• Title/Summary/Keyword: 횡단면적 곡선

Search Result 16, Processing Time 0.025 seconds

A Study on the Earth-work Volume Calculation for Route Alignment of Highway (도로선형의 결정에서 토공량 산정에 관한 연구)

  • 최재화;이석배;심정민
    • Journal of the Korean Society of Surveying, Geodesy, Photogrammetry and Cartography
    • /
    • v.11 no.2
    • /
    • pp.89-100
    • /
    • 1993
  • This paper is a study on the earth volume calculation using CAD and LISP(LIST Processing) in the route alignment. The utility enlargement in the industry field and the considerable progress of computer make the automatic design and manufacture for the development of CAD/CAM/CAE technique possible, and the automatic design of civil engineering works is continuously progressive. In this study we are intend to improve an effect of civil engineering work by the automatic earth volume calculation in route alignment. This paper aims to construct the automatic design system of civil engineering work and the procedures; (1) The programming of the self-scanning program of the land information introducing Digital Terrain Model concept in the map (2) Systematic algorithm construction using LISP and grafting CAD system (3) Automatic design and calculation of the mass curve and earth volume.

  • PDF

Evaluation of Optimal Grid Resolution for Hydrodynamic Proper Simulation (수리동역학적 모의를 위한 적정 격자해상도 산정방법)

  • Ahn, Jung-Min;Park, In-Hyeok;Lyu, Si-Wan;Hur, Young-Teck
    • Journal of Korean Society for Geospatial Information Science
    • /
    • v.20 no.1
    • /
    • pp.109-116
    • /
    • 2012
  • The effect of the grid resolution on the hydrodynamic simulation has been investigated by using CCHE2D and EFDC. Since a high resolution of the grid results in the increase of computation time, an appropriate grid resolution should be selected by considering the efficiency of simulation according to the objectives of projects. In order to understand the effect of grid resolution and determine the optimal grid resolution, several cases with different lateral grid resolutions have been simulated for the reach of Nakdong river at the confluence of Kumho river for the floods in 2006. Orthogonal curvilinear grids for the domain have been constructed from the survey products at the sections with the longitudinal interval of 20 m. Area-elevation curve and the comparison of simulated results with measured stage at the specific station have been used to check the effect of grid resolution. From the results, the existence of optimal grid resolution has been observed, which ensure both efficiency of computation and certainty of results.

Study on Hull Form Variation of Fore Body Based on Multiple Parametric Modification Curves (다중 파라메트릭 변환곡선 기반 선수 선형 변환기법 연구)

  • Park, Sung-Woo;Kim, Seung-Hyeon;Lee, Inwon
    • Journal of the Society of Naval Architects of Korea
    • /
    • v.59 no.2
    • /
    • pp.96-108
    • /
    • 2022
  • In this paper, we propose a systematic hull form variation technique which automatically satisfies the displacement constraint and guarantees a high level of fairness. This method is possible through multiple parameter correction curves. The present method is to improve the hull form variation method based on parametric modification function and consists of two sub-categories: SAC variation and section lines modification. For SAC variation, the utilization of two B-Spline curves satisfying GC1 condition led to the satisfaction of displacement constraint and high level of fairness at the same time. Section lines modification methods involves in using two fuctions: the first is the waterplane modification function combining two cubic splines. the other function is the sectional area modification function consisting of 2nd order polynomial over the DLWL(Design Load Waterline) and 3rd order polynomial below the DLWL, This function enables not only the fundamental U-V section shape variation but also systematically modified section lines. The present method is expected to be more useful in the hull form optimization process using CFD compared to the existing method.

Reservoir water surface slope measurement (저수지 수면경사 실측)

  • HwangBo, Jong-Gu;Oh, Seung Hyun;hong, jun hyuk;Kang, JinSung;Park, Dong Wan
    • Proceedings of the Korea Water Resources Association Conference
    • /
    • 2022.05a
    • /
    • pp.267-267
    • /
    • 2022
  • 댐 운영에 있어서 필요한 수문자료는 강수량, 수위, 유량, 저수량 자료 등이 있다. 이중 저수량은 주로 댐수위-저수용량 곡선식을 이용하여 계산한다. 댐수위-저수용량 곡선식은 댐 부근에서 계측 되는 한 개의 수위자료를 이용하여 저수용량을 산정하며, 이는 큰 저수지 면적과 저수지 수면이 일정하지 않다는 것을 고려할 때 큰 오차가 발생할 수 있다. 본 연구에서는 음향 도플러 유속계 ADCP(Acoustic Doppler Current Profiler) 이용하여 보성강댐 저수지 수면경사를 실측하고, 동시에 실시간 이동측위시스템인 RTK-GPS(Real Time Kinematic)를 이용하여 이를 검증하였다. ADCP는 유수의 흐름을 방해하지 않으면서 수중에 발사된 음파의 도플러 효과를 이용하여 유속, 유량 및 측량이 가능한 장비이며, RTK-GPS의 경우 정밀한 위치정보를 가지고 있는 기준국의 위상에 대한 보정치를 실시간으로 이용하여 오차가 ±0.03m 이하인 것으로 알려졌다. 보성강댐의 하류에서 ADCP와 RTK-GPS를 장착한 보트를 저수지 종방향으로 처음부터 끝까지 이동하여 약 7.5km 종단측량을 실시하였고 저수지 지형적 특성을 고려하여 약 700m마다 횡단측량을 실시하여 종방향뿐만 아니라 횡방향 수면차도 조사하였다. 그 결과 보성강댐의 상류로 갈수록 수면경사가 전체적으로 상승하는 경향을 보였지만 일부구간에서 수위가 하강하는 경우도 발생하였다. 이는 미약하지만 저수지 내에 흐름이 발생하고 이 흐름에 따른 통제가 변화되는 것과 중간에 유입되는 지류의 영향 등으로 구간별로 수면경사 차이가 발생하는 것으로 추정된다. 횡방향 수면차는 지류가 유입되는 일부구간에서 다소 차이를 보였지만 큰 영향을 없는 것으로 판단된다. 보성강댐 저수지 수면을 종방향 및 횡방향으로 실측한 결과 구간별로 차이를 보였으며 최대 EL. 126.60m, 최소 EL. 126.33m 나타났다. 댐 상류 부근의 수면높이 EL. 126.50m와 비교하면 +0.10m, -0.17m 차이를 보였으며 이는 저수량 산정에 큰 오차를 발생시킨다. 효과적인 댐 운영을 위해서는 유입량 및 유출량을 정확하게 산정하는 것도 필요하지만 저수량을 정확하게 파악하는 것 역시 필요하다. 저수량을 정확하게 산정하려면 수킬로미터가 넘는 저수지 크기를 고려하여 수면경사를 실시간으로 계측하는 등의 노력이 필요한 것으로 판단된다.

  • PDF

Assessment of Quantitative Analysis Methods for Lung F-18-Fluorodeoxyglucose PET (폐 종양 FDG PET 영상의 다양한 추적자 역학 분석 방법 개발과 유용성 고찰)

  • Kim, Joon-Young;Choi, Yong;Choi, Joon-Young;Lee, Kyung-Han;Kim, Sang-Eun;Choe, Yearn-Seong;Kim, Yong-Jin;Kim, Byung-Tae
    • The Korean Journal of Nuclear Medicine
    • /
    • v.32 no.4
    • /
    • pp.332-343
    • /
    • 1998
  • Purpose: The purpose of this study was to assess the diagnostic accuracy of various quantitation methods using F-18-fluorodeoxyglucose (FDG) in patients with malignant or benign lung lesion. Materials and Methods: 22 patients (13 malignant including 5 bronchoalverolar cell cancer; 9 benign lesions including 1 hamartoma and 8 active inflammation) were studied after overnight fasting. We performed dynamic PET imaging for 56 min after injection of 370 MBq (10 mCi) of FDG. Standardized uptake values normalized to patient's body weight and plasma glucose concentration (SUVglu) were calculated. The uptake rate constant of FDG and glucose metabolic rate were quantified using Patlak graphical analysis (Kpat and MRpat), three compartment-five parameter model (K5p, MR5p), and six parameter model taking into account heterogeneity of tumor tissue (K6p, MR6p). Areas under receiver operating characteristic curves (ROC) were calculated for each method. Results: There was no significant difference of rate constant or glucose metabolic rate measured by various quantitation methods between malignant and benign lesions. The area under ROC curve were 0.73 for SUVglu, 0.66 for Kpat, 0.77 for MRpat, 0.71 for K5p, 0.73 for MR5p, 0.70 for K6p, and 0.78 for MR6p. No significant difference of area under the ROC curve between these methods was observed except the area between Kpat vs. MRpat (p<0.05). Conclusion: Quantitative methods did not improve diagnostic accuracy in comparison with nonkinetic methods. However, the clinical utility of these methods needs to be evaluated further in patients with low pretest likelihood of active inflammation or bronchoalveolar cell carcinoma.

  • PDF

Spatial Variation Analysis of Soil Characteristics and Crop Growth accross the Land-partitioned Boundary I. Spatial Variation of Soil Physical Properties (구획경계선(區劃境界線)의 횡단면(橫斷面)에 따른 토양특성(土壤特性)과 작물생육(作物生育)에 관한 공간변이성(空間變異性) 분석(分析) 연구(硏究) I. 토양물리성(土壤物理性)의 공간변이성(空間變異性))

  • Park, Moo-Eon;Yoo, Sun-Ho
    • Korean Journal of Soil Science and Fertilizer
    • /
    • v.22 no.3
    • /
    • pp.163-172
    • /
    • 1989
  • In order to study spatial variability of soil physical properties accross the land-partitioned boundary on Hwadong silt clay loam soil (Fine clayey, mixed, mesic family of Aquic Hapludalfs), all measured data were analyzed by means of kriging, fractile diagram, smooth frequency distribution, and autocorrelation. Sampling for soil particle size distribution analysis was made at 225 intersections of $15{\times}15$ grid with 10m interval. Field capacity, bulk density and saturated hydraulic conductivity were measured in situ at 594 intersections of $33{\times}18$ grid with 2.5m interval in only $6,000m^2$ reselected from $22,500m^2$ of sampling area for particle size distribution analysis. Sampled or measured soil depths were 0 to 10cm 25 to 35cm and 50 to 60cm at each intersections. The results are summarized as follows: 1. The coefficient of variance (CV) of various physical properties ranges from 4.8 to 128.8%. Saturated hydraulic conductivity is classified into the high variation group with CV greater than 100%, while the low variation group with CV smaller than 10% consists of bulk density. Other properties belong to the medium variation group with CV between 10 and 100%. 2. The appropriate number of soil samples for the determination of various physical properties with error smaller than 10% are calculated as one for bulk density, six for field moisture capacity, 16 for silt, 19 for clay, 69 for sand and 686 for saturated hydraulic conductivity. 3. Smooth frequency distribution and fractile diagram show that saturated hydraulic conductivity is in lognormal distribution while other physical properties are in normal distribution. 4. Serial correlation analysis reveals that the soil physical properties have spatial dependence between two nearest neighbouring grid points. Autocorrelation analysis of physical properties measured between the serial grid points in the direction of south to north following section boundary shows that the zone of influence showing stationarity ranges from 7.5 to 40m. In the direction of east to west across section boundary, the autocorrelogram of many physical properties shows peaks with the periodic interval of 30m, which are similar to the partitioned land width. This reveals that the land-partitioned boundary causes soil variability.

  • PDF