FTIR spectroscopy can be used as a screening tool for organic matter quality in regenerating cutover peatlands

被引:263
作者
Artz, Rebekka R. E. [1 ]
Chapman, Stephen J. [1 ]
Robertson, A. H. Jean [1 ]
Potts, Jacqueline M. [2 ]
Laggoun-Defarge, Fatima [3 ]
Gogo, Sebastien [3 ]
Comont, Laure [3 ]
Disnar, Jean-Robert [3 ]
Francez, Andre-Jean [4 ]
机构
[1] Macaulay Inst, Soils Grp, Aberdeen AB15 8QH, Scotland
[2] Macaulay Inst, Biomath & Stat Scotland, Aberdeen AB15 8QH, Scotland
[3] Univ Orleans, CNRS, Inst Sci Terre Orleans, UMR 6113, F-45067 Orleans, France
[4] Univ Rennes 1, CNRS 6553 Ecobio, Interact Biol Transferts Matieres, F-35042 Rennes, France
关键词
Fourier-transform infrared spectroscopy; peat; organic matter quality; carbohydrates; C : N ratio; organic micro-remains;
D O I
10.1016/j.soilbio.2007.09.019
中图分类号
S15 [土壤学];
学科分类号
0903 [农业资源与环境]; 090301 [土壤学];
摘要
Vegetational changes during the restoration of cutover peatlands leave a legacy in terms of the organic matter quality of the newly formed peat. Current efforts to restore peatlands at a large scale therefore require low cost and high throughput techniques to monitor the evolution of organic matter. In this study, we assessed the merits of using Fourier transform infrared (FTIR) spectra to predict the organic matter composition in peat samples at various stages of peatland regeneration from five European countries. Using predictive partial least squares (PLS) analyses, we were able to reconstruct peat C:N ratio and carbohydrate signatures with reasonable accuracy, but not the micromorphological composition of vegetation remains. Despite utilising different size fractions, both carbohydrate (< 200 mu m fraction) and FTIR (bulk soil) analyses report on the composition of plant cell wall constituents in the peat and therefore essentially reveal the composition of the parent vegetational material. The accuracy of the FTIR-based PLS models for C:N ratios and carbohydrate signatures was adequate to allow for their use as initial screening tools in the evaluation of the present and future organic matter composition of peat during monitoring of restoration efforts. (c) 2007 Elsevier Ltd. All rights reserved.
引用
收藏
页码:515 / 527
页数:13
相关论文
共 47 条
[1]
The physicochemical and microbiological status of a restored bog in Quebec: Identification of relevant criteria to monitor success [J].
Andersen, Roxane ;
Francez, Andre-Jean ;
Rochefort, Line .
SOIL BIOLOGY & BIOCHEMISTRY, 2006, 38 (06) :1375-1387
[2]
Substrate utilisation profiles of microbial communities in peat are depth dependent and correlate with whole soil FTIR profiles [J].
Artz, Rebekka R. E. ;
Chapman, Stephen J. ;
Campbell, Colin D. .
SOIL BIOLOGY & BIOCHEMISTRY, 2006, 38 (09) :2958-2962
[3]
Separating the effects of litter quality and microenvironment on decomposition rates in a patterned peatland [J].
Belyea, LR .
OIKOS, 1996, 77 (03) :529-539
[4]
Chemical compositions of hardwood and softwood pulps employing photoacoustic Fourier transform infrared spectroscopy in combination with partial least-squares analysis [J].
Bjarnestad, S ;
Dahlman, O .
ANALYTICAL CHEMISTRY, 2002, 74 (22) :5851-5858
[5]
Organic matter sources and early diagenetic degradation in a tropical peaty marsh (Tritrivakely, Madagascar).: Implications for environmental reconstruction during the Sub-Atlantic [J].
Bourdon, S ;
Laggoun-Défarge, F ;
Disnar, JR ;
Maman, O ;
Guillet, B ;
Derenne, S ;
Largeau, C .
ORGANIC GEOCHEMISTRY, 2000, 31 (05) :421-438
[6]
Chapman S, 2003, FRONT ECOL ENVIRON, V1, P525, DOI 10.1890/1540-9295(2003)001[0525:EONPAB]2.0.CO
[7]
2
[8]
FTIR spectroscopy of peat in and bordering Scots pine woodland: relationship with chemical and biological properties [J].
Chapman, SJ ;
Campbell, CD ;
Fraser, AR ;
Puri, G .
SOIL BIOLOGY & BIOCHEMISTRY, 2001, 33 (09) :1193-1200
[9]
Cheshire M.V., 1979, NATURE ORIGIN CARBOH
[10]
Characterization of solid and aqueous phases of a peat bog profile using molecular fluorescence spectroscopy, ESR and FT-IR, and comparison with physical properties [J].
Cocozza, C ;
D'Orazio, V ;
Miano, TM ;
Shotyk, W .
ORGANIC GEOCHEMISTRY, 2003, 34 (01) :49-60