ONDA Yuichi
- Articles
- Why has Lake Kasumigaura become turbid?
T. Fukushima; S. Kawamura; T. Seki; Y. Onda; A. Imai; K. Matsu...
Verh. Internat. Verein. Limnol./29/p.732-737, 2005-01 - Characterization of diffuse pollutions from forested watersheds in Japan during storm events – its association with rainfall and watershed features.
Z. Zhang; T. Fukushima; Y. Onda; S. Mizugaki; T. Gomi; K....
Sci. Total Environ./390(1)/pp.215-226, 2008-01 - 分水線セグメント・システムの構成法則と流域の地形
恩田 裕一
地理学評論/60/p.8, 1987-01 - 土層の水貯留機能の水文特性および崩壊発生に及ぼす影響
恩田 裕一
地形/10/p.1, 1989-01 - 粒状体斜面の崩れを規定するメカニズム
恩田 裕一
第36回土質工学シンポジウム発表論文集, 1991-01 - Is the maximum stable angle of slope of granular assemblies omparable to the angle of shearing resistance?
恩田 裕一
Transactions Japanese Geomorphological Union./12/p.2, 1991-01 - Influence of water storage capacity in the regolith zone on hydrological characteristics, slope processes and slope form
恩田 裕一
Zeitschrift fiur Geomorphologie/36/p.2, 1992-01 - A Model on the Stability of slopes composed of ranular materials
恩田 裕一
Science Reponts, Institute of Geoscience UNiversity of Tsukuba, 1992-01 - The effects of topographic convergence and location of past land sides on subsurface water movement on Granitic hillslopes
恩田 裕一
Journal of Natural Disaster Science/14/p.45-58, 1992-01 - Effect of rock properties on the longitudiral profiles of river beds : Comparison of the mountain rivers in Granite and Paleozoic Sedinentary rock basins.
恩田 裕一
Geographical Review on Japan/66(4)/p.203-216, 1993-01 - Characteristics of sediment yield in four small catchments underlawin by different bed rocks
恩田 裕一
Bull. Environm. Res. Canter, Univ. of Tsukuba/18/p.99-104, 1993-01 - Reply to the preceding comment by N. Caine on Is the maximam stable angle of slope of gremular assemblies Comparark to the angle of sheaving resistane?
恩田 裕一
Transactions, Japanese Jeomorphological Union/14(4)/p.427-429, 1993-01 - Contrasting hydrological characteristics, slope processes and topography underlain by Paleozoic Sedimentary rocks and granite
恩田 裕一
Transactions, Japanese Geomorphological Union/15A/p.49-65, 1994-01 - Runoff characteristics and solute concentration on four small catchment with different bedrocks in the Abkuma mountains, Japan
恩田 裕一
Transactions, Japanese geomorphological Union/15A/p.31-48, 1994-01 - Seepage erasion and its imprecation to the formation of amphitheater recalled heads in case study at Obara, Japan
恩田 裕一
Earth Surface Processes and Landforms/19/p.627-640, 1994-01 - The critical rainfall condition inducing the debris flow in Yotagiri river, central Japan
恩田 裕一
新砂防/47(6)/p.34-37, 1995-01 - The influences of understories on the infiltration Capacities of Chamaecyparis obtusa plantations (I) : Experimental results using mist type rainfall simulator.
湯川 典子; 恩田 裕一
Journal of the Japanese Forestry Society/77(3)/pp.224-231, 1995-05 - The influences on the infiltration capacities of Chamaecyparis obtusa plantations ((]G0002[)) Laboratory experiments
恩田 裕一; 湯川 典子
Journal of Japanese Forestry Society/77(5)/pp.399-407, 1995-09 - Spatial variation in specific discharge of base flow in small catchment in Oe-yama region, western Japan.
恩田 裕一
Journal of Japan Society of Hydrological and Water Resources/9/p.489-497, 1996-01 - Acid neutralization process in Hinoki plantation, A study through a large scale sprinkling experiment.
竹中 千里; 恩田 裕一; 榊原 岳史; 笹間 崇; 酒井 佳美; 只木 良也; 野々田 稔郎
Japanese journal of forest environment/39(1)/pp.29-35, 1997-06 - An Experimental Study Identifying Sediment Sources Using Radio Nuclides
恩田 裕一; 竹中 千里; 神谷 義久; 浜島 靖典; 野々田 稔郎
砂防学会誌/50(4)/pp.19-24, 1997-11 - The study on the acid notarization mechanism on Hinoki plantations by large-scale sprinkling experiments
恩田 裕一
環境技術/26(10)/p.642-646, 1997-01 - An Experimental Study on the burrowing activity of river crabson subswrface water movement and piping erosion
恩田 裕一
Geomorphology/20/p.279-288, 1997-01 - Mechanism for the Instability of Slopes Composed of Granular Materials
恩田 裕一
Earth Surface Processes & Cand forms/22/p.401-411, 1997-01 - Mechanism for the instability of slopes composed of granular materials.
恩田 裕一
Earth Surface Processes and Landforms/22/p.401-411, 1997-01 - more...
- Why has Lake Kasumigaura become turbid?