Although the Hazen-Williams C factors are very important in the design, operation, and maintenance of water supply pipes, sufficient studies for them have been not reported in korea, which are based on experiments or measured data. Because of this, we have estimated C factors by measurement considering constraints in time precise safety diagnosis for multi-regional water supply system were performed. In this study, we confirmed constraints and variables characteristics of Hazen-Williams equation, and collected reliable C factors data of 174 by measurement, and analyzed their characteristics. According to collected data, the average value is 115.35, which is almost equal to the value of design standard or a little higher than it in korea. Also, among the equations suggested to determine C factor in the past, the C factors calculated by Sharp and Walski equation was closest to them in this study. In addition, to analyze collected C factors, use year and pipe diameter having high correlation with them were respectively divided into there categories. Analysis results showed that C factors evidently decreases depending on increases in use year, on the other hand, size of pipe diameter is proportional to value of them. In conclusion, this research showing evaluation and characteristics for C factors based on measured data will be used as practical reference in determining C factor in multi-regional water supply systems at a later date.

하천 또는 해안의 선박운항을 위한 도개교는 그 희소성으로 인해 최근에는 랜드마크로의 역할을 인정받으면서, 국외의 경우 세심 한 유지관리로 수십 년 이상 공용기간을 지속하고 있는 사례가 적지 않다. 국내 유일의 도개교인 영도대교는 부식과 노화로 철거 후, 2013년에 재가설 되었으며, 현재 1일 1회 도개를 실시하고 있다. 최근 교량의 안전과 유지관리에 대한 요구가 높아지면서 주기적인 안전진단이 수행되지 만 도개교에 대한 계측 및 분석 사례는 거의 없는 실정이다. 이에 본 연구에서는 도개교가 상승 및 하강하는 도개과정과 상시 사용상태에서의 계측자료를 토대로 구조해석을 실시하여 도개교의 응력, 진동, 반력 등 실제 거동을 분석하고자 하였으며, 이 결과는 추후 공용연수의 증가 및 도개횟수의 증가에 따른 교량거동의 변동 추세를 분석하기 위한 초기 자료로 활용될 수 있을 것으로 기대된다.

We compared equilibrium evaporation(Eequili) eddy-covariance(Eequili) with soil moisture data(ESMseries) which were measured with a 2 hours sampling interval at three points for a humid forest hillslope from May 5th to May 31th in 2009. Accumulations of Eeddy, Eequili for the study period were estimated as 2.52, 3.28 mm and those of ESMseries were ranged from 1.91 to 2.88 mm. It suggested that the eddy-covariance method considering the spatial heterogeneity of soil evaporation is useful to evaluate the soil evaporation. Method A, B and C were proposed using mean meterological data and daily moisture variation and the computations were compared to eddy-covariance method and equilibrium evaporation. The methods using soil moisture data can describe the variations of soil evaporation from eddy-covariance through simple moving average analysis. Method B showed a good matched with eddy-covariance method. This indicated that Dry Surface Layer (DSL) at 14:00 which was used for method B is important variable for the evaluation of soil evaporation. The total equilibrium evaporation was not significantly different to those of the others. However, equilibrium evaporation showed a problem in estimating soil evaporation because the temporal tendency of Eequili was not related with the those of the other methods. The improved understanding of the soil evaporation presented in this study will contribute to the understandings of water cycles in a forest hillslope.

국내 주요 3대 하천인 한강, 낙동강, 금강에 대하여 하상재료의 입도분포를 이용하는 방법과 수치모형을 이용하는 방법으로 조도계수를 연구하였고, 기존의 하천정비기본계획에서 제시하고 있는 조도계수와 비교 검토하였다. 일반적으로 하천의 흐름을 해석할 때 수리학적 모형을 주로 이용하고 있으며, 특히 1차원 홍수위 계산을 위해 HEC-2, HEC-RAS, FLDWAV 모형 등을 이용하고 있다. 이들 수치모형을 이용하여 정확한 홍수위를 계산하기 위해서는 정확한 지

A dual-porosity filmed agglomerate model for the porous cathode of the molten carbonate fuel has been investigated to predict the cell performance. A phenomenological treatment of molecular, kinetic and electrode parameters has been given. The major physical and chemical phenomena being modeled include mass transfer, ohmic losses and reaction kinetics at the electrodeelectrolyte interface. The model predicts steady-state cell performance given the above conditions that characterize the state of the electrode. Quasi-linearization and finite difference techniques are used to solve the coupled nonlinear differential equations. Also, the effective surface area of electrode pore was obtained by mercury porosimeter. The results of the investigation are presented in the form of plots of overpotential vs. current density with varied the electrode material, gas composition and mechanism. The predicted polarization curves are compared with the empirical data from 1 ㎠ cell. A fair correspondence is observed.