• 한국항해항만학회:학술대회논문집
• /
• 한국항해항만학회 2000년도 춘계학술대회논문집
• /
• pp.91-98
• /
• 2000

Derivation of stage-discharge relationship and characteristics for Yangsan river is presented in this paper. This research has been conducted as the second one after the first trial of 1997. The determination of discharge at a Yangsan river gauging was best made by measuring the flow velocities with a current meter and rod float. The rating curve obtained through 52 stage-discharge measurements on Yangsan river basin in 1999 is represented by Q=15.3540-140.6076H+182.44372$H^2$, which is discovered to be most excellent among other curves in reliability analysis. The capability of the observed stage-discharge data for Yangsan river was tested by HEC-RAS program, and its capability to reproduce discharge was investigated and compared with the computational results. Rating curve stability is determined on the basis of deviations in the stage-discharge relationship, utilization of specific gauge, and absolute differences between sequential stream flow measurements and an analysis residuals. Therefore it seems necessary to research method to obtain rating curve in a rigorous and accurate manner.

• 센서학회지
• /
• 제2권1호
• /
• pp.35-40
• /
• 1993

$Si_{3}N_{4}$ 박막의 코팅된 pH-ISFET의 게이트 부위 위에 lipase 효소를 고정화하여 FET(field effect transistor) 형지질(lipid) 센서를 제조하였다. 효소 고정화막 형성 물질로는 수용성 고분자인 polyvinyl alcohol(PVA)에 감광성기인 1-methyl-4-(formylstyryl) pyridinium methosulfate(SbQ)를 결합시킨 PVA-SbQ를 사용하였다. PVA-SbQ 수용액 (SbQ 1mole %, 10 wt%) $200{\mu}L$, bovine serum albumin (BSA) 7.5 mg, lipase 10 mg으로 구성 된 현탁액을 사용한 사진식각(photolithographic) 공정의 최적 조건은 피막의 상온 진공 건조 시간 45분, spin coater의 회전수 $5,000{\sim}6,000$ rpm, UV 노광시간 $20{\sim}30$초, 증류수 현상 시간 $30{\sim}40$초로 나타났다. 이렇게 구성된 지질 센서는 triacetin을 지질 시료로 하였을 때 $10{\sim}100$ mM의 농도 범위에서 직선성의 검정선을 나타내었다.

• 한국지열·수열에너지학회논문집
• /
• 제4권1호
• /
• pp.11-19
• /
• 2008

Groundwater flow in confined aquifer and heat transport in underground geologic media are using same governing equation(line source) like well fuction. Therefore the conventional slope method using only later data obtained from in-situ thermal response test to determine the thermal conductivity of vertical geothermal heat exchanger(GHEX) is basically identical with one of Theis straight line method of aquifer test under artesian condition. In case that the pumping rate(Q, $m^3$/d) and drawdown(s,m) which are used for input data of existing hydrogeologic computer programs for aquifer test are replaced and converted to supplying heat energy per unit length of bore hole(Q/L,w/m or Kcal/h.m) and temperatures (T,$^{\circ}C$)measured at in and out-let of GHEX as in put data respectively, thermal conductivity around geothermal heat exchanger can be easily estimated without any special modification of the existing hydrogeologic computer program. Two numbers of time series temperature variation data obtained from in situ geothermal response test are analized using Theismethods(standard curve and straight line method) by using existing aquifer test program and conventional Slope method proposed by ASHRAE. The results show that thermal conductivity values estimated by two straight methods are identical and the difference of estimated values between standard curve methods and Slope method are also within acceptable ranges. In general,the thermal conductivity estimated from Theis straight linemethod gives more accurate value than the one of Slope method due to that Slope method uses only visual matching otherwise Theis method uses automatic curve matching estimation with reducing RSS.

• Journal of Magnetics
• /
• 제2권3호
• /
• pp.72-75
• /
• 1997

The temperature dependent saturation magnetization curve of amorphous Fe67 Co18B14Si1, alloy was measured using a SQUID magnetometer and vibrating sample magnetometer from 5 K up to 800 K. Inelastic neutron neutron scattering measurements also have been used to study the long wavelength spin dynamics of this high Tc amorphous ferromagnetic alloy. The magnon dispersion curve exhibit the conventional quadratic relationship E = D (T) q2 + $\Delta$, typical of an iso=obtained from a low temperature magnetization curve, which was consistent with the value obtained from the analysis oif inelastic neutron scattering data after consideration of its temperature dependence.

• 정보보호학회논문지
• /
• 제14권2호
• /
• pp.15-22
• /
• 2004

위수가 q인 생성원 g를 사용하는 ElGamal형 서명기법에서는 서명되어질 각 문서마다 message nonce를 구간(0, q-1)에서 랜덤하게 선택해야 한다는 것은 잘 알려진 사실이다. H. Kuwakado와 H. Tanaka는 사용된 message nonce가 각각 0＜$textsc{k}$$_1$, $textsc{k}$$_2$$\leq$Ο(equation omitted)인 서명 두 개가 주어졌을 때, 서명자의 비밀키를 다항식 시간으로 계산해내는 알고리즘을 제안하였다. 최근 R. Gallant, R. Lambert, S. Vanstone등은 정수를 적절히 분해하여 타원곡선암호의 효율성을 개선하는 방법을 제안하였다. 이 논문에서는 타원곡선암호의 고속연산에서 사용되었던 정수의 분해기법을 Kuwakado등의 알고리즘에 적용하여 message nonce가 ｜$textsc{k}$$_1$｜, ｜$textsc{k}$$_2$｜인 경우에도 적용할 수 있도록 확장하고, 알고리즘의 효율성 및 공격의 완성도를 개선하였다.

• 한국농공학회지
• /
• 제38권3호
• /
• pp.127-136
• /
• 1996

The purpose of this study is to provide with information for the water resources development and management in stream management planning, such as information on the sediment trensport, design of dam and water facilities, river improvement and flood plains management. The major results obtained from the field measurement and analysis of the watershed characteristics, hydraulic and sediment characteristics are as follows ; 1. The rating curve formulas obtained from the analysis of the hydraulic characteristics data collected are ; Q-=110.563 $(H-0.474)^2$ for 0.7m$(H-0.146)^2$ for 0.4m$Sr=aX{^2} {_1} X^{c}{_2}$, in the experimental watershed.

• Journal of the Korean Society for Industrial and Applied Mathematics
• /
• 제6권2호
• /
• pp.25-30
• /
• 2002

Let $E/{\mathbb{Q}$ be an elliptic curve defined over rationals, P is a non-torsion rational point of E and $$S=\{[n]P{\mid}n{\in}{\mathbb{Z}}\}$$. then S is dense in the component of $E({\mathbb{R}})$ which contains the infinity in the usual Euclidean topology or in the topology defined by the invariant Haar measure and it is uniformly distributed.

• Journal of Magnetics
• /
• 제8권4호
• /
• pp.153-156
• /
• 2003

The values of crystalline-electric-field parameters $A_{nm}$ for $RFe_{11}$Ti $H_{x}$ (R=Tb,Ho) (x=0,l) are obtained by fitting calculations to the magnetization curves along the crystal axes at 4.2 K and higher temperatures. The insertion of H element in RFe$_{11}$Ti significantly affects CEF parameters $A_{nm}$ . By using exchange field 2${\mu}$$_{B}$ $H_{ex}$ derived by inelastic neutron scattering and fitted $A_{nm}$ , the calculations reproduce the experimental curves well.

• 대한수학회지
• /
• 제48권5호
• /
• pp.953-967
• /
• 2011

We show that the characteristic function $1S_{\underline{\alpha}}$ of any Harder-Narasimhan strata $S{\underline{\alpha}}\;{\subset}\;Coh_X^{\alpha}$ belongs to the spherical Hall algebra $H_X^{sph}$ of a smooth projective curve X (defined over a finite field $\mathbb{F}_q$). We prove a similar result in the geometric setting: the intersection cohomology complex IC(${\underline{S}_{\underline{\alpha}}$) of any Harder-Narasimhan strata ${\underline{S}}{\underline{\alpha}}\;{\subset}\;{\underline{Coh}}_X^{\underline{\alpha}}$ belongs to the category $Q_X$ of spherical Eisenstein sheaves of X. We show by a simple example how a complete description of all spherical Eisenstein sheaves would necessarily involve the Brill-Noether stratas of ${\underline{Coh}}_X^{\underline{\alpha}}$.

• 충청수학회지
• /
• 제15권2호
• /
• pp.1-12
• /
• 2003

L. H. Encinas, A. J. Menezes, and J. M. Masque in [2] proposed a classification of isomorphism classes of hyperelliptic curve of genus 2 over finite fields with characteristic different from 2 and 5. Y. Choie and D. Yun in [1] obtained for the number of isomorphic classes of hyperelliptic curves of genus 2 over $F_q$ using direct counting method. In this paper we will classify the isomorphism classes of hyperelliptic curves of genus 2 over $F_{2^n}$ for odd n, represented by an equation of the form $y^2+a_5y=x^5+a_8x+a_{10}(a_5{\neq}0)$.