• 한국운동역학회지
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• 제17권4호
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• pp.115-125
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• 2007

Grould Reaction force(GRF) is important in human movements and GRF measurements are one of the most frequently used tool in biomechanical studies. In the studies of the golf swing motion, people refer to GRF as weight transfer. A successful golf swing motion requires many segments activation sequences which are controled by the nerve system. Due to the inter- and intra-individual variability of the human movement and the movement strategies, reliability of the measurements are important in human movement studies. Previous golf researches were based on group studies and certain events' values were analyzed. The purposes of this study were to determine the number of trials for the reliable golf swing GRF data collection, to reveal the variability level of the meaningful components of the golf swing GRF, and to classify the types of the golf swing GRF patterns. Twenty three male professional golfers($26.4{\pm}6.6$ years, $174.3{\pm}5.2\;cm$, $71.3{\pm}6.5\;kg$) signed an informed consent form prior to participation in this study. GRFs of driver swings were collected with Kistler 9285 force platform and 9865A amplifier, and calculated by the KwonGRF program(Visol, Korea). Sampling frequency was 1080 Hz. GRF data were trimmed from 1.5 s prior to the impact to 0.5 s after the impact. The number of trials for the reliable GRF collection was determined when the change in floating mean overs the 25 % of the standard deviation of that variable. Variabilities of the variables were determined by the coefficient of variation(CV) of 10 %. The types of GRF patterns were determined by visual inspection of the peak GRF shapes. The minimum number of trials for the reliable golf swing GRF data collection was five. Ten-trial seems more conservative. The value of the peak GRF was more reliable than the value of the impact GRF. The CV of the peak GRF and impact GRF were 7.4 %, 15.2 %, respectively. Because of the +/- sigh of the peak GRF appearance time, it was impossible to calculate CV of the peak GRF appearance time. Golf swing GRF patterns were classified as sing peak type, double peak type, and plateau peak type. This classification suggests the presence of the different golf swing weight transfer strategies.

• 한국농공학회지
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• 제22권3호
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• pp.75-87
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• 1980

Most hydro]ogic phenomena are the complex and organic products of multiple causations like climatic and hydro-geological factors. A certain significant correlation on the run-off in river basin would be expected and foreseen in advance, and the effect of each these causual and associated factors (independant variables; present-month rainfall, previous-month run-off, evapotranspiration and relative humidity etc.) upon present-month run-off(dependent variable) may be determined by multiple regression analysis. Functions between independant and dependant variables should be treated repeatedly until satisfactory and optimal combination of independant variables can be obtained. Reliability of the estimated function should be tested according to the result of statistical criterion such as analysis of variance, coefficient of determination and significance-test of regression coefficients before first estimated multiple regression model in historical sequence is determined. But some error between observed and estimated run-off is still there. The error arises because the model used is an inadequate description of the system and because the data constituting the record represent only a sample from a population of monthly discharge observation, so that estimates of model parameter will be subject to sampling errors. Since this error which is a deviation from multiple regression plane cannot be explained by first estimated multiple regression equation, it can be considered as a random error governed by law of chance in nature. This unexplained variance by multiple regression equation can be solved by stochastic approach, that is, random error can be stochastically simulated by multiplying random normal variate to standard error of estimate. Finally hybrid model on estimation of monthly run-off in nonhistorical sequence can be determined by combining the determistic component of multiple regression equation and the stochastic component of random errors. Monthly run-off in Naju station in Yong-San river basin is estimated by multiple regression model and hybrid model. And some comparisons between observed and estimated run-off and between multiple regression model and already-existing estimation methods such as Gajiyama formula, tank model and Thomas-Fiering model are done. The results are as follows. (1) The optimal function to estimate monthly run-off in historical sequence is multiple linear regression equation in overall-month unit, that is; Qn=0.788Pn+0.130Qn-1-0.273En-0.1 About 85% of total variance of monthly runoff can be explained by multiple linear regression equation and its coefficient of determination (R2) is 0.843. This means we can estimate monthly runoff in historical sequence highly significantly with short data of observation by above mentioned equation. (2) The optimal function to estimate monthly runoff in nonhistorical sequence is hybrid model combined with multiple linear regression equation in overall-month unit and stochastic component, that is; Qn=0. 788Pn+0. l30Qn-1-0. 273En-0. 10+Sy.t The rest 15% of unexplained variance of monthly runoff can be explained by addition of stochastic process and a bit more reliable results of statistical characteristics of monthly runoff in non-historical sequence are derived. This estimated monthly runoff in non-historical sequence shows up the extraordinary value (maximum, minimum value) which is not appeared in the observed runoff as a random component. (3) "Frequency best fit coefficient" (R2f) of multiple linear regression equation is 0.847 which is the same value as Gaijyama's one. This implies that multiple linear regression equation and Gajiyama formula are theoretically rather reasonable functions.

• 한국지반환경공학회 논문집
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• 제7권6호
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• pp.101-111
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• 2006

현장타설말뚝은 상부의 연약층을 관통하여 하부의 강한 암반층 상부에 거치시키는 경우, 말뚝은 선단지지말뚝으로 간주되며, 최소단면에서 말뚝에 발생하는 응력이나 실제 요구되는 설계기준에 따라서 작용하중은 결정된다. 연약하거나 풍화된 암반의 일정 깊이까지 현장타설말뚝을 설치하는 경우, 선단지지력과 주면저항력에 의해 지지력이 발현된다. 선단지지력 성분은 말뚝의 극한지지력에서 큰 비중을 차지한다. 그러나, 일반적으로 주면저항력은 선단지지력에 비해 훨씬 작은 말뚝 침하시 발현된다. 또한, 선단지지력은 근입부 바닥에 잔존하는 슬라임에 의해 영향을 받는다. 따라서, 근입부에 슬라임을 얼마나 잘 확인하는가와 시공법에 따라 선단지지력의 신뢰도는 결정되게 된다. 이것은 실제로 매우 어렵고 고가이며, 깊은 근입부에서는 더욱 심각하다. 따라서 이들 요소들로 인해서 작용하중하에서 말뚝의 거동은 주면저항력에 의해 지배되게 된다. 따라서 현장타설말뚝의 거동예측을 위한 연구는 주로 주면저항력 발현기구에 관심을 가지게 되는 것이다. 본 연구에서는 말뚝 두부에서의 하중 조건을 변화시켜가며 암반에 근입된 현장타설말뚝의 거동 차이를 분석하기 위하여 수치 해석을 수행하였다. 또한, 거칠기 요소의 모델링 유무에 따른 주면부 거동 특성도 조사하였다.

• 대한소아치과학회지
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• 제45권1호
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• pp.65-74
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• 2018

본 연구의 목표는 측방 두부계측방사선 사진의 분석에 이용되는 소프트웨어의 소급성 확보와 측정값의 불확도를 계산하는 것이다. 또한 이를 이용해 소아에서 교정치료를 위한 계측값의 참고 표준을 얻기 위한 기반을 마련하고자 하였다. 교정치료를 위해 서울대학교 치과병원 소아치과에 내원한 6세에서 13세 사이 환아 중 1급 부정교합으로 진단 받은 환아 100명의 데이터를 수집하였다. 소급성 확보를 위해 방사선 촬영이 가능한 phantom 장비를 제작하였으며, 현재 사용중인 계측 소프트웨어를 이용하여 phantom 장비의 길이와 각도를 측정하여 소프트웨어의 교정값을 계산하였다. 불확도 계산을 위해 100명의 측방두부방사선영상 계측값과 반복측정에 의한 불확도와(A형 불확도) 최소분해능과 두부의 위치에 의한 불확도를(B형 불확도) 계산하였다. 이를 통해 합성표준불확도를 얻었으며 최종적으로 확장불확도를 계산하였다. 본 연구 결과 현재 사용중인 측방두부방사선사진 계측 프로그램이 높은 정확성과 신뢰도를 가지는 것을 확인하였다. 또한 교정값을 이용하여 계측값을 교정하였으며, 6 - 13세 한국인 소아에서의 교정계측치의 불확도를 계산하여 1급 부정교합 환아의 교정계측값의 95% 신뢰도를 가지는 분포범위를 제시하였다.

• IUGG한국위원회:학술대회논문집
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• IUGG한국위원회 2003년도 정기총회 및 학술발표회
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• pp.20-20
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• 2003

In the summers of 1997 and 1998 and in February of 2000 we made 570 measurements of the ambient geomagnetic field 120 cm above the pavement surface of State Route 130, south of Pahoa, the island of Hawaii using a three-component fluxgate magnetometer. We measured at every 15.2 m (50 feet) interval covering a distance of 6, 310 m (20, 704 ft) where both historic and pre-historic highly magnetic basalt flows underlie. We also collected 197 core samples from eight road cuts, 489 specimens of which were subject to AF demagnetizations at 5 - 10 mT level up to a maximum field of 60 mT. We observed significant inclination anomalies ranging from a minimum of $31^{\circ}$ to a maximum $40^{\circ}$ where a uniform inclination value of $36.7^{\circ}$ (International Geomagnetic Reference Field, IGRF) was expected. Since the mean of the observed inclinations is approximately $35^{\circ}$ we assume that the study area is slightly affected by the magnetic terrain effect to a systematically shallower inclinations for being located in the regionally sloping surface of the southern side of the island (Baag, et al., 1995). We observed inclination anomalies showing wider (spacial) wavelength (160 - 600 m) and higher amplitudes in the historic lava flows area than in the northern pre-historic flows. Our observations imply that preexisting inclination anomalies such as those that we observed would have been interpreted as paleosecular variation (PSV). These inclination anomalies can best be attributed to concealed underground highly magnetic dikes, channel type lava flows, on-and-off hydrothermal activities through fissure-like openings, etc. Both the within- and between-site dispersions of natural remanent magnetization (NRM) are largest (up to ${\pm}7^{\circ}$) above the flows of 1955, while the area of pre-historic flows in the northern part of the study area exhibit the smallest dispersion. Nevertheless, mean inclinations of each historic flow of 1955 and 1790 are almost identical to that of the corresponding present field, whereas mean of NRM (after AF demagnetization) inclinations for each of the four pre-historic lava flow units is twelve to thirteen degrees lower than the present field inclination. We observed three cases of very large inclination variations from within a single flow, the best fitting curves of which are linear, second and third order polynomials each from within a single flow, whereas no present field variations are observed. This phenomena can be attributed to the notion that local magnetic anomalies on the surface of an active volcano are not permanent, but are transient. Therefore we believe that local magnetic anomalies of an active volcano may be constantly modified due to on going subsurface injections and circulations of hot material and also due to wide spacial and temporal distribution of highly magnetic basaltic flows that will constantly modify the topography which will in turn modify the local ambient geomagnetic field (Baag, et al., 1995). Our observations bring into question the general reliability of PSV data inferred from volcanic rocks, because on-going various geologic and geophysical activities associated with active volcano would continuously deflect and modify the ambient geomagnetic field.

• 한국시뮬레이션학회논문지
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• 제23권1호
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• pp.21-31
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• 2014

본 논문에서는 조직관련 변수들의 연구를 위해 이직의도와 조직몰입을 목표(종속)변수로서 데이터마이닝 시뮬레이션을 실시하여 접근 방법을 찾고 분석결과 도출을 목적으로 하였다. 데이터마이닝 분석방법 중 CART 앙상블 기법을 활용하였다. 자료는 한국직업능력개발원의 인적자본기업패널조사 1차~3차(2005~2009)데이터를 사용하였다. 조직몰입 변수는 다항목 측정 사항에 대해 신뢰성, 단일차원성 검토를 실행 후 합산척도 변수를 생성하여 분석하였다. 본 연구 결과는 다음과 같다. 첫째, 이직의도에 대한 주요 결정요인은 신뢰, 커뮤니케이션, 인재 중시 풍조 아이템으로 나타났다. 둘째, 조직몰입에 대한 주요 결정요인은 신뢰, 근속기간, 혁신, 커뮤니케이션 아이템으로 나타났다. 데이터마이닝 방법의 CART 앙상블 방법으로 Bagging과 Arcing 알고리즘을 적용한 결과 Arc-x4 방법이 매우 높은 결정계수를 나타낸 시나리오를 추출했다. 본 연구에서는 데이터마이닝 방법 중 하나인 CART 앙상블 시뮬레이션을 통해 최대치의 결정계수, 최소치의 오류를 산출한 시나리오 모델을 도출하고 실무적 시사점을 제시하였으며 한계점 및 향후 연구에 대해 논의되었다.

• 한국치위생학회지
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• 제6권4호
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• pp.419-436
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• 2006

PURPOSE: The purpose of this study was to explore dental hygiene treatment fear and anxiety in dental patients. METHODS: The sample consisted of 466 dental patients who had received the dental hygiene treatment at 8 Dental Hospitals and Clinics in Daegu city between March and August 2006 studied. Dental hygienists recruited a questionnaire, which includes generalized anxiety sub-scale(4 items), specific fear sub-scale(5 items), distrust sub-scale(5 items), and catastrophic anxiety sub-scale(4 items). Minimum score is 1, and maximum score is 5. The research was designed to be a cross-sectional measured study. SAS statistical software was used for the analysis. The characteristics of the study sample were described by mean and standard deviation(SD) for continuous variables and by frequency and percentage for categorical variables. The Student's t-test and analysis of variance(ANOVA) were used to compare fear and anxiety score in demographic variables. A Pearson's correlation analysis was conducted for relationship among values of fear and anxiety for dental hygiene. Multiple regression analysis was performed to determine the factors associated with fear and anxiety related with dental hygiene. RESULTS: A total of 466 dental patients were analyzed, their average age${\pm}$SD was $37.7{\pm}12.9$ years(range: 15-79 yr). The mean value for dental hygiene fear and anxiety was 2.70(generalized anxiety 2.65, specific fear 2.93, distrust anxiety 2.72, and catastrophic anxiety 2.42, respectively). There was a statistically significant difference in gender(p<0.05), 2.81 for women was higher than 2.55 for men(p=.0000). The older we are, the higher fear and anxiety for dental hygiene treatment were. that is, under age of 20 years 2.49, 20 years 2.59, 30 years 2.69, 40 years 2.77, 50 years 2.88, 60 years 2.69, and over age of 70 2.45, respectively(p=.0321). Factors related to dental hygiene treatment fear and anxiety by multiple regressions were gender(${\square}$=0.18, p=0.0001), age(${\square}$=.07, p=.0058), and the time when visits dentist recently(${\square}$=.07, p=.0058). CONCLUSIONS: In conclusion, gender, age and the time when visits dentist recently were significantly associated with dental hygiene treatment fear and anxiety. We recommend that further research should investigate a dental hygiene treatment fear and anxiety by using more follow-up study.

• 정보처리학회논문지C
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• 제9C권2호
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• pp.247-256
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• 2002

무선 멀티캐스팅에서 이동 호스트가 같은 멀티캐스트 그룹 기지국으로 이동할 때 새로운 기지국으로부터 원하는 데이터를 즉시 수신하기 위해서는 기지국들간에 데이터 전달에 대한 정보교환이 필요하다. 그러나 기존의 기법들은 정보 교환시 소요되는 전달 시간과 오버헤드가 많아 비효율적이다. 또한 이동 호스트가 멀티캐스트에 참여하지 않는 기지국으로 이동할 때 전송지연을 피하기 위해서는 현재 기지국이 주변 기지국들에게 데이터를 미리 전달하는 사전 전달 기법을 사용한다. 그러나 기존의 사전 전달 기법에서는 이동호스트들이 짧은 시간 간격을 두고 연속 이동할 경우 현재 기지국이 같은 주변 기지국들에게 같은 데이터를 재전송하게 되어 중복 데이터가 발생할 수 있다. 본 논문에서는 이와 같은 문제를 해결하기 위한 기법으로 새로운 정보교환 기법인 IES(Information Exchange Scheme)를 제안한다. 제안된 IES에서는 멀티캐스트 그룹에 참여하는 기지국들이 국부적인 정보교환을 함으로써 필요한 시간과 오버헤드를 최소화하고 있다. 또한 IES에서는 이동 호스트의 연속적인 이동을 위해 주변 기지국들이 사전 전달받은 데이터를 일정기간 삭제를 보류함으로써 중복된 데이터 전송을 피할수 있다. 비용 산출과 시뮬레이션에 의해 기존 기법들과의 성능을 비교함으로서 제안된 기법의 성능을 확인한다.

• 정보처리학회논문지C
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• 제10C권4호
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• pp.471-478
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• 2003

오래 전부터 이동통신 서비스를 위한 통신 프로토콜이나 기능 요소들의 성능을 평가하기 위해서는 분석적 방법, 시뮬레이션 및 평가적 방법이 이용되어 왔다. 이중 시뮬레이션을 통한 평가 방법은 시스템 내부 구성 요소들의 연관 관계가 매우 복잡한 시스템을 테스트하는데 유용하게 사용되고 있으며, 이를 위해서는 이동통신 통화 특성을 반영하는 텔레트래픽 모델을 제시하고 있어야 한다. 텔레트래픽 모델은 일반적으로 트래픽 소스 모델과 네트워크 트랙픽 모델로 구성되어 있으며, 본 네트워크 트래픽 모델을 정의하기 위해 요구되는 실제 기지국 통화량 자료를 수집하고 분석한 결과를 제공하기 위한 것이다. 본 논문에서는 서울시를 상업, 주거, 준공업, 그리고 녹지 지역으로 되어 있는 도시계획 용도지역으로 구분하고, 여기에 설치되어 있는 기지국으로부터 실제 데이터를 시간대별로 수집하였다. 수집된 자료를 이용하여 각 지역별 기지국의 시간대별 통화량 분포와 최대 및 최소 발생 호 수 등을 제시하였다. 분석 결과는 보다 더 정확한 이동통신 네트워크 트래픽 모델을 정의하거나, 기존 이동통신 시뮬레이션 과정에서의 입력 자료로 사용할 수 있다.

• Restorative Dentistry and Endodontics
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• 제37권2호
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• pp.84-89
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• 2012

Objectives: This study analyzed the difference in color caused by different thickness in enamel layer of composite resins when applied with single and layering placement technique, and evaluated if the results agreed with the shade guide from the manufacturers to verify reliability of the color matching process of the manufacturers. Materials and Methods: For single composite resin samples, 6 mm diameter and 4 mm thickness cylindrical samples were fabricated using Ceram-X mono (DENTSPLY DeTrey) and CIE $L^*a^*b^*$ values were measured with spectrophotometer. Same process was done for layering composite resin samples, making 3 dentinal shade samples, 4 mm thickness, for each shade using Ceram-X duo (DENTSPLY DeTrey) and enamel shade resins were layered in 2 mm thickness and CIE $L^*a^*b^*$ values were measured. These samples were ground to 0.2 mm thickness each time, and CIE $L^*a^*b^*$ values were measured to 1 mm thickness of enamel shade resin. Results: Color difference (${\Delta}E^*$) between single and layering composite resin was 1.37 minimum and 10.53 maximum when layering thicknesses were between 1 mm and 2 mm and 6 out of 10 same shade groups suggested by manufacturer showed remarkable color difference at any thickness (${\Delta}E^*$ > 3.3). Conclusion: When using Ceram-X mono and duo for composite resin restoration, following the manufacturer's instructions for choosing the shade is not appropriate, and more accurate information for Ceram-X duo is needed on the variation and expression of the shades depending on the thickness of the enamel.