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Deep Learning in Geotechnical Engineering: A Critical Assessment of PINNs and Operator Learning

Deep Learning in Geotechnical Engineering: A Critical Assessment of PINNs and Operator Learning

์ด ๋…ผ๋ฌธ์€ ์ตœ๊ทผ ์ง€๋ฐ˜๊ณตํ•™ ๋ถ„์•ผ์— ๋„์ž…๋œ ์„ธ ๊ฐ€์ง€ ๋”ฅ๋Ÿฌ๋‹ ํ”„๋ ˆ์ž„์›Œํฌโ€”๋ฌผ๋ฆฌ ๊ธฐ๋ฐ˜ ์‹ ๊ฒฝ๋ง(PINN), ๋”ฅ ์—ฐ์‚ฐ์ž ๋„คํŠธ์›Œํฌ(DeepONet), ๊ทธ๋ž˜ํ”„ ๋„คํŠธ์›Œํฌ ์‹œ๋ฎฌ๋ ˆ์ดํ„ฐ(GNS)โ€”๋ฅผ ์ „ํ†ต์ ์ธ ์ˆ˜์น˜ ํ•ด๋ฒ•๊ณผ ์ง์ ‘ ๋น„๊ตํ•จ์œผ๋กœ์จ ์‹ค์šฉ์„ฑ์„ ํ‰๊ฐ€ํ•œ๋‹ค. ์ฒซ ๋ฒˆ์งธ ์‹คํ—˜์ธ ํŒŒ๋™ ์ „ํŒŒ ๋ฌธ์ œ๋Š” ๊ณ ์ฃผํŒŒ ๋™์  ์‘๋‹ต์„ ์ •ํ™•ํžˆ ํฌ์ฐฉํ•ด์•ผ ํ•˜๋Š” ์ „ํ˜•์ ์ธ ํ…Œ์ŠคํŠธ๋ฒ ๋“œ์ด๋‹ค. ์—ฌ๊ธฐ์„œ PINN์€ ๋ฌผ๋ฆฌ ๋ฐฉ์ •์‹์„ ์†์‹ค ํ•จ์ˆ˜์— ์ง์ ‘ ์‚ฝ์ž…ํ•˜๋Š” ๋ฐฉ์‹์ž„์—๋„ ๋ถˆ๊ตฌํ•˜๊ณ , ๋ฏธ๋ถ„ ์—ฐ์‚ฐ๊ณผ ์ตœ์ ํ™” ๊ณผ์ •์—์„œ ๋ฐœ์ƒํ•˜๋Š” ์ˆ˜์น˜์  ๋ถˆ์•ˆ์ •์„ฑ์œผ๋กœ ์ธํ•ด ์œ ํ•œ์ฐจ๋ถ„(FD) ๋Œ€๋น„ 90 000๋ฐฐ ๋А๋ ค์กŒ๋‹ค. ์˜ค์ฐจ ์ธก๋ฉด์—์„œ

Learning Physics
On the Testing of Seismicity Models

On the Testing of Seismicity Models

: ์ง€์ง„ ์œ„ํ—˜ ํ‰๊ฐ€๋Š” ์žฅ๊ธฐ๊ฐ„ ํ”ผํ•ด ๋ฐœ์ƒ ๊ฐ€๋Šฅ์„ฑ์„ ๋‚˜ํƒ€๋‚ด๋Š” ์ง€๋„ ์ œ์ž‘์— ๊ธฐ๋ฐ˜ํ•œ๋‹ค. ์ด๋Ÿฌํ•œ ์ง€๋„ ์ƒ์„ฑ์€ ์—ญ์‚ฌ์ ์ธ ์ง€์ง„ ๋ฐ์ดํ„ฐ, ์ €๊ฐ•๋„ ์ง€์ง„ ํ™œ๋™, ๊ตฌํ…๋ฒ ๋ฅดํฌ ๋ฆฌ์ฒ˜ ๋ฒ•์น™ ๋“ฑ ๋‹ค์–‘ํ•œ ์ ‘๊ทผ ๋ฐฉ์‹์„ ํฌํ•จํ•˜๋ฉฐ, ์ด๋“ค ๋ฐฉ๋ฒ•์˜ ์ฐจ์ด๋กœ ์ธํ•ด ๊ฐ๊ด€์ ์ธ ์ง€์ง„ ๋ชจ๋ธ ํ…Œ์ŠคํŠธ ๋ฐ ์ˆœ์œ„๋ฅผ ๋งค๊ธฐ๋Š” ํ†ต๊ณ„์  ๋ฐฉ๋ฒ•๋ก  ๊ฐœ๋ฐœ์ด ์ค‘์š”ํ•ด์กŒ๋‹ค. ๋ฏธ๊ตญ ์ง€์งˆ์กฐ์‚ฌ๊ตญ(USGS)์˜ ํ˜‘๋™ ์—ฐ๊ตฌ ๊ธฐ๊ด€์ธ CSEP(Collaboratory for the Study of Earthquake Predictability)๋Š” ์ด๋Ÿฌํ•œ ํ•„์š”์„ฑ์„ ์ถฉ์กฑํ•˜๊ธฐ ์œ„ํ•ด ์บ˜๋ฆฌํฌ๋‹ˆ์•„ ์ง€์—ญ์„ ๋Œ€์ƒ์œผ๋กœ ํ•œ RELM(Re

Model Physics
Peak Nothing: Recent Trends in Mineral Resource Production

Peak Nothing: Recent Trends in Mineral Resource Production

: 1. ์—ฐ๊ตฌ ๋ฐฐ๊ฒฝ ๋ฐ ๋ชฉ์  ๋…ผ๋ฌธ์€ ๊ด‘๋ฌผ ์ž์›์˜ ์ƒ์‚ฐ ๋™ํ–ฅ์„ ๋ถ„์„ํ•˜๊ณ , ์ด๋ฅผ ํ†ตํ•ด ๋ฏธ๋ž˜์˜ ์ž์› ๊ณ ๊ฐˆ ๊ฐ€๋Šฅ์„ฑ์— ๋Œ€ํ•œ ์ดํ•ด๋ฅผ ์ œ๊ณตํ•˜๋ ค๊ณ  ํ•œ๋‹ค. ํŠนํžˆ, ๊ณผ๊ฑฐ์— ๋งŽ์€ ์›๋ฃŒ๊ฐ€ ๋ฌผ๋ฅ˜์  ํŠน์„ฑ์„ ๋ณด์˜€์ง€๋งŒ, ์ตœ๊ทผ์—๋Š” ์ง€์ˆ˜ ์„ฑ์žฅ ๋˜๋Š” ์ดˆ์ง€์ˆ˜ ์„ฑ์žฅ์„ ๋‚˜ํƒ€๋‚ด๋Š” ํ˜„์ƒ์„ ๊ด€์ฐฐํ•œ๋‹ค. 2. ๋ถ„์„ ๋ฐฉ๋ฒ• ๋…ผ๋ฌธ์€ ๋ฏธ๊ตญ ์ง€์งˆ์กฐ์‚ฌ๊ตญ(USGS)์˜ ๋ฐ์ดํ„ฐ๋ฅผ ๊ธฐ๋ฐ˜์œผ๋กœ, ๋‹ค์–‘ํ•œ ๋น„์žฌ์ƒ ์ž์›์˜ ์—ฐ๋„๋ณ„ ์ƒ์‚ฐ๋Ÿ‰์„ ๋ถ„์„ํ•œ๋‹ค. ์ด๋ฅผ ํ†ตํ•ด ๋ˆ„์  ์ƒ์‚ฐ๋Ÿ‰๊ณผ ๋ถ„๋‹น ์„ฑ์žฅ๋ฅ  ๊ฐ„์˜ ๊ด€๊ณ„๋ฅผ ๊ทธ๋ž˜ํ”„๋กœ ๋‚˜ํƒ€๋‚ด๊ณ , ์ด๋“ค ๊ทธ๋ž˜ํ”„์—์„œ ์ถ”์„ธ ๋ณ€ํ™”๋ฅผ ํ™•์ธํ•œ๋‹ค. 3. ์ฃผ์š” ๊ฒฐ๊ณผ ์ดˆ๊ธฐ ๋ฌผ๋ฅ˜ ๋ชจ๋ธ : ๊ณผ๊ฑฐ์—๋Š” ๋งŽ์€

Physics
A short note on the two most recent large EQs of New Zealand (Mw=7.0 on   September 3rd, 2010 and Mw=6.1 on February 21st, 2011). A typical example of   tidally triggered large EQs by the M1 tidal component

A short note on the two most recent large EQs of New Zealand (Mw=7.0 on September 3rd, 2010 and Mw=6.1 on February 21st, 2011). A typical example of tidally triggered large EQs by the M1 tidal component

๋ณธ ๋…ผ๋ฌธ์€ ์กฐ์„ ํŒŒ๋™์ด ํฐ ์ง€์ง„ ๋ฐœ์ƒ์— ๋ฏธ์น˜๋Š” ์˜ํ–ฅ์„ ๋ถ„์„ํ•˜๋ฉฐ, ํŠนํžˆ M1 ์„ฑ๋ถ„์˜ ์—ญํ• ์„ ๊ฐ•์กฐํ•˜๊ณ  ์žˆ๋‹ค. ์ด ์—ฐ๊ตฌ๋Š” 2010๋…„๊ณผ 2011๋…„ ๋‰ด์งˆ๋žœ๋“œ์—์„œ ๋ฐœ์ƒํ•œ ๋‘ ์ฐจ๋ก€์˜ ๋Œ€๊ทœ๋ชจ ์ง€์ง„(Mw 7.0 ๋ฐ Mw 6.1)์„ ํ†ตํ•ด ์กฐ์„ ํŒŒ๋™์ด ์ง€์ง„ ๋ฐœ์ƒ์— ์ค‘์š”ํ•œ ์—ญํ• ์„ ํ•˜๋Š”์ง€ ๊ฒ€์ฆํ•˜๊ณ ์ž ํ•œ๋‹ค. ์„œ๋ก  ์„œ๋ก ์—์„œ๋Š” ๋Œ€๋ถ€๋ถ„์˜ ์ง€์ง„ํ•™๊ณ„๊ฐ€ ํฐ ์ง€์ง„์€ ์‹œ๊ฐ„์ ์œผ๋กœ ์˜ˆ์ธก ๋ถˆ๊ฐ€๋Šฅํ•˜๋‹ค๊ณ  ๋ณด๋Š” ๊ด€์ ์„ ์†Œ๊ฐœํ•œ๋‹ค. ๊ทธ๋Ÿฌ๋‚˜ ํ†ต๊ณ„์ ์œผ๋กœ ์ž˜ ์•Œ๋ ค์ง„ ๋ฌผ๋ฆฌ์  ๋ฉ”์ปค๋‹ˆ์ฆ˜, ์ฆ‰ ํƒœ์–‘ ๋‹ฌ ๋ฐ ์ง€๊ตฌ ์ค‘๋ ฅ ์ƒํ˜ธ์ž‘์šฉ์œผ๋กœ ์ƒ์„ฑ๋˜๋Š” ์กฐ์„ ํŒŒ๋™์ด ํŠน์ • ์‹œ์ ์— ์ง€์ง„ ๋ฐœ์ƒ์„ ์œ ๋ฐœํ•  ์ˆ˜ ์žˆ๋‹ค๋Š” ์ ์„

Physics
5,000,000 Delays -- Some Statistics

5,000,000 Delays -- Some Statistics

: ๋ณธ ๋…ผ๋ฌธ์€ VLBI ์ง€์—ฐ ์‹œ๊ฐ„ ๋ฐ์ดํ„ฐ๋ฅผ ํ†ตํ•ด ์ฒœ๋ฌธํ•™์˜ ์žฅ๊ธฐ์  ๋ฐœ์ „์„ ๋ถ„์„ํ•˜๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค. 5,000,000๊ฐœ ์ด์ƒ์˜ VLBI ์ง€์—ฐ ์‹œ๊ฐ„์ด ์ˆ˜์ง‘๋œ ๊ฒƒ์€ ์ฒœ๋ฌธํ•™ ๋ถ„์•ผ์—์„œ ์ค‘์š”ํ•œ ์ด์ •ํ‘œ๋กœ, ์ด๋ฅผ ํ†ตํ•ด ๋‹ค์–‘ํ•œ ํ†ต๊ณ„์™€ ํŒจํ„ด์„ ํŒŒ์•…ํ•  ์ˆ˜ ์žˆ๊ฒŒ ๋˜์—ˆ์Šต๋‹ˆ๋‹ค. ๊ด€์ธก ์„ธ์…˜๊ณผ ์—ญ๋Ÿ‰ ๋ถ„์„ ๊ด€์ธก ์„ธ์…˜์€ 24์‹œ๊ฐ„ ์„ธ์…˜์ด ๊ฐ€์žฅ ๋งŽ์ด ์ด๋ฃจ์–ด์กŒ์œผ๋ฉฐ, ์ด๋Š” ์—ฐ๊ตฌ์˜ ์ค‘์š”์„ฑ์„ ๋ฐ˜์˜ํ•ฉ๋‹ˆ๋‹ค. ํŠนํžˆ, 18์‹œ๊ฐ„ ์ด์ƒ ์ง€์†๋œ ์„ธ์…˜ ์ˆ˜๊ฐ€ ์ „์ฒด ์„ธ์…˜ ์ค‘ ์ƒ๋‹น ๋ถ€๋ถ„์„ ์ฐจ์ง€ํ•˜๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค. ์ด๋Ÿฌํ•œ ์žฅ๊ธฐ ๊ด€์ธก์€ ๋ฐ์ดํ„ฐ์˜ ์ •ํ™•์„ฑ๊ณผ ์‹ ๋ขฐ์„ฑ์„ ๋†’์ด๋Š” ๋ฐ ์ค‘์š”ํ•œ ์—ญํ• ์„ ํ•ฉ๋‹ˆ๋‹ค. ์—ญ๋Ÿ‰ ๋ถ„์„์—์„œ

Physics
Primary Initiation of Submarine Canyons

Primary Initiation of Submarine Canyons

1. ์ด๋ก ์  ๋ฐฐ๊ฒฝ๊ณผ ๊ฐ€์„ค ์ €์ž์ธ J. Marvin Herndon๋Š” ๋ณธ ๋…ผ๋ฌธ์—์„œ ์ง€๊ตฌ์˜ ์ดˆ๊ธฐ ๊ธฐ์›์„ ๋ชฉ์„ฑ๊ณผ ์œ ์‚ฌํ•œ ๊ฐ€์Šคํ–‰์„ฑ์œผ๋กœ ์ œ์•ˆํ•œ๋‹ค. ์ด๋Ÿฌํ•œ ๊ฐ€์„ค์€ ํƒœ์–‘๊ณ„ ๋‚ด์™ธ์—์„œ ๊ด€์ฐฐ๋˜๋Š” ๋‹ค์–‘ํ•œ ํ–‰์„ฑ ๊ตฌ์กฐ์™€ ์ผ์น˜ํ•˜๋ฉฐ, ํŠนํžˆ ์™ธ๊ณ„ ํ–‰์„ฑ ์ค‘ ์ผ๋ถ€๊ฐ€ ๋ณ„๊ณผ ๊ฐ™์€ ํฌ๊ธฐ์˜ ๊ฐ€์Šคํ–‰์„ฑ์„ ํฌํ•จํ•˜๊ณ  ์žˆ๋‹ค๋Š” ์ ์„ ๊ทผ๊ฑฐ๋กœ ํ•œ๋‹ค. Herndon์€ ์ด ์ดˆ๊ธฐ ์ƒํƒœ์—์„œ ์ง€๊ตฌ๋Š” ์•ฝ 300๊ฐœ์˜ ํ˜„์žฌ ์ง€๊ตฌ ์งˆ๋Ÿ‰์— ํ•ด๋‹นํ•˜๋Š” ์ˆ˜์†Œ์™€ ํ—ฌ๋ฅจ ๋“ฑ ํœ˜๋ฐœ์„ฑ ์›์†Œ๋ฅผ ํฌํ•จํ•œ ๊ฑฐ๋Œ€ํ•œ ๊ฐ€์Šค ํ–‰์„ฑ์ด์—ˆ๋‹ค๊ณ  ์ฃผ์žฅํ•œ๋‹ค. 2. ์ „์ง€๊ตฌ ํƒˆ๊ธฐ ์—ญํ•™ ์ „์ง€๊ตฌ ํƒˆ๊ธฐ ์—ญํ•™์€ ์ด ์ดˆ๊ธฐ ์ƒํƒœ์—์„œ ๋ฐœ์ƒํ•˜๋Š” ์ค‘์š”ํ•œ ์—ญํ•™์ 

Physics
Hydrogen Geysers: Explanation for Observed Evidence of Geologically   Recent Volatile-Related Activity on Mercurys Surface

Hydrogen Geysers: Explanation for Observed Evidence of Geologically Recent Volatile-Related Activity on Mercurys Surface

: ์ด ๋…ผ๋ฌธ์€ ์ˆ˜์„ฑ์˜ ์ง€ํ˜• ํ˜•์„ฑ์— ๋Œ€ํ•œ ์ƒˆ๋กœ์šด ์ด๋ก ์„ ์ œ์‹œํ•˜๊ณ  ์žˆ์œผ๋ฉฐ, ๊ทธ ์ค‘์‹ฌ์—๋Š” ํœ˜๋ฐœ์„ฑ ํ™œ๋™๊ณผ ์ฒ ์˜ ์—ญํ• ์ด ์žˆ์Šต๋‹ˆ๋‹ค. ์ €์ž๋Š” ๊ธฐ์กด ๋ชจ๋ธ๋“ค๊ณผ๋Š” ๋‹ค๋ฅธ ๊ด€์ ์„ ํ†ตํ•ด ์ˆ˜์„ฑ์˜ ํ•ต์— ์—„์ฒญ๋‚œ ์–‘์˜ ์ˆ˜์†Œ๊ฐ€ ํฌํ•จ๋˜์–ด ์žˆ๋‹ค๋Š” ๊ฐ€์„ค์„ ๋‚ด์„ธ์šฐ๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค. 1. ํœ˜๋ฐœ์„ฑ ํ™œ๋™์˜ ์ค‘์š”์„ฑ ์ˆ˜์„ฑ ํ‘œ๋ฉด์—์„œ ๋ฐœ๊ฒฌ๋œ '๋น„์ •์ƒ์ ์ธ ์ง€ํ˜•'์€ ํœ˜๋ฐœ์„ฑ ํ™œ๋™์œผ๋กœ ์ธํ•ด ํ˜•์„ฑ๋˜์—ˆ๋‹ค๋Š” ์ฃผ์žฅ์ด ์ œ๊ธฐ๋˜์—ˆ์Šต๋‹ˆ๋‹ค. ์ด๋Ÿฌํ•œ ์ง€ํ˜•์€ ์ˆ˜์„ฑ์˜ ๊ณ ์œ ํ•œ ํŠน์ง• ์ค‘ ํ•˜๋‚˜๋กœ, ๊ทธ ์›์ธ์„ ๊ทœ๋ช…ํ•˜๋Š” ๊ฒƒ์€ ํ–‰์„ฑ ๊ณผํ•™์— ์ค‘์š”ํ•œ ์˜๋ฏธ๋ฅผ ๊ฐ–์Šต๋‹ˆ๋‹ค. 2. ์ˆ˜์„ฑ ํ•ต ๋‚ด๋ถ€์˜ ํœ˜๋ฐœ์„ฑ ์š”์†Œ ์ €์ž๋Š” ์ดˆ๊ธฐ ํƒœ์–‘๊ณ„์—์„œ ๋ฐœ์ƒํ•œ

Physics
New Zealand pathway towards Asia-Pacific and global e-VLBI research and   development

New Zealand pathway towards Asia-Pacific and global e-VLBI research and development

๋ณธ ๋…ผ๋ฌธ์€ ๋‰ด์งˆ๋žœ๋“œ์˜ ์ฒœ๋ฌธํ•™ ๋ฐœ์ „ ๊ณผ์ •์—์„œ ์ค‘์š”ํ•œ ์ „ํ™˜์ ์ด ๋˜๋Š” ์˜คํด๋žœ๋“œ ๊ณต๊ณผ๋Œ€ํ•™(AUT)์˜ ์—ญํ• ์„ ์ง‘์ค‘์ ์œผ๋กœ ๋ถ„์„ํ•˜๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค. ํŠนํžˆ, 2005๋…„๋ถ€ํ„ฐ ์‹œ์ž‘๋œ AUT์˜ ๋…ธ๋ ฅ์€ ๋‰ด์งˆ๋žœ๋“œ๊ฐ€ ๊ตญ์ œ์ ์ธ VLBI ๋„คํŠธ์›Œํฌ์— ํ•ฉ๋ฅ˜ํ•˜๋Š” ๊ณ„๊ธฐ๊ฐ€ ๋˜์—ˆ์œผ๋ฉฐ, ์ด๋Š” ์•„์‹œ์•„ ํƒœํ‰์–‘ ์ง€์—ญ์—์„œ ์ฒœ๋ฌธํ•™ ์—ฐ๊ตฌ ๊ฐœ๋ฐœ์„ ์ฃผ๋„ํ•˜๋Š” ์ค‘์š”ํ•œ ๋‹จ๊ณ„๋กœ ํ‰๊ฐ€๋ฉ๋‹ˆ๋‹ค. 1. ์—ญ์‚ฌ์  ๋ฐฐ๊ฒฝ ๋ฐ ์ดˆ๊ธฐ ๋ฐœ์ „ ๋…ผ๋ฌธ์€ ๋‰ด์งˆ๋žœ๋“œ์˜ ์ฒœ๋ฌธํ•™ ์—ญ์‚ฌ๋ฅผ ๊ฐ„๋žตํ•˜๊ฒŒ ์†Œ๊ฐœํ•˜๋ฉฐ, ํŠนํžˆ 1948๋…„ ํ˜ธ์ฃผ CSIRO์—์„œ ์ง„ํ–‰๋œ ๋ฐ”๋‹ค๋ฅผ ๊ฑฐ์šธ๋กœ ์‚ฌ์šฉํ•œ ๊ฐ„์„ญ๊ณ„ ์„ค์น˜ ์‹คํ—˜์„ ์–ธ๊ธ‰ํ•ฉ๋‹ˆ๋‹ค. ์ด ์‹คํ—˜์€ ๋ผ๋””์˜คํŒŒ ์›์ฒœ์˜ ์œ„์น˜

Physics Astrophysics
No Image

Stone structures in the Syrian Desert

: ์ด ์—ฐ๊ตฌ๋Š” ์‹œ๋ฆฌ์•„ ์‚ฌ๋ง‰์—์„œ ๋ฐœ๊ฒฌ๋œ ๋‚ ๊ฐœ ๋‹ฌ๋ฆฐ ๊ทธ๋ฌผ(kite)๊ณผ ๊ด€๋ จ๋œ ์„์กฐ ๊ตฌ์กฐ๋ฌผ์„ ์ค‘์‹ฌ์œผ๋กœ ๊ณ ๋Œ€ ์ธ๊ฐ„์˜ ์ƒํ™œ ๋ฐฉ์‹์— ๋Œ€ํ•œ ํ†ต์ฐฐ๋ ฅ์„ ์ œ๊ณตํ•ฉ๋‹ˆ๋‹ค. ์ด๋“ค ๊ตฌ์กฐ๋ฌผ์€ ๋‹จ์ˆœํžˆ ๋™๋ฌผ์„ ํฌํšํ•˜๊ณ  ์‚ดํ•ดํ•˜๋Š” ๋ฐ๋งŒ ์‚ฌ์šฉ๋˜์ง€ ์•Š๊ณ , ์‹๋Ÿ‰ ๋ณด์กด ๋ฐ ์‚ฌ๋ƒฅ๊ฐ ์œ ์ง€์—๋„ ์ค‘์š”ํ•œ ์—ญํ• ์„ ํ–ˆ์Šต๋‹ˆ๋‹ค. ์ด๋Ÿฌํ•œ ๋ฐœ๊ฒฌ์€ ๊ณ ๋Œ€ ์ธ๋ฅ˜๊ฐ€ ์–ด๋–ป๊ฒŒ ์ž์›์„ ๊ด€๋ฆฌํ•˜๊ณ  ์ƒ์กด์— ํ•„์š”ํ•œ ๊ธฐ์ˆ ์„ ๋ฐœ์ „์‹œ์ผฐ๋Š”์ง€๋ฅผ ์ดํ•ดํ•˜๋Š” ๋ฐ ์ค‘์š”ํ•œ ๋‹จ์„œ๋ฅผ ์ œ๊ณตํ•ฉ๋‹ˆ๋‹ค. ๋‚ ๊ฐœ ๋‹ฌ๋ฆฐ ๊ทธ๋ฌผ์˜ ์กด์žฌ๋Š” ๋ฐฉ์‚ฌ์„ฑ ํƒ„์†Œ ๋ถ„์„์„ ํ†ตํ•ด ํ™•์ธ๋˜์—ˆ์œผ๋ฉฐ, ๊ฐ€์žฅ ์˜ค๋ž˜๋œ ๊ตฌ์กฐ๋ฌผ์€ ์•ฝ 9์ฒœ ๋…„ ์ „๋ถ€ํ„ฐ 11์ฒœ ๋…„ ์ „๊นŒ์ง€ ๊ฑฐ์Šฌ๋Ÿฌ ์˜ฌ๋ผ๊ฐ‘๋‹ˆ๋‹ค

Physics
No Image

Abusir: from Pliny the Elder to Google Maps

: ๋ณธ ๋…ผ๋ฌธ์€ ์ด์ง‘ํŠธ ์•„๋ถ€์‹œ๋ฅด ์œ ์ ์ง€์˜ ๋ฐœ๊ตด๊ณผ ์—ฐ๊ตฌ ๊ณผ์ •์„ ์ค‘์‹ฌ์œผ๋กœ, ํ˜„๋Œ€ ๊ธฐ์ˆ ์ธ ๊ตฌ๊ธ€ ๋งต ์œ„์„ฑ ์ด๋ฏธ์ง€ ์ฒ˜๋ฆฌ๋ฅผ ํ†ตํ•ด ๊ณ ๊ณ ํ•™์  ๋ฐœ๊ฒฌ์ด ์–ด๋–ป๊ฒŒ ์ด๋ฃจ์–ด์งˆ ์ˆ˜ ์žˆ๋Š”์ง€๋ฅผ ๊นŠ์ด ์žˆ๊ฒŒ ๋ถ„์„ํ•˜๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค. ํŠนํžˆ, ์ฒด์ฝ” ์›์ •๋Œ€์™€ ์ดํƒˆ๋ฆฌ์•„ ํ•™์ž๋“ค์˜ ์—ญํ• ์— ์ดˆ์ ์„ ๋งž์ถ”์–ด ์•„๋ถ€์‹œ๋ฅด ํ”ผ๋ผ๋ฏธ๋“œ ๋ณตํ•ฉ์ฒด์˜ ์—ญ์‚ฌ์  ๋ฐฐ๊ฒฝ๊ณผ ํ˜„๋Œ€ ์—ฐ๊ตฌ ๋ฐฉ๋ฒ•๋ก ์„ ๋‹ค๋ฃจ๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค. ๋…ผ๋ฌธ์€ ์•„๋ถ€์‹œ๋ฅด ์œ ์ ์ง€๊ฐ€ 14๊ฐœ์˜ ํ”ผ๋ผ๋ฏธ๋“œ๋กœ ๊ตฌ์„ฑ๋˜์–ด ์žˆ์œผ๋ฉฐ, ์ด๋“ค ๊ตฌ์กฐ๋ฌผ์˜ ํ’ˆ์งˆ์ด ์ œ4์™•์กฐ๋ณด๋‹ค ์—ด๋“ฑํ•˜๋‹ค๋Š” ์ ์„ ๊ฐ•์กฐํ•ฉ๋‹ˆ๋‹ค. ์ด๋Ÿฌํ•œ ์ฐจ์ด๋Š” ์™•๊ถŒ์˜ ์•ฝํ™” ๋˜๋Š” ๊ฒฝ์ œ ์ƒํ™ฉ์˜ ์•…ํ™”์™€ ๊ด€๋ จ์ด ์žˆ์„ ๊ฒƒ์œผ๋กœ ์ถ”์ •๋ฉ๋‹ˆ๋‹ค

Physics
Floating Extensional Flows

Floating Extensional Flows

๋ณธ ๋…ผ๋ฌธ์€ ๋น™ํ•˜ ์‹œํŠธ์˜ ํ™•์žฅ ํ๋ฆ„์— ๋Œ€ํ•œ ์‹ฌ๋„ ์žˆ๋Š” ๋ชจ๋ธ๋ง๊ณผ ๋ถ„์„์„ ํ†ตํ•ด, ๋‰ดํ„ด ์œ ์ฒด์™€ ๋น„๋‰ดํ„ด ์œ ์ฒด ์‚ฌ์ด์˜ ์ค‘์š”ํ•œ ์—ญํ•™์  ์ฐจ์ด๋ฅผ ํƒ๊ตฌํ•œ๋‹ค. ์ด ์—ฐ๊ตฌ๋Š” ํŠนํžˆ ๋น™ํ•˜๊ฐ€ ๋ฐ”๋‹ค ์œ„๋กœ ๋– ์˜ค๋ฅด๋ฉด์„œ ๋ฐœ์ƒํ•˜๋Š” ํ™•์žฅ ํ๋ฆ„์— ์ดˆ์ ์„ ๋งž์ถ”๊ณ  ์žˆ๋‹ค. 1. ๋น™ํ•˜ ์‹œํŠธ์˜ ๊ธฐ๋ณธ ํŠน์„ฑ ์ „๋‹จ ํ๋ฆ„ : ๋น™ํ•˜์˜ ์ค‘์‹ฌ๋ถ€๋Š” ์ง€๋ฐ˜์— ๊ณ ์ •๋˜์–ด ์žˆ์œผ๋ฉฐ, ์ฃผ๋œ ํ๋ฆ„์€ ์ „๋‹จ ํ๋ฆ„์ด๋‹ค. ํ™•์žฅ ํ๋ฆ„ : ์ค‘๋ ฅ์— ์˜ํ•ด ๋ณ€ํ˜•๋˜๋Š” ๋น™ํ•˜๋Š” ๋‘๊ป˜๊ฐ€ ์ถฉ๋ถ„ํžˆ ์–‡์•„์ง€๋ฉด ๋ฐ”๋‹ค ์œ„๋ฅผ ๋– ๋‹ค๋‹ ์ˆ˜ ์žˆ๋‹ค. ์ด๋•Œ์˜ ํ๋ฆ„์„ ํ™•์žฅ ํ๋ฆ„์ด๋ผ ๋ถ€๋ฅธ๋‹ค. 2. ๋‰ดํ„ด ์œ ์ฒด์™€ ๋น„๋‰ดํ„ด ์œ ์ฒด์˜ ๋น„๊ต ๋‰ดํ„ด ์œ ์ฒด : ์ ์„ฑ์ด ์ผ์ •ํ•œ

Physics
No Image

The cradle of pyramids in satellite images

๋ณธ ๋…ผ๋ฌธ์€ ์œ„์„ฑ ์ด๋ฏธ์ง€์™€ ์›๊ฒฉ ๊ฐ์ง€ ๊ธฐ๋ฒ•์ด ์–ด๋–ป๊ฒŒ ์ด์ง‘ํŠธ ๊ณ ๋Œ€ ์œ ์  ๋ฐœ๊ตด์— ํ™œ์šฉ๋  ์ˆ˜ ์žˆ๋Š”์ง€๋ฅผ ํƒ๊ตฌํ•˜๊ณ  ์žˆ๋‹ค. ์ €์ž๋Š” ๊ตฌ๊ธ€ ๋งต์Šค์˜ ์ด๋ฏธ์ง€ ์ฒ˜๋ฆฌ ๊ธฐ๋Šฅ๊ณผ SIR C/X SAR ๋ ˆ์ด๋” ์‹œ์Šคํ…œ์„ ๋น„๊ต ๋ถ„์„ํ•จ์œผ๋กœ์จ, ์›๊ฒฉ ๊ฐ์ง€ ๊ธฐ๋ฒ•์˜ ํšจ๊ณผ์„ฑ์„ ์ž…์ฆํ•˜๋ ค๊ณ  ๋…ธ๋ ฅํ•œ๋‹ค. 1. ์›๊ฒฉ ๊ฐ์ง€ ๊ธฐ๋ฒ•์˜ ์ค‘์š”์„ฑ ๋…ผ๋ฌธ์€ ๊ณ ๊ณ ํ•™์—์„œ ์›๊ฒฉ ๊ฐ์ง€ ๊ธฐ๋ฒ•์ด ์ค‘์š”ํ•œ ์—ญํ• ์„ ํ•œ๋‹ค๋Š” ์ ์„ ๊ฐ•์กฐํ•˜๊ณ  ์žˆ๋‹ค. ํŠนํžˆ, SIR C/X SAR ๋ ˆ์ด๋” ์‹œ์Šคํ…œ๊ณผ ๊ตฌ๊ธ€ ๋งต์Šค์˜ ์ด๋ฏธ์ง€๋ฅผ ๋น„๊ต ๋ถ„์„ํ•จ์œผ๋กœ์จ, ์ด๋Ÿฌํ•œ ๊ธฐ์ˆ ๋“ค์ด ์ด์ง‘ํŠธ ๊ณ ๋Œ€ ์œ ์  ๋ฐœ๊ตด์— ์–ด๋–ป๊ฒŒ ํ™œ์šฉ๋  ์ˆ˜ ์žˆ๋Š”์ง€ ์„ค๋ช…ํ•œ๋‹ค. 2. ๊ตฌ๊ธ€

Physics

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