All Stories

  1. On the dynamics of aligned inertial particles settling in a quiescent, stratified two-layer medium
  2. Decadal evolution of fluvial islands and its controlling factors along the lower Yangtze River
  3. Morphodynamics and depositional architecture of mid‐channel bars in large Amazonian rivers
  4. Controls on the Leeside Angle of Dunes in Shallow Unidirectional Flows
  5. River Damming Impacts on Fish Habitat and Associated Conservation Measures
  6. On the origin of chevron marks and striated grooves, and their use in predicting mud bed rheology
  7. On the settling of aligned spherical particles in various quiescent media
  8. Shifted sediment-transport regimes by climate change and amplified hydrological variability in cryosphere-fed rivers
  9. Field Evidence for the Initiation of Isolated Aeolian Sand Patches
  10. The Paraná River in the argentine plain: A review of its evolution and contemporary characteristics
  11. On the submerged low-Cauchy-number canopy dynamics under unidirectional flows
  12. Effects of low clay concentrations on nearly isotropic turbulence
  13. Beyond just floodwater
  14. How Do Vulnerable People in Bangladesh Experience Environmental Stress From Sedimentation in the Haor Wetlands? An Exploratory Study
  15. The dynamic floor of Yellowstone Lake, Wyoming, USA: The last 14 k.y. of hydrothermal explosions, venting, doming, and faulting
  16. Amplification of downstream flood stage due to damming of fine-grained rivers
  17. Sand mining impact on Poyang Lake: a case study based on high-resolution bathymetry and sub-bottom data
  18. The morphology of fluvial‐tidal dunes: Lower Columbia River, Oregon/Washington, USA
  19. Sedimentary pyrite in carbonaceous shales of the Mamfe Cretaceous basin, SW Cameroon: Morphologies, composition, pyrite framboid size frequency distribution, and formation pathways
  20. Topographic perturbation of turbulent boundary layers by low‐angle, early‐stage aeolian dunes
  21. On the turbulence dynamics induced by a surrogate seagrass canopy
  22. The Influence of Three‐Dimensional Topography on Turbulent Flow Structures Over Dunes in Unidirectional Flows
  23. Sand, gravel, and UN Sustainable Development Goals: Conflicts, synergies, and pathways forward
  24. Unsteady dynamics of turbulent flow in the wakes of barchan dunes modulated by overlying boundary-layer structure
  25. Correction to: The mysterious grooves of Volcán Bárcena: a review of the role of streamwise counter-rotating vortices during erosion by dilute pyroclastic density currents
  26. The mysterious grooves of Volcán Bárcena: a review of the role of streamwise counter-rotating vortices during erosion by dilute pyroclastic density currents
  27. The Effect of Biofilms on Turbulent Flow Over Permeable Beds
  28. Using multibeam backscatter strength to analyze the distribution of manganese nodules: A case study of seamounts in the Western Pacific Ocean
  29. The sedimentary architecture of hyperpycnites produced by transient turbulent flows in a shallow lacustrine environment
  30. Rapid gravity flow transformation revealed in a single climbing ripple
  31. Interpreting pre-vegetation landscape dynamics: The Cambrian Lower Mount Simon Sandstone, Illinois, U.S.A.
  32. Influence of Dunes on Channel‐Scale Flow and Sediment Transport in a Sand Bed Braided River
  33. Why do large, deep rivers have low-angle dune beds?: COMMENT
  34. Alluvial architecture of mid‐channel fluvial–tidal barforms: The mesotidal Lower Columbia River, Oregon/Washington, USA
  35. Dune-scale cross-strata across the fluvial-deltaic backwater regime: Preservation potential of an autogenic stratigraphic signature
  36. The Pace of Human-Induced Change in Large Rivers: Stresses, Resilience, and Vulnerability to Extreme Events
  37. Source apportionment of soil heavy metals in fluvial islands, Anhui section of the lower Yangtze River: comparison of APCS–MLR and PMF
  38. An integrated process‐based model of flutes and tool marks in deep‐water environments: Implications for palaeohydraulics, the Bouma sequence and hybrid event beds
  39. Drainage and erosion of Cambodia’s great lake in the middle-late Holocene: The combined role of climatic drying, base-level fall and river capture
  40. Novel Environment Enables PIV Measurements of Turbulent Flow around and within Complex Topographies
  41. Soft-sediment deformation structures as indicators of tectono-volcanic activity during evolution of a lacustrine basin: A case study from the Upper Triassic Ordos Basin, China
  42. Secondary Flows and Vortex Structure Associated With Isolated and Interacting Barchan Dunes
  43. Dunes in the world’s big rivers are characterized by low-angle lee-side slopes and a complex shape
  44. Experimental evidence of amplitude modulation in permeable-wall turbulence
  45. River bank instability from unsustainable sand mining in the lower Mekong River
  46. River temperature and the thermal-dynamic transport of sediment
  47. Time is running out for sand
  48. Spatial Scales of Turbulent Flow Structures Associated With Interacting Barchan Dunes
  49. Small- and large- scale soft-sediment deformations in a Triassic lacustrine delta caused by overloading and seismicity in the Ordos Basin, central China
  50. PIV measurements of turbulent flow overlying large, cubic- and hexagonally-packed hemisphere arrays
  51. Observations and scaling of tidal mass transport across the lower Ganges–Brahmaputra delta plain: implications for delta management and sustainability
  52. Author Correction: Anthropogenic stresses on the world’s big rivers
  53. Quantification of bedform dynamics and bedload sediment flux in sandy braided rivers from airborne and satellite imagery
  54. Sedimentologic and palaeoenvironmental evolution of the Mamfe Cretaceous Basin (SW Cameroon): Evidence from lithofacies analysis, tectonics and evaporite minerals suite
  55. Describing fluvial systems: linking processes to deposits and stratigraphy
  56. Anthropogenic stresses on the world’s big rivers
  57. Hydrodynamic modelling of tidal-fluvial flows in a large river estuary
  58. On the Causes of Pulsing in Continuous Turbidity Currents
  59. Experimental study of turbulent flow over and within cubically packed walls of spheres: Effects of topography, permeability and wall thickness
  60. The adaptation of dunes to changes in river flow
  61. The Impact of Nonequilibrium Flow on the Structure of Turbulence Over River Dunes
  62. Turbulent Flow Structure Associated With Collision Between Laterally Offset, Fixed-Bed Barchan Dunes
  63. The sedimentology of river confluences
  64. Early burial mud diapirism and its impact on stratigraphic architecture in the Carboniferous of the Shannon Basin, County Clare, Ireland
  65. ‘Boundary’: mapping and visualizing climatically changed landscapes at Kaskawulsh Glacier and Kluane Lake, Yukon
  66. Turbulence Links Momentum and Solute Exchange in Coarse-Grained Streambeds
  67. The significance of superimposed dunes in the Amazon River: Implications for how large rivers are identified in the rock record
  68. The influence of tributary flow density differences on the hydrodynamic behavior of a confluent meander bend and implications for flow mixing
  69. Linking the local vertical variability of permeability and porosity to newly-interpreted lithofacies in the lower Mt. Simon CO2 reservoir
  70. The planform mobility of river channel confluences: Insights from analysis of remotely sensed imagery
  71. An evaluation of the use of a multibeam echo-sounder for observations of suspended sediment
  72. The influence of flow discharge variations on the morphodynamics of a diffluence-confluence unit on a large river
  73. Length scales and statistical characteristics of outer bank roughness for large elongate meander bends: The influence of bank material properties, floodplain vegetation and flow inundation
  74. River piracy and drainage basin reorganization led by climate-driven glacier retreat
  75. A numerical investigation into the importance of bed permeability on determining flow structures over river dunes
  76. Cavitation erosion of bedrock channels
  77. Extreme flood-driven fluvial bank erosion and sediment loads: direct process measurements using integrated Mobile Laser Scanning (MLS) and hydro-acoustic techniques
  78. Three-dimensional flow structure and bed morphology in large elongate meander loops with different outer bank roughness characteristics
  79. Fluvial sediment supply to a mega-delta reduced by shifting tropical-cyclone activity
  80. Comparing the transitional behaviour of kaolinite and bentonite suspension flows
  81. On the evolution and form of coherent flow structures over a gravel bed: Insights from whole flow field visualization and measurement
  82. The alluvial architecture of a suspended sediment dominated meandering river: the Río Bermejo, Argentina
  83. Bedform genesis in bedrock substrates: Insights into formative processes from a new experimental approach and the importance of suspension-dominated abrasion
  84. Spatial variability in bank resistance to erosion on a large meandering, mixed bedrock-alluvial river
  85. Modulation of outer bank erosion by slump blocks: Disentangling the protective and destructive role of failed material on the three-dimensional flow structure
  86. The role of discharge variability in determining alluvial stratigraphy
  87. Extremes in dune preservation: Controls on the completeness of fluvial deposits
  88. Predicting bedforms and primary current stratification in cohesive mixtures of mud and sand
  89. Fluvio-deltaic avulsions during relative sea-level fall
  90. Grain-Size Controls On the Morphology and Internal Geometry of River-Dominated Deltas
  91. Mid to late Holocene geomorphological and sedimentological evolution of the fluvial–tidal zone
  92. Preface
  93. Bed form genesis from bed defects under unidirectional, oscillatory, and combined flows
  94. Effect of bed permeability and hyporheic flow on turbulent flow over bed forms
  95. A unified model for bedform development and equilibrium under unidirectional, oscillatory and combined-flows
  96. The impact of significant input of fine sediment on benthic fauna at tributary junctions: a case study of the Bermejo-Paraguay River confluence, Argentina
  97. A New Phase Diagram for Combined-Flow Bedforms
  98. Scales and causes of heterogeneity in bars in a large multi-channel river: Río Paraná, Argentina
  99. Flow structure and channel morphodynamics of meander bend chute cutoffs: A case study of the Wabash River, USA
  100. Coherent Flow Structures at Earth's Surface
  101. LES of barchan dunes
  102. Paragenetic sequences of carbonate and sulphide minerals of the Mamfe Basin (Cameroon): Indicators of palaeo-fluids, palaeo-oxygen levels and diagenetic zones
  103. A flume experiment on the effect of channel width on the perturbation and recovery of flow in straight pools and riffles with smooth boundaries
  104. Discrimination of bed form scales using robust spline filters and wavelet transforms: Methods and application to synthetic signals and bed forms of the Río Paraná, Argentina
  105. Decimeter-scale in situ mapping of modern cross-bedded dune deposits using parametric echo sounding: A new method for linking river processes and their deposits
  106. Monitoring the generation and evolution of the sediment plume behind towed fishing gears using a multibeam echosounder
  107. Three-dimensional gravity-current flow within a subaqueous bend: Spatial evolution and force balance variations
  108. Deposits of the sandy braided South Saskatchewan River: Implications for the use of modern analogs in reconstructing channel dimensions in reservoir characterization
  109. Velocity Mapping Toolbox (VMT): a processing and visualization suite for moving-vessel ADCP measurements
  110. Bedforms: views and new perspectives from the third international workshop on Marine and River Dune Dynamics (MARID3)
  111. Application of a roughness-length representation to parameterize energy loss in 3-D numerical simulations of large rivers
  112. Flow fields, bed shear stresses, and suspended bed sediment dynamics in bifurcations of a large river
  113. Quantification of the relation between surface morphodynamics and subsurface sedimentological product in sandy braided rivers
  114. Modelling hydrodynamics in the Rio Paraná, Argentina: An evaluation and inter-comparison of reduced-complexity and physics based models applied to a large sand-bed river
  115. Mitigating land loss in coastal Louisiana by controlled diversion of Mississippi River sand
  116. Tributary, distributary and other fluvial patterns: What really represents the norm in the continental rock record?
  117. Sediment mobility and bed armoring in the St Clair River: insights from hydrodynamic modeling
  118. A versatile refractive-index-matched flow facility for studies of complex flow systems across scientific disciplines
  119. Quantifying the dynamics of flow within a permeable bed using time-resolved endoscopic particle imaging velocimetry (EPIV)
  120. An experimental study of discharge partitioning and flow structure at symmetrical bifurcations
  121. Extreme sediment pulses generated by bend cutoffs along a large meandering river
  122. Bed morphology, flow structure, and sediment transport at the outlet of Lake Huron and in the upper St. Clair River
  123. Depositional processes, bedform development and hybrid bed formation in rapidly decelerated cohesive (mud-sand) sediment flows
  124. Particle-image velocimetry measurements of flow over interacting barchan dunes
  125. Wavelets Application to Study the Bedforms of Parana River
  126. Evolution and sedimentology of a channel fill in the sandy braided South Saskatchewan River and its comparison to the deposits of an adjacent compound bar
  127. Sedimentation in deep-sea lobe-elements: implications for the origin of thickening-upward sequences
  128. Preface to Decadal Issue
  129. On determining the geometric and kinematic characteristics of coherent flow structures over a gravel bed: a new approach using combined PLIF-PIV
  130. Fluvial form in modern continental sedimentary basins: Distributive fluvial systems: COMMENT
  131. Coherent flow structures in a depth-limited flow over a gravel surface: The influence of surface roughness
  132. Can we distinguish flood frequency and magnitude in the sedimentological record of rivers?
  133. Response of river-dominated delta channel networks to permanent changes in river discharge
  134. Quantification of braided river channel change using archival digital image analysis
  135. A new methodology for the quantitative visualization of coherent flow structures in alluvial channels using multibeam echo-sounding (MBES)
  136. On the relationship between flow and suspended sediment transport over the crest of a sand dune, Río Paraná, Argentina
  137. Monitoring Suspended Sediment Dynamics Using MBES
  138. The influence of dunes on mixing in a migrating salt-wedge: Fraser River estuary, Canada
  139. Suspended sediment transport and deposition over a dune: Río Paraná, Argentina
  140. The Sedimentology and Alluvial Architecture of a Large Braid Bar, Rio Parana, Argentina
  141. Morphology, flow structure, and suspended bed sediment transport at two large braid-bar confluences
  142. A Phase Diagram for Turbulent, Transitional, and Laminar Clay Suspension Flows
  143. A pilot study of the efficacy of residuum lodges for managing sediment delivery to impoundment reservoirs
  144. Coherent flow structures in a depth-limited flow over a gravel surface: The role of near-bed turbulence and influence of Reynolds number
  145. Discussion of “Transition from Ripples to Dunes” by Arved J. Raudkivi
  146. River response to lateral ground tilting: a synthesis and some implications for the modelling of alluvial architecture in extensional basins
  147. Causes of rapid mixing at a junction of two large rivers: Río Paraná and Río Paraguay, Argentina
  148. The dynamics of turbulent, transitional and laminar clay-laden flow over a fixed current ripple
  149. Reply to Discussion of Imran et al. on “The orientation of helical flow in curved channels” by Corney et al., Sedimentology, 53, 249-257
  150. Comparison of Fixed- and Moving-Vessel Flow Measurements with an aDp in a Large River
  151. The influence of scale, slope and channel geometry on the flow dynamics of submarine channels
  152. The relationship between channel avulsion, flow occupancy and aggradation in braided rivers: insights from an experimental model
  153. Meander-Bend Evolution, Alluvial Architecture, and the Role of Cohesion in Sinuous River Channels: A Flume Study
  154. Dynamics of a river channel confluence with discordant beds: Flow turbulence, bed load sediment transport, and bed morphology
  155. Electrical Resistance Tomography for Suspended Sediment Measurements in Open Channel Flows Using a Novel Sensor Design
  156. Bar-top hollows: A new element in the architecture of sandy braided rivers
  157. Flow structure in sinuous submarine channels: Velocity and turbulence structure of an experimental submarine channel
  158. Mean flow, turbulence structure, and bed form superimposition across the ripple-dune transition
  159. The orientation of helical flow in curved channels
  160. The sedimentology and alluvial architecture of the sandy braided South Saskatchewan River, Canada
  161. Bed forms in bimodal sand-gravel sediments: laboratory and field analysis
  162. Form roughness and the absence of secondary flow in a large confluence–diffluence, Rio Paraná, Argentina
  163. Morphology and flow fields of three-dimensional dunes, Rio Paraná, Argentina: Results from simultaneous multibeam echo sounding and acoustic Doppler current profiling
  164. The fluid dynamics of river dunes: A review and some future research directions
  165. Response of sand dunes to variations in tidal flow: Fraser Estuary, Canada
  166. Development and testing of a numerical code for treatment of complex river channel topography in three-dimensional CFD models with structured grids
  167. Measuring flow velocity and sediment transport with an acoustic Doppler current profiler
  168. Whole flow field dynamics and velocity pulsing within natural sediment-laden underflows
  169. Sedimentology and kinematics of a large, retrogressive growth-fault system in Upper Carboniferous deltaic sediments, western Ireland
  170. Measuring Velocity and Shear Stress over Dunes with Acoustic Doppler Profiler
  171. Relationship between sediment supply and avulsion frequency in braided rivers
  172. Three-Dimensional Sedimentary Architecture of a Large, Mid-Channel Sand Braid Bar, Jamuna River, Bangladesh
  173. Sedimentology of the Bengal shelf, Bangladesh: comparison of late Miocene sediments, Sitakund anticline, with the modern, tidally dominated shelf
  174. The use and application of GPR in sandy fluvial environments: methodological considerations
  175. The physical scale modelling of braided alluvial architecture and estimation of subsurface permeability
  176. Computational fluid dynamics and the physical modelling of an upland urban river
  177. Turbulence Modulation in Clay-Rich Sediment-Laden Flows and Some Implications for Sediment Deposition
  178. Quantitative visualization of flow fields associated with alluvial sand dunes: Results from the laboratory and field using ultrasonic and acoustic doppler anemometry
  179. Turbulence and Coherent Flow Structures Associated with Bedform Amalgamation: An Experimental Study of the Ripple-Dune Transition
  180. Ripple formation induced by biogenic mounds—comment
  181. Morphological evolution and dynamics of a large, sand braid-bar, Jamuna River, Bangladesh
  182. The Western Irish Namurian Basin reassessed
  183. Turbulence and Secondary Flow over Sediment Stripes in Weakly Bimodal Bed Material
  184. Three-dimensional structure of flow at a confluence of river channels with discordant beds
  185. Fluid and sediment dynamics of upper stage plane beds
  186. Scour in large braided rivers and the recognition of sequence stratigraphic boundaries
  187. Discussion and Closure: Bed-Load Motion at High Shear Stress: Dune Washout and Plane-Bed Flow
  188. Preservation of planar laminae due to migration of low-relief bed waves over aggrading upper-stage plane beds: comparison of experimental data with theory
  189. Effects of Bed Discordance on Flow Dynamics at Open Channel Confluences
  190. Turbulent flow structure at concordant and discordant open-channel confluences
  191. A scheme for resampling, filtering, and subsampling unevenly spaced laser Doppler anemometer data
  192. Mean flow and turbulence structure over fixed, two-dimensional dunes: implications for sediment transport and bedform stability
  193. Particle Size and Velocity Discrimination in a Sediment-Laden Turbulent Flow Using Phase Doppler Anemometry
  194. Three-Dimensional Flow Structure at Open-Channel Diversions
  195. Effect of Orientation and Size of Helley‐Smith Sampler on Its Efficiency
  196. On experimental reflected density currents and the interpretation of certain turbidites
  197. Drag reduction in turbulent muddy seawater flows and some sedimentary consequences
  198. Bed morphology and sedimentology at the confluence of unequal depth channels
  199. Braided rivers: perspectives and problems
  200. Mechanisms of anabranch avulsion within gravel-bed braided rivers: observations from a scaled physical model
  201. On the entrainment of sediment and initiation of bed defects: insights from recent developments within turbulent boundary layer research
  202. The morphology and dynamics of low amplitude bedwaves upon upper stage plane beds and the preservation of planar laminae
  203. Discussion of “ Development of Bed Features ” by Arved J. Raudkivi and Hans‐H. Witte (September, 1990, Vol. 116, No. 9)
  204. Sedimentology and event timing of a catastrophic volcaniclastic mass flow, Volcan Hudson, Southern Chile
  205. Mixing-layer distortion at the confluence of channels of different depth
  206. REPLY
  207. Fluidization pipes in volcaniclastic mass flows, Volcan Hudson, Southern Chile
  208. Earthquakes, Rivers and Ice: Scientific Research at the Laguna San Rafael, Southern Chile, 1986
  209. Flow, sediment transport and bedform dynamics over the transition from dunes to upper-stage plane beds: implications for the formation of planar laminae
  210. Sediment transport and bed morphology at river channel confluences
  211. Closure to “Separation Zone at Open‐Channel Junctions” by James L. Best and Ian Reid (November, 1984)
  212. The morphology of river channel confluences
  213. Flow separation—a physical process for the concentration of heavy minerals within alluvial channels
  214. Separation Zone at Open‐Channel Junctions