-derived carbon in soil respiration and microbial biomass determined by C-14 and C-13. Soil Biol. Biochem. 40: 625–637. Kuzyakov Y. Root-derived carbon in soil respiration and microbial
Jegyzetek 1 Az alapadatok forrásai: Bratislava, Státny Archív, inv. č. 13. St. Martin, Liber Baptisatorum ab Anno 1738 4ta Septembris, p.377: 1741.október 16.Stephanus Antonius, P. Joanes Christophorus
NMR data and assignments δ(ppm): C 1 = 149.3; C 2 = 133.2; C 3 = 132.1; C 4 = 129.8; C 5 = 129.4; C 6 = 124.4; C 7 = 120.4; C 8 = 58.02; C 9 = 55.11; C 10 = 55.07; C 11 = 48.72; C 12 = 48.67; C 13 = 46.52; C 14 = 21.16. IR data
H01L Agriculture and food chemistry A21D, A23B, A23C, A23D, A23F, A23G, A23J, A23K, A23L, C12C, C12F, C12G, C12H, C12J, C13D, C13F, C13J, C13K
with literature data. Therefore, for example, under the same conditions of thermolysis the initial temperature of decomposition for K[AuCl 4 ] is 145 °C, but for Rb[AuBr 4 ] is 125 °C [ 13 ]. In case of double complex salts [Co(NH 3 ) 6 ][AuX 4 ] X 2
1 HNMR spectrum of S dl C 13 CNMR spectral analysis 13 CNMR spectrum of S dl C ( Fig. 4 ) shows well-separated and clear signals. From this it is understood
above 500 °C. This can be attributed to endothermic dehydroxylation (or alternatively, dehydration) to produce disordered metakaolin (Al 2 Si 2 O 7 ). Dehydroxylation continued up to 900 °C [ 13 , 14 ]. This may be attributed to the gradual oxolation of
Calorim . 2004 ; 76 : 123 – 132 . 10.1023/B:JTAN.0000027811.80036.6c . 13. Farjas , J , Roura , P . Isoconversional analysis of solid state transformations. A critical review. Part I
, 62 , 505 – 507 . 10.1248/cpb.c13-00988 13. Zhang , Q. ; Wu , H. ; Wen , C. ; Sun , F. ; Yang
.0823 -0.1 C 13 H 16 O 7 283.0710, 107.0572 p-Cresol glucuronide 8 8.85 291.0146 291