哪能仁慈 发表于 2025-3-21 20:04:03
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Klaus Füsser product holds the metal in a gross oxidation state of 3.2 to 3.7; the intermediate surface V (V) species occurs in tetrahedral and octahedral coordination (SERS, NMR-MAS). O. oxidizes back to V(V) (peroxo intermediate); halogens give V(IV)X, which can be converted to V(IV)R. The active V(III) reactSLUMP 发表于 2025-3-22 07:40:44
Klaus Füsseronitor it is in general impractical to use methods specific for individual or small groups of pesticides, and consequently, we are developing multi-residue techniques. Because of the need to be certain of the identity of the pesticide being detected in a sample at the very low concentrations impliedcardiovascular 发表于 2025-3-22 11:45:54
Klaus Füssero modelling approaches, the US EPA EXAMS II and Mackay Fugacity has been carried out for 6 organic pollutants by comparison of results from field samples to model predictions. EXAMS II was found to produce quantitative predictions that compared well with measured concentrations for some of the polluCOMMA 发表于 2025-3-22 15:13:24
Klaus Füsseras not carefully been carried out, even the most advanced analytical instruments and sophisticated computer techniques cannot prevent that the final analysis results are questionable..Nevertheless, new generations of analytical methods and instruments provide ever higher degrees of separation and loobviate 发表于 2025-3-22 19:59:33
Klaus Füsseras not carefully been carried out, even the most advanced analytical instruments and sophisticated computer techniques cannot prevent that the final analysis results are questionable..Nevertheless, new generations of analytical methods and instruments provide ever higher degrees of separation and lo阶层 发表于 2025-3-23 01:12:36
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Klaus Füsserrepresent portions of hydrothermally altered sub-ducted oceanic lithosphere that resided at great depth (≫ diamond stability limit) before diapiric uprise and final cumulate segregation. The evolution of these rocks is compared with that of the sparsely diamondiferous alpine peridotites which probab极为愤怒 发表于 2025-3-23 06:00:19
Klaus Füsser that early lithospheric stretching beneath the ridge allows seawater penetration in the lower crust when it is still very hot, through permeability created by shear zones and associated synkinematic cracks. Therefore, hydration of the lower crust starts at high temperature (750°C), in contrast with