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suspension
Turbidity currents regulate the transport and settling of microplastics in a deep-sea submarine canyon
Coupled channel–floodplain dynamics and resulting stratigraphic architecture viewed through a mass-balance lens
Magma / Suspension Rheology
Frictional Melting in Magma and Lava
Microstructure and Time-Dependent Behavior of STx-1b Calcium Montmorillonite Suspensions
Abstract Particle-laden flows or turbidity currents along the seafloor are important to the formation and erosion of submarine topography. To understand the mass-transport process, flume tests were carried out with a continuous supply of quartz-laden suspension. The vertical and horizontal velocities were extracted by two pairs of ultrasound Doppler velocity profilers installed at different angles with respect to the bed-normal direction. Due to the head intrusion into the ambient water, the sediment in the suspension was continuously lifted up and mixed, leaving lobes and clefts. The velocity-maximum layer acted as the main sediment conveyor and divided the body into wall and jet regions. The concentration distribution was also quantified based on the relationship between the fluid density and the intensity of light attenuation obtained using a video recording. An area of high sediment concentration was observed just behind the head frontal area. Analysis of the velocity and concentration distribution demonstrated that sediment in the turbidity current was transported mainly by head movement and that continuous sedimentation took place in the wall region. The results indicate that a turbidity current proceeds while maintaining an ordered inner dynamic structure.
LOW-FREQUENCY ELECTRICAL CONDUCTIVITY OF AQUEOUS KAOLINITE SUSPENSIONS II: COUNTERION EFFECTS AND ESTIMATING STERN LAYER MOBILITIES OF COUNTERIONS
The Effect of Clay Type On the Properties of Cohesive Sediment Gravity Flows and Their Deposits
Low-frequency electrical conductivity of aqueous kaolinite suspensions: surface conductance, electrokinetic potentials and counterion mobility
Flow Behavior of Ponded Turbidity Currents
THE ROLE OF MONO- AND DIVALENT IONS IN THE STABILITY OF KAOLINITE SUSPENSIONS AND FINE TAILINGS
High-Density Mud Suspensions and Cross-Shelf Transport: On the Mechanism of Gelling Ignition
In situ High-Temperature Experiments
Isotropic/nematic and sol/gel transitions in aqueous suspensions of size selected nontronite NAu1
Experimental Deposition of Carbonate Mud From Moving Suspensions: Importance of Flocculation and Implications For Modern and Ancient Carbonate Mud Deposition
DYNAMIC RHEOLOGICAL PROPERTIES OF SODIUM PYROPHOSPHATE-MODIFIED BENTONITE SUSPENSIONS FOR LIQUEFACTION MITIGATION
Deflocculant consumption of clay suspensions as a function of specific surface area and cation exchange capacity
Fluvial features on Titan: Insights from morphology and modeling
Abstract Organo-clay fabric and physico-chemistry of marine mud play important roles in early sediment diagenesis including the development of mass physical properties, consolidation behavior, and sequestration of organic matter (OM) in sediments over geologic time. Transmission electron microscopy (TEM) images of nano- and microfabric reveal that organic matter is sequestered following enzymatic digestion despite the pervasive openness of pore-fluid pathways observed in 3D rotated images. The locations of sequestered organic matter correspond to those predicted by modeling of the potential energy of interaction. Initial flume experiments on high porosity clay-mineral-rich mud deposited under dynamic flow and static (vertical settlement) conditions demonstrate differences in clay fabric and the distribution of organic matter (we define the term organo-clay fabric as the contiguous association and arrangement of organic matter and clay domains). These differences in organo-clay fabric impact the preservation-degradation mechanisms and dynamics during depositional and burial processes. Organo-clay fabric and physico-chemical modeling of potential energy fields coupled with direct observations of organo-clay fabric, three-dimensional (3-D) clay fabric reconstructions, sediment static and dynamic properties, and controlled flume experiments are providing new insight into the developmental history of sedimentary sequences, nano- to macroscale environmental processes, and diagenesis from unconsolidated mud to shale.