The phrase "available sediments" is correct and usable in written English.
It can be used in contexts related to geology, environmental science, or any field discussing sedimentary materials that can be accessed or utilized.
Example: "The researchers collected samples from the available sediments to analyze the historical climate data."
Alternatives: "accessible sediments" or "present sediments".
Because the simulation was a minimal model and used the simplest formulae and boundary condition, the main discussion will be restricted to the case of sparse available sediments.
Our computation shows that the mean annual discharge (RI = 2.33 yrs) can transport only 0to10%0% of the total available sediments.
A simple stochastic cellular automaton model is proposed for simulating bedload transport, especially for cases with a low transport rate and where available sediments are very sparse on substrates in a subaqueous system.
A few events are close to the bankfull level, but with a high return period (RI > 40 years), and therefore, not effective to transport most of the available sediments.
In the personal experience of the author, during preliminary runs and at early stages of actual runs of flume experiments for different purposes, it is often observed that sand patches occur with thin sand sheets under conditions of sparsely available sediments.
Halophila ovalis grows on a variety of substrates and is often the first to colonize newly available sediments [ 5, 17].
The available data demonstrates that the available sediment sources for the compared studied sites are similar.
Class interval size, sediment-rating curve fitting techniques, and available sediment data influence effective discharge results.
The initial state of the bed was almost flat, with some small random variation, for the available sediment (sand slabs), while the substrate was perfectly flat.
In comparable coastal environments with similar available sediment sources the tsunami size (represented as the tsunami run up height) is reflected in the resulting deposits.
The first step to understanding the evolution of the geomagnetic field over this time is the compilation and assessment of all available sediment records.
