Users may use the erosion rates option 3: Equation (E = A*Tau^NTau^n) and Bed Properties Using SEDB, BEDLAY, BEDBDN, and BEDDDN, if sediment core datasets are available in addition to the SEDFlume datasets (Figure 1). The sediment core samples present physical characteristics of sediment bed such as porosity, specific gravity, and grain size fractions with respect to sampling depths. Such sediment core samples are usually collected with much higher spatial density and much wider spatial coverage compared to SEDFlume samples. With the erosion rates option 3, the user can use sediment core datasets when configuring initial conditions for physical properties of sediment bed and, at the same time, use SEDFlume datasets when specifying erosion rate properties of sediment bed in the model.
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For erosion properties of sediment bed, the erosion rates option 3 employs the same approach as the erosion rates option 2. Specifically, the SEDFlume datasets provide the measurements of erosion rates (cm/s) as a function of applied shear stress (dynes/cm2), and the relationship between erosion rates and shear stress can be defined using Jones and Lick (2001)’s approach as:
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where E is erosion rate (cm/s), τb is bed shear stress (N/m2), τcr is critical shear stress (N/m2), and A and n are the fitted parameters based on the SEDFlume core data. With the erosion rates option 3, then, the SEDZLJ algorithm in EFDC+ computes the erosion rates using Equation (1) based on user-defined three erosion rate parameters (A, n, and τcr) and a maximum erosion rate (Emax), which are obtained from the SEDFlume study. The maximum erosion rate is employed for each bed layer in order to prevent the prediction of unrealistically high erosion rates, which might occur due to the exponential formulation of Equation (1) when a high shear stress is applied.
Figure 1 Selection of Erosion Rates Option 3: Equation (E = A*Tau^NTau^n) and Bed Properties Using SEDB, BEDLAY, BEDBDN, and BEDDDN - General Tab.
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Figure 2 Erosion Rates Option 3 - Initialization of Sediment Beds.
The Active and Deposited Sediments Erosion Matrix in Erosion Rate Matrix (cm/s) for Active & Deposited Sediment Bed in the Erosion Rates tab (Figure 3) is used as a lookup table for calculating erosion rates in active & deposition deposited bed layers as a function of their D50 size during the model simulation. The user may see that the first row of this matrix presents the Erosion Multiplier (A), Erosion Exponent (n), and Maximum Erosion Rate (cm/s). To fill this lookup table, the user may utilize the SEDFlume core test results or can adjust them manually for model calibration.
Note: The lookup table for critical shear stresses (τcr) in active & deposition deposited bed layers is specified in the Sediment Bed tap.
Figure 3 Erosion Rates Option 3 - Erosion Rates Tab.
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The user may enter the Number of SEDFlume Cores and then assign the measurements for physical and erosion properties associated with each core. For example, if the SEDFlume data consists of the measurements for three sediment cores, the user can set the Number of SEDFlume Cores as three, then the drop-down will be populated with three cores in the Sediment Erosion Bed Characteristics frame. The name of each core in the drop-down box can be modified by the user manually.
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In SEDFlume Measured Erosion Rates matrix, the user may enter the erosion properties measured from each SEDFlume core such as Erosion Multiplier (A), Erosion Exponent (Nn), and Maximum Erosion Rate (cm/s) for each vertical layer.
The sampling location of each SEDFlume core also needs to be entered in Easting (m) and Northing (m) Coordinates for utilizing the Core Assignment features of EFDC_Explorer.
Figure 4 Erosion Rates Option 3 - Core Definitions Tab.
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