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      지리산 주변 산지하천의 step-pool 구조 특성 = Characteristics of step-pool structure in the mountain streams around Mt. Jiri

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      https://www.riss.kr/link?id=A105349331

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      다국어 초록 (Multilingual Abstract)

      The height of the steps was almost the same as the grain size of bed materials and increased with channel slope. The step widths and step wavelengths are almost the same size, and the step wavelength was decreased when the channel slope was increased. It was analyzed that there was a clear correlation between channel width and step width, and the step width increases with channel width. In addition, the step wavelength was scaled by channel width, and the step height is governed by the grain size of the rock forming the step, so that the profile structure of the step-pool was changed according to the channel slope. the scale of the pool was found to be highly correlated with the channel width, grain size, and slope gradient. Therefore, the characteristics of step-pool structure in mountain streams were influenced by various factors, but it can be explained as the grain size, channel width and channel slope.
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      The height of the steps was almost the same as the grain size of bed materials and increased with channel slope. The step widths and step wavelengths are almost the same size, and the step wavelength was decreased when the channel slope was increased....

      The height of the steps was almost the same as the grain size of bed materials and increased with channel slope. The step widths and step wavelengths are almost the same size, and the step wavelength was decreased when the channel slope was increased. It was analyzed that there was a clear correlation between channel width and step width, and the step width increases with channel width. In addition, the step wavelength was scaled by channel width, and the step height is governed by the grain size of the rock forming the step, so that the profile structure of the step-pool was changed according to the channel slope. the scale of the pool was found to be highly correlated with the channel width, grain size, and slope gradient. Therefore, the characteristics of step-pool structure in mountain streams were influenced by various factors, but it can be explained as the grain size, channel width and channel slope.

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      참고문헌 (Reference)

      1 Wohl, E. E., "Velocity characteristics along a small step-pool channel" 25 (25): 353-367, 2000

      2 Oh, S. W., "The research of step pool sequence in the mountain stream" 7 (7): 33-52, 2000

      3 Chin, A., "The morphologic structure of step-pools in mountain streams" 27 (27): 191-204, 1999

      4 Ashida, K., "Structure and friction law of flow over a step-pool bedform" 29 (29): 391-403, 1986

      5 Chin, A., "Step-pools in stream channels" 13 (13): 391-408, 1989

      6 Abrahams, A. D., "Step-pool streams: adjustment to maximum flow resistance" 31 (31): 2593-2602, 1995

      7 Whittaker, J. G., "Sediment transport in step-pool streams, Sediment Transport in Gravel-bed Rivers" Wiley 545-579, 1982

      8 Montgomery, D. R., "Pool spacing in forest channels" 31 (31): 1097-1105, 1995

      9 Grant, G. E., "Pattern and origin of stepped-bed morphology in high-gradient streams, Western Cascades, Oregon" 102 (102): 340-352, 1990

      10 Costa, J. E., "Paleohydraulic reconstruction of flash-flood peaks from boulder deposits in the Colorado Front Range" 94 (94): 986-1004, 1983

      1 Wohl, E. E., "Velocity characteristics along a small step-pool channel" 25 (25): 353-367, 2000

      2 Oh, S. W., "The research of step pool sequence in the mountain stream" 7 (7): 33-52, 2000

      3 Chin, A., "The morphologic structure of step-pools in mountain streams" 27 (27): 191-204, 1999

      4 Ashida, K., "Structure and friction law of flow over a step-pool bedform" 29 (29): 391-403, 1986

      5 Chin, A., "Step-pools in stream channels" 13 (13): 391-408, 1989

      6 Abrahams, A. D., "Step-pool streams: adjustment to maximum flow resistance" 31 (31): 2593-2602, 1995

      7 Whittaker, J. G., "Sediment transport in step-pool streams, Sediment Transport in Gravel-bed Rivers" Wiley 545-579, 1982

      8 Montgomery, D. R., "Pool spacing in forest channels" 31 (31): 1097-1105, 1995

      9 Grant, G. E., "Pattern and origin of stepped-bed morphology in high-gradient streams, Western Cascades, Oregon" 102 (102): 340-352, 1990

      10 Costa, J. E., "Paleohydraulic reconstruction of flash-flood peaks from boulder deposits in the Colorado Front Range" 94 (94): 986-1004, 1983

      11 Whittaker, J. G., "Origin of step-pool systems in mountain streams" ASCE 108 (108): 758-773, 1982

      12 Grant, G. E., "Origin of step-pool sequences in high gradient streams: a flume experiment" 523-532, 1991

      13 Chin, A., "On the stability of step-pool mountain streams" 106 (106): 59-70, 1998

      14 Hayward, J. A., "Hydrology and stream sediments from Torlesse stream catchment" New Zealand, Lincoln College, Tussock Grasslands and Mountain Lands Institute 236-, 1980

      15 Ashida, K., "Generation and geometric features of step-pool bed forms" 27 (27): 341-353, 1984

      16 Fujita, N., "Experimental flume study on the bed-step formation in bedrock channels" (21) : 25-40, 1996

      17 Tatsuya, O., "Characteristics of step-pool morphology in the mountain streams of Japan, Disaster Mitigation of Debris Flows, Slope Failures and Landslides" Universal Academy Press, Inc. 379-390, 2006

      18 Montgomery, D. R., "Channel-reach morphology in mountain drainage basins" 109 (109): 596-611, 1997

      19 Yamamoto, K., "Channel specific analysis" Public Works Research Institute 56-64, 1988

      20 Wohl, E. E., "Channel bed-steps along Nahal Yael, Negev desert, Israel" 9 (9): 117-126, 1994

      21 Wohl, E. E., "Bedrock channel morphology" 113 (113): 1205-1212, 2001

      22 Chartrand, S. M., "Alluvial architecture in headwater streams with special emphasis on step-pool topography" 25 (25): 583-600, 2000

      23 Rosgen, D. L., "A classification of natural rivers" 22 (22): 169-199, 1994

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      2021-01-01 평가 등재학술지 유지 (재인증) KCI등재
      2018-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2015-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2011-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2009-01-01 평가 등재학술지 유지 (등재유지) KCI등재
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      2005-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2002-07-01 평가 등재학술지 선정 (등재후보2차) KCI등재
      2000-01-01 평가 등재후보학술지 선정 (신규평가) KCI등재후보
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      학술지 인용정보
      기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
      2016 0.5 0.5 0.57
      KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
      0.55 0.54 0.781 0.22
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