scispace - formally typeset
J

Jean-Louis Rajot

Researcher at University of Paris

Publications -  110
Citations -  5173

Jean-Louis Rajot is an academic researcher from University of Paris. The author has contributed to research in topics: Mineral dust & Aeolian processes. The author has an hindex of 40, co-authored 108 publications receiving 4653 citations. Previous affiliations of Jean-Louis Rajot include Centre national de la recherche scientifique & Pierre-and-Marie-Curie University.

Papers
More filters
Journal ArticleDOI

Influence of shrubs on soil characteristics and their function in Sahelian agro-ecosystems in semi-arid Niger

TL;DR: In this paper, different shrub species in fallow sites following a gradient from 350-650 mm precipitation were examined and two different areas were distinguished: an area under the canopy of the shrubs and an area in the nearby open land.
Journal ArticleDOI

Characterization of iron oxides in mineral dust aerosols: Implications for light absorption

TL;DR: In this article, a volume fraction of iron oxides in aggregates was determined from measurements and significant differences in the single-scattering albedo, ω0, were found between hematite- and goethite-clay aggregates, although these calculations involved several important assumptions about the partition of hematites and Goethite in size-resolved aggregates.
Journal ArticleDOI

Measurement and data analysis methods for field‐scale wind erosion studies and model validation

TL;DR: In this paper, the authors outline important principles to consider in conducting large scale wind erosion studies and propose strategies of windblown sediment data collection for use in model validation and development, including consideration of sediment characteristics, sediment sampling, and meteorological stations.
Journal Article

Characterization of iron oxides in mineral dust aerosols : implications for light absorption (art. no. D21207)

TL;DR: In this article, a volume fraction of iron oxides in aggregates was determined from measurements and significant differences in the single-scattering albedo, ω0, were found between hematite- and goethite-clay aggregates, although these calculations involved several important assumptions about the partition of hematites and Goethite in size-resolved aggregates.