The behavior of the trace elements and isotopic features are influenced in their turn by the phase equilibria, by the physical character of the partial melting and partial crystallization processes, and by the way in which a magma interacts with its wall rocks.
By studying the asymptotic behavior of the trace of the heat kernels, we see that, if the norm of the magnetic field diverges at infinity faster than the scalar potential, only the magnetic field contributes to the leading asymptotic and that only the scalar potential does if the opposite under mild conditions.
This study examined the morphology of the burrows and their associated lithofacies to interpret the environmental conditions under which they were produced as well as the behavior and identity of the trace maker.
How exactly does the causal mechanical model avoid the (disastrous) conclusion that any successful explanation of the behavior of the gas must trace the trajectories of individual molecules?
To characterize the behavior of anthropogenic trace substances within the urban water cycle, knowledge on the impact of natural and technical barriers is essential.
The results indicated that the behavior of toxic trace elements in river water are likely controlled by their interactions with particulate Fe, Al, and Ti compounds.
The co-deposition behavior of a trace of copper and zinc as an impurity in cyanide baths for silver plating was studied by means of a radioactive tracer.
We study the asymptotic behavior of the time delay (defined as the trace of the Eisenbud Wigner time delay operator) for scattering by potential and by magnetic field with two compact supports as the separation of supports goes to infinity.
Additionally, we reconstructed migratory behavior of the ancestors of Elaenia to trace the origin of austral long-distance migration in the genus and assess its role in the diversification of the genus.
In this study, we focus on the behavior of geogenic, toxic trace elements, particularly As, Cs, Cd, and Pb, during their transportation in two rivers for irrigation commonly used in monsoon Asia; one river originates from an active volcano, Mt. Asama, and the other originates from a currently inactive volcano, Yatsugatake Mountains in Nagano, Japan.
Formally, the robustness of the system is defined as: (4) where ϕ is the specification of the functionality in temporal logic and T p is the trace representing the behavior of the system under perturbation p. This notion of robustness corresponds to a mean functionality, that is, describes on average how the system behaves under perturbations.
