scispace - formally typeset
M

M. Mingarro

Researcher at Complutense University of Madrid

Publications -  24
Citations -  540

M. Mingarro is an academic researcher from Complutense University of Madrid. The author has contributed to research in topics: Diffusion (business) & Sorption. The author has an hindex of 12, co-authored 23 publications receiving 453 citations.

Papers
More filters
Journal ArticleDOI

Role of bentonite colloids on europium and plutonium migration in a granite fracture

TL;DR: In this article, the effects of the presence of bentonite colloids on the migration of highly sorbing elements, such as Eu and Pu, in a granite environment were investigated.
Journal ArticleDOI

Diffusion coefficients and accessible porosity for HTO and 36Cl in compacted FEBEX bentonite

TL;DR: In this article, the authors compared the behavior of the conservative anionic species 36Cl− with HTO (neutral and conservative tracer, tritiated water) in a wide range of clay dry densities.
Journal ArticleDOI

Inverse modeling of tracer experiments in FEBEX compacted Ca-bentonite

TL;DR: In this paper, the authors present the numerical interpretation of diffusion and permeation experiments by solving the inverse transport problem which is formulated as the minimization of a weighted least squares criterion measuring the differences between computed and measured concentration values.
Journal ArticleDOI

Solute transport properties of compacted Ca-bentonite used in FEBEX project

TL;DR: Experiments were carried out using compacted FEBEX bentonite, which is the reference material for the Spanish concept of radioactive waste disposal, and were interpreted by means of available analytical solutions that allow the estimation of diffusion coefficients and, in some cases, distribution coefficients.
Journal ArticleDOI

DI-B experiment: planning, design and performance of an in situ diffusion experiment in the Opalinus Clay formation

TL;DR: The DI-B experiment is a long-term, natural-scale, in situ diffusion experiment, which is being performed in the Opalinus Clay formation at the Mont Terri Underground Rock Laboratory (URL), in Switzerland, employing nonradioactive tracers as mentioned in this paper.