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For VPSPr case 1 seeding activity was markedly reduced in the uppermost fractions (1 and 2) in which the ~8 kDa PrPres was found.
The uppermost fractions 15-200) from the density gradient contains the bulk of the plasma membrane and were pooled, diluted in 5 volumes HB-II and pelleted by centrifugation at 100,000 × g for 1.5 h at 4°C.
Direct geological records only document the crustal or uppermost fraction of our planet while the deeper parts remain totally outside of our reach.
Estimated cDCE mole fractions in the DNAPL increased towards the DNAPL interface with the uppermost mole fraction of 0.04 comparable to literature laboratory data.
It is interesting to note that VPSPr seeding activity was reduced in the uppermost two fractions characterised by ~8 kDa PrPres.
First, the uppermost platelet-deprived fraction was removed with a sterile syringe.
Following overnight centrifugation the uppermost three 1 ml fractions were discarded, and the next 9 fractions (numbers 4 to 12) collected.
The uppermost layer of supernatant (soluble fraction) and pellet (insoluble fraction) were subjected to SDS-PAGE and stained with Coomassie Blue.
Bulk soils and soil fractions of the uppermost A horizons were analyzed for OC concentrations, radiocarbon (14C) contents, total pedogenic iron oxide concentration and oxalate extractable proportions of iron (FeOX) oxides.
The most sensitive nitrate-N-related parameters were the denitrification rate in soil (denitr) and the fraction of nutrient uptake in the uppermost soil layer (uptsoil1) of the three dominant land use classes (i.e. arable land, forest and pastures).
The observed mineral distribution is most likely controlled by the weathering of clay minerals in the uppermost part of the profile and translocation of clay fractions down the profile (lessivage).
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