요한 효과적인 전략을 제시하였다.

쌍천 지하댐의 효용성 평가를 위한 지표수-지하수 통합 수문해석

김남원,나한나,정일문,Kim, Nam-Won,Na, Han-Na,Chung, Il-Moon 대한자원환경지질학회 2011 자원환경지질 Vol.44 No.6

지속가능한 지하수 자원의 개발과 관리능력의 수단으로서의 지하댐의 이용과 그 효율성에 관한 분석을 수행하기 위해 완전연동형 지표수-지하수 통합해석 모형인 SWAT-MODFLOW를 쌍천유역에 적용하여 지하댐 건설에 따른 영향평가를 수행하였다. 지하댐 건설 후에는 댐 상류의 지하수위 상승이 일어나며 하류부는 지하수가 감소하는 현상이 나타난다. 이에 따라 지표수-지하수의 상호교환량은 상류에서 더 커지는 것으로 나타났다. 지하댐 건설에 따라 상류부 대수층의 저류량이 증가함으로써 가용한 지하수의 개발량은 그만큼 증가하는 것으로 나타났다. 본 연구를 통해 지하댐의 기능이 대수층의 가용 저류량을 증대시키는 매우 유용한 시설임을 확인할 수 있었고, 통합 수문해석 방법론은 지하댐 건설에 따른 영향 뿐 아니라 설계와 운영을 평가하기 위한 적절한 기법으로 이용될 수 있을 것으로 판단된다. In this study, the usefulness of underground dam as a means for the sustainable development of groundwater, and its performance in the management of groundwater resources were analyzed. The fully integrated SWAT-MODFLOW was applied to the Ssangcheon watershed in Korea to evaluate the effectiveness of groundwater dam construction. After construction, the groundwater level raised in the upstream area of groundwater dam while lowered in the downstream area. Also, it is shown that the exchange rate of river-aquifer interactions increased in the upper area of the dam. Since the storage capacity of the aquifer largely increased in the upper area of the dam, the exploitable groundwater could be greatly increased as much. This study demonstrated that a groundwater dam was a very useful measure to increase the available storativity of groundwater aquifers. It also represented that the combined analysis using SWAT-MODFLOW was helpful for the design and opeation of groundwater dam in the Ssangcheon watershed.

논문 : 진천지역 지하수 함양량의 시공간적 변동특성

정일문 ( Il Moon Chung ),나한나 ( Han Na Na ),이덕수 ( Deok Su Lee ),김남원 ( Nam Won Kim ),이정우 ( Jeong Woo Lee ),이재명 ( Jae Myung Lee ) 대한지질공학회 2011 지질공학 Vol.21 No.4

지하수 항양량은 기후조건, 토지이용, 수리지질학적 비균질성에 의해 시공간적인 변동성을 나타내는 수문량이므로 통합 지표수-지하수 모델 기반의 시공간변동성을 갖는 일단위 함양량의 추정이 필요하다. 진천지역을 대상으로 SWAT-MODFLOW 통합모형이 일단위 함양량 추정에 사용되었으며 추정된 함양량의 시변성은 국가 지하수 관측망과 기초조사 기간(2009-2010)중에 설치된 자동관측망 자료와 잘 부합하는 것을 확인하였다. 진천지역을 포함한 미호천 유역 평균 지하수 함양량은 강수대비 20.8%로 나타났는데 이는 해석적 방법인 기저유출 분리법의 결과와도 잘 일치하였다. 통합모델링 기반의 함양량 산정은 국가 지하수 관리를 위해 유용하게 활용될 수 있을 것으로 판단된다. Because groundwater recharge shows spatial-temporal variability due to climatic conditions, it is necessary to investigate land use and hydrogeological heterogeneity, and estimate the spatial variability in the daily recharge ratc based on an integrated surface-groundwater model. The integrated SWAT-MODFLOW model was applied to compute physically based daily groundwater recharge in the Jincheon region. The temporal variations in estimated recharge were calibrated using the observed groundwater head at several National Groundwater Monitoring Stations and at automatic groundwater-monitoring sites constructed during the Basic Groundwater Investigation Project (2009-2010). For the whole Mihocheon watershed, including the Jincheon region, the average groundwater recharge rate is estimated to be 20.8% of the total rainfall amount which is in good agreement with the analytically estimated recharge rate. The proposed methodology will be a useful tool in the management of groundwater in Korea

하천유출량과 지하수위 변동을 고려한 정읍지역의 지하수 함양량 추정

정일문 ( Il Moon Chung ),나한나 ( Han Na Na ),김남원 ( Nam Won Kim ) 대한지질공학회 2009 대한지질공학회 학술발표회논문집 Vol.2009 No.-

제주도 한천유역의 함양 지체시간 산정

김남원 ( Nam Won Kim ),나한나 ( Han Na Na ),정일문 ( Il Moon Chung ) 한국환경과학회 2014 한국환경과학회지 Vol.23 No.4

In this work, the delay time for groundwater recharge was estimated by comparing simulated recharges by means of SWAT(Soil and Water Assessment Tool) model and WTF(Water Table Fluctuation) method. The delay time for groundwater recharge means that the time when the water from rainfall travelled through vadose zone just after getting out of soil zone bottom. As measuring this delay time is almost impossible, we used to compare the estimated values from modeling(SWAT) and analytic method(WTF). The test site is Hancheon watershed which has 8 groundwater measurement stations. The results show that the altitude has a linear relationship with the estimated delay time values. To validate these results, we conducted corelation analysis between transformed groundwater levels and observed ones. The results showed that computed groundwater levels have good corelation(R2=0.97, 0.87, respectively). The estimated delay time would be used for the groundwater behaviour characteristics in vadose zone. As recharge rates vary according to the height, the delay time is thought to be an import variable for the proper groundwater recharge estimation.

통합수문모형을 이용한 제주 한천유역의 지하수 변동 특성 모의

김남원 ( Nam Won Kim ),나한나 ( Han Na Na ),정일문 ( Il Moon Chung ) 한국환경과학회 2013 한국환경과학회지 Vol.22 No.5

To investigate groundwater variation characteristics in the Hancheon watershed, Jeju Island, an integrated hydrologic component analysis was carried out. For this purpose, SWAT-MODFLOW which is an integrated surface-groundwater model was applied to the watershed for continuous watershed hydrologic analysis as well as groundwater modeling. First, ephemeral stream characteristics of Hancheon watershed can be clearly simulated which is unlikely to be shown by a general watershed hydrologic model. Second, the temporally varied groundwater recharge can be properly obtained from SWAT and then spatially distributed groundwater recharge can be made by MODFLOW. Finally, the groundwater level variation was simulated with distributed groundwater pumping data. Since accurate recharge as well as abstraction can be reflected into the groundwater modeling, more realistic hydrologic component analysis and groundwater modeling could be possible.

제주 외도천 유역의 통합 물수지 분석

김남원 ( Nam Won Kim ),정일문 ( Il Moon Chung ),나한나 ( Han Na Na ) 한국환경과학회 2015 한국환경과학회지 Vol.24 No.4

Hydrologic component analysis was conducted to investigate water budget characteristics the Oedocheon watershed, Jeju Island. For this purpose, integrated SWAT-MODFLOW model was applied to this watershed for continuous surface water-groundwater modeling. Pasture and forest-deciduous are the major land use types and these affect general hydrologic component ratio. The spatio-temporal groundwater recharge can be obtained from SWAT and then distributed groundwater recharge can be reproduced by MODFLOW. The groundwater level variation was simulated with distributed groundwater pumping data. The water budget in this watershed was compared with the previous estimated result by Jeju-Do(2013). As this result considered discharge to the coastal side, the discrepancy was found. However, it was found that the overall tendency of both analyses were similar.

제주도 유출분석을 위한 한계유출 모의기법 개발

정일문 ( Il Moon Chung ),이정우 ( Jeong Woo Lee ),김지태 ( Ji Tae Kim ),나한나 ( Han Na Na ),김남원 ( Nam Won Kim ) 한국환경과학회 2011 한국환경과학회지 Vol.20 No.10

In Jeju island, runoff has frequently happened when the rainfall depth is over a threshold value. To simulated this characteristic rainfall-runoff model structure has to be modified. In this study, the TRSM (Threshold Runoff Simulation Method) was developed to overcome the limitations of SWAT in applying to the hydrologic characteristics of Jeju island. When the precipitation and soil water are less than threshold value, we revised the SWAT routine not to make surface/lateral or groundwater discharge. For Hancheon watershed, the threshold value was set as 80% of soil water through the analysis of rainfall-runoff relationship. Through the simulation of test watershed, it was proven that TRSM performed much better in simulating pulse type stream flow for the Hancheon watershed.

제주 천미천 유역의 간헐하천 유출특성 모의 방안

김남원 ( Nam Won Kim ),정일문 ( Il Moon Chung ),나한나 ( Han Na Na ) 한국환경과학회 2013 한국환경과학회지 Vol.22 No.5

In this study, a method of simulating ephemeral stream runoff characteristics in Jeju watershed is newly suggested. The process based conceptual-physical scheme is established based on the SWAT-K and applied to Cheonmi-cheon watershed which shows the typical pattern of ephemeral stream runoff characteristics. For the proper simulation of this runoff, the intermediate flow and baseflow are controlled to make downward percolation should be dominant. The result showed that surface runoff simulated by using the modified scheme showed good agreement with observed runoff data. In addition, it was found that the estimated runoff directly affected the groundwater recharge rate. This conceptual model should be continuously progressed including rainfall interception, spatially estimated evapotranspiration and so forth for the reasonable simulation of the hydrologic characteristics in Jeju island.