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Between 1 to 4% of total C was extracted by hot water in both soils compared to 18 to 32% of total C hydrolyzed by HCl.
Boxplots in Fig. 2 show the variability of total C by biomass category.
Although there were quantitative differences in the amount of C released, both soils showed similar percentages of non-hydrolyzable carbon (18 25% of total C for upland soil, and 24 32% of total C for wetland soil).
Even after mechanical shaking, > 53 μm and 2 53 μm fractions accounted for 37%and41%1% of total C, respectively.
However, geostatistical analysis of total C and N contents provided a useful means to calculate spatial distribution patterns of these properties.
This finding demonstrates the need for high resolution survey data for the prediction of total C at the hillslope and catchment scale.
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Of this estimate, snags contributed 34.5% of total C-stock.
A repeated measure logistic regression was performed on the IHC scores of total c-Jun and phospho-c-Jun using the GENMOD procedure in SAS version 9.2 (SAS Institute, Cary, NC).
We have developed a proximity assay for quantification of total c-MET expression in FFPE specimens.
In wildtype bone marrow derived macrophages, the kinetics of c-jun activation also followed similar kinetic profiles, as judged by the electorphoretic shift of total c-jun (Fig. 3C).
(G ) C-peptide secretion was shown as a percentage of total C-peptide content (n = 4).
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