0000000000562995

AUTHOR

Alain Durand

showing 5 related works from this author

Biogeochemical Cycle of Silica in an Apolyhaline Interdunal Holocene Lake (Chad, N'Guigmi Region, Niger)

1999

During the Holocene, the apolyhaline conditions in interdunal ephemeral lakes in the Lake Chad region led to various diagenetic processes, which resulted in: (a) clay authigenesis, (b) organic matter lithification (plants and cyanobacterial mats), (c) precipitation of sodium silicate (magadiite, kenyaite, zeolite), and (d) chert neoformation. Each step in this diagenetic process involves silica, which can be highly mobile under such conditions. Therefore, the paleoenvironmental variations can be investigated using the Si cycle.http://link.springer. de/link/service/journals/00114/bibs/9086010/90860475.htm</HEA

chemistry.chemical_classificationBiogeochemical cycleEcologyEphemeral keyGeochemistrySodium silicateGeneral MedicineDiagenesischemistry.chemical_compoundchemistryOrganic matterPrecipitationLithificationEcology Evolution Behavior and SystematicsHoloceneGeologyNaturwissenschaften
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Quasi-decadal signals of Sahel rainfall and West African monsoon since the mid-twentieth century

2013

[1] Sahel rainfall shows pronounced decadal variability and a negative trend between wet conditions in the 1950s–1960s and dry ones in the 1970s–1980s. Using continuous wavelet transform, the quasi-decadal variability (QDV) of rainfall reveals zonal contrasts. The highest QDV is identified in the 1950s–1960s over western Sahel and in the 1970s–1980s over eastern Sahel. The quasi-decadal atmospheric anomalies have been reconstructed using Fourier transform for the 1950s–1960s and the 1970s–1980s, respectively, and assessed by the composite analysis of the QDV phases for the periods before and after 1968. Over western Sahel, the rainfall QDV in the 1950s–1960s is related to the North Atlantic…

Atmospheric Science010504 meteorology & atmospheric sciencesWavelet coherenceIntertropical Convergence Zone0207 environmental engineering02 engineering and technologySubtropicsMonsoon01 natural sciencesTroposphereSea surface temperatureWest africanGeophysics13. Climate actionSpace and Planetary ScienceClimatologyEarth and Planetary Sciences (miscellaneous)Moisture convergence020701 environmental engineeringGeology0105 earth and related environmental sciencesJournal of Geophysical Research: Atmospheres
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The natural hydrous sodium silicates from the northern bank of Lake Chad : occurrence, petrology and genesis

2005

Abstract Hydrous sodium silicates sometimes associated with zeolites, form in an alkaline environment, in which there is a high concentration of dissolved silica. Such an environment existed during the Holocene in N'Guigmi interdunal depressions (Lake Chad), which led to the precipitation of various types of hydrous sodium silicates, including magadiite, kenyaite, and zeolites. Scanning electron and optical microscope observations allow several microstructures to be distinguished. These microstructures result from either precipitation sequences or a transformation along a diagenetic gradient. New petrological, microstructural and geochemical data confirm the transformation of magadiite into…

Dissolved silicaStratigraphySodiumGeochemistrychemistry.chemical_elementMineralogyGeologyDebrisDiagenesischemistrySilicate mineralsSedimentary rockPrecipitationHoloceneGeology
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Evolution des paysages Sahélines au cours des six dernières décennies dans la région de Niamey : de la disparition de la brousse tigrée à l'encroutem…

2010

In the Sahel, the rapid increase of the population during the last decades and the climate variation lead to an important environmental degradation. This work aims to measure the impacts of the human pressure on ecosystem during the six last decades. A diachronic cartography of a 100 km² area close to Niamey was done with aerial photographs (1950 and 1975) and GPS measurements (2009). Results showed that the tiger bush vegetation was completely cleared between 1950 and 2009 while the fallow decreases from 7 % to 1 %. In the sandy valley, the increase of cultivated fields from 20,7 % (1950) to 69,4 % (1975) favoured wind and water erosions which allowed surface soil crusting. Between 1975 an…

région de Niameyhuman pressureaerial photographsphotos aériennesSahel[SDU.STU] Sciences of the Universe [physics]/Earth Sciencessoil crustingsoils degradation[SDU.STU]Sciences of the Universe [physics]/Earth Sciencesdégradation des solspression anthropiqueencroûtement SahelNiame
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Nuclear magnetic resonance spectroscopy of phosphorus in Becker's dystrophy

1991

[INFO.INFO-IM] Computer Science [cs]/Medical Imaging
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