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Experimental data for adsorption capacity of Cr6+, Pb2+, Ni2+ and Cd2+ from aqueous solution by activated carbon (Tables 1, 2, 3, 4).
The decline in organic carbon (Tables 3, 5) might be responsible for N upgrading that was similar to the results of other researchers (Sangwan et al. 2008; Karmegam and Daniel 2009).
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At the organismal scale, denitrification is regulated by O2 and levels of available inorganic N and respirable carbon (C) (Table 1).
A similar carbon recovery was observed in the fermentation by the wild type utilizing stored crude glycerol supplemented with activated stone carbon (Table 1).
Soil cores from a historic fen in Switzerland, with similar agricultural management over ~ 140 years, recorded 16 49% loss of 'pre-drainage' organic carbon ('Table 2' of [39]).
Accordingly, if the negative charge is located on N(1) or N(2), they will be preferentially attack the electrophilic carbon (Table 5) in alkylation reactions.
This is supported by the negative and significant (P ≤ 0.01) correlation (r = −0.85**) between the soil bulk density and organic carbon (Table 7).
1D NMR spectra in combination with HSQC spectrum demonstrated 15 carbons, which were classified into three methyl, six methylenes (one olefinic carbon, one oxygenated carbon), three methines (two olefinic carbons) and three quaternary carbons (one olefinic carbon) (Table 2).
Total root colonization was significantly correlated with pH total nitrogen, organic carbon, and electrical conductivity, while total spore density was significantly correlated with total nitrogen, available phosphorus, available potassium and organic carbon (Table 6).
The estimated asymptotic maximum carbon stock in the stands increased to 484 (±26) Mg C ha−1 with the inclusion of dead-tree carbon (Table 1) Dead trees in unthinned plots typically represent suppression mortality as tree density decreases through time.
Seedlings of sco1-1 rarely survived past the cotyledon stage unless they were provided with supplementary carbon (Table 1).
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