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Determination of an unknown source term temperature distribution for the sub-diffusion equation at the initial and final data of nonlocal sub-diffusion sources given by initial and finite temperature. Their mathematical statements
Subdiffusion of volcanic earthquakes is subdiffusive at both volcanoes. The aging phenomenon is commonly observed in the “event-time-averaged” mean
Subdiffusion of volcanic earthquakes is subdiffusive at both volcanoes. The aging phenomenon is commonly observed in the “event-time-averaged” mean
Maximum principle and its application for the nonlinear time-fractional diffusion equations with Cauchy-Dirichlet conditionsIn this paper, a maximum principle for the one-dimensional sub-diffusion equation with Atangana
Self-similar fluctuations in a turbulent plasma for the description of subdiffusive process.
Anomalous diffusion of volcanic earthquakes stochastic process exhibits a subdiffusive phenomenon. The jump probability distribution well obeys
Segmental Mean Square Displacement: Field-Cycling 1H Relaxometry vs Neutron Scattering to monitor the crossover in the segmental subdiffusion from the Rouse to the constrained Rouse regime
Segmental Mean Square Displacement: Field-Cycling 1H Relaxometry vs Neutron Scattering to monitor the crossover in the segmental subdiffusion from the Rouse to the constrained Rouse regime
Anomalous diffusion of volcanic earthquakes stochastic process exhibits a subdiffusive phenomenon. The jump probability distribution well obeys
Self-similar fluctuations in a turbulent plasma for the description of subdiffusive process.
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