We investigate the spatiotemporal nonlocality underlying fractional-derivative models as a
possible explanation for regional-scale anomalous dispersion with heavy tails. Properties of …

Temporary storage of solutes in streams is often controlled by flow‐induced uptake in
hyporheic zones. This phenomenon accounts for the tails that are generally observed …

Numerical schemes and stability criteria are developed for solution of the one-dimensional
fractional advection-dispersion equation (FRADE) derived by revising Fick's first law …

In the present research, neuro-fuzzy-based group method of data handling (NF-GMDH) has
been applied to evaluate the longitudinal dispersion coefficient in rivers. The NF-GMDH …

The longitudinal dispersion coefficient is a key parameter in determining the distribution of
pollution concentration, especially in temporally time-varying source cases after full cross …

Laboratory experiments are presented that model the exchange processes between a river
and dead-water zones created by groin fields. The measurement methods include particle …

Using a new channel shape equation for straight channels and a more versatile channel
shape or local flow depth equation for natural streams a method is developed for prediction …

Theoretical methods have been developed to estimate the longitudinal dispersion
coefficients (k) in natural rivers. The triple integral expression for longitudinal dispersion …

In this work, we compare solute transport and hyporheic exchange in vegetated and
unvegetated reaches of Säva Brook, an agricultural stream in Sweden subject to extreme …

Researchers must determine the storage parameter values to understand the storage
processes and compare them across streams. These parameters are highly variable in time …