Upper and lower plane bed definitions revised
国立国会図書館館内限定公開
収録元データベースで確認する
国立国会図書館デジタルコレクション
デジタルデータあり
公開元のウェブサイトで確認する
DOI[10.1186/s40645-022-00481-8]のデータに遷移します
全国の図書館の所蔵
国立国会図書館以外の全国の図書館の所蔵状況を表示します。
所蔵のある図書館から取寄せることが可能かなど、資料の利用方法は、ご自身が利用されるお近くの図書館へご相談ください
書誌情報
この資料の詳細や典拠（同じ主題の資料を指すキーワード、著者名）等を確認できます。
- 資料種別
- 記事
- 著者・編者
- Koji OhataHajime NaruseNorihiro Izumi
- 出版年月日等
- 2022-04-25
- 出版年（W3CDTF）
- 2022-04-25
- タイトル（掲載誌）
- Progress in earth and planetary science
- 巻号年月日等（掲載誌）
- 9(23)
- 掲載巻
- 9(23)
- ISSN（掲載誌）
- 2197-4284
- ISSN-L（掲載誌）
- 2197-4284
- 本文の言語コード
- eng
- DOI
- 10.1186/s40645-022-00481-8
- 国立国会図書館永続的識別子
- info:ndljp/pid/12307834
- コレクション（共通）
- コレクション（障害者向け資料：レベル1）
- コレクション（個別）
- 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- 収集根拠
- オンライン資料収集制度
- 受理日（W3CDTF）
- 2022-07-11T20:40:38+09:00
- 保存日（W3CDTF）
- 2022-07-11
- 記録形式（IMT）
- application/pdf
- オンライン閲覧公開範囲
- 国立国会図書館内限定公開
- デジタル化資料送信
- 図書館・個人送信対象外
- 遠隔複写可否（NDL）
- 可
- 掲載誌（国立国会図書館永続的識別子）
- info:ndljp/pid/12307811
- 連携機関・データベース
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- 要約等
- Sedimentary structures in ancient deposits are clues to reconstruct past geohazards. While parallel lamination formed by plane beds is one of the most common sedimentary structures in event deposits such as turbidites, the formative conditions for plane beds remain unclear. In the literature, two types of plane beds (upper and lower plane beds) exist and are supposed to develop under different shear stresses, particle sizes, and flow regimes. Here, we present new phase diagrams based on the compilation of existing data regarding formative hydraulic conditions for plane beds to clarify the formation processes associated with the two types of plane beds. The diagrams indicated that the data form two separate populations and the gap between them corresponds to the threshold condition of the particle entrainment into suspension. Lower plane beds form when sediment particles move only as bed load. This phase space can be discerned from fine sand to gravel and differs from the conventional view in which the formation of the lower plane bed is limited to grain sizes above 0.7 mm. In addition, our phase diagrams suggest that upper plane beds appear under conditions of the active suspended load. Our analyses demonstrate that the suspended load contributes to the formation of plane beds, whereas other mechanisms can also produce fine-grained plane beds in flows with low bed shear stress. Thus, the results of this study suggest that the existing interpretations on fine-grained parallel lamination such as Bouma’s Td division need to be reconsidered. The bedform phase diagrams newly established in this study will be useful for estimating the flow conditions from the geologic records of event beds.
- DOI
- 10.1186/s40645-022-00481-8
- オンライン閲覧公開範囲
- インターネット公開
- 著作権情報
- © The Author(s) 2022.This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder.
- 関連情報
- Upper and lower plane bed definitions revised
- 関連情報（URI）
- 参照
- Density stratification controls the bedform phase diagram of saline‐gravity currents versus open‐channel flowsモデル実験から理解する沖積河川の堆積・侵食・地形発達作用
- 参照
- Reconstruction of flow conditions from 2004 Indian Ocean tsunami deposits at the Phra Thong island using a deep neural network inverse modelNew Bedform Phase Diagrams and Discriminant Functions for Formative Conditions of Bedforms in Open‐Channel FlowsAn approach to the sediment transport problem from general physicsThe mechanics of dunes and antidunes in erodible-bed channelsMeasurement of hydraulic and sediment transport variables in a small recirculating flumeRepresentation of Bed Configurations in Depth-Velocity-Size DiagramsDetecting allocyclic signals in volcaniclastic fluvial successions: Facies, architecture and stacking pattern from the Cretaceous of central Patagonia, ArgentinaA field investigation of the relationship between oscillation ripple spacinng and the near-bottom water orbital motionsEffect of bed permeability and hyporheic flow on turbulent flow over bed formsClimbing‐ripple successions in turbidite systems: depositional environments, sedimentation rates and accumulation timesDunes in the world’s big rivers are characterized by low-angle lee-side slopes and a complex shapeExperiments on the Transporting Power of Sea CurrentsSediment transport in oscillatory sheet flowOn the stability of lower stage plane beds and the absence of current ripples in coarse sandsShallow erosion beneath turbidity currents and its impact on the architectural development of turbidite sheet systemsEmplacement of massive deposits by sheet flowRevisiting the linear theory of sand dune formationPreservation of planar laminae due to migration of low‐relief bed waves over aggrading upper‐stage plane beds: comparison of experimental data with theoryUpper-Regime Plane BedBedforms in a tidally modulated ridge and runnel shoreface (Berck-Plage; North France): implications for the geological recordExperiments on the Transporting Power of Sea Currents: DiscussionFlume Experiments on Lower-Flow-Regime Bed Forms in Coarse SandTransition between Two Bed-Load Transport Regimes: Saltation and Sheet FlowConcentrations in oscillatory sheet flow for well sorted and graded sandsDepositional Record of Tidal-Flat Sedimentation in the Permian Coal Measures of Central India: Barakar Formation, Mohpani Coalfield, Satpura Gondwana BasinBed Form Response to Nonsteady FlowsA New Bedform Stability Diagram, with Emphasis on the Transition of Ripples to Plane Bed in Flows over Fine Sand and SiltThe occurrence of Paleodictyon in shallow-marine deposits of the Upper Cretaceous Mikasa Formation, Hokkaido Island, northern Japan: Implications for spatiotemporal variation of the Nereites ichnofaciesA New Phase Diagram for Combined-Flow BedformsInstability of erodible bedsSummary of alluvial channel data from flume experiments, 1956-61Subaqueous sediment density flows: Depositional processes and deposit typesThe Total Sediment Load of StreamsThe exceptional sediment load of fine-grained dispersal systems: Example of the Yellow River, ChinaThe Legend of A. F. ShieldsBed forms in the Lower Red Deer River, AlbertaBedforms of the Tana River, NorwayA Sharp View on River Dune Transition to Upper Stage Plane BedWAVE-FORMED SEDIMENTARY STRUCTURES—A CONCEPTUAL MODELFluvial HydrodynamicsFlume Experiments on the Transition from Ripples to Lower Flat Bed with Increasing Sand SizeVelocity and Concentration Distributions in Sheet Flow above Plane BedsComputations of Total Sediment Discharge, Niobrara River near Cody, NebraskaField investigation of bedform morphodynamics under combined flowThe significance of superimposed dunes in the Amazon River: Implications for how large rivers are identified in the rock recordLaboratory studies of total load and apparent bed load9.10 Bedforms in Sand-Bedded RiversFlume Study of Silt Transportation and DepositionSummary of alluvial-channel data from Rio Grande conveyance channel, New Mexico, 1965-69The Northwest Atlantic Mid‐Ocean Channel of the Labrador Sea: II. Deposition of parallel laminated levee‐muds from the viscous sublayer of low density turbidity currentsBedform migration and bed‐load transport in some rivers and tidal environmentsThreshold for particle entrainment into suspensionSome aspects of the application of the theory of sediment transportation to engineering problemsMotion of Contact‐Load Particles at High Shear StressStacked fluvial and tide‐dominated estuarine deposits in high‐frequency (fourth‐order) sequences of the Eocene Central Basin, SpitsbergenVelocity and Concentration Profiles in Sheet-Flow Layer of Movable BedTransport Scaling of Dune Dimensions in Shallow Flows<i>In situ</i> measurements of fine sediment infiltration (FSI) in gravel‐bed rivers with a hydropeaking flow regimeBED MATERIAL TRANSPORT AND THE MORPHOLOGY OF ALLUVIAL RIVER CHANNELSTransportational cyclic steps created by flow over an erodible bed. Part 1. ExperimentsEfficient organic carbon burial in the Bengal fan sustained by the Himalayan erosional systemSedimentary facies of the tide-dominated paleo-Changjiang (Yangtze) estuary during the last transgressionSOME FLUME EXPERIMENTS WITH A FINE SILTLaboratory Study of Transport of Fine SandGeometry and dynamics of wave ripples in the nearshore zone of a coarse sandy beachOrigin of hummocky and swaley cross-stratification— The controlling influence of unidirectional current strength and aggradation rateExperiments on Oscillatory-Flow and Combined-Flow Bed Forms: Implications for Interpreting Parts of the Shallow-Marine Sedimentary RecordTransport of terrestrial organic carbon to the oceans by rivers: re-estimating flux- and burial ratesForms of Bed Roughness in Alluvial ChannelsBed configuration in steady unidirectional water flows; Part 2, Synthesis of flume dataFinite-amplitude river dunesFlume studies with fine and coarse sandsA Simple Universal Equation for Grain Settling VelocitySediment Transport, Part III: Bed forms and Alluvial RoughnessPalaeoproterozoic terrestrial sedimentation in the Beasley River Quartzite, lower Wyloo Group, Western AustraliaFlow, sediment transport and bedform dynamics over the transition from dunes to upper‐stage plane beds: implications for the formation of planar laminaeSticky stuff: Redefining bedform prediction in modern and ancient environmentsFacies architecture of individual basin‐plain turbidites: Comparison with existing models and implications for flow processesThe Transportation of Debris by Running WaterFlume width and water depth effects in sediment-transport experimentsUpper‐regime parallel lamination as the result of turbulent sediment transport and low‐amplitude bed formsIncipient sediment motion on non-horizontal slopesSediment Transport, Part II: Suspended Load TransportSediment Deposition from Turbidity Currents活発な浮遊砂を伴う小規模河床波の線形安定解析急勾配移動床流れにおける河床波の形状, 伝播特性砂れんと砂堆の発生領域についてEmplacement of massive deposits by sheet flowDigitized dataset from "Compilation of alluvial channel data : laboratory and field"
- 参照（URI）
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- 学術機関リポジトリデータベース雑誌記事索引データベースCrossref科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベース学術機関リポジトリデータベースCrossrefCrossref
- 書誌ID（NDLBibID）
- 12307834