• 제목/요약/키워드: Transitional zone volume

검색결과 3건 처리시간 0.018초

혈액, 초음파 검사 결과를 이용한 전립선이행대용적의 상관관계 연구: 기초질환이 없는 30대를 대상으로 (A Study on the Correlations between Total Prostate Volume and Prostate Transition Zone Volume Assessed Using Blood and Ultrasound Tests: in the Healthy Korean Men in Thirties)

  • 김상현
    • 한국방사선학회논문지
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    • 제11권5호
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    • pp.407-412
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    • 2017
  • 본 연구는 혈액 검사 결과인 전립선특이항원(PSA) 및 전립선특이항원밀도 (PSAD), 전립선 경직장 초음파 (TRUS)를 이용한 전립선 전체용적 (TPV), 나이등 변수와 전립선이행대용적 (PTZV)과 상관관계를 연구하여 임상적 지표로 활용하고자 한다. 2007년 6월부터 2016년 4월 까지 전립선에 대한 치료력이 없는 건강한 30대 성인 남성으로 TRUS와 PSA, PSAD 혈액 검사를 실시한 총 68명을 후향적으로 분석하였다. 초음파 장비는 Siemens Acuson sequoia 512)와 탐촉자 Siemens EC~10C5 Endocavitary를 이용하였다. 통계 처리의 경우, SPSS 18.0 각 변수와 표준 편차의 평균을 계산하는 데 사용하고, 피어슨 상관관계 분석을 수행 하였다. 변수들의 기술 통계량은 TPV; $24.27{\pm}6.60$, PTZV; $6.99{\pm}6.60$, PSA; $2.12{\pm}2.76$와 PSAD; $0.281{\pm}0.1$이고. 전립선 이행용적과 변수의 상관 계수는 PSAD; 0.831, TPV; 0.707, 나이; 0.398, 그리고 PSA; 0.118이었다. PSA 및 연령과의 양의 크기의 상관관계지만, PSAD, TPV가 높은 상관관계를 보였다. 따라서, 기저 질환이 없는 30대 남성의 PTZV는 TPV와 PSAD를 통해 예측할 수 있다.

A zonal hybrid approach coupling FNPT with OpenFOAM for modelling wave-structure interactions with action of current

  • Li, Qian;Wang, Jinghua;Yan, Shiqiang;Gong, Jiaye;Ma, Qingwei
    • Ocean Systems Engineering
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    • 제8권4호
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    • pp.381-407
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    • 2018
  • This paper presents a hybrid numerical approach, which combines a two-phase Navier-Stokes model (NS) and the fully nonlinear potential theory (FNPT), for modelling wave-structure interaction. The former governs the computational domain near the structure, where the viscous and turbulent effects are significant, and is solved by OpenFOAM/InterDyMFoam which utilising the finite volume method (FVM) with a Volume of Fluid (VOF) for the phase identification. The latter covers the rest of the domain, where the fluid may be considered as incompressible, inviscid and irrotational, and solved by using the Quasi Arbitrary Lagrangian-Eulerian finite element method (QALE-FEM). These two models are weakly coupled using a zonal (spatially hierarchical) approach. Considering the inconsistence of the solutions at the boundaries between two different sub-domains governed by two fundamentally different models, a relaxation (transitional) zone is introduced, where the velocity, pressure and surface elevations are taken as the weighted summation of the solutions by two models. In order to tackle the challenges associated and maximise the computational efficiency, further developments of the QALE-FEM have been made. These include the derivation of an arbitrary Lagrangian-Eulerian FNPT and application of a robust gradient calculation scheme for estimating the velocity. The present hybrid model is applied to the numerical simulation of a fixed horizontal cylinder subjected to a unidirectional wave with or without following current. The convergence property, the optimisation of the relaxation zone, the accuracy and the computational efficiency are discussed. Although the idea of the weakly coupling using the zonal approach is not new, the present hybrid model is the first one to couple the QALE-FEM with OpenFOAM solver and/or to be applied to numerical simulate the wave-structure interaction with presence of current.

독도 및 그 주변 해산 중력 이상의 지구조적 해석 (Structural Implications of Gravity Anomalies around Dok Island and its Surrounding Seamounts in the East Sea)

  • 김원균;김창환;박찬홍;한현철;권문상;민경덕;김백수;최영섭
    • 자원환경지질
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    • 제33권6호
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    • pp.537-545
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    • 2000
  • Shipborne gravity data are analyzed to investigate crustal structure under Dok Island and its surrounding seamounts located in border of Ulleung Basin and Oki Bank in the East Sea. Relatively low free-air gravity anomaly compared with the volume of seamounts may be explainable by isostatic compensation. From 1 st to 3rd Dokdo Seamounts, the decrease of free-air and Bouguer gravity anomalies implies the different degree of isostatic compensation, crustal thickness or/and density contrast. 3-D gravity modelling shows that seamounts have the mirror roots for regional Airy isostatic compensation, and from Ulleung Basin to Oki Bank, Moho discontinuity deepens and the density of crust is decreases. The results infer that study area is transitional zone from thin oceanic to thick continental crust. The depth of Moho discontinuity is about 15∼16 km, which may be interpreted as an uplifting of Mantle to shallow depth comparing with other borders of the Ulleung Basin.

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