Titlebook: Ice Core Studies of Global Biogeochemical Cycles; Robert J. Delmas Conference proceedings 1995 Springer-Verlag Berlin Heidelberg 1995 Aero

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H2O2 and HCHO in Polar Snow and Their Relation to Atmospheric Chemistry,nd ice cores is limited by our lack of understanding of the atmosphere-snow transfer functions for the two species. Continuous H.O. records going back into the last century have been obtained from Dye 3 and Summit in central Greenland and Siple in west Antarctica, with some measurements preserved ba

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Combustion Carbonaceous Aerosols in the Atmosphere: Implications for Ice Core Studies,articulate phase. Hese particles are primarily composed of a carbonaceous (organic and/or soot carbon) core which has been rapidly coated by hydrophilic substances formed by numerous interactions with other gaseous airborne substances; the most important of such reactions is the oxidative conversion

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Boreal Biomass Burning Over the Last 80 Years Recorded in a Summit-Greenland Ice Core,, SO.. and C.O..) has been achieved along a 32.7-m-depth firn Summit (Central Greenland) core which spans the 1908–1989 time period. One of the noticeable feature of these chemical records is the frequent presence of narrow ammonium-rich snow layers in which enhanced concentrations of formate, glyco

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L. A. Barried the most artifact-free. Baby machines incubate “mother cells” under normal conditions and collects their “babies,” producing cell cultures that are similar not only in cell cycle phase but also in age. Several macroscale and microfluidic baby machines have been applied to synchronized cell researc

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