Abstract

Rhizodeposition is an important pathway of atmospheric C-input to soil, however, quantity and quality of plant rhizodeposition are insufficiently known. Therefore, the composition and diurnal dynamics of water-soluble root-derived substances and products of their interaction with sandy soil were investigated in maize plants ( Zea mays L.) by pyrolysis-field ionization mass spectrometry (Py-FIMS). In both night- and day-rhizodeposits the C, N and S concentrations were larger by factors ranging from 3.0 to 9.7 than the samples from non-cropped soil. The rhizodeposition was larger during the day than during the night-time and the composition of these deposits was different. The largest differences in the Py-FI mass spectra resulted from signals assigned to amino acids (aspartic acid, asparagine, glutamic acid, leucine, isoleucine, hydroxyproline and phenylalanine) and carbohydrates, in particular pentoses, which were exuded in the photosynthetic period. Marker signals in the Py-FI mass spectra and the curves of their thermal volatilization provided unequivocal evidence for the occurrence of free amino acids in the day-rhizodeposits. Other compounds detected in the Py-FI mass spectra were interpreted as constituents of rhizodeposits (lipids, suberin, fatty acids) or products of the interaction of rhizodeposits and microbial metabolites with stable soil organic matter (lignin dimers and alkylaromatics). It was concluded that the diurnal dynamics in the molecular-chemical composition between day- and night-rhizodeposits resulted from the exudation carbohydrates and amino acids during the photosynthetic period, the deposition of other root-derived compounds such as lipids, suberin and fatty acids, and the microbial metabolism of all available organic compounds in the rhizosphere. Furthermore, applications of the presented approach in C-turnover and phytoremediation research, and for risk assessment of genetically modified crops are proposed.

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