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*Corresponding Author. Tel: +82-52-259-2262 E-mail: [email protected] (H.-J. Cho) J. Korea Water Resour. Assoc. Vol. 49, No. 11 (2016), pp. 941-949 pISSN 1226-6280 doi: 10.3741/JKWRA.2016.49.11.941 eISSN 2287-6138 Estimation of discharge coefficients of the broad-crested side weir with various levee's side slope of main channel Kang, Ho-Seon a ใ†Cho, Hong-Je b * a National Disaster Management Research Institute b Dept., of Civil & Environmental Engrg., University of Ulsan Paper number: 16-060 Received: 13 July 2016; Revised: 22 September 2016 / 29 September 2016; Accepted: 29 September 2016 Abstract The flow characteristics of the broad-crested side weir considering the leveeโ€™s side slope of main channel (ESch) was investigated through hydraulic experiment in order to estimate the discharge coefficient equation. For applicability to actual river, leveeโ€™s side slope of main channel 1:0.5, 1:1 and 1:2 were selected. Experimental results show that the new estimated equation for the discharge coefficient including ESch is reasonable and effective in actual applications by comparing estimated and measured discharge over side weirs. Through a multiple linear regression analysis the importance of variabes were ordered as ESch > h/yu > L/yu > Fru. Especially the discharge coefficient equation without Fru was suggested, and the high applicability was reviewed by comparing the measured and calculated overflow of broad-chested side weir. Keywords: Leveeโ€™s side slope, Hydraulic experiment, Discharge coefficient, Broad-crested side weir ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ์— ๋”ฐ๋ฅธ ๊ด‘์ •ํšก์›”๋ฅ˜์œ„์–ด์˜ ์œ ๋Ÿ‰๊ณ„์ˆ˜ ์‚ฐ์ • ๊ฐ•ํ˜ธ์„  a ใ†์กฐํ™์ œ b * a ๊ตญ๋ฆฝ์žฌ๋‚œ์•ˆ์ „์—ฐ๊ตฌ์›, b ์šธ์‚ฐ๋Œ€ํ•™๊ต ๊ณต๊ณผ๋Œ€ํ•™ ๊ฑด์„คํ™˜๊ฒฝ๊ณตํ•™๋ถ€ ์š” ์ง€ ๊ตญ๋ณธ ์—ฐ๊ตฌ์—์„œ๋Š” ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ(ESch)์— ๋”ฐ๋ฅธ ๊ด‘์ •ํšก์›”๋ฅ˜์œ„์–ด์—์„œ์˜ ํ๋ฆ„๋ณ€ํ™”๋ฅผ ์ˆ˜๋ฆฌ๋ชจํ˜•์‹คํ—˜์„ ํ†ตํ•ด ๋ถ„์„ํ•˜๊ณ , ๊ทธ์— ๋”ฐ๋ฅธ ์œ ๋Ÿ‰๊ณ„ ์ˆ˜์‚ฐ์ •์‹์„ ์ œ์‹œํ•˜์˜€๋‹ค. ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ๋Š” ์‹ค์ œ ํ•˜์ฒœ์—์„œ์˜ ์ ์šฉ์„ฑ์„ ๊ณ ๋ คํ•˜์—ฌ 1:0.5, 1:1, 1:2๋ฅผ ์„ ์ •ํ•˜์˜€๋‹ค. ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ๊ฐ€ ํฌํ•จ๋œ ๊ด‘์ •ํšก์›”๋ฅ˜ ์œ„์–ด์˜ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‚ฐ์ •์‹์€ ๊ธฐ์กด์˜ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‚ฐ์ •์‹ ๋ณด๋‹ค ํ•ฉ๋ฆฌ์ ์ด๊ณ  ์ ์šฉ์„ฑ์ด ๋†’์€ ๊ฒƒ์œผ๋กœ ํ™•์ธ๋˜์—ˆ๋‹ค. ๋‹ค์ค‘ํšŒ๊ท€๋ถ„์„๊ฒฐ๊ณผ ๋ณ€์ˆ˜ ์ค‘ ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ ์‚ฌ๋ฉด๊ฒฝ์‚ฌ(ESch)>ํšก์›”๋ฅ˜์œ„์–ด๋†’์ด-์ƒ๋ฅ˜์ˆ˜์‹ฌ๋น„(h/yu)>ํšก์›”๋ฅ˜์œ„์–ด๊ธธ์ด-์ƒ๋ฅ˜์ˆ˜์‹ฌ๋น„(L/yu)>์ƒ๋ฅ˜ ํ‘ธ๋ฅด๋“œ์ˆ˜(Fru)์˜ ์ˆœ์„œ๋กœ ์ค‘์š”๋„๊ฐ€ ๋†’์€ ๊ฒƒ์œผ๋กœ ๋‚˜ํƒ€ ๋‚ฌ๋‹ค. ํŠนํžˆ ๊ธฐ์กด์˜ ์—ฐ๊ตฌ์™€ ๊ฐœ์ˆ˜๋กœ ํ๋ฆ„์—์„œ ๊ฐ€์žฅ ์ค‘์š”ํ•œ ์ธ์ž์ธ Froude ์ˆ˜๊ฐ€ ํฌํ•จ๋˜์ง€ ์•Š์€ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‚ฐ์ •์‹์„ ์ œ์•ˆํ•˜์˜€์œผ๋ฉฐ, ๊ทธ ์ ์šฉ์„ฑ๋„ ๋†’์€ ๊ฒƒ ์œผ๋กœ ๋‚˜ํƒ€๋‚ฌ๋‹ค. ํ•ต์‹ฌ์šฉ์–ด: ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ, ์ˆ˜๋ฆฌ๋ชจํ˜•์‹คํ—˜, ์œ ๋Ÿ‰๊ณ„์ˆ˜, ๊ด‘์ •ํšก์›”๋ฅ˜์œ„์–ด ยฉ 2016 Korea Water Resources Association. All rights reserved. 1. ์„œ ๋ก  ์ตœ๊ทผ ๊ธฐํ›„๋ณ€ํ™”๋กœ ์ธํ•œ ์ง‘์ค‘ํ˜ธ์šฐ๋ฐœ์ƒ, ๋„์‹œํ™”๋กœ ์ธํ•œ ์œ ์ถœ ๋Ÿ‰์ฆ๊ฐ€๋กœ ํ™์ˆ˜ํ”ผํ•ด์ž ์žฌ๋Šฅ์ด ์ง€์†์ ์œผ๋กœ ์ฆ๊ฐ€ํ•˜๊ณ  ์žˆ๋‹ค. ํ™ ์ˆ˜๋Ÿ‰์„ ์œ ์—ญ ๋‚ด์— ๋ถ„๋‹ด์‹œํ‚ค๊ธฐ ์œ„ํ•ด ๊ฐ•์šฐ ์œ ์ถœ์ˆ˜๋ฅผ ์ผ์‹œ ์ €๋ฅ˜ ํ•˜์—ฌ ์œ ์ถœ๋Ÿ‰์„ ์กฐ์ ˆํ•˜๋Š” Off-line๋ฐฉ์‹์˜ ์ €๋ฅ˜์ง€๋ฅผ ๊ฑด์„คํ•˜๋Š” ๋ฐฉ์•ˆ์ด ์ œ์‹œ๋˜๊ณ  ์žˆ๋‹ค. Off-line ์ €๋ฅ˜์ง€์˜ ์œ ์ž…๋ถ€์— ์„ค์น˜๋˜๋Š” ํšก์›”๋ฅ˜์œ„์–ด๋Š” ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ํ๋ฆ„๋ฐฉํ–ฅ์— ํ‰ํ–‰ํ•˜๊ฒŒ ์„ค์น˜๋˜๋Š” ์ˆ˜ ๊ณต๊ตฌ์กฐ๋ฌผ๋กœ, ๋ณธ๋ฅ˜์˜ ์ˆ˜์‹ฌ์ด ํšก์›”๋ฅ˜์œ„์–ด์˜ ๋†’์ด๋ณด๋‹ค ๋†’์„ ๊ฒฝ ์šฐ ์œ„์–ด๋ฅผ ํ†ตํ•ด ์œ ๋Ÿ‰์„ ์ €๋ฅ˜์ง€๋กœ ๋ฐฐ์ œํ•˜๊ฒŒ ๋˜๋ฉฐ ์—๋„ˆ์ง€ ์†Œ์‚ฐ, ์ˆ˜์œ„์˜ ์•ˆ์ •, ์ผ์ •์œ ๋Ÿ‰์˜ ์ทจ์ˆ˜ ๋ฐ ๋ถ„๋ฐฐ, ํ™์ˆ˜์†Œํ†ต ๋“ฑ์˜ ๋ชฉ์ ์œผ
Transcript
Page 1: Estimation of discharge coefficients of the broad-crested ...

*Corresponding Author. Tel: +82-52-259-2262

E-mail: [email protected] (H.-J. Cho)

J. Korea Water Resour. Assoc. Vol. 49, No. 11 (2016), pp. 941-949 pISSN 1226-6280

doi: 10.3741/JKWRA.2016.49.11.941 eISSN 2287-6138

Estimation of discharge coefficients of the broad-crested side weir with various

levee's side slope of main channel

Kang, Ho-Seonaใ†Cho, Hong-Je

b*

aNational Disaster Management Research InstitutebDept., of Civil & Environmental Engrg., University of Ulsan

Paper number: 16-060

Received: 13 July 2016; Revised: 22 September 2016 / 29 September 2016; Accepted: 29 September 2016

Abstract

The flow characteristics of the broad-crested side weir considering the leveeโ€™s side slope of main channel (ESch) was investigated

through hydraulic experiment in order to estimate the discharge coefficient equation. For applicability to actual river, leveeโ€™s side slope

of main channel 1:0.5, 1:1 and 1:2 were selected. Experimental results show that the new estimated equation for the discharge coefficient

including ESch is reasonable and effective in actual applications by comparing estimated and measured discharge over side weirs.

Through a multiple linear regression analysis the importance of variabes were ordered as ESch > h/yu > L/yu > Fru. Especially the

discharge coefficient equation without Fru was suggested, and the high applicability was reviewed by comparing the measured and

calculated overflow of broad-chested side weir.

Keywords: Leveeโ€™s side slope, Hydraulic experiment, Discharge coefficient, Broad-crested side weir

๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ์— ๋”ฐ๋ฅธ ๊ด‘์ •ํšก์›”๋ฅ˜์œ„์–ด์˜ ์œ ๋Ÿ‰๊ณ„์ˆ˜ ์‚ฐ์ •

๊ฐ•ํ˜ธ์„ aใ†์กฐํ™์ œ

b*

a๊ตญ๋ฆฝ์žฌ๋‚œ์•ˆ์ „์—ฐ๊ตฌ์›,

b์šธ์‚ฐ๋Œ€ํ•™๊ต ๊ณต๊ณผ๋Œ€ํ•™ ๊ฑด์„คํ™˜๊ฒฝ๊ณตํ•™๋ถ€

์š” ์ง€

๊ตญ๋ณธ ์—ฐ๊ตฌ์—์„œ๋Š” ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ(ESch)์— ๋”ฐ๋ฅธ ๊ด‘์ •ํšก์›”๋ฅ˜์œ„์–ด์—์„œ์˜ ํ๋ฆ„๋ณ€ํ™”๋ฅผ ์ˆ˜๋ฆฌ๋ชจํ˜•์‹คํ—˜์„ ํ†ตํ•ด ๋ถ„์„ํ•˜๊ณ , ๊ทธ์— ๋”ฐ๋ฅธ ์œ ๋Ÿ‰๊ณ„

์ˆ˜์‚ฐ์ •์‹์„ ์ œ์‹œํ•˜์˜€๋‹ค. ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ๋Š” ์‹ค์ œ ํ•˜์ฒœ์—์„œ์˜ ์ ์šฉ์„ฑ์„ ๊ณ ๋ คํ•˜์—ฌ 1:0.5, 1:1, 1:2๋ฅผ ์„ ์ •ํ•˜์˜€๋‹ค. ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ๊ฐ€ ํฌํ•จ๋œ ๊ด‘์ •ํšก์›”๋ฅ˜

์œ„์–ด์˜ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‚ฐ์ •์‹์€ ๊ธฐ์กด์˜ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‚ฐ์ •์‹ ๋ณด๋‹ค ํ•ฉ๋ฆฌ์ ์ด๊ณ  ์ ์šฉ์„ฑ์ด ๋†’์€ ๊ฒƒ์œผ๋กœ ํ™•์ธ๋˜์—ˆ๋‹ค. ๋‹ค์ค‘ํšŒ๊ท€๋ถ„์„๊ฒฐ๊ณผ ๋ณ€์ˆ˜ ์ค‘ ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ

์‚ฌ๋ฉด๊ฒฝ์‚ฌ(ESch)>ํšก์›”๋ฅ˜์œ„์–ด๋†’์ด-์ƒ๋ฅ˜์ˆ˜์‹ฌ๋น„(h/yu)>ํšก์›”๋ฅ˜์œ„์–ด๊ธธ์ด-์ƒ๋ฅ˜์ˆ˜์‹ฌ๋น„(L/yu)>์ƒ๋ฅ˜ ํ‘ธ๋ฅด๋“œ์ˆ˜(Fru)์˜ ์ˆœ์„œ๋กœ ์ค‘์š”๋„๊ฐ€ ๋†’์€ ๊ฒƒ์œผ๋กœ ๋‚˜ํƒ€

๋‚ฌ๋‹ค. ํŠนํžˆ ๊ธฐ์กด์˜ ์—ฐ๊ตฌ์™€ ๊ฐœ์ˆ˜๋กœ ํ๋ฆ„์—์„œ ๊ฐ€์žฅ ์ค‘์š”ํ•œ ์ธ์ž์ธ Froude ์ˆ˜๊ฐ€ ํฌํ•จ๋˜์ง€ ์•Š์€ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‚ฐ์ •์‹์„ ์ œ์•ˆํ•˜์˜€์œผ๋ฉฐ, ๊ทธ ์ ์šฉ์„ฑ๋„ ๋†’์€ ๊ฒƒ

์œผ๋กœ ๋‚˜ํƒ€๋‚ฌ๋‹ค.

ํ•ต์‹ฌ์šฉ์–ด: ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ, ์ˆ˜๋ฆฌ๋ชจํ˜•์‹คํ—˜, ์œ ๋Ÿ‰๊ณ„์ˆ˜, ๊ด‘์ •ํšก์›”๋ฅ˜์œ„์–ด

ยฉ 2016 Korea Water Resources Association. All rights reserved.

1. ์„œ ๋ก 

์ตœ๊ทผ ๊ธฐํ›„๋ณ€ํ™”๋กœ ์ธํ•œ ์ง‘์ค‘ํ˜ธ์šฐ๋ฐœ์ƒ, ๋„์‹œํ™”๋กœ ์ธํ•œ ์œ ์ถœ

๋Ÿ‰์ฆ๊ฐ€๋กœ ํ™์ˆ˜ํ”ผํ•ด์ž ์žฌ๋Šฅ์ด ์ง€์†์ ์œผ๋กœ ์ฆ๊ฐ€ํ•˜๊ณ  ์žˆ๋‹ค. ํ™

์ˆ˜๋Ÿ‰์„ ์œ ์—ญ ๋‚ด์— ๋ถ„๋‹ด์‹œํ‚ค๊ธฐ ์œ„ํ•ด ๊ฐ•์šฐ ์œ ์ถœ์ˆ˜๋ฅผ ์ผ์‹œ ์ €๋ฅ˜

ํ•˜์—ฌ ์œ ์ถœ๋Ÿ‰์„ ์กฐ์ ˆํ•˜๋Š” Off-line๋ฐฉ์‹์˜ ์ €๋ฅ˜์ง€๋ฅผ ๊ฑด์„คํ•˜๋Š”

๋ฐฉ์•ˆ์ด ์ œ์‹œ๋˜๊ณ  ์žˆ๋‹ค. Off-line ์ €๋ฅ˜์ง€์˜ ์œ ์ž…๋ถ€์— ์„ค์น˜๋˜๋Š”

ํšก์›”๋ฅ˜์œ„์–ด๋Š” ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ํ๋ฆ„๋ฐฉํ–ฅ์— ํ‰ํ–‰ํ•˜๊ฒŒ ์„ค์น˜๋˜๋Š” ์ˆ˜

๊ณต๊ตฌ์กฐ๋ฌผ๋กœ, ๋ณธ๋ฅ˜์˜ ์ˆ˜์‹ฌ์ด ํšก์›”๋ฅ˜์œ„์–ด์˜ ๋†’์ด๋ณด๋‹ค ๋†’์„ ๊ฒฝ

์šฐ ์œ„์–ด๋ฅผ ํ†ตํ•ด ์œ ๋Ÿ‰์„ ์ €๋ฅ˜์ง€๋กœ ๋ฐฐ์ œํ•˜๊ฒŒ ๋˜๋ฉฐ ์—๋„ˆ์ง€ ์†Œ์‚ฐ,

์ˆ˜์œ„์˜ ์•ˆ์ •, ์ผ์ •์œ ๋Ÿ‰์˜ ์ทจ์ˆ˜ ๋ฐ ๋ถ„๋ฐฐ, ํ™์ˆ˜์†Œํ†ต ๋“ฑ์˜ ๋ชฉ์ ์œผ

Page 2: Estimation of discharge coefficients of the broad-crested ...

H.-S. Kang and H.-J. Cho / Journal of Korea Water Resources Association 49(11) 941-949942

(a) Longitudinal Cross-section (b) Plan

Fig. 1. Definition sketch of a rectangular side weir flow

๋กœ ์‚ฌ์šฉ๋œ๋‹ค.

์šฐ๋ฆฌ๋‚˜๋ผ๋Š” ํ˜„์žฌ off-line ์ €๋ฅ˜์ง€ ์œ ์ž…๋Ÿ‰ ์‚ฐ์ • ์‹œ์—๋Š” De

Marchi (1934) ๊ณต์‹๊ณผ ์ด๋ฅผ ๊ทผ๊ฑฐ๋กœ ํ•œ ์‹คํ—˜์‹์„ ์ฃผ๋กœ ์‚ฌ์šฉํ•˜

๊ณ  ์žˆ์œผ๋ฉฐ, ํŠนํžˆ De Marchi ๊ณต์‹์„ ์ด์šฉํ•˜์—ฌ ํšก์›”๋ฅ˜๋Ÿ‰์„ ์‚ฐ์ •

ํ•  ๊ฒฝ์šฐ ์œ ๋Ÿ‰๊ณ„์ˆ˜๋ฅผ 0.623์œผ๋กœ ๊ณ ์ •ํ•˜์—ฌ ์‚ฌ์šฉํ•˜๋„๋ก ํ•˜๊ณ  ์žˆ

๋‹ค. ๋˜ํ•œ ์ตœ๊ทผ ์šฐ์ˆ˜์ €๋ฅ˜์‹œ์„ค ์„ค์น˜์‚ฌ์—… ํƒ€๋‹น์„ฑ ์กฐ์‚ฌ ๋ฐ ๊ธฐ๋ณธ๊ณ„

ํš ์ž‘์„ฑ ์š”๋ น(๊ตญ๋ฏผ์•ˆ์ „์ฒ˜, 2015)์—์„œ๋Š” ํ˜ผํ•ฉ์‹์„ ์‚ฌ์šฉํ•˜๋„

๋ก ๋˜์–ด ์žˆ์œผ๋ฉฐ, ์ด๋•Œ ์œ ๋Ÿ‰๊ณ„์ˆ˜๋Š” 0.623์œผ๋กœ ๊ณ ์ •ํ•˜์—ฌ ์‚ฌ์šฉํ•˜

๋„๋ก ๋˜์–ด์žˆ์ง€๋งŒ ๊ฐœ๋žต์ ์ธ ๊ฐ’์ด๋ผ ๋ช…์‹œ๋˜์–ด ์‹ ๋ขฐํ•  ๋งŒํ•œ ๊ฐ’์€

๋˜์ง€ ๋ชปํ•˜๊ณ  ์žˆ๋‹ค. ํŠนํžˆ ํƒ์ง€ ๋ฐ ๋„์‹œ๊ฐœ๋ฐœ์‚ฌ์—… ๋“ฑ์œผ๋กœ ์ธํ•ด ์ฆ

๊ฐ€๋œ ํ™์ˆ˜๋Ÿ‰์„ ์›”๋ฅ˜์‹œํ‚ฌ ๋ชฉ์ ์œผ๋กœ ์ด์šฉ๋˜๋Š” off-line ์ €๋ฅ˜์ง€

์— ์ ํ•ฉํ•œ ์‹ ๋ขฐํ•  ๋งŒํ•œ ์œ ๋Ÿ‰๊ณ„์ˆ˜๊ฐ€ ์ œ์‹œ๋˜์–ด ์žˆ์ง€ ์•Š์œผ๋ฏ€๋กœ,

์ด์— ๋Œ€ํ•œ ์‹คํ—˜ ๋ฐ ๊ฒ€์ฆ์ด ์š”๊ตฌ๋˜๊ณ  ์žˆ๋‹ค.

ํšก์›”๋ฅ˜์œ„์–ด์— ๋Œ€ํ•œ ์—ฐ๊ตฌ ์ดˆ๊ธฐ์—๋Š” ์‚ฌ๊ฐํ˜• ๋‹จ๋ฉด์˜ ์˜ˆ์—ฐํšก

์›”๋ฅ˜์œ„์–ด์˜ ์œ ๋Ÿ‰๊ณ„์ˆ˜ ์‚ฐ์ถœ์— ์ง‘์ค‘๋˜์—ˆ์œผ๋ฉฐ, ์ตœ๊ทผ์—๋Š” ์‹คํ—˜

์‹ค์ด ์•„๋‹Œ ํ•˜์ฒœ์—์„œ์˜ ์ ์šฉ์„ฑ์„ ์œ„ํ•˜์—ฌ ์‚ฌ๋‹ค๋ฆฌ๊ผด ํ˜•ํƒœ์˜ ์ˆ˜๋กœ

์— ์„ค์น˜๋œ ๊ด‘์ •ํšก์›”๋ฅ˜์œ„์–ด์—์„œ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹์„ ์‚ฐ์ •ํ•˜๋Š” ์—ฐ๊ตฌ

๊ฐ€ ์ด๋ฃจ์–ด์กŒ๋‹ค.

ํšก์›”๋ฅ˜์œ„์–ด์— ๋Œ€ํ•œ ์›”๋ฅ˜๋Ÿ‰ ์‚ฐ์ •์‹๊ณผ ์œ ๋Ÿ‰๊ณ„์ˆ˜ ์‚ฐ์ •์‹์€

De Marchhi (1934)๊ฐ€ ์ฒ˜์Œ ์ œ์‹œํ•˜์˜€์œผ๋ฉฐ, ํšก์›”๋ฅ˜์œ„์–ด์˜ ๊ธธ

์ด๋ฐฉํ–ฅ์— ๋”ฐ๋ผ ์œ„์–ด์˜ ์œ ๋Ÿ‰๊ณ„์ˆ˜๊ฐ€ ์ผ์ •ํ•˜๋‹ค๊ณ  ๊ฐ€์ •ํ•˜์˜€๋‹ค.

Subramanya์™€ Awasthy (1972) ๋Š” ์ˆ˜๊ฐ€ ์œ ๋Ÿ‰๊ณ„์ˆ˜์˜

์ฃผ๋œ ๋ณ€์ˆ˜์ž„์„ ๋ฐํžˆ๊ณ , ์ƒ๋ฅ˜์™€ ์‚ฌ๋ฅ˜์— ๋Œ€ํ•œ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹์„ ์ œ

์•ˆํ•˜์˜€๋‹ค. Ranga et al. (1979)์€ ์˜ˆ์—ฐ์œ„์–ด์™€ ๊ด‘์ •์œ„์–ด๋ฅผ ๊ตฌ๋ถ„

ํ•˜์—ฌ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹์„ ์ œ์•ˆํ•˜์˜€๊ณ , Hager (1987), Cheong (1991)

๋ฐ Jilili and Borghei (1996)๋Š” ํšก์›”๋ฅ˜ ๋†’์ด์— ๋”ฐ๋ฅธ ์œ ๋Ÿ‰๊ณ„์ˆ˜

์‹์„ ์ œ์•ˆํ•œ ๋ฐ” ์žˆ๋‹ค. ๋˜ํ•œ Ali Uyumaz (1997)์€ ์œ„์–ด๊ธธ์ด์™€

ํ•˜๋„ ํญ ๋น„๋ฅผ ๊ณ ๋ คํ•˜๊ณ  ์ƒ๋ฅ˜์™€ ์‚ฌ๋ฅ˜๋ฅผ ๊ตฌ๋ถ„ํ•˜์—ฌ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹์„

์ œ์•ˆํ•˜์˜€์œผ๋ฉฐ, Honar and Keshavarzi (2009)๋Š” ๊ด‘์ •ํšก์›”๋ฅ˜

์œ„์–ด์˜ ์ธก๋ฒฝ์˜ ํ˜•์ƒ์„ ์›ํ˜•์œผ๋กœ ํ•˜์—ฌ ์›”๋ฅ˜๋ถ€ ์ธก๋ฒฝํ˜•์ƒ ๋ณ€ํ™”์—

๋”ฐ๋ฅธ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‚ฐ์ •์— ๋Œ€ํ•˜์—ฌ ์—ฐ๊ตฌํ•˜์˜€์œผ๋‚˜, ํšก์›”๋ฅ˜์œ„์–ด์˜

ํ˜•์ƒ๋ณ€ํ™”๋Š” ๊ณ ๋ คํ•˜์ง€ ์•Š์•˜๋‹ค.

Park and Lee (2010)์€ ํญ์ด ๋„“์€ ์ง์‚ฌ๊ฐํ˜• ์ˆ˜๋กœ์—์„œ ๊ธฐ์กด

์˜ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹์ด ์ˆ˜์— ์ง€๋ฐฐ๋ฅผ ๋ฐ›๋Š” ํ•œ๊ณ„๋ฅผ ๊ตฌ๋ช…ํ•˜์—ฌ,

์œ„์–ด์˜ ์ œ์›์„ ๋ฐ˜์˜ํ•˜๋Š” ๋ฌด์ฐจ์› ๋ณ€์ˆ˜๋ฅผ ๊ณ ๋ คํ•œ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹์„

์ œ์•ˆํ•œ ๋ฐ” ์žˆ์œผ๋‚˜ ์œ„์–ด ์ž์ฒด์˜ ํ˜•์ƒ์€ ๊ณ ๋ ค๋˜์ง€ ์•Š์•˜๋‹ค. Yoon

and Cho (2011)๋Š” ์‹ค์ œํ•˜์ฒœ ๋‹จ๋ฉด์— ๊ฐ€๊นŒ์šด ์‚ฌ๋‹ค๋ฆฌ๊ผด ๋‹จ๋ฉด์˜

์ˆ˜๋กœ์—์„œ ์‚ฌ๋‹ค๋ฆฌ๊ผด ๊ด‘์ •ํšก์›”๋ฅ˜์œ„์–ด์— ๋Œ€ํ•œ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹์„ ์ƒ

๋ฅ˜์™€ ์‚ฌ๋ฅ˜๋กœ ๊ตฌ๋ถ„ํ•˜์—ฌ ์ œ์‹œํ•˜์˜€์œผ๋ฉฐ, ๊ด‘์ •ํšก์›”๋ฅ˜์œ„์–ด์˜ ๊ธฐ

ํ•˜ํ•™์ ํ˜•์ƒ์— ๋”ฐ๋ผ ๋ณธ๋ฅ˜ ๋ฐ ํšก์›”๋ฅ˜์œ„์–ด์˜ ์›”๋ฅ˜๋Ÿ‰์ด ํฐ ์˜ํ–ฅ์„

๋ฐ›์„ ๊ฒƒ์œผ๋กœ ์˜ˆ์ƒํ•œ ๋ฐ” ์žˆ๋‹ค.

๊ธฐ์กด์˜ ์—ฐ๊ตฌ์—์„œ๋Š” ํ•˜์ฒœ๋ณธ๋ฅ˜์˜ ๋‹จ๋ฉด์„ ์ง์‚ฌ๊ฐํ˜• ๋˜๋Š” ์‚ฌ

๋‹ค๋ฆฌ๊ผด ๋“ฑ์œผ๋กœ ๊ณ ์ •์‹œํ‚จ ๋‹จ์ผ ์ˆ˜๋กœ์—์„œ ํšก์›”๋ฅ˜์œ„์–ด์— ๋Œ€ํ•œ

๊ฒ€ํ† ๊ฐ€ ์ด๋ฃจ์–ด์ ธ ์™”์œผ๋‚˜, ์‹ค์ œ ํ•˜์ฒœ์— ์ ์šฉํ•˜๊ธฐ ์œ„ํ•ด์„œ๋Š” ๋‹ค

์–‘ํ•œ ๋ณธ๋ฅ˜์˜ ๋‹จ๋ฉด ํ˜•์ƒ์ด๋‚˜ ์ œ๋ฐฉ์‚ฌ๋ฉด์˜ ๊ฒฝ์‚ฌ ๋“ฑ์ด ๊ณ ๋ ค๋˜์–ด์•ผ

ํ•œ๋‹ค. ์ฆ‰, ์œ„์–ด๊ฐ€ ์„ค์น˜๋œ ํ›„์—๋„ ํšก์›”๋ฅ˜์œ„์–ด์—์„œ ๋ฐœ์ƒํ•  ์ˆ˜ ์žˆ

๋Š” ์ˆ˜์œ„๋ณ€ํ™”, ์œ ์†๋ณ€ํ™” ๋ฐ ํ๋ฆ„๋ฐฉํ–ฅ ๋ณ€ํ™” ๋“ฑ์˜ ํ๋ฆ„์–‘์ƒ์ด ๋ณธ

๋ฅ˜์กฐ๊ฑด์— ๋”ฐ๋ผ ๋‹ค๋ฅด๊ฒŒ ๋‚˜ํƒ€๋‚  ๊ฒƒ์œผ๋กœ ์˜ˆ์ธก๋˜์ง€๋งŒ, ์ด์— ๋Œ€ํ•œ

์—ฐ๊ตฌ๋Š” ์ง„ํ–‰๋œ ๋ฐ”๊ฐ€ ์—†๋‹ค. ๊ตญ๋‚ด ํ•˜์ฒœ์„ค๊ณ„๊ธฐ์ค€์—์„œ๋Š” ํ•˜์ฒœ ์ œ

๋ฐฉ๊ฒฝ์‚ฌ๋ฅผ 1:3์ด์ƒ์œผ๋กœ ์ œ์•ˆํ•˜๊ณ  ์žˆ์œผ๋‚˜ ์‹ค์ œ ๋„์‹ฌ์ง€์˜ ํ•˜์ฒœ

์˜ ๊ฒฝ์šฐ ์ˆ˜์ง์ธ ์ œ๋ฐฉ๋ถ€ํ„ฐ ๋‹ค์–‘ํ•˜๊ฒŒ ์„ค๊ณ„๋˜์–ด ์žˆ๋‹ค. ๋ณธ ์—ฐ๊ตฌ์—

์„œ๋Š” ํšก์›”๋ฅ˜์œ„์–ด๊ฐ€ ์„ค์น˜๋˜๋Š” ๋ณธ๋ฅ˜์˜ ๋‹ค์–‘ํ•œ ์ œ๋ฐฉ๊ฒฝ์‚ฌ์กฐ๊ฑด์—

๋Œ€ํ•ด์„œ ์ •ํ™•ํ•œ ํšก์›”๋ฅ˜๋Ÿ‰์„ ์‚ฐ์ •ํ•  ์ˆ˜ ์žˆ๋Š” ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹์„ ์ œ์•ˆ

ํ•˜์˜€๋‹ค.

2. ํšก์›”๋ฅ˜์œ„์–ด ๊ธฐ๋ณธ์ด๋ก 

ํšก์›”๋ฅ˜์œ„์–ด ํ๋ฆ„์— ๋Œ€ํ•œ ๊ธฐ๋ณธ์ด๋ก ์‹์€ Fig. 1์— ๋‚˜ํƒ€๋‚ธ ๋ฐ”

์™€ ๊ฐ™์ด ์ง์‚ฌ๊ฐํ˜• ํšก์›”๋ฅ˜์œ„์–ด์— ๋Œ€ํ•œ ํ•˜์ƒ๊ฒฝ์‚ฌ์™€ ๋‹จ๋ฉด์ด ์ผ์ •

ํ•œ ์ˆ˜๋กœ์— ๋Œ€ํ•œ ์œ ๋Ÿ‰๊ณต์‹์ธ ์‹ (1)๊ณผ ๊ฐ™๋‹ค.

(1)

์—ฌ๊ธฐ์„œ, ๋Š” ํšก์›”๋ฅ˜๋Ÿ‰, , ๋Š” ํšก์›”๋ฅ˜ ์ „โ€คํ›„ ๋ณธ๋ฅ˜์œ ๋Ÿ‰,

์€ ์œ ๋Ÿ‰๊ณ„์ˆ˜, ๋Š” ํšก์›”๋ฅ˜์œ„์–ด์—์„œ ์ธก์ •ํ•œ ์ˆ˜์‹ฌ, ๋Š” ํšก์›”๋ฅ˜์œ„

์–ด ๋†’์ด, ์€ ์œ„์–ด ํญ, ๋Š” ํ๋ฆ„๋ฐฉํ–ฅ๊ฑฐ๋ฆฌ, ๋Š” ๋ณธ๋ฅ˜ํ•˜ํญ, ๋Š”

์ค‘๋ ฅ๊ฐ€์†๋„์ด๋‹ค.

Lee and Holley (2002)๋Š” ์‚ฌ๋‹ค๋ฆฌ๊ผด ์ˆ˜๋กœ์— ์„ค์น˜๋œ ์‚ฌ๋‹ค๋ฆฌ๊ผด

Page 3: Estimation of discharge coefficients of the broad-crested ...

H.-S. Kang and H.-J. Cho / Journal of Korea Water Resources Association 49(11) 941-949 943

Fig. 2. Definition sketch of a traperzoidal side weir flow

Fig. 3. Schematic description of experimental facility

Fig. 4. Observation points of flow of main channel

Fig. 5. Shape of side slope of main channel (

)

๊ด‘์ •์œ„์–ด์— ๋Œ€ํ•œ ์›”๋ฅ˜๋Ÿ‰ ์‚ฐ์ •์‹์„ ์‹ (2)์™€ ๊ฐ™์ด ์ œ์•ˆํ•˜์˜€๋‹ค.

(2)

์—ฌ๊ธฐ์„œ, ๋Š” ์ „์œ ๋Ÿ‰๊ณ„์ˆ˜์ด๊ณ , ๋Š” ์ž ์ˆ˜๋ณด์ •๊ณ„์ˆ˜์ด๋‹ค. ์€

์‚ฌ๋‹ค๋ฆฌ๊ผด ํšก์›”๋ฅ˜์œ„์–ด์˜ ์ €๋ฉดํญ์ด๊ณ , ๋Š” ์œ„์–ด์˜ ์ธก๋ฉด๊ฒฝ์‚ฌ

์ด๋‹ค. ๋Š” ํšก์›”๋ฅ˜์œ„์–ด์˜ ํ•˜๋ฅ˜๋ถ€ ๋ณธ๋ฅ˜ํ•˜๋„์˜ ์ค‘์‹ฌ์ˆ˜์œ„์ด๊ณ ,

ํšก์›”๋ฅ˜์œ„์–ด ๋งˆ๋ฃจ๊ฐ€ ๊ธฐ์ค€์ด๋‹ค. Yoon and Cho (2011)๋Š” ์‹ค์ œ

ํ•˜์ฒœ์— ์ ์šฉ์„ฑ์ด ๋†’์€ ์‚ฌ๋‹ค๋ฆฌ๊ผด ์ˆ˜๋กœ์˜ ๊ด‘์ •ํšก์›”๋ฅ˜์œ„์–ด์˜ ์œ 

๋Ÿ‰๊ณ„์ˆ˜๋ฅผ ์‚ฐ์ •ํ•˜๊ธฐ ์œ„ํ•ด ์œ„์–ด ํ๋ฆ„์˜ ์ฃผ์š” ๋ณ€์ˆ˜๋“ค์ธ ์ƒ๋ฅ˜

์ˆ˜, ์œ„์–ด ๋†’์ด ๋ฐ ๊ธธ์ด, ๋ณธ๋ฅ˜ ์ˆ˜๋กœ ํญ ๋ฐ ๊ฒฝ์‚ฌ ๋“ฑ์„ ๊ณ ๋ ค

ํ•˜์˜€๊ณ , Fig. 2์™€ ๊ฐ™์€ ์‚ฌ๋‹ค๋ฆฌ๊ผด ํšก์›”๋ฅ˜์œ„์–ด์— ๋Œ€ํ•ด ์‹ (1)๊ณผ ์‹

(2)๋ฅผ ๊ธฐ์ดˆ๋กœ ํ•œ ์‹ (3)๊ณผ ์‹ (4)๋ฅผ ๊ธฐ๋ณธ์ด๋ก ์‹์œผ๋กœ ์ œ์•ˆํ•˜์˜€๋‹ค.

(3)

(4)

์—ฌ๊ธฐ์„œ, ์€ ์œ„์–ด๊ธธ์ด, ๋Š” ์œ„์–ด๋ถ€ ํ‰๊ท ์ˆ˜์‹ฌ, ๋Š” ์œ„์–ด๋†’์ด,

๋Š” ์œ„์–ด๋ถ€ ์ธก๋ฉด์˜ ๊ฒฝ์‚ฌ, ์€ ์œ ๋Ÿ‰๊ณ„์ˆ˜๋กœ์„œ ํšก์›”๋ฅ˜์œ„์–ด

์˜ ๊ธธ์ด๋ฐฉํ–ฅ์— ๋”ฐ๋ผ ๋ณ€ํ•˜์ง€ ์•Š๊ณ  ์ผ์ •ํ•˜๋‹ค. ๋ณธ ์—ฐ๊ตฌ์—์„œ๋Š” ์‹

(3)๊ณผ ์‹(4)๋ฅผ ๊ธฐ๋ณธ์ด๋ก ์‹์œผ๋กœ ํ•˜์—ฌ ๊ด‘์ •ํšก์›”๋ฅ˜์œ„์–ด์˜ ๊ธฐํ•˜

ํ•™์  ํ˜•์ƒ์„ ๊ณ ๋ คํ•œ ์œ ๋Ÿ‰๊ณ„์ˆ˜๋ฅผ ์‚ฐ์ •ํ•˜์˜€๋‹ค.

3. ์‹คํ—˜์กฐ๊ฑด ๋ฐ ๊ฒฐ๊ณผ๋ถ„์„

3.1 ์ˆ˜๋ฆฌ์‹คํ—˜ ์กฐ๊ฑด

๊ธฐ๋ณธ์ ์ธ ์ˆ˜๋ฆฌ์‹คํ—˜ ์žฅ์น˜๋Š” Fig. 3๊ณผ ๊ฐ™๊ณ , ๊ธธ์ด 14.0 m, ํญ

0.6 m, ๋†’์ด 0.2 m, ๊ฐ€๋ณ€๊ฒฝ์‚ฌ์˜ ๊ฐœ์ˆ˜๋กœ ์‹คํ—˜์žฅ์น˜๋ฅผ ์ด์šฉํ•˜์˜€

์œผ๋ฉฐ, ์ด๋•Œ ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ๋ฅผ 1:0.5, 1:1, 1:2๋กœ ๋ณ€ํ™”

์‹œ์ผœ ์‹คํ—˜์„ ์ง„ํ–‰ํ•˜์˜€๋‹ค.

์ธก์ ์˜ ์œ„์น˜๋Š” Fig. 4์™€ ๊ฐ™์ด ์ˆ˜๋กœ์— ์ด 35๊ฐœ์˜ ํšก๋‹จ๋ฉด์„

์„ค์ •ํ•˜์˜€๊ณ , ํšก์›”๋ฅ˜์œ„์–ด๊ฐ€ ์„ค์น˜๋˜๋Š” ์ˆ˜๋กœ ์ค‘์‹ฌ๋ถ€ 4.4 m ๊ตฌ๊ฐ„

์—์„œ ๋ณธ๋ฅ˜ ํ๋ฆ„๋ณ€ํ™”๋ฅผ ์„ธ๋ฐ€ํ•˜๊ฒŒ ๊ด€์ฐฐํ•˜๊ธฐ ์œ„ํ•ด 0.2 m์˜ ์กฐ๋ฐ€

ํ•œ ๊ฐ„๊ฒฉ์œผ๋กœ ๊ตฌ์„ฑํ•˜์˜€๋‹ค. ๋‚˜๋จธ์ง€ ๊ตฌ๊ฐ„์€ 0.5 m ๊ฐ„๊ฒฉ์œผ๋กœ ๊ตฌ์„ฑ

ํ•˜์—ฌ ์ˆ˜๋กœ ์ค‘์‹ฌ์—์„œ ์ˆ˜์‹ฌ๊ณผ ์œ ์†์„ ์ธก์ •ํ•˜์˜€์œผ๋ฉฐ, ํฌ์ธํŠธ๊ฒŒ

์ด์ง€์™€ 2์ฐจ์› ์ „์ž์‹์œ ์†๊ณ„ VM 801-H๋ฅผ ์ด์šฉํ•˜์˜€๋‹ค. ๊ทธ๋ฆฌ

๊ณ  ํšก์›”๋ฅ˜๋Ÿ‰์€ ์œ ๋„์ˆ˜๋กœ๋ฅผ ํ†ตํ•ด ์ €์ˆ˜์กฐ๋กœ ์œ ์ž…์‹œํ‚จ ํ›„ ์˜ˆ์—ฐ์œ„

์–ด ๋ฐ ์ˆ˜์กฐ๋ฅผ ์ด์šฉํ•˜์—ฌ ์ธก์ •ํ•˜์˜€์œผ๋ฉฐ, ๊ด‘์ •ํšก์›”๋ฅ˜์˜ ํญ(๋‘๊ป˜)

์€ 2 cm์ด๊ณ  ์œ„์–ด์˜ ์›”๋ฅ˜ ํ๋ฆ„๋ฐฉํ–ฅ์˜ ๊ธธ์ด๋ฅผ ๋‚˜ํƒ€๋‚ธ๋‹ค.

Off-line ์ €์ˆ˜์ง€์˜ ์„ค๊ณ„๊ธฐ์ค€๊ณผ ์น˜์ˆ˜ํšจ๊ณผ์— ๊ด€ํ•œ ์—ฐ๊ตฌ

(2006, ๋Œ€ํ•œ์ฃผํƒ๊ณต์‚ฌ)์—์„œ off-line ์ €๋ฅ˜์ง€์˜ ๊ตญ๋‚ด ์žฌํ•ด์˜ํ–ฅ

ํ‰๊ฐ€์„œ๋ฅผ ์กฐ์‚ฌํ•œ ๊ฒฐ๊ณผ, ์ €๋ฅ˜์ง€๊ฐ€ ์„ค์น˜๋œ ํ•˜์ฒœ์—์„œ ํšก์›”๋ฅ˜์œ„

์–ด ํŠน์„ฑ์€ ๊ฐ€ 0.3~16.25 (ํ‰๊ท  4.04), ๋Š” 0.44~0.97

(ํ‰๊ท  0.76), ๋Š” 0.37~58.27 (ํ‰๊ท  7.79)๋กœ ์„ค๊ณ„๋˜์—ˆ๊ณ ,

๋Š” 0.31~1.03์˜ ์กฐ๊ฑด์„ ๊ฐ€์ง€๊ณ  ์žˆ์€ ๊ฒƒ์œผ๋กœ ์กฐ์‚ฌ๋˜์—ˆ๋‹ค.

์ด๋ฅผ ์ฐธ๊ณ ํ•˜์—ฌ ๋ณธ ์—ฐ๊ตฌ์˜ ์ˆ˜๋ฆฌ์‹คํ—˜ ์žฅ์น˜๋ฅผ ์„ค๊ณ„ํ•˜์˜€์œผ๋ฉฐ, ๋ณธ

๋ฅ˜์ˆ˜๋กœ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ์— ๋”ฐ๋ฅธ ํšก์›”๋ฅ˜์œ„์–ด์˜ ํ๋ฆ„ํŠน์„ฑ์„

๋ถ„์„ํ•˜๊ธฐ ์œ„ํ•˜์—ฌ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ๋ฅผ 1:0.5, 1:1, 1:2๋กœ ๋ณ€ํ™”์‹œ์ผœ

ํšก์›”๋ฅ˜์œ„์–ด์— ๋Œ€ํ•œ ์‹คํ—˜์„ ํ•˜์˜€๋‹ค. ์‹คํ—˜์— ์‚ฌ์šฉ๋œ ๋ณธ๋ฅ˜์ˆ˜๋กœ

์˜ ํšก๋‹จ๋ฉดํ˜•์ƒ์€ Fig. 5์— ๋‚˜ํƒ€๋‚ด์—ˆ๋‹ค.

์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ์— ๋”ฐ๋ผ ์‚ฌ์šฉ๋œ ์‹คํ—˜์กฐ๊ฑด ๋ฐ ๋ฐฉ๋ฒ•์€ Table 1

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Table 1. Range of test variables

Channel Shape (m3/sec)

(%)

1:0.5 Trapezoidal

5.0, 3.0, 1.00.020โˆผ0.030

(at a 0.005 interval)

0.1โˆผ0.7

(at a 0.2 interval)0.41โˆผ1.59 7.4ร—10

4 ~ 1.06ร—10

61:1 Trapezoidal

1:2 Trapezoidal

(a) =1.0

(b) =3.0

(c) =5.0

Fig. 6. Variation of at the slope of 0.1%

(a) =1.0

(b) =3.0

(c) =5.0

Fig. 7. Variation of at the slope of 0.3%

๊ณผ ๊ฐ™๋‹ค. ์ฆ‰, ๋ณธ๋ฅ˜์˜ ์œ ๋Ÿ‰ ์กฐ๊ฑด์€ 0.020 m3/sec, 0.025 m

3/sec,

0.030 m3/sec์ด๊ณ , ํ”„๋ฃจ๋“œ์ˆ˜ ์™€ ํšก์›”๋ฅ˜์œ„์–ด ๋†’์ด(0.06 m)-

์ƒ๋ฅ˜์ˆ˜์‹ฌ๋น„ ๋ฅผ ๊ณ ๋ คํ•˜๊ธฐ ์œ„ํ•ด ํ•˜์ƒ๊ฒฝ์‚ฌ๋ฅผ 0.1~0.7%๊นŒ

์ง€ 0.2% ๊ฐ„๊ฒฉ์œผ๋กœ 4๊ฐ€์ง€ ๊ฒฝ์šฐ๋กœ ํ•˜์˜€๋‹ค. ๋˜ํ•œ ์œ„์–ด์˜ ๊ธธ์ด๋ฅผ

1.0 m, 0.6 m, 0.2 m๋กœ ํ•˜์—ฌ L/B๊ฐ€ 5.0, 3.0, 1.0์œผ๋กœ ๋ณ€ํ™”์‹œ์ผฐ๊ณ 

์œ„์–ดํญ์€ 0.02 m๋กœ ๊ณ ์ •ํ•˜์˜€๋‹ค. ๋”ฐ๋ผ์„œ ๋ณธ ์—ฐ๊ตฌ์—์„œ ์‹ค์‹œํ•œ

์ด ์‹คํ—˜ํšŸ์ˆ˜๋Š” ๋ณธ๋ฅ˜ ์ˆ˜๋กœ์˜ ๊ฐ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ๋ณ„๋กœ 36case, ์ฆ‰

๋ชจ๋‘ 108case์— ๋Œ€ํ•ด ์‹คํ—˜ํ•˜์˜€๋‹ค. ๊ทธ๋ฆฌ๊ณ  ์‹คํ—˜์‹œ Reynolds์ˆ˜

๊ฐ€ ๋„ˆ๋ฌด ์ž‘๊ฒŒ ๋˜๋ฉด ์ธต๋ฅ˜ํ๋ฆ„์—์„œ์˜ ์ ์„ฑํšจ๊ณผ๊ฐ€ ๋‚˜ํƒ€๋‚  ์ˆ˜ ์žˆ

๋‹ค. ๋ณธ ์‹คํ—˜์กฐ๊ฑด์—์„œ์˜ Reynolds์ˆ˜๊ฐ€ 7.4ร—104 ~ 1.06ร—10

6๋กœ

์„œ ๋‚œ๋ฅ˜ํ๋ฆ„์„ ๋‚˜ํƒ€๋‚ด๋ฏ€๋กœ ์ ์„ฑํšจ๊ณผ๋Š” ๊ณ ๋ คํ•˜์ง€ ์•Š์•˜์œผ๋ฉฐ,

๋ชจ๋“  ํ๋ฆ„์—์„œ ์ ์šฉ์„ฑ์ด ๋†’์„ ๊ฒƒ์œผ๋กœ ํŒ๋‹จ๋œ๋‹ค.

3.2 ํšก์›”๋ฅ˜์œ„์–ด์˜ ํ๋ฆ„ํŠน์„ฑ ๋ถ„์„

๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ์— ๋”ฐ๋ผ ํšก์›”๋ฅ˜์œ„์–ด๋ถ€์˜ ํ๋ฆ„ํŠน

์„ฑ์€ ํšก์›”๋ฅ˜์œ„์–ด์˜ ํญ๊ณผ ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ํ๋ฆ„์กฐ๊ฑด ๋ณ€ํ™”์— ๋”ฐ๋ผ

๋‹ฌ๋ผ์ง€๋ฏ€๋กœ, ํšก์›”๋ฅ˜์œ„์–ด์˜ ํญ๊ณผ ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์œ ๋Ÿ‰๋ณ€ํ™”์— ๋”ฐ

๋ฅธ ํšก์›”๋ฅ˜์œ„์–ด๋ถ€์™€ ํšก์›”๋ฅ˜์œ„์–ด ์ƒยทํ•˜๋ฅ˜๋ถ€์˜ ์˜ ๋ณ€ํ™”๋ฅผ ๋ถ„

์„ํ•˜์˜€๋‹ค. ์ด๋•Œ ์‚ฌ์šฉํ•œ ์กฐ๊ฑด์€ ์ˆ˜๋กœ๊ฒฝ์‚ฌ 0.1~0.7% (0.2% ๊ฐ„

๊ฒฉ), ์œ ๋Ÿ‰ 20~30 (5 ๊ฐ„๊ฒฉ)์ด๋ฉฐ, ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ค‘์‹ฌ์—์„œ

์ธก์ •๋œ ์ž๋ฃŒ๋ฅผ ์ด์šฉํ•˜์—ฌ ๋ถ„์„ํ•˜์˜€๋‹ค. ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด

๊ฒฝ์‚ฌ์— ๋”ฐ๋ฅธ ํšก์›”๋ฅ˜์œ„์–ด๋ถ€ ๋ณ€ํ™”๋ฅผ Fig. 6~9์— ๋‚˜ํƒ€๋‚ด์—ˆ๋‹ค.

์ˆ˜๋กœ๊ฒฝ์‚ฌ๊ฐ€ 0.1%์ผ ๊ฒฝ์šฐ, ๋ณธ๋ฅ˜์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ๊ฐ€ ๊ธ‰ํ• ์ˆ˜๋ก

ํšก์›”๋ฅ˜์œ„์–ด ์ƒ๋ฅ˜๋ถ€์—์„œ ๊ฐ€ ์ฆ๊ฐ€ํ•˜๊ธฐ ์‹œ์ž‘ํ•˜์—ฌ ์œ„์–ดํญ์˜

์•ฝ 2/3์ง€์ ๊นŒ์ง€ ๊ฐ€ ์ฆ๊ฐ€ํ•˜๋‹ค๊ฐ€, ํšก์›”๋ฅ˜์œ„์–ด ํ•˜๋ฅ˜๋ถ€์—์„œ๋Š”

๊ฐ€ ๊ฐ์†Œํ•˜๋Š” ๊ฒฝํ–ฅ์„ ๋ณด์ธ๋‹ค. ์ˆ˜๋กœ๊ฒฝ์‚ฌ 0.3%์˜ ๊ฒฝ์šฐ๋Š” ๋ณธ๋ฅ˜

์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ๊ฐ€ ๊ธ‰ํ• ์ˆ˜๋ก ํšก์›”๋ฅ˜์œ„์–ด๋ถ€์—์„œ ์œ ๋Ÿ‰์ด ํด ๊ฒฝ

์šฐ ๊ณ„์†ํ•ด์„œ ๊ฐ€ ์ฆ๊ฐ€ํ•˜๋Š” ๊ฒฝํ–ฅ์„ ๋ณด์ด๋ฉฐ, ์™„๋งŒํ•  ์ˆ˜๋ก์ˆ˜๋กœ

๊ฒฝ์‚ฌ 0.1%์™€ ๋น„์Šทํ•œ ๊ฒฝํ–ฅ์„ ๋ณด์ด๋ฉฐ ๊ฐ์†Œํ•œ๋‹ค. ์ˆ˜๋กœ๊ฒฝ์‚ฌ๊ฐ€

0.5% ๋ฐ 0.7%๋กœ ์ปค์ง€๋Š” ๊ฒฝ์šฐ์—๋Š” ์œ„์–ด์ƒ๋ฅ˜๋ถ€์—์„œ ๊ฐ€ 1.0

๋„˜๋Š” ๊ฒƒ์œผ๋กœ ๋‚˜ํƒ€๋‚ฌ๊ณ , ์œ„์–ด์ค‘์‹ฌ๋ถ€์—์„œ ์œ„์–ดํ•˜๋ฅ˜๋ถ€๊นŒ์ง€๋Š”

๊ณ„์†ํ•ด์„œ ๊ฐ€ ๊ฐ์†Œํ•˜๋Š” ๊ฒฝํ–ฅ์„ ๋ณด์ธ๋‹ค. ๋˜ํ•œ ์ˆ˜๋กœ๊ฒฝ์‚ฌ

0.3%์—์„œ ๋ถ€ํ„ฐ ํšก์›”๋ฅ˜๋ถ€์—์„œ ๊ฐ€ 1์ด ๋„˜๋Š” ์ง€์—ญ์ด ์กฐ๊ธˆ์”ฉ

๋‚˜ํƒ€๋‚˜๋Š” ๊ฒƒ์„ ํ™•์ธํ•˜์˜€๊ณ , ์ˆ˜๋กœ๊ฒฝ์‚ฌ๊ฐ€ 0.5% ์ด์ƒ์ด ๋˜๋ฉด

ํšก์›”๋ฅ˜์œ„์–ด์˜ ์ „๋ฐ˜๋ถ€๋Š” ๊ฐ€ ๊ฑฐ์˜ ๋Œ€๋ถ€๋ถ„ 1์ด ๋„˜๋Š” ๊ฒƒ์œผ๋กœ

๋‚˜ํƒ€๋‚ฌ๋‹ค.

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H.-S. Kang and H.-J. Cho / Journal of Korea Water Resources Association 49(11) 941-949 945

(a) =1.0

(b) =3.0

(c) =5.0

Fig. 8. Variation of at the slope of 0.5%

(a) =1.0

(b) =3.0

(c) =5.0

Fig. 9. Variation of at the slope of 0.7%

3.3 ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ์— ๋”ฐ๋ฅธ ํšก์›”๋ฅ˜์œ„์–ด ์œ ๋Ÿ‰

๊ณ„์ˆ˜์‹

๊ธฐ์กด์˜ ํšก์›”๋ฅ˜์œ„์–ด์— ๋Œ€ํ•œ ์—ฐ๊ตฌ๋Š” ์œ„์–ด์ž์ฒด์˜ ํ˜•์ƒ์ด๋‚˜

ํฌ๊ธฐ ๋ฐ ๋†’์ด ๋“ฑ์— ๋”ฐ๋ฅธ ํ๋ฆ„ํ˜„์ƒ ๊ตฌ๋ช…๊ณผ ์œ ๋Ÿ‰๊ณ„์ˆ˜ ์‚ฐ์ •์— ์ง‘

์ค‘๋˜์–ด ์™”์œผ๋‚˜, ๋ณธ ์—ฐ๊ตฌ์—์„œ๋Š” ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ์—

๋”ฐ๋ผ ๊ด‘์ •ํšก์›”๋ฅ˜์œ„์–ด์˜ ์›”๋ฅ˜๋Ÿ‰ ๋ณ€ํ™”๋ฅผ ์ถ”์ •ํ•˜๋Š”๋ฐ ์ฃผ์•ˆ์ ์„

๋‘์—ˆ๋‹ค.

๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ํ˜•ํƒœ์™€ ๊ด‘์ •ํšก์›”๋ฅ˜์œ„์–ด์˜ ๋†’์ด, ๊ธธ์ด, ์‚ฌ๋ฉด๊ฒฝ

์‚ฌ, ์œ„์–ด ์ƒ๋ฅ˜๋ถ€์— ๋ณด ์„ค์น˜ ์œ ๋ฌด ๋“ฑ ๋‹ค์–‘ํ•œ ์กฐ๊ฑด์€ ๊ด‘์ •ํšก์›”๋ฅ˜

์œ„์–ด์˜ ์›”๋ฅ˜๋Ÿ‰๊ณผ ์œ ๋Ÿ‰๊ณ„์ˆ˜ ๋“ฑ์— ์˜ํ–ฅ์„ ๋ฏธ์น˜๊ฒŒ ๋œ๋‹ค. ๋”ฐ๋ผ์„œ

๊ธฐ์กด์˜ ์—ฐ๊ตฌ์„ฑ๊ณผ๋ฅผ ๋ฉด๋ฐ€ํžˆ ๋ถ„์„ํ•˜์—ฌ, ๋ณธ ์—ฐ๊ตฌ์˜ ์ฃผ๋œ ๊ณผ์ œ์ธ

๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ์— ๋”ฐ๋ฅธ ์›”๋ฅ˜๋Ÿ‰๊ณผ ์œ ๋Ÿ‰๊ณ„์ˆ˜ ๋“ฑ์— ๋น„

๊ต์  ํฐ ์˜ํ–ฅ์„ ๋ฏธ์น  ๊ฒƒ์œผ๋กœ ํŒ๋‹จ๋˜๋Š” ์ธ์ž๋“ค์„ ์„ ์ •ํ•˜์—ฌ ์‹

(5)์— ๋‚˜ํƒ€๋‚ด์—ˆ๋‹ค.

(5)

์—ฌ๊ธฐ์„œ, ์€ ์œ ๋Ÿ‰๊ณ„์ˆ˜, ๋Š” ์ƒ๋ฅ˜ ํ”„๋ฃจ๋“œ์ˆ˜, ์€ ํšก์›”๋ฅ˜์œ„

์–ด ๊ธธ์ด, ๋Š” ์ˆ˜๋กœ ํญ, ๋Š” ์ƒ๋ฅ˜์ˆ˜์‹ฌ, ๋Š” ํšก์›”๋ฅ˜์œ„์–ด ๋†’์ด,

๋Š” ํ•˜์ƒ๊ฒฝ์‚ฌ, ๋Š” ๋ณธ๋ฅ˜์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ์ด๋‹ค.

์‹ (5)์— ๋‚˜ํƒ€๋‚ธ ์ฃผ์š” ์ธ์ž๋“ค์— ๋Œ€ํ•œ ์ฐจ์›ํ•ด์„์„ ํ†ตํ•ด, ์‹ (6)

๊ณผ ๊ฐ™์€ ๋ฌด์ฐจ์› ๋งค๊ฐœ๋ณ€์ˆ˜์˜ ์กฐํ•ฉ์œผ๋กœ ์žฌ๊ตฌ์„ฑํ•˜์˜€๋‹ค.

(6)

์‹ (6)์˜ ๊ฐ ์ธ์ž๋“ค์„ ๋…๋ฆฝ๋ณ€์ˆ˜๋กœ ๊ฐ€์ •ํ•˜๋ฉด, ์‹ (7)๊ณผ ๊ฐ™์ด

๋‹ค์ค‘์„ ํ˜•ํšŒ๊ท€์‹์œผ๋กœ ๋‚˜ํƒ€๋‚ผ ์ˆ˜ ์žˆ๋‹ค.

(7)

์‹ (7)์— ๋‚˜ํƒ€๋‚ธ ๋‹ค์ค‘์„ ํ˜•ํšŒ๊ท€์‹์„ ์ด์šฉํ•˜์—ฌ ๋งค๊ฐœ๋ณ€์ˆ˜์—

๋Œ€ํ•œ ์ตœ์ ํ™”๋กœ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹์„ ๊ฒฐ์ •ํ•˜์˜€๋‹ค. ๊ธฐ์กด์˜ ์„ฑ๊ณผ๋“ค์—

๋”ฐ๋ฅด๋ฉด, ์œ ๋Ÿ‰๊ณ„์ˆ˜ ์‚ฐ์ •์‹œ ๋ชจ๋“  ๋งค๊ฐœ๋ณ€์ˆ˜๊ฐ€ ํฌํ•จ๋œ ๊ฒƒ๋ณด๋‹ค ์ค‘

์š”๋„ ๋ฐ ๊ธฐ์—ฌ๋„๊ฐ€ ๋†’์€ 3~4๊ฐœ์˜ ๋ณ€์ˆ˜๋ฅผ ํ™œ์šฉํ•˜๋Š” ๊ฒƒ์ด ํšจ๊ณผ์ 

์ธ ๊ฒƒ์œผ๋กœ ์ œ์•ˆ๋˜์–ด ์žˆ๋‹ค. ๋ณธ ์—ฐ๊ตฌ์—์„œ๋„ ๊ฐ ๋งค๊ฐœ๋ณ€์ˆ˜์˜ ์ค‘์š”๋„

๋ฅผ ๋ถ„์„ํ•˜์—ฌ , , , ๋“ฑ 4๊ฐœ ๋ณ€์ˆ˜๋ฅผ ์„ ์ •ํ•˜์˜€๋‹ค.

์‹ (7)๋ฅผ ๊ธฐ๋ณธ๋ฐฉ์ •์‹์œผ๋กœ ํ•˜์—ฌ ๊ฐ ๋งค๊ฐœ๋ณ€์ˆ˜์˜ ์ค‘์š”๋„๋ฅผ ํ™•

์ธํ•˜๊ธฐ ์œ„ํ•˜์—ฌ ๊ฐ๊ฐ์˜ ๋งค๊ฐœ๋ณ€์ˆ˜๋“ค์„ ์กฐํ•ฉํ•˜์—ฌ ๋‹ค์ค‘ํšŒ๊ท€๋ถ„์„

์„ ์‹œํ–‰ํ•˜์˜€์œผ๋ฉฐ, ํ˜•์ƒ๋ณ„๋กœ ์ผ๋ถ€ ๊ฒฐ๊ณผ๋ฅผ Table 2์— ์ˆ˜๋กํ•˜์˜€

๋‹ค(์—ฌ๊ธฐ์„œ, ๋Š” ๋ณ€์ˆ˜์˜ ๊ฐœ์ˆ˜, ์€ ๊ฒฐ์ •๊ณ„์ˆ˜). ๋ถ„์„ํ•œ ๊ฒฐ๊ณผ,

>>> ์˜ ์ˆœ์„œ๋กœ ์ค‘์š”๋„๊ฐ€ ๋†’์€ ๊ฒƒ์œผ๋กœ ๋‚˜ํƒ€

๋‚ฌ๋‹ค.

๋”ฐ๋ผ์„œ ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ๋ฅผ ๊ณ ๋ คํ•œ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹์„

์ƒยท์‚ฌ๋ฅ˜๋ฅผ ํ†ตํ•ฉํ•˜์—ฌ ์ ์šฉํ•  ์ˆ˜ ์žˆ๋Š” ์‹ (8), (9)์™€ ์ƒ๋ฅ˜์— ์ ์šฉ

์„ฑ์ด ๋” ๋†’์€ ์‹ (10)์œผ๋กœ ๊ตฌ๋ถ„ํ•˜์—ฌ ์ œ์‹œํ•˜์˜€๋‹ค.

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H.-S. Kang and H.-J. Cho / Journal of Korea Water Resources Association 49(11) 941-949946

Table 2. Analysis of the importance of experimental parameters

No. of Variables CASE Residual

2

(

,

) 0.654 0.417

(

,

) 0.790 0.377

(

,

) 0.791 0.375

(,

) 0.689 0.421

(,

) 0.688 0.422

3

(

,

,

) 0.791 0.385

(

,

,

) 0.697 0.426

(,,

) 0.778 0.361

(

,

,

) 0.801 0.358

(,,

) 0.797 0.359

(,,

) 0.799 0.363

4

(

,,,

) 0.589 0.483

(,

,,

,

) 0.502 0.478

(

,

,,

) 0.655 0.466

(

,

,,

) 0.638 0.425

(

,

,,

) 0.802 0.358

(

,

,,

) 0.802 0.358

(

,

,,

) 0.804 0.355

(,

,

,

) 0.804 0.357

5

(

,

,

,,,) 0.585 0.659

(

,,

,,

) 0.804 0.353

(

,,

,

,

) 0.805 0.354

(

,

,,,

) 0.804 0.354

(

,

,,,

) 0.802 0.358

(

,

,,,

) 0.802 0.358

6 (,

,

,,

,

) 0.805 0.353

(8)

(9)

์—ฌ๊ธฐ์„œ, โˆผ, โˆผ,

โˆผ, โˆผ์ด๋‹ค.

(10)

์—ฌ๊ธฐ์„œ, โˆผ, โˆผ,

โˆผ์ด๋‹ค.

4. ๊ฒฐ๊ณผ๋ถ„์„ ๋ฐ ๋น„๊ต๊ฒ€ํ† 

์ œ์‹œ๋œ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹์˜ ์ ์šฉ์„ฑ์„ ํ™•์ธํ•˜๊ธฐ ์œ„ํ•˜์—ฌ ์‹ค์ธก๋œ

์ž๋ฃŒ์™€ ๊ณ„์‚ฐ๋œ ์ž๋ฃŒ๋ฅผ ๋น„๊ตํ•˜์˜€๋‹ค. Fig. 10์€ , ,

์˜ 3๊ฐœ์˜ ๋ณ€์ˆ˜๋กœ ์ œ์•ˆ๋œ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹ (8)์— ์˜ํ•ด ๊ณ„์‚ฐ๋œ

๊ณผ ์‹ค์ธก๋œ

์˜ ๋น„๊ต์ด๋ฉฐ, Fig. 11์€ ๊ณ„์‚ฐ๋œ ์™€ ์‹ค์ธก๋œ

๋ฅผ ๋น„๊ตํ•œ ๊ทธ๋ž˜ํ”„์ด๋‹ค. ์‹ค์ธก๋œ ์œ ๋Ÿ‰๊ณผ ๊ณ„์‚ฐ๋œ ์œ ๋Ÿ‰์ด 9.7%

์˜ ์ ˆ๋Œ€ํ‰๊ท ์˜ค์ฐจ๋ฅผ ๋ณด์ด๊ณ  ์žˆ์–ด ์‹ค์ธก๋œ ํšก์›”๋ฅ˜๋Ÿ‰๊ณผ ๋น„๊ต์ 

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H.-S. Kang and H.-J. Cho / Journal of Korea Water Resources Association 49(11) 941-949 947

Fig. 10. Comparison of calculated and computed

Fig. 11. Comparison of calculated and computed

Fig. 12. Comparison of calculated and computed

Fig. 13. Comparison of calculated and computed

Fig. 14. Comparison of calculated and computed

Fig. 15. Comparison of calculated and computed

์ž˜ ์ผ์น˜ํ•˜๋Š” ๊ฒƒ์œผ๋กœ ๋‚˜ํƒ€๋‚ฌ๋‹ค.

Fig. 12๋Š” , , , ์˜ 4๊ฐœ ๋ณ€์ˆ˜๋กœ ์ œ์•ˆ๋œ ์œ ๋Ÿ‰

๊ณ„์ˆ˜์‹ (9)์— ์˜ํ•ด ๊ณ„์‚ฐ๋œ ๊ณผ ์ธก์ •๋œ

์„ ๋น„๊ตํ•œ ๊ฒƒ์ด๋ฉฐ,

Fig. 13์€ ์„ ์ด์šฉํ•˜์—ฌ ๊ณ„์‚ฐ๋œ ์›”๋ฅ˜๋Ÿ‰๊ณผ ์ธก์ •๋œ ์›”๋ฅ˜๋Ÿ‰์„

๋น„๊ตํ•œ ๊ฒฐ๊ณผ์ด๋‹ค. ์‹ค์ธก๋œ ์›”๋ฅ˜๋Ÿ‰๊ณผ ๊ณ„์‚ฐ๋œ ์›”๋ฅ˜๋Ÿ‰์ด 7.46%

์ ˆ๋Œ€ํ‰๊ท ์˜ค์ฐจ๋ฅผ ๋ณด์ด๊ณ  ์žˆ์–ด ๊ณ„์‚ฐ๋œ ๊ฐ’์˜ ์ ์šฉ์„ฑ์ด ๋†’์€

๊ฒƒ์œผ๋กœ ํŒ๋‹จ๋œ๋‹ค.

๊ทธ๋ฆฌ๊ณ , ์ƒ๋ฅ˜์กฐ๊ฑด์—์„œ ์ œ์•ˆ๋œ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹ (10)์˜ ์ ์šฉ์„ฑ

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H.-S. Kang and H.-J. Cho / Journal of Korea Water Resources Association 49(11) 941-949948

Fig. 16. Verification of present relations using the experimental

data of Yoon, Yeong & Cho(2011)

(Subcritical)

Fig. 17. Verification of present relations using the experimental data

of Yoon, Yeong & Cho(2011)

(Subcritical)

Fig. 18. Verification of present relations using the experimental

data of Yoon, Yeong & Cho(2011)

(All)

Fig. 19. Verification of present relations using the experimental data

of Yoon, Yeong & Cho(2011)

(All)

์„ ํ™•์ธํ•˜๊ธฐ ์œ„ํ•˜์—ฌ ์‹ค์ธก๋œ ์ž๋ฃŒ์™€ ๊ณ„์‚ฐ๋œ ์ž๋ฃŒ๋ฅผ ๋น„๊ตํ•˜์˜€

๋‹ค. Fig. 14๋Š” ๊ณ„์‚ฐ๋œ ๊ณผ ์ธก์ •๋œ

์„ ๋น„๊ตํ•œ ๊ฒฐ๊ณผ์ด๋ฉฐ,

Fig. 17์€ ๊ณ„์‚ฐ๋œ ์›”๋ฅ˜๋Ÿ‰๊ณผ ์ธก์ •๋œ ์›”๋ฅ˜๋Ÿ‰์„ ๋น„๊ตํ•œ ๊ฒฐ๊ณผ์ด

๋‹ค. ์‹ค์ธก๋œ ํšก์›”๋ฅ˜๋Ÿ‰๊ณผ ๊ณ„์‚ฐ๋œ ํšก์›”๋ฅ˜๋Ÿ‰์ด 8.56%์˜ ์ ˆ๋Œ€ํ‰

๊ท ์˜ค์ฐจ๋ฅผ ๋ณด์ด๊ณ  ์žˆ์–ด ๋ณธ ์—ฐ๊ตฌ์—์„œ ์ œ์•ˆํ•œ ๊ฐ’์˜ ์ ์šฉ์„ฑ์ด

๋น„๊ต์  ๋†’์€ ๊ฒƒ์œผ๋กœ ํŒ๋‹จ๋œ๋‹ค. Fig. 16์—์„œ ๊ณ„์‚ฐ์น˜ ๊ณผ ์ธก์ •

์น˜ ์˜ ์ƒ๊ด€์„ฑ์ด ์ž‘์€ ๊ฒƒ์œผ๋กœ ๋‚˜ํƒ€๋‚˜์ง€๋งŒ, ํšก์›”๋ฅ˜๋Ÿ‰ ๋Š”

๊ณ„์‚ฐ์น˜์™€ ์ธก์ •์น˜๊ฐ€ ์–‘ํ˜ธํ•œ ์ƒ๊ด€์„ฑ์„ ๋‚˜ํƒ€๋‚ด๋Š” ์ด์œ ๋Š” ํšก์›”๋ฅ˜

๋Ÿ‰์„ ์ง€๋ฐฐํ•˜๋Š” ๋งค๊ฐœ๋ณ€์ˆ˜๋“ค์— ๊ธฐ์ธํ•œ๋‹ค. ๋ณธ ์—ฐ๊ตฌ์—์„œ๋Š” ์‹ (3)

๊ณผ ์‹ (4)์—์„œ ์œ„์–ด์˜ ํšก์›”๋ฅ˜๋Ÿ‰ ๋ฅผ ์‹ค์ธกํ•˜์—ฌ ์œ ๋Ÿ‰๊ณ„์ˆ˜

์„ ์‚ฐ์ •ํ•˜๊ฒŒ ๋œ๋‹ค. ์‹ (3)๊ณผ ์‹ (4)์˜ ์— ๋Œ€ํ•œ ์ฃผ์š” ๋ณ€์ˆ˜๋Š”

์œ ๋Ÿ‰๊ณ„์ˆ˜

, ํšก์›”๋ฅ˜์œ„์–ด ๊ธธ์ด(), ์œ„์–ด ์›”๋ฅ˜์ˆ˜์‹ฌ()์ด

๋‹ค. ๊ทธ๊ฒฐ๊ณผ Fig. 16์— ๋‚˜ํƒ€๋‚ธ ๊ณ„์‚ฐ์น˜ ์€ ์‹ (10)์„ ์‚ฌ์šฉํ•œ

๊ฐ’์ด๋ฉฐ, ์‹ (10)์€ ํšก์›”๋ฅ˜์œ„์–ด ๊ธธ์ด ์„ ํฌํ•จํ•˜์ง€ ์•Š์œผ๋ฏ€๋กœ,

์ธก์ •์น˜ ์— ๋Œ€ํ•ด ์ƒ๊ด€์„ฑ์ด ๋‚ฎ์€ ๊ฒƒ์œผ๋กœ ๋‚˜ํƒ€๋‚ฌ๋‹ค. ๊ทธ๋Ÿฐ๋ฐ

๊ณ„์‚ฐ์น˜ ํšก์›”๋ฅ˜๋Ÿ‰์—๋Š” ํšก์›”๋ฅ˜์œ„์–ด ๊ธธ์ด๊ฐ€ ํฌํ•จ๋˜๋ฏ€๋กœ Fig.

15์™€ ๊ฐ™์ด ๊ณ„์‚ฐ์น˜์™€ ์ธก์ •์น˜์˜ ์ƒ๊ด€๊ด€๊ณ„๊ฐ€ ๋†’์€ ๊ฒƒ์œผ๋กœ ๋‚˜ํƒ€

๋‚ฌ๋‹ค.

๋ณธ ์—ฐ๊ตฌ์—์„œ ์ง„ํ–‰๋œ ์‹คํ—˜์„ ํ†ตํ•ด ์ธก์ •๋œ ๋งค๊ฐœ๋ณ€์ˆ˜ ๋ฐ ํšก์›”

๋ฅ˜๋Ÿ‰์„ ๊ธฐ์กด์˜ ์—ฐ๊ตฌ์ž๋“ค์ด ์ œ์‹œํ•œ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹์„ ์ด์šฉํ•˜์—ฌ ๊ณ„

์‚ฐ๋œ ํšก์›”๋ฅ˜๋Ÿ‰๊ณผ ๋น„๊ต๋ฅผ ํ†ตํ•ด, ๋ณธ ์—ฐ๊ตฌ์„ฑ๊ณผ์˜ ์ ์šฉ์„ฑ์„ ๊ฒ€ํ† 

ํ•˜์˜€๋‹ค. ๊ธฐ์กด์˜ ์—ฐ๊ตฌ์„ฑ๊ณผ ์ค‘ ์ตœ๊ทผ์— ์‚ฌ๋‹ค๋ฆฌ๊ผด ๊ด‘์ •ํšก์›”๋ฅ˜์œ„

์–ด์˜ ์œ ๋Ÿ‰๊ณ„์ˆ˜๋ฅผ ์‚ฐ์ •ํ•œ Yoon and Cho (2011)์™€ Park and

Lee (2010)์˜ ์‹คํ—˜์กฐ๊ฑด๊ณผ ๊ฒฐ๊ณผ๊ฐ€ ์œ ์‚ฌํ•˜๋ฏ€๋กœ ์ด์— ๋Œ€ํ•ด ๋น„๊ต

๋ถ„์„ํ•˜์˜€๋‹ค.

Yoon and Cho (2011)์—์„œ ์ œ์‹œ๋œ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹ ์ค‘ ์ƒ๋ฅ˜์กฐ๊ฑด

์—์„œ ๊ณ„์‚ฐ๋œ ํšก์›”๋ฅ˜๋Ÿ‰๊ณผ ์ธก์ •๋œ ํšก์›”๋ฅ˜๋Ÿ‰์„ ๋น„๊ตํ•œ ๊ฒฐ๊ณผ ์ ˆ๋Œ€

ํ‰๊ท ์˜ค์ฐจ๊ฐ€ 23.9%์˜€๊ณ , ๊ทธ ๊ฒฐ๊ณผ๋ฅผ Fig. 16~17์— ๋‚˜ํƒ€๋‚ด์—ˆ๋‹ค.

Fig. 18 ๋ฐ Fig. 19๋Š” ์ „์ฒด์กฐ๊ฑด์— ๋Œ€ํ•œ ๋น„๊ต ๊ฒฐ๊ณผ์ด๋ฉฐ, ์ ˆ๋Œ€ํ‰

๊ท ์˜ค์ฐจ๋Š” 29.73%๋กœ ๋‚˜ํƒ€๋‚ฌ๋‹ค. ์ ˆ๋Œ€ํ‰๊ท ์˜ค์ฐจ๊ฐ€ ๋ณธ ์—ฐ๊ตฌ์—์„œ

์ œ์‹œ๋œ ์‹๋ณด๋‹ค ๋†’๊ฒŒ ๋‚˜ํƒ€๋‚˜, ์ œ์•ˆ๋œ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹์ด ๋” ์ •ํ™•ํ•œ

ํšก์›”๋ฅ˜๋Ÿ‰์„ ์‚ฐ์ •ํ•  ์ˆ˜ ์žˆ์Œ์„ ์˜๋ฏธํ•œ๋‹ค.

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H.-S. Kang and H.-J. Cho / Journal of Korea Water Resources Association 49(11) 941-949 949

๊ฐ์‚ฌ์˜ ๊ธ€

์ด ๋…ผ๋ฌธ์€ 2014๋…„ ์šธ์‚ฐ๋Œ€ํ•™๊ต ์—ฐ๊ตฌ๋น„์— ์˜ํ•˜์—ฌ ์—ฐ๊ตฌ๋˜์—ˆ์Œ.

5. ๊ฒฐ ๋ก 

๋ณธ ์—ฐ๊ตฌ์—์„œ๋Š” ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ๋ฅผ ๋ณ€ํ™”์‹œ์ผœ ๊ด‘์ •

ํšก์›”๋ฅ˜์œ„์–ด ์„ค์น˜ ์‹œ ๋ณธ๋ฅ˜์˜ ํ๋ฆ„์กฐ๊ฑด์˜ ๋ณ€ํ™”์— ๋”ฐ๋ฅธ ์œ ๋Ÿ‰๊ณ„์ˆ˜

์‹์„ ์‚ฐ์ •ํ•˜๊ธฐ ์œ„ํ•œ ์ˆ˜๋ฆฌ์‹คํ—˜์„ ์‹ค์‹œํ•˜์˜€๋‹ค. ์ธก์ •๋œ ์‹คํ—˜์„ฑ

๊ณผ๋ฅผ ์„ ํ–‰์—ฐ๊ตฌ์ธ ๊ธฐ์กด์˜ ์—ฐ๊ตฌ ์„ฑ๊ณผ์™€ ๋น„๊ต๋ถ„์„ํ•˜์˜€์œผ๋ฉฐ, ๋ณธ

๋ฅ˜์ˆ˜๋กœ ํ˜•์ƒ์— ๋”ฐ๋ฅธ ํ๋ฆ„ํŠน์„ฑ์˜ ๋ณ€ํ™”์— ๋Œ€ํ•œ ์ค‘์š”์„ฑ์„ ํ™•์ธํ• 

์ˆ˜ ์žˆ์—ˆ๋‹ค. ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ๋ฅผ ๊ณ ๋ คํ•˜์—ฌ ์œ ๋Ÿ‰๊ณ„์ˆ˜

์‹์„ ์‚ฐ์ •ํ•˜์˜€์œผ๋ฉฐ, ์—ฐ๊ตฌ๊ฒฐ๊ณผ๋ฅผ ์š”์•ฝํ•˜๋ฉด ๋‹ค์Œ๊ณผ ๊ฐ™๋‹ค.

1) De Marchi ์ด๋ก ์—์„œ์˜ ์ผ์ •๋น„์—๋„ˆ์ง€ ๊ฐ€์ •์€ ์‚ฌ๋‹ค๋ฆฌ๊ผด ์ˆ˜

๋กœ์˜ ์‚ฌ๋‹ค๋ฆฌ๊ผด ๊ด‘์ •์œ„์–ด์—์„œ๋„ ํƒ€๋‹นํ•œ ๊ฒƒ์œผ๋กœ ๋ถ„์„๋˜์—ˆ

๊ณ , ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ๊ฐ€ ์™„๋งŒํ•ด ์งˆ์ˆ˜๋ก ๋น„์—๋„ˆ์ง€

์ฐจ๊ฐ€ ๊ฐ์†Œํ•˜๋Š” ๊ฒฝํ–ฅ์„ ๋ณด์—ฌ ์•ˆ์ •์ ์ธ ํ๋ฆ„์„ ์œ ์ง€ํ•  ์ˆ˜ ์žˆ

๋‹ค๋Š” ๊ฒƒ์„ ํ™•์ธํ•˜์˜€๋‹ค.

2) ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ๊ฐ€ ๊ธ‰ํ• ์ˆ˜๋ก ํšก์›”๋ฅ˜์œ„์–ด ์„ค์น˜

์ „ยทํ›„์— ๋Œ€ํ•œ ๋น„์—๋„ˆ์ง€๋น„๋Š” ์ปค์ง€๋Š” ๊ฒƒ์œผ๋กœ ๋‚˜ํƒ€๋‚ฌ๊ณ , ์ˆ˜

๋กœ ๊ฒฝ์‚ฌ๊ฐ€ 0.5% ์ด์ƒ์ผ ๋•Œ๋Š” ์ „์ฒด์˜ ํ๋ฆ„์ด ์ƒ๋ฅ˜์—์„œ ์‚ฌ๋ฅ˜

๋กœ ๋ฐ”๋€Œ๋ฉด์„œ ๋น„์—๋„ˆ์ง€๋น„๊ฐ€ 1๋ณด๋‹ค ์ปค์ง€๋Š” ์ง€์—ญ์ด ๋‚˜ํƒ€๋‚ฌ๋‹ค.

3) ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ์— ๋Œ€ํ•œ ๋ณ€์ˆ˜ ๋ฅผ ๋„์ž…ํ•˜์—ฌ

์ƒˆ๋กœ์šด ๊ด‘์ •ํšก์›”๋ฅ˜์œ„์–ด์˜ ์œ ๋Ÿ‰๊ณ„์ˆ˜ ์‚ฐ์ •์‹์„ ์ œ์•ˆํ•˜์˜€

๋‹ค. ์ƒ๋ฅ˜์™€ ์‚ฌ๋ฅ˜๋ฅผ ๋ชจ๋‘ ํฌํ•จํ•˜๋Š” ์กฐ๊ฑด์—์„œ ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ

๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ๊ฐ€ ๋ณ€ํ™”๋  ๋•Œ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹์€ > >

> ์˜ ์ˆœ์„œ๋กœ ์ค‘์š”๋„๊ฐ€ ๋†’์Œ์„ ํ™•์ธํ•˜์˜€๊ณ , ๋‹ค์ค‘

ํšŒ๊ท€๋ถ„์„์„ ํ†ตํ•˜์—ฌ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹์„ ์ œ์•ˆํ•˜์˜€๋‹ค. ์ƒˆ๋กญ๊ฒŒ ์ œ

์•ˆ๋œ ์‹์„ ์ด์šฉํ•˜์—ฌ ์‚ฐ์ •๋œ ๊ณผ ํšก์›”๋ฅ˜๋Ÿ‰ ์„ ์‹ค์ธก์น˜

๋“ฑ๊ณผ ๋น„๊ตํ•˜์—ฌ ์ ์šฉ์„ฑ์„ ํ™•์ธํ•˜์˜€๋‹ค.

4) ์ƒ๋ฅ˜ํ๋ฆ„์—์„œ ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ๊ฐ€ ๋ณ€ํ™”๋  ๋•Œ, ๊ด‘

์ •ํšก์›”๋ฅ˜์œ„์–ด์˜ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹์€ , , ๋“ฑ ์ฃผ์š” 3

๋ณ€์ˆ˜๋งŒ์œผ๋กœ ์ œ์‹œํ•˜์˜€๋‹ค. ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹์—์„œ ๊ฐ ์ธ์ž์˜ ์ค‘์š”

๋„๋Š” > > ์ˆœ์œผ๋กœ ๋‚˜ํƒ€๋‚ฌ์œผ๋ฉฐ, ์ˆ˜๊ฐ€ ์ž‘์„

์ˆ˜๋ก ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹ ๋‚ด์—์„œ ์˜ ์ƒ๊ด€์„ฑ์ด ๋†’์€ ๊ฒƒ์œผ๋กœ ํ™•

์ธ๋˜์—ˆ๋‹ค.

5) ๊ฐœ์ˆ˜๋กœ ํ๋ฆ„์—์„œ ๊ฐ€์žฅ ์ค‘์š”ํ•œ ์ธ์ž๋Š” ์ด์ง€๋งŒ, ์œ ๋Ÿ‰๊ณ„

์ˆ˜์‹์— ๋ฅผ ํฌํ•จํ•˜์ง€ ์•Š๋Š” ์ˆ˜์‹์„ ๋ณ‘ํ–‰ํ•ด์„œ ์ œ์•ˆํ•˜์˜€

๋‹ค. ์ด๋ฅผ ์ด์šฉํ•ด์„œ ์‚ฐ์ •ํ•œ ์œ ๋Ÿ‰๊ณ„์ˆ˜์‹ ๊ณผ ์œŒ๋ฅ˜๋Ÿ‰์„ ์‹ค

์ธก์น˜์™€ ๋น„๊ตํ•œ ๊ฒฐ๊ณผ ๊ทธ ์ ์šฉ์„ฑ์ด ๋†’์€ ๊ฒƒ์œผ๋กœ ๋‚˜ํƒ€๋‚ฌ๋‹ค.

6) ์ƒ๋ฅ˜์กฐ๊ฑด์—์„œ ๋ณธ๋ฅ˜์ˆ˜๋กœ์˜ ์ œ๋ฐฉ์‚ฌ๋ฉด๊ฒฝ์‚ฌ๊ฐ€ ๋ณ€ํ™”๋  ๋•Œ ์œ 

๋Ÿ‰๊ณ„์ˆ˜์‹์€ > > ์˜ ์ˆœ์„œ๋กœ ์ค‘์š”๋„๊ฐ€ ๋†’๊ฒŒ

๋‚˜ํƒ€๋‚ฌ์œผ๋ฉฐ, ์ƒ๋ฅ˜ํ๋ฆ„์—์„œ ์˜ ์ƒ๊ด€์„ฑ์ด ๋†’์€ ๊ฒƒ์œผ๋กœ

ํ™•์ธ๋˜์—ˆ๋‹ค.

References

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Journal of Hydraulic Engineering, ASCE, Vol. 125, No.

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from traperzoidal channel.โ€ Journal of Hydraulic Engineering,

ASCE, Vol. 117, No. 4, pp. 461-475.

De March, G. (1934). โ€œEssay on the performance of lateral weirs.โ€

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formula for broad crested side weir.โ€ Journal of Korea Water

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