83 research outputs found

    Assessment and Spatiotemporal Variation Analysis of Water Quality in the Zhangweinan River Basin, China

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    AbstractSpatiotemporal variation analysis of water quality and identification of water pollution sources in river basins is very important for water resources protection and sustainable utilization. In this study, fuzzy comprehensive analysis and two statistical methods including cluster analysis and seasonal Kendall test method were used to evaluate the spatiotemporal variation of water quality in the Zhangweinan River basin. The results for spatial cluster analysis and assessment on water quality at 19 monitoring sites indicated that water quality in the Zhangweinan River basin could be classified into two regions according to pollution levels. One is the Zhang River basin located in northwest of the Zhangweinan River basin where water quality is good. Another one includes the Wei River and eastern plain of the Zhangweinan River basin, and the water pollution in this region is serious, where the pollutants from point sources flow into the river and the water quality changes greatly. The results of temporal cluster analysis and seasonal Kendall test indicated that the sampling periods may be classified into three periods during 2002-2009 according to water quality. Results of temporal cluster analysis and seasonal Kendall test indicated that the study periods may be classified into three periods and two different trends was detected during the period of 2002-2009. The first period was the year of 2002-2003, during which water quality had deteriorated and serious pollution was observed in the Wei River basin and eastern plain of the Zhangweinan River basin. The second period was the year of 2004-2006, during which water quality became better. The year of 2007-2009 is the third period, during which water quality had been improved greatly. Despite that water quality in the Zhangweinan River basin had been improved during the period of 2004-2009, water quality in the Wei River (southwestern part of the basin), the Wei Canal River and the Zhangweixin River (eastern plain of the basin) is still poor. These results provide may useful information for better pollution control strategies in the Zhangweinan River basin

    Coastal Fish Research

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    This book is a collection of a series of articles on several aspects of coastal fish biology and ecology. Coastal fish are key components of marine ecosystems, and the aim of this book is to present relevant research on these wonderful animals and to provide insights for future research in this field

    Controlling Factors of Microplastic Riverine Flux and Implications for Reliable Monitoring Strategy

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    Embargo until December 12, 2022A significant proportion of marine plastic debris and microplastics is assumed to be derived from river systems. In order to effectively manage plastic contamination of the marine environment, an accurate quantification of riverine flux of land-based plastics and microplastics is imperative. Rivers not only represent pathways to the ocean, but are also complex ecosystems that support many life processes and ecosystem services. Yet riverine microplastics research is still in its infancy, and many uncertainties still remain. Major barriers exist in two aspects. First, nonharmonized sampling methodologies make it problematic for compiling data across studies to better estimate riverine fluxes of microplastics globally; Second, the significant spatiotemporal variation of microplastics in rivers which was affected by the river characteristics, MPs properties, etc. also have important influence on the estimation of riverine MPs fluxes. In this study, we made a comprehensive review from the above two aspects based on published peer-reviewed studies and provide recommendations and suggestions for a reliable monitoring strategy of riverine MPs, which is beneficial to the further establish sampling methods for rivers in different geographical locations. Besides, methods for achieving a high level of comparability across studies in different geographical contexts are highlighted. Riverine microplastic flux monitoring is another important part of this manuscript. The influential factors and calculation methods of microplastic flux in rivers are also discussed in this paper.acceptedVersio

    ๊ณ ํ•ด์ƒ๋„ ์ดˆ๋ถ„๊ด‘์˜์ƒ์„ ํ™œ์šฉํ•œ ํ•˜์ฒœ ๋ถ€์œ ์‚ฌ๋†๋„ ๊ณ„์ธก๊ธฐ๋ฒ• ๊ฐœ๋ฐœ

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    ํ•™์œ„๋…ผ๋ฌธ(๋ฐ•์‚ฌ) -- ์„œ์šธ๋Œ€ํ•™๊ต๋Œ€ํ•™์› : ๊ณต๊ณผ๋Œ€ํ•™ ๊ฑด์„คํ™˜๊ฒฝ๊ณตํ•™๋ถ€, 2022. 8. ์„œ์ผ์›.๊ธฐ์กด์˜ ํ•˜์ฒœ ๋ถ€์œ ์‚ฌ ๋†๋„ ๊ณ„์ธก์€ ์ƒ˜ํ”Œ๋ง ๊ธฐ๋ฐ˜ ์ง์ ‘๊ณ„์ธก ๋ฐฉ์‹์— ์˜์กดํ•˜์—ฌ ์‹œ๊ณต๊ฐ„์  ๊ณ ํ•ด์ƒ๋„ ์ž๋ฃŒ ์ทจ๋“์ด ์–ด๋ ค์šด ์‹ค์ •์ด๋‹ค. ์ด๋Ÿฌํ•œ ํ•œ๊ณ„์ ์„ ๊ทน๋ณตํ•˜๊ธฐ ์œ„ํ•ด ์ตœ๊ทผ ์œ„์„ฑ๊ณผ ๋“œ๋ก ์„ ํ™œ์šฉํ•˜์—ฌ ์ดฌ์˜๋œ ๋‹ค๋ถ„๊ด‘ ํ˜น์€ ์ดˆ๋ถ„๊ด‘ ์˜์ƒ์„ ํ†ตํ•ด ๊ณ ํ•ด์ƒ๋„์˜ ๋ถ€์œ ์‚ฌ๋†๋„ ์‹œ๊ณต๊ฐ„๋ถ„ํฌ๋ฅผ ๊ณ„์ธกํ•˜๋Š” ๊ธฐ๋ฒ•์— ๋Œ€ํ•œ ์—ฐ๊ตฌ๊ฐ€ ํ™œ๋ฐœํžˆ ์ง„ํ–‰๋˜๊ณ  ์žˆ๋‹ค. ํ•˜์ง€๋งŒ, ๋‹ค๋ฅธ ํ•˜์ฒœ ๋ฌผ๋ฆฌ๋Ÿ‰ ๊ณ„์ธก์— ๋น„ํ•ด ๋ถ€์œ ์‚ฌ ๊ณ„์ธก ์—ฐ๊ตฌ๋Š” ํ•˜์ฒœ์— ๋”ฐ๋ผ ๋ถ€์œ ์‚ฌ๊ฐ€ ๋‹ค์–‘ํ•˜๊ฒŒ ๋ถ„ํฌํ•˜๊ณ  ๋‹ค๋ฅธ ๋ถ€์œ ๋ฌผ์งˆ ํ˜น์€ ํ•˜์ƒ์— ์˜ํ•œ ๋ฐ”๋‹ฅ ๋ฐ˜์‚ฌ์˜ ์˜ํ–ฅ ๋•Œ๋ฌธ์— ๋ถ„๊ด‘ ์ž๋ฃŒ๋ฅผ ํ†ตํ•ด ์ •ํ™•ํ•œ ๋ถ€์œ ์‚ฌ๋†๋„ ๋ถ„ํฌ๋ฅผ ์žฌํ˜„ํ•˜๊ธฐ ์–ด๋ ค์šด ์‹ค์ •์ด๋‹ค. ํŠนํžˆ, ๋ถ€์œ ์‚ฌ ๋ถ„๊ด‘ ํŠน์„ฑ์— ์˜ํ–ฅ์„ ๋ฏธ์น˜๋Š” ์ž…๋„๋ถ„ํฌ, ๊ด‘๋ฌผํŠน์„ฑ, ์นจ๊ฐ•์„ฑ ๋“ฑ์ด ํ•˜์ฒœ์— ๋”ฐ๋ผ ๊ฐ•ํ•œ ์ง€์—ญ์„ฑ์„ ๋‚˜ํƒ€๋‚ด๊ธฐ์— ์ด๋Ÿฌํ•œ ์š”์ธ์—์„œ ์•ผ๊ธฐ๋˜๋Š” ๋ถ„๊ด‘๋‹ค์–‘์„ฑ์œผ๋กœ ์ธํ•ด ํŠน์ • ์‹œ๊ธฐ์™€ ์ง€์—ญ์—๋งŒ ์ ํ•ฉํ•œ ์›๊ฒฉํƒ์‚ฌ ๊ธฐ๋ฐ˜ ๊ณ„์ธก ๋ชจํ˜•๋“ค์ด ๊ฐœ๋ฐœ๋˜์–ด ์™”๋‹ค. ๋ณธ ์—ฐ๊ตฌ์—์„œ๋Š” ์ด๋Ÿฌํ•œ ๋ถ„๊ด‘๋‹ค์–‘์„ฑ์„ ๋ฐ˜์˜ํ•˜์—ฌ ๋‹ค์–‘ํ•œ ํ•˜์ฒœ ๋ฐ ์œ ์‚ฌ ์กฐ๊ฑด์—์„œ ์ ์šฉ ๊ฐ€๋Šฅํ•œ ๊ณ ํ•ด์ƒ๋„ ์ดˆ๋ถ„๊ด‘์˜์ƒ์„ ํ™œ์šฉํ•œ ํ•˜์ฒœ ๋ถ€์œ ์‚ฌ๋†๋„ ๊ณ„์ธก๋ฐฉ๋ฒ•์„ ๊ฐœ๋ฐœํ•˜๊ธฐ ์œ„ํ•ด ์ดˆ๋ถ„๊ด‘ ๊ตฐ์ง‘ํ™” ๊ธฐ๋ฒ•๊ณผ ๋‹ค์–‘ํ•œ ํŒŒ์žฅ๋Œ€์˜ ๋ถ„๊ด‘ ๋ฐด๋“œ๋ฅผ ํ•™์Šตํ•  ์ˆ˜ ์žˆ๋Š” ๊ธฐ๊ณ„ํ•™์Šต ํšŒ๊ท€ ๋ชจํ˜•์„ ๊ฒฐํ•ฉํ•˜์—ฌ CMR-OV๋ผ๋Š” ๋ฐฉ๋ฒ•๋ก ์„ ์ œ์‹œํ•˜์˜€๋‹ค. CMR-OV ๊ฐœ๋ฐœ ๋ฐ ๊ฒ€์ฆ์€ 1) ์‹คํ—˜์  ์—ฐ๊ตฌ๋ฅผ ํ†ตํ•œ ํ•˜์ฒœ ๋ถ€์œ ์‚ฌ ๋ถ„๊ด‘ ํŠน์„ฑ์˜ ์ฃผ์š” ๊ต๋ž€ ์š”์ธ ๋ถ„์„, 2) ์ตœ์  ํšŒ๊ท€๋ชจํ˜• ์„ ์ • ๋ฐ ์ดˆ๋ถ„๊ด‘ ํด๋Ÿฌ์Šคํ„ฐ๋ง๊ณผ์˜ ๊ฒฐํ•ฉ, 3) ํ˜„์žฅ์ ์šฉ์„ฑ ํ‰๊ฐ€์˜ ๊ณผ์ •์„ ๊ฑฐ์ณ ์ˆ˜ํ–‰๋˜์—ˆ๋‹ค. ์‹คํ—˜์  ์—ฐ๊ตฌ์—์„œ๋Š” ์šฐ์„  ์‹ค๋‚ด ์‹คํ—˜์‹ค์—์„œ ํšก๋ฐฉํ–ฅ ํ˜ผํ•ฉ๊ธฐ๋ฅผ ํ™œ์šฉํ•˜์—ฌ ๋ฐ”๋‹ฅ ๋ฐ˜์‚ฌ๋ฅผ ์ œ๊ฑฐํ•˜๊ณ  ์™„์ „ ํ˜ผํ•ฉ๋œ ์ƒํƒœ์—์„œ ๋ถ€์œ ์‚ฌ์˜ ๊ณ ์œ  ์ดˆ๋ถ„๊ด‘ ์ŠคํŽ™ํŠธ๋Ÿผ ์ž๋ฃŒ๋ฅผ ์ˆ˜์ง‘ํ•˜์˜€๋‹ค. ์ด๋ฅผ ๋ฐ”ํƒ•์œผ๋กœ ์‹ค์ œ ํ•˜์ฒœ๊ณผ ์œ ์‚ฌํ•œ ์กฐ๊ฑด์˜ ์‹ค๊ทœ๋ชจ ์˜ฅ์™ธ ์ˆ˜๋กœ ์‹คํ—˜์—์„œ ๋‹ค์–‘ํ•œ ์œ ์‚ฌ ํŠน์„ฑ(์ž…๋„ ๋ฐ ๊ด‘๋ฌผ)๊ณผ ํ•˜์ƒ ํŠน์„ฑ(์‹์ƒ ๋ฐ ๋ชจ๋ž˜)์— ๋Œ€ํ•œ ์ดˆ๋ถ„๊ด‘ ์ž๋ฃŒ๋ฅผ ์ˆ˜์ง‘ํ•˜์—ฌ ๊ณ ์œ  ์ดˆ๋ถ„๊ด‘ ์ŠคํŽ™ํŠธ๋Ÿผ๊ณผ ๋น„๊ตํ•˜์˜€๋‹ค. ๊ทธ ๊ฒฐ๊ณผ, ๋ถ€์œ ์‚ฌ์˜ ๋ถ„๊ด‘ ํŠน์„ฑ์€ ์œ ์‚ฌ์˜ ์ข…๋ฅ˜ ๋ฐ ์ž…๋„์— ๋”ฐ๋ผ ๋†๋„ ์ฆ๊ฐ€์— ๋”ฐ๋ฅธ ์ดˆ๋ถ„๊ด‘ ์ŠคํŽ™ํŠธ๋Ÿผ์˜ ๋ฐ˜์‚ฌ์œจ ๋ณ€ํ™”๊ฐ€ ์ƒ์ดํ•˜๊ฒŒ ๋‚˜ํƒ€๋‚ฌ๋‹ค. ๋˜ํ•œ, 1 m ์ดํ•˜์˜ ์–•์€ ์ˆ˜์‹ฌ ์กฐ๊ฑด์—์„œ๋Š” ๋ฐ”๋‹ฅ ๋ฐ˜์‚ฌ์˜ ์˜ํ–ฅ์œผ๋กœ ํ•˜์ƒ ์ข…๋ฅ˜์— ๋”ฐ๋ผ ์ดˆ๋ถ„๊ด‘ ์ŠคํŽ™ํŠธ๋Ÿผ์˜ ๊ฐœํ˜•์ด ํฌ๊ฒŒ ๋ณ€ํ™”ํ•˜์˜€์œผ๋ฉฐ, ๊ณ ๋†๋„์˜ ๋ถ€์œ ์‚ฌ๊ฐ€ ๋ถ„ํฌํ•  ๋•Œ๋„ ๋ฐ”๋‹ฅ ๋ฐ˜์‚ฌ๊ฐ€ ํฌ๊ฒŒ ์˜ํ–ฅ์„ ๋ฏธ์น˜๋Š” ๊ฒƒ์„ ํ™•์ธํ•˜์˜€๋‹ค. ์ด๋Ÿฌํ•œ ๋ถ„๊ด‘๋‹ค์–‘์„ฑ์ด ๋ฐ˜์˜๋œ ๋ถ€์œ ์‚ฌ๋†๋„์™€ ์ดˆ๋ถ„๊ด‘ ์ž๋ฃŒ์˜ ๊ด€๊ณ„๋ฅผ ๊ตฌ์ถ•ํ•˜๊ธฐ ์œ„ํ•˜์—ฌ ๊ธฐ๊ณ„ํ•™์Šต ๊ธฐ๋ฐ˜ ๋žœ๋คํฌ๋ ˆ์ŠคํŠธ ํšŒ๊ท€ ๋ชจํ˜•๊ณผ ๊ฐ€์šฐ์‹œ์•ˆ ํ˜ผํ•ฉ ๋ชจํ˜• ๊ธฐ๋ฐ˜ ์ดˆ๋ถ„๊ด‘ ๊ตฐ์ง‘ ๊ธฐ๋ฒ•์„ ๊ฒฐํ•ฉํ•œ CMR-OV๋ฅผ ์ ์šฉํ•œ ๊ฒฐ๊ณผ, ๊ธฐ์กด ์—ฐ๊ตฌ๋“ค์—์„œ ์ฃผ๋กœ ํ™œ์šฉ๋œ ๋ฐด๋“œ๋น„ ๊ธฐ๋ฐ˜์˜ ๋ชจํ˜•๊ณผ ๋‹จ์ผ ๊ธฐ๊ณ„ํ•™์Šต๋ชจํ˜•์— ๋น„ํ•ด ์ •ํ™•๋„๊ฐ€ ํฌ๊ฒŒ ํ–ฅ์ƒํ•˜์˜€๋‹ค. ํŠนํžˆ, ๊ธฐ์กด ์ตœ์  ๋ฐด๋“œ๋น„ ๋ถ„์„ (OBRA) ๋ฐฉ๋ฒ•์€ ๋น„์„ ํ˜•์„ฑ์„ ๊ณ ๋ คํ•ด๋„ ์ข์€ ์˜์—ญ์˜ ํŒŒ์žฅ๋Œ€๋งŒ์„ ๊ณ ๋ คํ•˜๋Š” ํ•œ๊ณ„์ ์œผ๋กœ ์ธํ•ด ๋ถ„๊ด‘๋‹ค์–‘์„ฑ์„ ๋ฐ˜์˜ํ•˜์ง€ ๋ชปํ•˜๋Š” ๊ฒƒ์œผ๋กœ ๋ฐํ˜€์กŒ๋‹ค. ํ•˜์ง€๋งŒ, CMR-OV๋Š” ํญ ๋„“์€ ํŒŒ์žฅ๋Œ€ ์˜์—ญ์„ ๊ณ ๋ คํ•จ๊ณผ ๋™์‹œ์— ๋†’์€ ์ •ํ™•๋„๋ฅผ ์‚ฐ์ถœํ•˜์˜€๋‹ค. ์ตœ์ข…์ ์œผ๋กœ CMR-OV๋ฅผ ํ™ฉ๊ฐ•์˜ ์ง์„ ๊ตฌ๊ฐ„ ๋ฐ ์‚ฌํ–‰๊ตฌ๊ฐ„๊ณผ ๋‚™๋™๊ฐ•๊ณผ ํ™ฉ๊ฐ•์˜ ํ•ฉ๋ฅ˜๋ถ€์— ์ ์šฉํ•˜์—ฌ ํ˜„์žฅ๊ฒ€์ฆ์„ ์ˆ˜ํ–‰ํ•œ ๊ฒฐ๊ณผ, ๊ธฐ์กด ๋ชจํ˜• ๋Œ€๋น„ ์ •ํ™•๋„์™€ ๋ถ€์œ ์‚ฌ ๋†๋„ ๋งตํ•‘์˜ ์ •๋ฐ€์„ฑ์—์„œ ํฐ ๊ฐœ์„ ์ด ์žˆ์—ˆ์œผ๋ฉฐ, ๋น„ํ•™์Šต์ง€์—ญ์—์„œ๋„ ๋†’์€ ์ •ํ™•๋„๋ฅผ ์‚ฐ์ถœํ•˜์˜€๋‹ค. ํŠนํžˆ, ํ•˜์ฒœ ํ•ฉ๋ฅ˜๋ถ€์—์„œ๋Š” ์ดˆ๋ถ„๊ด‘ ๊ตฐ์ง‘์„ ํ†ตํ•ด ๋‘ ํ•˜์ฒœ ํ๋ฆ„์˜ ๊ฒฝ๊ณ„์ธต์„ ๋ช…ํ™•ํžˆ ๊ตฌ๋ณ„ํ•˜์˜€์œผ๋ฉฐ, ์ด๋ฅผ ๋ฐ”ํƒ•์œผ๋กœ ์ง€๋ฅ˜์™€ ๋ณธ๋ฅ˜์— ๋Œ€ํ•ด ๊ฐ๊ฐ ๋ถ„๋ฆฌ๋œ ํšŒ๊ท€๋ชจํ˜•์„ ๊ตฌ์ถ•ํ•˜์—ฌ ๋ณต์žกํ•œ ํ•ฉ๋ฅ˜๋ถ€ ๊ทผ์—ญ ๊ฒฝ๊ณ„์ธต์—์„œ์˜ ๋ถ€์œ ์‚ฌ ๋ถ„ํฌ๋ฅผ ๋ณด๋‹ค ์ •ํ™•ํ•˜๊ฒŒ ์žฌํ˜„ํ•˜์˜€๋‹ค. ๋˜ํ•œ, ๋‚˜์•„๊ฐ€์„œ ์žฌํ˜„๋œ ๊ณ ํ•ด์ƒ๋„์˜ ๋ถ€์œ ์‚ฌ ๊ณต๊ฐ„๋ถ„ํฌ๋ฅผ ๋ฐ”ํƒ•์œผ๋กœ ํ˜ผํ•ฉ๋„๋ฅผ ์‚ฐ์ •ํ•œ ๊ฒฐ๊ณผ, ๊ธฐ์กด ์ ๊ณ„์ธก ๋Œ€๋น„ ์ƒ์„ธํ•˜๊ฒŒ ๋ถ€์œ ์‚ฌ ํ˜ผํ•ฉ์— ๋Œ€ํ•œ ์ •๋Ÿ‰์  ํ‰๊ฐ€๊ฐ€ ๊ฐ€๋Šฅํ•œ ๊ฒƒ์œผ๋กœ ๋‚˜ํƒ€๋‚ฌ๋‹ค. ๋”ฐ๋ผ์„œ, ๋ณธ ์—ฐ๊ตฌ์—์„œ ๊ฐœ๋ฐœํ•œ ์ดˆ๋ถ„๊ด‘์˜์ƒ ๊ธฐ๋ฐ˜ ๋ถ€์œ ์‚ฌ ๊ณ„์ธก ๊ธฐ์ˆ ์„ ํ†ตํ•ด ์ถ”ํ›„ ํ•˜์ฒœ ์กฐ์‚ฌ ๋ฐ ๊ด€๋ฆฌ ์‹ค๋ฌด์˜ ์ •ํ™•์„ฑ ๋ฐ ํšจ์œจ์„ฑ์„ ํฌ๊ฒŒ ์ฆ์ง„ํ•  ์ˆ˜ ์žˆ์„ ๊ฒƒ์œผ๋กœ ๊ธฐ๋Œ€๋œ๋‹ค.The conventional measurement method of suspended sediment concentration (SSC) in the riverine system is labor-intensive and time-consuming since it has been conducted using the sampling-based direct measurement method. For this reason, it is challenging to collect high-resolution datasets of SSC in rivers. In order to overcome this limitation, remote sensing-based techniques using multi- or hyper-spectral images from satellites or UAVs have been recently carried out to obtain high-resolution SSC distributions in water environments. However, suspended sediment in rivers is more dynamic and spatially heterogeneous than those in other fields. Moreover, the sediment and streambed properties have strong regional characteristics depending on the river type; thus, only models suitable for a specific period and region have been developed owing to the increased spectral variability of the water arising from various types of suspended matter in the water and the heterogeneous streambed properties. Therefore, to overcome the limitations of the existing monitoring system, this study proposed a robust hyperspectral imagery-based SSC measurement method, termed cluster-based machine learning regression with optical variability (CMR-OV). This method dealt with the spectral variability problem by combining hyperspectral clustering and machine learning regression with the Gaussian mixture model (GMM) and Random forest (RF) regression. The hyperspectral clustering separated the complex dataset into several homogeneous datasets according to spectral characteristics. Then, the machine learning regressors corresponding to clustered datasets were built to construct the relationship between the hyperspectral spectrum and SSC. The development and validation of the proposed method were carried out through the following processes: 1) analysis of confounding factors in the spectral variability through experimental studies, 2) selection of an optimal regression model and validation of hyperspectral clustering, and 3) evaluation of field applicability. In the experimental studies, the intrinsic hyperspectral spectra of suspended sediment were collected in a completely mixed state after removing the bottom reflection using a horizontal rotating cylinder. Then, hyperspectral data on various sediment properties (particle size and mineral contents) and river bed properties (sand and vegetation) were collected from sediment tracer experiments in field-scale open channels under different hydraulic conditions and compared with intrinsic hyperspectral spectra. Consequently, the change of the hyperspectral spectrum was different according to the sediment type and particle size distribution. In addition, under the shallow water depth condition of 1 m or less, the shape of the hyperspectral spectrum changed significantly depending on the bed type due to the bottom reflectance. The bottom reflectance substantially affected the hyperspectral spectrum even when the high SSC was distributed. As a result of combining the GMM and RF regression with building a relationship between the SSC and hyperspectral data reflecting the spectral variability, the accuracy was substantially improved compared to the other methods. In particular, even when nonlinearity is considered based on the existing optimal band ratio analysis (OBRA) method, spectral variability could not be reflected due to the limitation of considering only a narrow wavelength range. On the other hand, CMR-OV showed high accuracy while considering a wide range of wavelengths with clusters having distinct spectral characteristics. Finally, the CMR-OV was applied to the straight and meandering reaches of the Hwang River and the confluence of the Nakdong and Hwang Rivers in South Korea to assess field applicability. There was a remarkable improvement in the accuracy and precision of SSC mapping under various river conditions compared to the existing models, and CMR-OV showed robust performance even with non-calibrated datasets. At the river confluence, the mixing pattern between the main river and tributary was apparently retrieved from CMR-OV under optically complex conditions. Compared to the non-clustered model, hyperspectral clustering played a primary role in improving the performance by separating the water bodies originating from both rivers. It was also possible to quantitatively evaluate the complicated mixing pattern in detail compared to the existing point measurement. Therefore, it is expected that the accuracy and efficiency of river investigation will be significantly improved through the SSC measurement method presented in this study.Abstract of dissertation i List of figures ix List of tables xvii List of abbreviations xix List of symbols xxii 1. Introduction 1 2. Theoretical research 13 2.1.1 Pre-processing of hyperspectral image (HSI) 19 2.1.2 Optical characteristics of suspended sediment in rivers 28 2.1.2.1 Theory of solar radiation transfer in rivers 28 2.1.2.2 Heterogeneity of sediment properties 33 2.1.2.3 Effects of bottom reflectance 38 2.1.2.4 Vertical distribution of suspended sediment 41 2.1.3 Retrieval of suspended sediment from remote sensing data 46 2.1.3.1 Remote sensing-based regression approach 46 2.1.3.2 Clustering of remote sensing data 52 2.2 Mapping of suspended sediment concentration in rivers 56 2.2.1 Traditional method for spatial measurement 56 2.2.2 Spatial measurement at river confluences 57 2.2.2.1 Dynamics of flow and mixing at river confluences 57 2.2.2.2 Field experiments in river confluences 64 3. Experimental studies 68 3.1 Experimental cases 68 3.2 Laboratory experiment 74 3.2.1 Experimental setup 74 3.2.2 Experimental method 78 3.3 Field-scale experiments in River Experiment Center 83 3.3.1 Experiments in the straight channel 83 3.3.2 Experiments in the meandering channel 96 3.4 Field survey 116 3.4.1 Study area and field measurement 116 3.4.2 Hydraulic and sediment data in rivers with simple geometry 122 3.4.3 Hydraulic and sediment data in river confluences 126 3.5 Analysis of hyperspectral data of suspended sediment 141 3.5.1 Hyperspectral data of laboratory experiment 142 3.5.2 Hyperspectral data of field-scale experiments 146 3.5.2.1 Effect of bottom reflectance 146 3.5.2.2 Principal component analysis of the effect of suspended sediment properties 154 4. Development of suspended sediment concentration estimator using UAV-based hyperspectral imagery 164 4.1 Outline of Cluster-based Machine learning Regression with Optical Variability (CMR-OV) 164 4.2 Pre-processing of hyperspectral images 168 4.3 Regression models and clustering technique 173 4.3.1 Index-based regression models 173 4.3.2 Machine learning regression models 175 4.3.3 Relevant band selection 183 4.3.4 Gaussian mixture model for clustering 185 4.3.5 Performance criteria 188 4.4 Model development and evaluation 189 4.4.1 Comparison of regression models 189 4.4.1.1 OBRA-based explicit models 189 4.4.1.2 Machine learning-based implicit models 194 4.4.2 Assessment of hyperspectral clustering 200 4.4.3 Spatio-temporal SSCV mapping using CMR-OV 215 5. Evaluation of field applicability of CMR-OV 225 5.1 Outline of field applicability test 225 5.2 Cross-applicability validation of CMR-OV 227 5.3 Assessment of field applicability in rivers with simple geometry 234 5.4 Assessment of field applicability in river confluences 241 5.4.1 Classification of river regions using hyperspectral clustering 241 5.4.2 Retrievals of SSCV map 258 5.4.3 Mixing pattern extraction from SSCv map 271 6. Conclusions and future study 274 6.1 Conclusions 274 6.2 Future directions 278 Reference 280 Appendix 308 Appendix A. Breakthrough curve (BTC) analysis 308 Appendix B. Experimental data 310 Appendix B. 1. BTCs of in-situ measured SSC from field-scale experiments 310 Appendix B. 2. Dataset of spectra from hyperspectral images and corresponding SSC in rivers 330 Appendix C. CMR-OV code 331 ๊ตญ๋ฌธ์ดˆ๋ก 337๋ฐ•

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