The fact that ooids larger than 2 mm in diameter are moved along the sediment–water boundary in an otherwise low-energy setting is best explained by wandering dunes (bedform model, Anderson et al. 2020) interrupted by peak hydrodynamic levels assigned to punctuated storm events. A limited ...
Drought severity is determined by the boundary RDIst value: extremely dry (≤−2.00), severely dry (−1.5 to −1.99), moderately dry (−1 to −1.49), near normal (0.00 to −0.99), normal (0.99 to 0.00), moderately wet (1.49 to 1.00), very wet (1.99 to 1.5), and ...
To ensure consistency in ROI analysis and the minimization of spatial inhomogeneity effects (Figure S1, Supplementary Materials), only the periphery calf muscle inferior to the fibula bone in the central seven slices was studied (starting with the second slice), with the ROI upper boundary defined...
In general, an increase in the transverse gradient is the result of adverse water and sediment conditions combined with boundary conditions [14]. Changes in water and sediment conditions are the primary reasons for a significant increase in the transverse gradient, while human activities within the ...
Assuming fast grain boundary diffusion and mass conservation, the diffusive exchange between the two minerals can be written as(A.2)ϕplgDplgjLplg∂Cplgj∂r|r=Lplg=ϕcpxDcpxjLcpx∂Ccpxj∂r|r=Lcpx, where ϕ denotes the mineral modal abundance, and L is the effective grain ...