PubMed · 9068363
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J E Burns. 1996. Equivalent half-value layers.. https://pubmed.ncbi.nlm.nih.gov/9068363/
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On the basis of anomalous isotopic compositions of oxygen and magnesium, 14 oxide grains from two primitive meteorites (Bishunpur and Semarkona) have been identified as circumstellar condensates. One corundum grain has a high 18O/16O ratio and isotopic compositions of magnesium, calcium, and titanium that are compatible with a formation in ejecta of a type II supernova that was about 15 times the mass of the sun. The other grains have oxygen, magnesium, and titanium compositions that are consistent with a formation around asymptotic giant branch (AGB) stars with a range of mass and initial composition. The large range of aluminum/magnesium in circumstellar corundum and spinel is considered to reflect various stages of back-reaction between condensed corundum and gaseous magnesium in cooling stellar ejecta.
In an oxisol-spodosol system developed on the terrestrial surface of the lower Tapajós Valley, the determination of total mercury (Hg), organic carbon (C), iron and aluminum oxy-hydroxide (Fe(cdb) and Al(cdb)) concentrations in the surface soil horizons are used to characterise the geochemical processes controlling the accumulation of Hg in soils under natural vegetation cover and in deforested and cultivated sites. Oxisols from the plateau have homogeneous and relatively high background Hg contents and burdens constituting an important natural reservoir of Hg for the region (90-210 ng/g dry wt. and 19-33 mg/m2 for the first 20 cm). The Fe(cdb) and Al(cdb) contents associated with the fine fraction (< 63 microns) of the soil suggest that oxy-hydroxides and, particularly Al-substituted Fe oxy-hydroxides, control the Hg concentrations observed in all of the soils of the study region. Consequently, the geochemistry of these minerals along the slopes governs the accumulation or the release of the Hg according to the natural evolution of the soil cover and/or following the degradation of soils by erosion after deforestation and cultivation. These observations have important implications for the interpretation of Hg contamination patterns observed in Amazonian aquatic systems that could be linked to different drainage sources of Hg from the terrestrial surface. The sandification and podzolisation that is characteristic of the evolution of numerous pedological systems in the equatorial Amazon could be responsible for exportation of the naturally accumulated Hg, as for other metals, by acidic complexation and migration to the black waters of the Amazon. In the central Amazon region, as a result of the fragility of the soil cover, deforestation and cultivation, affecting principally the superficial soil, promote the selective erosion of fine particles enriched in oxides and Hg. The erosion of soil could be responsible for an important release of Hg, transported in particulate form by drainage waters.
The efficacy of the Al chelating drugs deferoxamine (DFO) and the hydoxypyridones (HPs): 1,2-dimethyl-3-hydroxypyrid-4-one (L1), 1-[3-hydroxy-2-methyl-4-oxopyridyl]-2-ethanesulfonic acid (L6), 1-benzyl-(4-carboxylic acid)-3-hydroxy-2-methyl-4-oxopyridine (Bzcal) and 1-(p-methylbenzyl)-2-ethyl-3-hydroxypyrid-4-one (MeBzEM) in increasing Al excretion and reducing tissue Al accumulation has been compared in adult male rats which had previously received Al nitrate nonahydrate i.p. at 0.16 mmol/kg per day for 2 months. At the end of this period, DFO was injected s.c. and the HPs were given by gavage at 0.89 mmol/kg per day for five consecutive days. Total urines were collected 24 h after each chelator administration. Following chelation treatment animals were killed and samples of brain, bone, liver, kidney, and spleen were collected. DFO administration increased to about 4 x the cumulative urinary Al elimination for 5 days, while the excretion of Al into urine caused by Bzcal, L1, and MeBzEM administration was about twice that of the control group. On the other hand, treatment with Bzcal, DFO, and MeBzEM for 5 days significantly reduced the Al levels in bone by 31, 33, and 29%, and the Al concentrations in brain by 46, 69, and 71%, respectively. These results suggest that oral administrations of MeBzEM and Bzcal can be potential alternatives to parenteral administration of DFO in Al removal.