Profiling Rhizosphere Chemistry: Evidence from Carbon and Nitrogen K-Edge XANES and Pyrolysis-FIMS

被引:28
作者
Gillespie, A. W. [1 ]
Walley, F. L. [1 ]
Farrell, R. E. [1 ]
Leinweber, P. [2 ]
Schlichting, A. [2 ]
Eckhardt, K. -U. [2 ]
Regier, T. Z. [3 ]
Blyth, R. I. R. [3 ]
机构
[1] Univ Saskatchewan, Dept Soil Sci, Saskatoon, SK S7N 5A8, Canada
[2] Univ Rostock, Inst Land Use, D-18051 Rostock, Germany
[3] Canadian Light Source Inc, Saskatoon, SK S7N 0X4, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
SOIL ORGANIC-MATTER; X-RAY-ABSORPTION; PARTICLE-SIZE FRACTIONS; MOLECULAR-CHEMICAL CHARACTERIZATION; MASS-SPECTROMETRY; WHOLE SOILS; NEXAFS SPECTROSCOPY; HUMIC SUBSTANCES; FINE-STRUCTURE; PLANT;
D O I
10.2136/sssaj2008.0273
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The rhizosphere is a region of complex interactions among plants, sod, and microbiota and by its very nature, it presents many technical challenges to the analyst. Whereas previous studies have generally focused on root exudation in artificial systems, we compared whole-soil samples from bulk and rhizosphere soils developed under field pea (Pisum sativa L.). Synchrotron-based C and N K-edge x-ray absorption near-edge structure (XANES) spectroscopy and pyrolysis field-ionization mass-spectrometry (Py-FIMS) were used to investigate plant effects on the organic chemistry of the rhizosphere in a growth chamber experiment. Soil type appeared to play a significant role in the development of the rhizosphere. Indeed, the C and N K-edge XANES analyses revealed patterns of rhizosphere development that were strongly influenced by soil type. Relative to the bulk soil, pea rhizospheres developed on a clay sod showed increases in heterocyclic N compounds, proteins, and carboxylates. Pea rhizospheres developed on a sandy clay loam sod showed increased nitroaromatic compounds and reduced aromatics, while proteins, carbohydrates, and carboxylic compounds remained unchanged relative to the bulk soils. Pyrolysis mass spectrometry results showed that rhizosphere processes promote selective enrichment of lipid compounds (alkanes, alkenes, alkylamides, alkylaromatics, and alkyl, benzoic, and phthalic esters) with a concomitant depletion of carbohydrates, proteins, phenols, and lignins. These results suggest enhanced decomposition of labile organic matter at a molecular level in the rhizosphere, presumably as a result of enhanced microbial activity. The presence of nitroaromatic and alkylamide compounds in the rhizosphere indicates a unique cycling of N in this region. Synchrotron-based analysis of whole sods offers useful, corroborating information regarding the organic chemistry of the rhizosphere when compared with established pyrolytic techniques.
引用
收藏
页码:2002 / 2012
页数:11
相关论文
共 85 条
[1]   X-ray photoelectron spectroscopy of nitrogen functional groups in soil humic acids [J].
Abe, T ;
Watanabe, A .
SOIL SCIENCE, 2004, 169 (01) :35-43
[2]   Plant-induced changes in soil structure: Processes and feedbacks [J].
Angers, DA ;
Caron, J .
BIOGEOCHEMISTRY, 1998, 42 (1-2) :55-72
[3]  
[Anonymous], 1904, Arb. Der Dtsch. Landwirtsch. Ges, DOI DOI 10.12691/AEES-1-6-1
[4]   FIXATION OF NITRITE NITROGEN DURING THE HUMIFICATION OF ALPHA-NAPHTHOL IN SOIL SUSPENSIONS [J].
AZHAR, ES ;
VERHE, R ;
PROOT, M ;
SANDRA, P ;
VERSTRAETE, W .
JOURNAL OF AGRICULTURAL AND FOOD CHEMISTRY, 1989, 37 (01) :262-266
[5]  
Badalucco L, 2001, BOOKS SOIL PLANT ENV, P159
[6]  
Badalucco L., 2007, The Rhizosphere, Biochemistry and Organic Substances at the Soil-Plant Interface, VSecond, P111, DOI DOI 10.1201/9781420005585.CH4
[7]  
BALDOCK JA, 1992, BIOGEOCHEMISTRY, V16, P1, DOI 10.1007/BF02402261
[8]  
Brady NC, 1999, NATURE PROPERTIES SO, DOI DOI 10.1023/A:1016012810895.3
[9]  
Brimecombe MJ., 2007, The Rhizosphere Biochemistry and Organic Substances at the Soil-Plant Interface, VSecond, P73, DOI DOI 10.1201/9781420005585.CH3
[10]   Organic geochemical studies of soils from the Rothamsted classical experiments - V. The fate of lipids in different long-term experiments [J].
Bull, ID ;
van Bergen, PF ;
Nott, CJ ;
Poulton, PR ;
Evershed, RP .
ORGANIC GEOCHEMISTRY, 2000, 31 (05) :389-408