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1.
J Magn Reson ; 171(1): 157-62, 2004 Nov.
Artículo en Inglés | MEDLINE | ID: mdl-15504695

RESUMEN

The RARE imaging method was used to monitor the cooking of single rice kernels in real time and with high spatial resolution in three dimensions. The imaging sequence is optimized for rapid acquisition of signals with short relaxation times using centered out RARE. Short scan time and high spatial resolution are critical factors in the investigation of the cooking behavior of rice kernels since time and spatial averaging may lead to erroneous results. The results are confirming the general pattern of moisture ingress that has been suspected from previous (more limited) studies. Water uptake as determined by analysis of the MRI time series recorded during cooking compares well with gravimetric studies. This allows using these real-time MRI data for developing and validating models that describe the effect of kernel microstructure on its cooking behavior.


Asunto(s)
Culinaria , Imagen por Resonancia Magnética/métodos , Oryza , Procesamiento de Imagen Asistido por Computador , Factores de Tiempo , Agua
2.
Chemosphere ; 48(9): 919-31, 2002 Sep.
Artículo en Inglés | MEDLINE | ID: mdl-12222787

RESUMEN

The composition of amorphous and condensed soil/sediment organic matter (SOM) domains was investigated for one soil sample and four sediment samples. These samples were oxidized with persulfate to remove amorphous SOM, before and after which the composition of SOM was studied by thermogravimetric analysis, pyrolysis-GC/MS, and cross polarization magic angle spinning 13C-NMR. Comparison of the SOM composition before and after oxidation showed that condensed SOM was more thermostable and less polar than amorphous SOM. Condensed SOM was relatively low in O-alkyl C and carboxyl C and it was likely to contain only small amounts of labile organic components (carbohydrates, peptides, fatty acids). Apart from these general characteristics, the composition of the condensed and amorphous domains appeared to be highly dependent on the origin and nature of the SOM investigated. Condensed domains in relatively undecomposed SOM were enriched in aliphatic C, whereas condensed domains in relatively weathered SOM were enriched in aromatic C. Altogether, the compositional changes upon persulfate oxidation were similar to the compositional changes upon humification, which supports the idea that weathered SOM is more condensed than the original material.


Asunto(s)
Sedimentos Geológicos/química , Suelo , Isótopos de Carbono/química , Cromatografía de Gases y Espectrometría de Masas , Espectroscopía de Resonancia Magnética , Compuestos Orgánicos/análisis , Oxidación-Reducción
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