• Journal of Biosystems Engineering
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• 제37권3호
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• pp.155-165
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• 2012

This study was performed to offer the data for design of the seedling bed transfer equipment to make the automation of working process in a plant factory. The seedling bed transfer equipment pushing the seedling bed with bearing wheels on the rail for interconnecting each working process by a pneumatic cylinder was made and examined. The examined transfer force to push the seedling bed with a weight of 178.9 N by the pneumatic cylinder with length of 60 cm and section area of 5 $cm^2$ was measured by experiments. The examined transfer forces was compared with theoretical ones calculated by the theoretical formula derived from dynamic system analysis according to the number of the seedling bed and pushing speed of the pneumatic cylinder head at no load. The transfer function of the equipment with the input variable as the pushing speed $V_{h0}$(m/s) and the output variable as the transfer force f(t)(N) was represented as $F(s)=(V_{h0}/k)(s+B/M)/(s(s^2+Bs/M+1/(kM))$ where M(kg), k(m/N) and B(Ns/m) are the mass of the bed, the compression coefficient of the pneumatic cylinder and the dynamic friction coefficient between the seedling bed and the rail, respectively. The examined transfer force curves and the theoretical ones were represented similar wave forms as to use the theoretical formular to design the device for the seedling bed transfer. The condition of no vibration of the transfer force curve was $kB^2>4M$. The condition of transferring the bed by the repeatable impact and vibration force according to difference of transfer distance of the pneumatic cylinder head from that of the bed was as $Ce^{-\frac{3{\pi}D}{2\omega}}<-1$, where ${\omega}=\sqrt{\frac{1}{kM}-\frac{B^2}{4M^2}}$, $C=\{\frac{\frac{B}{2M}-\frac{1}{kB}}{\omega}\}$, $D=\frac{B}{2M}$. The examined mean peak transfer force represented 4 times of the stead state transfer force. Therefore it seemed that the transfer force of the pneumatic cylinder required for design of the push device was 4Bv where v is the pushing speed.

• 한국지반신소재학회논문집
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• 제18권4호
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• pp.263-272
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• 2019

본 연구에서는 중구경 현장타설말뚝의 활성화를 위하여, 말뚝재하시험을 이용한 지지력 특성을 평가하였으며, 그 결과를 설계지지력 예측방법과 비교하였다. 정재하시험 결과, 말뚝의 강도가 높은 경우에 낮은 강도에 비하여 약 2.4배 수준의 허용지지력을 나타내는 것으로 평가되었고, 동재하시험 결과에서는 높은 말뚝 강도의 경우가 낮은 경우보다 약 1.4배~1.5배 수준의 허용지지력을 나타내는 것으로 분석되었다. 정재하시험과 동재하시험의 허용지지력에 대한 비교 결과, 동일한 침하량 조건에서는 그 차이가 3%~6% 범위를 나타내었다. 그리고 재하시험 결과와 설계지지력 예측방법을 이용한 지지력 산정결과를 비교한 결과, 선단지지력 및 주면마찰력에 대한 하중분담율에 있어서, FHWA 제안식이 보다 합리적인 예측이 가능한 것으로 확인되었다.

• 농업과학연구
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• 제17권2호
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• pp.102-114
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• 1990

본 연구는 배수갑문의 관리 및 운용 상황을 알기 위하여 삽교호를 모형으로 분석하였으며, 수리모형실험을 통하여 농지개량사업 계획설계기준의 제안식을 검토한 결과는 다음과 같다. 1. 삽교호의 9개년간의 평균 개문(開門)높이 4.13m이었고, 평균 조작연수(操作連數)는 4.04연(連), 연(年)평균 조작회수는 67회(回)이었으며, 배제시간은 연(年)평균 192시간 32분, 1회(回) 평균 2시간 53분 이었다. 2. 삽교호를 통하여 공급한 용수는 연(年)평균 8,815만톤으로 삽교호 유효저수량의 약 1.4배이며, 월별 최대 양수월(揚水月)인 5월의 양수량은 평균 2,956 만톤/년으로 유효저수량의 약 1/2을 양수하였다. 3. 설계기준에 제시된 오리피스 공식은 수중오리피스에서 완전오리피스 형태로 바뀌는 경계영역에서 급격한 배제량의 단절이 나타났으며, 이는 실제 수리현상과 다르므로 개선되어야 한다. 4. 오리피스의 공식은 수중과 완전으로 구분하여 사용하고 있으나, 내 외수위 및 수문 개방도를 고려하여 유량계수를 적용하면 수중 및 완전 오리피스의 모든 경우에도 $q=C{\cdot}W\sqrt{2gH_1}$의 공식을 적용할 수 있다.

• 전자공학회논문지S
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• 제36S권2호
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• pp.120-130
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• 1999

본 연구에서는 복권형 하이브리드 스테핑 전동기의 회전자 위치 함수로 주어지는 순시 상전류식을 유도하여 Laad Angle에 따른 순시 상전류값의 변화를 보이고, 특히 여자 펄스 인가후 ${\pi}/2$ 시점의 수닛 상전류값으로부터 회전자 위치 정보를 얻을 수 있음을 이론식 및 컴퓨터 시뮬레이션에 의해 확인하였다. 이러한 사실으로부터 복권형 하이브리드 스테핑 전동기의 폐루프 운전을 위해 회전자 위치 검출기를 사용하지 않고 전동기의 파라미터가 고려된 최적 Lead Angle이 실현된 여자 펄스를 생성시키는 제어기를 마이크로컨트롤러에 의해 구성하고 실험하였다. 구성된 제어기는 A/D 변환기, 프로그래머블 입.출력 타이머 및 전동기 속도에 대한 최적 Lead Angle 값을 갖는 변환 테이블 등의 기능을 갖는 마이크로컨트롤러와 또한 전동기의 속도와 여자 펄스 인가후 ${\pi}/2$ 시점의 순시 상전류값에 대한 정토오크 발생영역에 해당하는 Lead Angle 값을 갖는 변환 테이블을 위한 ROM 등으로 구성되어 외부 부가회로를 최소화하였으며, 전동기의 파라미터 등의 변화에 따른 제어량의 병환 테이블이 내용과 제어 S/W 에 의존함으로써 유연성을 확보하였다. 이와 같이 구성된 복권형 하이브리드 스테핑 전동기의 회전자 위 센서리스 최적 Lead Angle 시의 순시 상전류 파형과 유사한 파형을 얻음으로써 최적 Lead Angle 이 실현되었음을 확인할 수 있었다.

• 한국구조물진단유지관리공학회 논문집
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• 제22권2호
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• pp.161-168
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• 2018

이 연구는 CRC기둥강도곡선의 비탄성영역에 대한 해석적 고찰이다. CRC기둥강도곡선의 비탄성영역은 최대 잔류응력 크기 $0.5{\sigma}_y$와 Bleich이론을 기초로 하고 있다. 이는 실제로 알려진 최대 압축 잔류응력의 크기가 $0.3{\sigma}_y$인 경우 보다 다소 보수적이다. 본 연구는 열압연강재의 최대 압축 잔류응력의 크기를 $0.3{\sigma}_y$으로 고려하여 그에 따른 기둥강도곡선과 접선탄성계수 Et를 제안하고 이를 CRC에서 제안하고 있는 값들과 각각 비교 고찰한다. 축 압축력을 받는 비탄성 기둥의 응력은 기둥에 작용하는 하중이 좌굴을 일으키기 전에 재료의 비례한도를 넘어 항복점에 도달할 것이다. 따라서 점차적인 단면의 항복 상태에 따른 기둥강도곡선을 검토할 필요가 있다. 본 연구는 최대 압축 잔류응력 ${\sigma}_r=0.5{\sigma}_y$을 사용하여 재료의 항복에 따른 임계하중 곡선식을 유도하고 이를 CRC기둥강도곡선과 비교 고찰한다.

• 한국수산과학회지
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• 제30권5호
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• pp.691-699
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• 1997

본 연구에서는 트롤그물의 유수저항 특성 및 그 저항을 그물의 구조, 규격 등으로 정도 높게 표현해내는 방법을 얻어내는 것을 목약으로 하여, 벽 면적이 $S(m^2)$되는 트롤그물이 유속 $\nu\;(m/sec)$에서 받는 유수저항 R(kg)을 $R=kSv^2$으로 표시하고, 지금까지 행해진 저항실험 결과들을 수집하여 윗 식의 형태로 정리하였으며, 저항계수 $k(kg{\cdot}sec^2/m^4)$를 전보 에서 구한 저항식에 의해 해석하였다. 그 결과, k는 그물 입구의 단면 을 $S_m\;(m^2)$, 흐름에 수직인 평면에 대한 그물의 총 투영면적을 $S_n\;(m^2)$, 그물감의 대표치수를 $\lambda$($={\pi}d^2/2lsin2\varphi;\;d$ : 그물실의 지름, 2l : 그물코의 크기, $2\varphi$ 그물코의 전개각)라 할때, 저층 트롤과 중층 트롤에서 각각 $$k=4.5(\frac{S_n}{S_m})^{1.2}v^{-0.2}$$ in case of bottom trawl nets and as $$k=5.1\lambda^{-0.1}(\frac{S_n}{S_m})^{1.2}v^{-0.2}$$ 및 $$k=5.1\lambda^{-0.1}(\frac{S_n}{S_m})^{1.2}v^{-0.2}$$ 으로 표시할 수 있었고, 이들에서 $S_n/S_m$의 값은 각각의 그물과 벽 면적이 같은 원추형 자루그물로부터 구해도 된다는 것을 알 수 있었으며, 설계 방식이 일반화 되어 있는 그물들의 경우는 유수저항 R(kg)을 저층 트롤과 중층 트롤에서 각각 $$R=1.5\;S\;v^{1.8}$$ 및 $$R=0.7\;S\;v^{1.8}$$으로 표시해도 좋다는 것을 알 수 있었다.

• 한국의학물리학회지:의학물리
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• 제9권2호
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• pp.77-88
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• 1998

쐐기형 선량분포는 임상에 많이 응용하고 있으며 고정쐐기여과판은 선질의 강화와 조사면 주위 의 산란선 증가, 등선량 각도의 불일치, 여과판의 장착 및 취급이 부정확하고 어려우며 입체조형 방사선 치료시 많은 조사면을 입체방향으로 중첩시킴으로서 발생되는 선량의 불균질을 방지하고 동적입체방사선조형치료(dynamic 3D conformal radiotherapy) 및 선량강도조절치료(intensity modulation radiotherapy)를 가능케 하는 동적쐐기여과판을 고안 제작한다. 동적쐐기여과판은 콜리메이터를 움직이면서 선량율을 변화시켜서 최적한 쐐기각의 등량곡선을 얻을 수 있도록 미분치료표(segmented treatment tables: STT) 유도하며 표준형의 STT를 컴퓨터에 입력시킨다. STT에 의하여 생성되는 동적쐐기여과판의 특성과 조직내 선량분포를 쐐기각, 조사변의 크기, 조사선량율둥 여러 조건하에서 측정 분석함으로서 방사선 감수성이 높은 장기 내의 종양과 저항성 이 강한 악성종양치료에 도움을 주며 전반적인 방사선치료 성과를 향상시키고자 한다. 연세암센터에서 가동되는 선형가속기 (Varian Clinac-2100C/D)를 이용하여 6MV 와 10MV 광자선과 쐐기각이 15$^{\circ}$, 30$^{\circ}$, 45$^{\circ}$, 60$^{\circ}$이고 정사각형 조사면의 한변이 4cm 부터 20cm 범위를 0.5cm 간격으로 콜리메이터를 움직이면서 선량 변동량을 표시하는 미분치료표 (STT)를 작성하였다. 쐐기투과선량인자 (wedge transmission factor) 는 표준 물팬텀내에 표준전리함을 장치하고 열린조사면과 미분치료표에 의한 쐐기조사면의 선량비료서 결정하였다. 쐐기여과판에 의한 조직내선량분포와 등량곡선 및 프로파일은 필름으로 측정하고 영상선량측정기로 작성하였다. 수식으로 유도한 미분치료표(segmented treatment tables: STT) 은 쐐기여과판의 쐐기각과 일치하였으며 쐐기투과선량인자는 쐬기각이 클수록 감소하였으며 조사변이 클수록 적어졌고 조사면 크기와의 관계는 비선형적이었다. 동적쐐기여과판에 의한 등량곡선의 쐐기 기울기는 고형여과판보다 더욱 일치된 경사각을 유지하였다. 심부선량백율은 열린조사면에 의한 것과 거의 비슷하였으며 고형쐐기여과판의 심부율보다 약간 줄어들었다. 동적쐐기여과판은 고형쐐기여과판보다 사용상, 선량측정 및 선량분포에 서 장점이 많으며 피부와 여과판사이의 길이가 길어서 침대에 부딪치는 일이 없고 피부의 산란선 오염이 감소되어 치료효과를 상승시킬 수 있다. 동적쐐기조사방법을 개발함으로서 지금까지 방사선 후유증과 종양의 불균일한 선량배열로 치료의 어려움이 있었던 분야를 개척할 수 있으며 동적입체 방사선조형치료 (dynamic 3D conformal radiotherapy) 및 선량강도조정치료 (intensity modulation radiotherapy)를 가능하게 함으로서 방사선치료성과를 향상시킬 수 있다.

• 한국농공학회지
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• 제19권1호
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• pp.4296-4311
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• 1977

This study was conducted to derive an Instantaneous Unit Hydrograph for the accurate and reliable unitgraph which can be used to the estimation and control of flood for the development of agricultural water resources and rational design of hydraulic structures. Eight small watersheds were selected as studying basins from Han, Geum, Nakdong, Yeongsan and Inchon River systems which may be considered as a main river systems in Korea. The area of small watersheds are within the range of 85 to 470$\textrm{km}^2$. It is to derive an accurate Instantaneous Unit Hydrograph under the condition of having a short duration of heavy rain and uniform rainfall intensity with the basic and reliable data of rainfall records, pluviographs, records of river stages and of the main river systems mentioned above. Investigation was carried out for the relations between measurable unitgraph and watershed characteristics such as watershed area, A, river length L, and centroid distance of the watershed area, Lca. Especially, this study laid emphasis on the derivation and application of Instantaneous Unit Hydrograph (IUH) by applying Nash's conceptual model and by using an electronic computer. I U H by Nash's conceptual model and I U H by flood routing which can be applied to the ungaged small watersheds were derived and compared with each other to the observed unitgraph. 1 U H for each small watersheds can be solved by using an electronic computer. The results summarized for these studies are as follows; 1. Distribution of uniform rainfall intensity appears in the analysis for the temporal rainfall pattern of selected heavy rainfall event. 2. Mean value of recession constants, Kl, is 0.931 in all watersheds observed. 3. Time to peak discharge, Tp, occurs at the position of 0.02 Tb, base length of hlrdrograph with an indication of lower value than that in larger watersheds. 4. Peak discharge, Qp, in relation to the watershed area, A, and effective rainfall, R, is found to be {{{{ { Q}_{ p} = { 0.895} over { { A}^{0.145 } } }}}} AR having high significance of correlation coefficient, 0.927, between peak discharge, Qp, and effective rainfall, R. Design chart for the peak discharge (refer to Fig. 15) with watershed area and effective rainfall was established by the author. 5. The mean slopes of main streams within the range of 1.46 meters per kilometer to 13.6 meter per kilometer. These indicate higher slopes in the small watersheds than those in larger watersheds. Lengths of main streams are within the range of 9.4 kilometer to 41.75 kilometer, which can be regarded as a short distance. It is remarkable thing that the time of flood concentration was more rapid in the small watersheds than that in the other larger watersheds. 6. Length of main stream, L, in relation to the watershed area, A, is found to be L=2.044A0.48 having a high significance of correlation coefficient, 0.968. 7. Watershed lag, Lg, in hrs in relation to the watershed area, A, and length of main stream, L, was derived as Lg=3.228 A0.904 L-1.293 with a high significance. On the other hand, It was found that watershed lag, Lg, could also be expressed as {{{{Lg=0.247 { ( { LLca} over { SQRT { S} } )}^{ 0.604} }}}} in connection with the product of main stream length and the centroid length of the basin of the watershed area, LLca which could be expressed as a measure of the shape and the size of the watershed with the slopes except watershed area, A. But the latter showed a lower correlation than that of the former in the significance test. Therefore, it can be concluded that watershed lag, Lg, is more closely related with the such watersheds characteristics as watershed area and length of main stream in the small watersheds. Empirical formula for the peak discharge per unit area, qp, ㎥/sec/$\textrm{km}^2$, was derived as qp=10-0.389-0.0424Lg with a high significance, r=0.91. This indicates that the peak discharge per unit area of the unitgraph is in inverse proportion to the watershed lag time. 8. The base length of the unitgraph, Tb, in connection with the watershed lag, Lg, was extra.essed as {{{{ { T}_{ b} =1.14+0.564( { Lg} over {24 } )}}}} which has defined with a high significance. 9. For the derivation of IUH by applying linear conceptual model, the storage constant, K, with the length of main stream, L, and slopes, S, was adopted as {{{{K=0.1197( {L } over { SQRT {S } } )}}}} with a highly significant correlation coefficient, 0.90. Gamma function argument, N, derived with such watershed characteristics as watershed area, A, river length, L, centroid distance of the basin of the watershed area, Lca, and slopes, S, was found to be N=49.2 A1.481L-2.202 Lca-1.297 S-0.112 with a high significance having the F value, 4.83, through analysis of variance. 10. According to the linear conceptual model, Formular established in relation to the time distribution, Peak discharge and time to peak discharge for instantaneous Unit Hydrograph when unit effective rainfall of unitgraph and dimension of watershed area are applied as 10mm, and $\textrm{km}^2$ respectively are as follows; Time distribution of IUH {{{{u(0, t)= { 2.78A} over {K GAMMA (N) } { e}^{-t/k } { (t.K)}^{N-1 } }}}} (㎥/sec) Peak discharge of IUH {{{{ {u(0, t) }_{max } = { 2.78A} over {K GAMMA (N) } { e}^{-(N-1) } { (N-1)}^{N-1 } }}}} (㎥/sec) Time to peak discharge of IUH tp=(N-1)K (hrs) 11. Through mathematical analysis in the recession curve of Hydrograph, It was confirmed that empirical formula of Gamma function argument, N, had connection with recession constant, Kl, peak discharge, QP, and time to peak discharge, tp, as {{{{{ K'} over { { t}_{ p} } = { 1} over {N-1 } - { ln { t} over { { t}_{p } } } over {ln { Q} over { { Q}_{p } } } }}}} where {{{{K'= { 1} over { { lnK}_{1 } } }}}} 12. Linking the two, empirical formulars for storage constant, K, and Gamma function argument, N, into closer relations with each other, derivation of unit hydrograph for the ungaged small watersheds can be established by having formulars for the time distribution and peak discharge of IUH as follows. Time distribution of IUH u(0, t)=23.2 A L-1S1/2 F(N, K, t) (㎥/sec) where {{{{F(N, K, t)= { { e}^{-t/k } { (t/K)}^{N-1 } } over { GAMMA (N) } }}}} Peak discharge of IUH) u(0, t)max=23.2 A L-1S1/2 F(N) (㎥/sec) where {{{{F(N)= { { e}^{-(N-1) } { (N-1)}^{N-1 } } over { GAMMA (N) } }}}} 13. The base length of the Time-Area Diagram for the IUH was given by {{{{C=0.778 { ( { LLca} over { SQRT { S} } )}^{0.423 } }}}} with correlation coefficient, 0.85, which has an indication of the relations to the length of main stream, L, centroid distance of the basin of the watershed area, Lca, and slopes, S. 14. Relative errors in the peak discharge of the IUH by using linear conceptual model and IUH by routing showed to be 2.5 and 16.9 percent respectively to the peak of observed unitgraph. Therefore, it confirmed that the accuracy of IUH using linear conceptual model was approaching more closely to the observed unitgraph than that of the flood routing in the small watersheds.

• 한국농공학회지
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• 제16권2호
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• pp.3361-3394
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• 1974

The purpose of this thesis is to disclose some characteristics of water consumption in relation to the quantities of dry matters through the growing period for two statured varieties of paddy rice which are a tall statured variety and a short one, including the water consumption during seedling period, and to find out the various coefficients of evapotranspiration that are applicable for the water use of an expected yield of the two varieties. PAL-TAL, a tall statured variety, and TONG-lL, a short statured variety were chosen for this investigation. Experiments were performed in two consecutive periods, a seedling period and a paddy field period, In the investigation of seedling period, rectangular galvanized iron evapotranspirometers (91cm${\times}$85cm${\times}$65cm) were set up in a way of two levels (PAL-TAL and TONG-lL varieties) with two replications. A standard fertilization method was applied to all plots. In the experiment of paddy field period, evapotanspiration and evaporation were measured separately. For PAL-TAL variety, the evapotranspiration measurements of 43 plots of rectangular galvanized iron evapotranspirometer (91cm${\times}$85cm${\times}$65cm) and the evaporation measurements of 25 plots of rectangular galvanized iron evaporimeter (91cm${\times}$85cm${\times}$15cm) have been taken for seven years (1966 through 1972), and for TONG-IL variety, the evapotranspiration measurements of 19 plots and the evaporation measurements of 12 plots have been collected for two years (1971 through 1972) with five different fertilization levels. The results obtained from this investigation are summarized as follows: 1. Seedling period 1) The pan evaporation and evapotranspiration during seedling period were proved to have a highly significant correlation to solar radiation, sun shine hours and relative humidity. But they had no significant correlation to average temperature, wind velocity and atmospheric pressure, and were appeared to be negatively correlative to average temperature and wind velocity, and positively correlative to the atmospheric pressure, in a certain period. There was the highest significant correlation between the evapotranspiration and the pan evaporation, beyond all other meteorological factors considered. 2) The evapotranpiration and its coefficient for PAL-TAL variety were 194.5mm and 0.94∼1.21(1.05 in average) respectively, while those for TONG-lL variety were 182.8mm and 0.90∼1.10(0.99 in average) respectively. This indicates that the evapotranspiration for TONG-IL variety was 6.2% less than that for PAL-TAL variety during a seedling period. 3) The evapotranspiration ratio (the ratio of the evapotranspiration to the weight of dry matters) during the seedling period was 599 in average for PAL-TAL variety and 643 for TONG-IL variety. Therefore the ratio for TONG-IL was larger by 44 than that for PAL-TAL variety. 4) The K-values of Blaney and Criddle formula for PAL-TAL variety were 0.78∼1.06 (0.92 in average) and for TONG-lL variety 0.75∼0.97 (0.86 in average). 5) The evapotranspiration coefficient and the K-value of B1aney and Criddle formular for both PAL-TAL and TONG-lL varieties showed a tendency to be increasing, but the evapotranspiration ratio decreasing, with the increase in the weight of dry matters. 2. Paddy field period 1) Correlation between the pan evaporation and the meteorological factors and that between the evapotranspiration and the meteorological factors during paddy field period were almost same as that in case of the seedling period (Ref. to table IV-4 and table IV-5). 2) The plant height, in the same level of the weight of dry matters, for PAL-TAL variety was much larger than that for TONG-IL variety, and also the number of tillers per hill for PAL-TAL variety showed a trend to be larger than that for TONG-IL variety from about 40 days after transplanting. 3) Although there was a tendency that peak of leaf-area-index for TONG-IL variety was a little retarded than that for PAL-TAL variety, it appeared about 60∼80 days after transplanting. The peaks of the evapotranspiration coefficient and the weight of dry matters at each growth stage were overlapped at about the same time and especially in the later stage of growth, the leaf-area-index, the evapotranspiration coefficient and the weight of dry matters for TONG-IL variety showed a tendency to be larger then those for PAL-TAL variety. 4) The evaporation coefficient at each growth stage for TONG-IL and PAL-TALvarieties was decreased and increased with the increase and decrease in the leaf-area-index, and the evaporation coefficient of TONG-IL variety had a little larger value than that of PAL-TAL variety. 5) Meteorological factors (especially pan evaporation) had a considerable influence to the evapotranspiration, the evaporation and the transpiration. Under the same meteorological conditions, the evapotranspiration (ET) showed a increasing logarithmic function of the weight of dry matters (x), while the evaporation (EV) a decreasing logarithmic function of the weight of dry matters; 800kg/10a x 2000kg/10a, ET=al+bl logl0x (bl>0) EV=a2+b2 log10x (a2>0 b2<0) At the base of the weight of total dry matters, the evapotranspiration and the evaporation for TONG-IL variety were larger as much as 0.3∼2.5% and 7.5∼8.3% respectively than those of PAL-TAL variety, while the transpiration for PAL-TAL variety was larger as much as 1.9∼2.4% than that for TONG-IL variety on the contrary. At the base of the weight of rough rices the evapotranspiration and the transpiration for TONG-IL variety were less as much as 3.5% and 8.l∼16.9% respectively than those for PAL-TAL variety and the evaporation for TONG-IL was much larger by 11.6∼14.8% than that for PAL-TAL variety. 6) The evapotranspiration coefficient, the evaporation coefficient and the transpiration coefficient and the transpiration coefficient were affected by the weight of dry matters much more than by the meteorological conditions. The evapotranspiratioa coefficient (ETC) and the evaporation coefficient (EVC) can be related to the weight of dry matters (x) by the following equations: 800kg/10a x 2000kg/10a, ETC=a3+b3 logl0x (b3>0) EVC=a4+b4 log10x (a4>0, b4>0) At the base of the weights of dry matters, 800kg/10a∼2000kg/10a, the evapotranspiration coefficients for TONG-IL variety were 0.968∼1.474 and those for PAL-TAL variety, 0.939∼1.470, the evaporation coefficients for TONG-IL variety were 0.504∼0.331 and those for PAL-TAL variety, 0.469∼0.308, and the transpiration coefficients for TONG-IL variety were 0.464∼1.143 and those for PAL-TAL variety, 0.470∼1.162. 7) The evapotranspiration ratio, the evaporation ratio (the ratio of the evaporation to the weight of dry matters) and the transpiration ratio were highly affected by the meteorological conditions. And under the same meteorological condition, both the evapotranspiration ratio (ETR) and the evaporation ratio (EVR) showed to be a decreasing logarithmic function of the weight of dry matters (x) as follows: 800kg/10a x 2000kg/10a, ETR=a5+b5 logl0x (a5>0, b5<0) EVR=a6+b6 log10x (a6>0 b6<0) In comparison between TONG-IL and PAL-TAL varieties, at the base of the pan evaporation of 343mm and the weight of dry matters of 800∼2000kg/10a, the evapotranspiration ratios for TONG-IL variety were 413∼247, while those for PAL-TAL variety, 404∼250, the evaporation ratios for TONG-IL variety were 197∼38 while those for PAL-TAL variety, 182∼34, and the transpiration ratios for TONG-IL variety were 216∼209 while those for PAL-TAL variety, 222∼216 (Ref. to table IV-23, table IV-25 and table IV-26) 8) The accumulative values of evapotranspiration intensity and transpiration intensity for both PAL-TAL and TONG-IL varieties were almost constant in every climatic year without the affection of the weight of dry matters. Furthermore the evapotranspiration intensity appeared to have more stable at each growth stage. The peaks of the evapotranspiration intensity and transpiration intensity, for both TONG-IL and PAL-TAL varieties, appeared about 60∼70 days after transplanting, and the peak value of the former was 128.8${\pm}$0.7, for TONG-IL variety while that for PAL-TAL variety, 122.8${\pm}$0.3, and the peak value of the latter was 152.2${\pm}$1.0 for TONG-IL variety while that for PAL-TAL variety, 152.7${\pm}$1.9 (Ref.to table IV-27 and table IV-28) 9) The K-value in Blaney & Criddle formula was changed considerably by the meteorological condition (pan evaporation) and related to be a increasing logarithmic function of the weight of dry matters (x) for both PAL-TAL and TONG-L varieties as follows; 800kg/10a x 2000kg/10a, K=a7+b7 logl0x (b7>0) The K-value for TONG-IL variety was a little larger than that for PAL-TAL variety. 10) The peak values of the evapotranspiration coefficient and k-value at each growth stage for both TONG-IL and PAL-TAL varieties showed up about 60∼70 days after transplanting. The peak values of the former at the base of the weights of total dry matters, 800∼2000kg/10a, were 1.14∼1.82 for TONG-IL variety and 1.12∼1.80, for PAL-TAL variety, and at the base of the weights of rough rices, 400∼1000 kg/10a, were 1.11∼1.79 for TONG-IL variety and 1.17∼1.85 for PAL-TAL variety. The peak values of the latter, at the base of the weights of total dry matters, 800∼2000kg/10a, were 0.83∼1.39 for TONG-IL variety and 0.86∼1.36 for PAL-TAL variety and at the base of the weights of rough rices, 400∼1000kg/10a, 0.85∼1.38 for TONG-IL variety and 0.87∼1.40 for PAL-TAL variety (Ref. to table IV-18 and table IV-32) 11) The reasonable and practicable methods that are applicable for calculating the evapotranspiration of paddy rice in our country are to be followed the following priority a) Using the evapotranspiration coefficients based on an expected yield (Ref. to table IV-13 and table IV-18 or Fig. IV-13). b) Making use of the combination method of seasonal evapotranspiration coefficient and evapotranspiration intensity (Ref. to table IV-13 and table IV-27) c) Adopting the combination method of evapotranspiration ratio and evapotranspiration intensity, under the conditions of paddy field having a higher level of expected yield (Ref. to table IV-23 and table IV-27). d) Applying the k-values calculated by Blaney-Criddle formula. only within the limits of the drought year having the pan evaporation of about 450mm during paddy field period as the design year (Ref. to table IV-32 or Fig. IV-22).