• Electrical & Electronic Materials
• /
• v.8 no.3
• /
• pp.254-260
• /
• 1995

A method is described for the design and fabrication of the sensor interface circuits on the Clark electrodes for the dissolved oxygen(DO). The discussion includes a method for the +5 V single-supply driving for the sensor circuits, which has low power comsumption for the front-end electronics. DO probe under test is composed of the Clark electrode with silver anode, gold cathode and the electrolyte of half saturated KCI solution and the FEP teflon memtrance for the oxygen penetration. Typical polarograms for the DO probes by using this sensor circuit reveals high accuracy over 99% of the I to V conversion. Partial pressure of oxygen obtained from the polarograms are well suited to the results calculated. It is expected that the proposed sensor circuits can be utilized into the customized IC for the battery-driven small-size DO meters.

• Proceedings of the Korean Information Science Society Conference
• /
• 2002.10d
• /
• pp.439-441
• /
• 2002

본 논문은 Catmull-Clark 서브디비전 서피스(subdivision surfaces)를 포워드 디퍼렌싱(forward differencing)을 이용하여 효율적으로 evaluation 해서 렌더링하는 알고리즘을 제안하고 있다. 포워드 디퍼렌싱은 순수한 다항식만을 evaluation 할 수 있다. 그러나 Catmull-Clark 서브디비전 서피스는 순수한 다항식이 아니다. 그러므로, Catmull-Clark 서피스를 정규 패치들(regular patches)로 분리하고, 그 패치들에 대한 다항식을 만들고, 포워드 디퍼렌싱을 사용해서 evaluation 하면 된다. 본 알고리즘의 장점은 전통적인 리커시브(recursive) 서브디비전 기법에 비해 메모리의 요구가 적다. 즉, [1]과 마찬가지로 서브디비전 깊이(subdivision depth)에 독립적으로 항상 상수(constant) 메모리 양 만큼만 요구된다.

• Proceedings of the Korean Society of Agricultural Engineers Conference
• /
• 1999.10c
• /
• pp.537-543
• /
• 1999

While there are to estimating design discharge , we are in trouble with how to separate area, Because discharges will be different depending on the shape of area even though there are same size of area . This study is for a reasonable presentation of design discharge method where there are changing characteristcs of area with SCS and Clark theory by sung HEC-1 Model. While we were Estimating desgin discharge with separating area in a relation to Time of Concentration(Tc) with SCS , Clark method, we found that if there are no variation of Tc the value of a discharge is not changed where shapes of area are different though. And from the result of analysis with SCS and Clark method, we ascertained that discharge by the SCS method was more bigger than that of the Clark where Area is less than 100ha. On the other hand, Clark method is more bigger in the more 1000ha.

• International Journal of CAD/CAM
• /
• v.6 no.1
• /
• pp.139-148
• /
• 2006

Catmull-Clark subdivision scheme provides a powerful method for building smooth and complex surfaces. But the number of faces in the uniformly refined meshes increases exponentially with respect to subdivision depth. Adaptive tessellation reduces the number of faces needed to yield a smooth approximation to the limit surface and, consequently, makes the rendering process more efficient. In this paper, we present a new adaptive tessellation method for general Catmull-Clark subdivision surfaces. Different from previous control mesh refinement based approaches, which generate approximate meshes that usually do not interpolate the limit surface, the new method is based on direct evaluation of the limit surface to generate an inscribed polyhedron of the limit surface. With explicit evaluation of general Catmull-Clark subdivision surfaces becoming available, the new adaptive tessellation method can precisely measure error for every point of the limit surface. Hence, it has complete control of the accuracy of the tessellation result. Cracks are avoided by using a recursive color marking process to ensure that adjacent patches or subpatches use the same limit surface points in the construction of the shared boundary. The new method performs limit surface evaluation only at points that are needed for the final rendering process. Therefore it is very fast and memory efficient. The new method is presented for the general Catmull-Clark subdivision scheme. But it can be used for any subdivision scheme that has an explicit evaluation method for its limit surface.

• Proceedings of the Korea Water Resources Association Conference
• /
• 2016.05a
• /
• pp.550-550
• /
• 2016

본 연구에서는 Clark 모형을 기반으로 한 홍수유출 앙상블 멤버 생성기법을 개발하였다. Clark 모형의 매개변수인 집중시간과 저류상수는 불확실성을 가진다. 본 연구에서는 집중시간과 저류상수가 가지고 있는 불확실성을 해결하기 위하여 적절한 확률분포를 선정하였다. 집중시간에 적절한 확률분포는 집중시간이 가지고 있는 특성과 확률분포가 가지고 있는 특성을 비교 및 분석하여 선정하였다. 선정된 확률분포는 감마분포와 대수정규분포이다. 저류상수에 적절한 확률분포는 저류 상수와 집중시간의 관계를 분석하여 선정하였다. 선정된 확률분포는 집중시간에서 선정한 확률분포와 동일하다. 본 연구에서는 이지호 등(2013)의 연구에서 집중시간과 저류상수 사이에 뚜렷한 관계를 확인하고 이에 적합한 이변량 확률분포를 선정하였다. 선정된 이변량 확률분포는 이변량 감마분포와 이변량 대수정규분포이다. 이변량 감마분포는 집중시간과 저류상수에 적용 가능한 Smith, Adelfang and Tubb's(SAT) 이변량 감마분포를 선정하였다. SAT 이변량 감마분포와 이변량 대수정규분포의 적합도 검정방법은 K-S 검정을 이용하였다. 본 연구에서는 SAT 이변량 감마분포와 이변량 대수정규분포로 Random Number Generation 실시하였다. 생성된 집중시간과 저류상수의 앙상블 멤버는 Clark 모형을 이용하여 홍수유출 앙상블 멤버를 생성한다. 제안된 홍수유출 앙상블 멤버 생성기법은 방림 유역을 대상 검토하였다.

• Journal of Korea Water Resources Association
• /
• v.36 no.2
• /
• pp.211-221
• /
• 2003

The objectives of this study are to analyze the effects of time-area curve on Clark's watershed runoff method in addition to propose a GIS-based objective method for creating time-area curve. For the relative comparison of the variation of time-area curve to those of travel time and storage coefficient of Clark method, runoff sensitivities are performed on Soyang- and Chungju-dam watersheds for 1990. 9. 10~9. 14 event. The dimensionless time-area curve in HEC-1 that can be utilized in the case that the curve is not supplied is also tested in this study. The important results obtained in this study are as follows: The effects of time-area curve created by either GIS-based objective method or dimensionless curve are not significant for runoff analysis; The storage coefficient (K) and travel time( t$_{c}$), Clark's other two model parameters, are more sensitive than time-area curve for peak flow simulation. Therefore, it can be concluded that the parameters K and t$_{c}$ are more carefully estimated rather than time-area curve, when Clark method is used for runoff analysis.

• Water for future
• /
• v.27 no.4
• /
• pp.85-94
• /
• 1994

A Sensitivity analysis on the model parameters involved in the Clark watershed routing method is made to demonstrate the effect of each parameter on the magnitude of 50-year design flood for small urban streams. As for the rainfall parameter the time distribution pattern of design storm was selected. For short duration storms Huff, Yen & Chow and Japanese Central type distributions were selected and the Mononobe distribution of 24-hour design storm was also selected and tested for Clark method application. The effect of SCS runoff curve number for effective rainfall and the methods of subbasin division for time-area curve were also tested. The routing parameter, i.e. the storage constant(K), was found to be the dominating parameter once design storm is selected. A multiple regression formula for K correlated with the drainage area and main channel slope of the basin is proposed for the use in urban stream practice for the determination of design flood by Clark method.

• KOREAN JOURNAL OF CROP SCIENCE
• /
• v.19
• /
• pp.39-46
• /
• 1975

The optimum plot size and shape for soybean yield trials were estimated by using two different soybean varieties, Kumkang-daelip and Clark. Long narrow shape plot was generaIly showed lower C.V. value as compared to the plots consisted of more row number with short row length. The results obtained in this experiment provided the optimum size and shape of plots for Clark as 1. 4m x 6m, and for Kumkang-dailip as 1.4m $\times$ 9m, respectively.

• KSCE Journal of Civil and Environmental Engineering Research
• /
• v.33 no.1
• /
• pp.157-170
• /
• 2013

In this study, flood runoff characteristics is analyzed according to subbasin divisions by physically based rainfall-runoff model and appropriate number of subbasin divisions is suggested for midsize test basins. The Clark method, a lumped model in HEC-HMS, and the ModClark method, a semi-distributed model are used to simulate rainfall-runoff processes on Andong-reservoir basin, Imha-reservoir basin, and Pyeongchang river basin. The test basins were divided into nine subdivision cases by equal-area subdivision method such as single basin, 3, 5, 6, 7, 9, 10, 12, and 15 subbasins, and compared the simulated and observed values in terms of the peak flow and the peak time. The simulation results indicated that the peak flows tended to increase and the peak time shifted earlier as the number of subdivisions increased and this tendency weakened after the certain number of subdivisions. In this research, the specific number of subdivision was defined as the minimum number of subdivision considering both peak flow and peak time. Consequently, the minimum number of subdivisions is determined as 5 for Andong and Imha reservoir basins and 7 for Pyeongchang river basin.

• Journal of Wetlands Research
• /
• v.18 no.2
• /
• pp.121-131
• /
• 2016

The determination of feasible design flood is the most important to control flood damage in river management. Concentration time and storage constant in the Clark unit hydrograph method mainly affects magnitude of peak flood and shape of hydrograph. Model parameters should be calibrated using observed discharge but due to deficiency of observed data the parameters have been adopted by empirical formula. This study is to suggest concentration time and storage constant based on the observed rainfall-runoff data at GongDo stage station in the Ansung river basin. To do this, five criteria have been suggested to compute root mean square error(RMSE) and residual of oserved value and computed one. Once concentration time and storage constant have been determined from three rainfall-runoff event selected at the station, the five criteria based on observed hydrograph and computed hydrograph by the Clark model have been computed to determine the value of concentration time and storage constant. A criteria has been proposed to determine concentration time and storage constant based on the results of the observed hydrograph and the Clark model. It has also been shown that an exponent value of concentration time-cumulative area curve should be determined based on the shape of watershed.