Nanoscale evidence of contrasted processes for root-derived organic matter stabilization by mineral interactions depending on soil depth

被引:67
作者
Rumpel, Cornelia [1 ]
Baumann, Karen [1 ]
Remusat, Laurent [2 ]
Dignac, Marie-France [1 ]
Barre, Pierre [3 ]
Deldicque, Damien [3 ]
Glasser, Gunnar [4 ]
Lieberwirth, Ingo [4 ]
Chabbi, Abad [1 ,5 ]
机构
[1] CNRS INRA UPMC UPEC IRD ParisAgroTech, CNRS, IEES, Thiverval Grignon, France
[2] Univ Paris 04, IMPMC, UMR CNRS 7590, MNHN,UPMC,IRD, F-75231 Paris 05, France
[3] CNRS, ENS Geol, Paris, France
[4] Max Planck Inst Polymer Res, D-55128 Mainz, Germany
[5] INRA, UR P3F, Ctr INRA Poitou Charentes, Lusignan, France
关键词
Organic matter stabilization; Subsoil; Organo-mineral interactions; Metal oxides NanoSIMS; SUBSOIL HORIZONS; FOREST SOILS; CARBON; NANOSIMS; DECOMPOSITION; LIGNIN; PARTICLES; STABILITY; CHEMISTRY; SURFACES;
D O I
10.1016/j.soilbio.2015.02.017
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Up to now stabilization of organic matter (OM) in soils due to mineral interactions has been assessed mainly by correlations between carbon and iron and/or aluminum oxides evidencing that metal oxides may be principal stabilization agents. The nature and Unorphology of stabilized OM are poorly known. Taking advantage of a field experiment, the aim of our study was to analyze the fate of C-13 and N-15 labeled root material at 30 and 90 cm depths after three years of incubation and to characterize the nature of OM stabilized by interactions with metal oxides. Our methodological approach included isolation of metal oxides by physical fractionation and visualization of their interaction with OM using NanoSIMS. We concentrated metal oxides in a fraction corresponding to our objectives: the heavy fraction (>3 g cm(-3)) of fine silt. NanoSIMS analyses of this fraction allowed us to locate unlabeled OM and OM either double labeled or carrying one single label in association with metal oxides. Our results suggest that decoupling of C and N may have happened during OM stabilization within the timeframe of the 3 year field experiment. Scanning electron microscopy (SEM) after NanoSIMS analyzes, indicated that N-15 labeled OM at 90 cm were well-defined ovoid OM particles resembling to microbial cells in interaction with Fe, Al and Ti oxides. At 30 cm depth, OM associated with metal oxides was C-13 and N-15 labeled unstructured material, possibly derived from plant debris. We suggest that at the two soil depths under investigation different processes might be at work, leading to association of OM with mineral compounds of the isolated fraction: in upper soil layers, decomposed plant material may directly interact with metal oxides, whereas in deep mineral soil, OM could mainly interact with metal oxides after microbial turnover. Both types of interactions may be fairly stable as they persisted after ultrasonication and salt extraction. (C) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:82 / 88
页数:7
相关论文
共 36 条
[1]   Assessing the extent of decomposition of natural organic materials using solid-state C-13 NMR spectroscopy [J].
Baldock, JA ;
Oades, JM ;
Nelson, PN ;
Skene, TM ;
Golchin, A ;
Clarke, P .
AUSTRALIAN JOURNAL OF SOIL RESEARCH, 1997, 35 (05) :1061-1083
[2]  
Balesdent J., 1991, SCI SOL, V29, P95
[3]   Mineral control of carbon pools in a volcanic soil horizon [J].
Basile-Doelsch, I. ;
Amundson, R. ;
Stone, W. E. E. ;
Borschneck, D. ;
Bottero, J. Y. ;
Moustier, S. ;
Masin, F. ;
Colin, F. .
GEODERMA, 2007, 137 (3-4) :477-489
[4]   Changes in litter chemistry and soil lignin signature during decomposition and stabilisation of 13C labelled wheat roots in three subsoil horizons [J].
Baumann, Karen ;
Sanaullah, Muhammad ;
Chabbi, Abad ;
Dignac, Marie-France ;
Bardoux, Gerard ;
Steffens, Markus ;
Koegel-Knabner, Ingrid ;
Rumpel, Cornelia .
SOIL BIOLOGY & BIOCHEMISTRY, 2013, 67 :55-61
[5]   Stabilised carbon in subsoil horizons is located in spatially distinct parts of the soil profile [J].
Chabbi, A. ;
Koegel-Knabner, I. ;
Rumpel, C. .
SOIL BIOLOGY & BIOCHEMISTRY, 2009, 41 (02) :256-261
[6]   The Microbial Efficiency-Matrix Stabilization (MEMS) framework integrates plant litter decomposition with soil organic matter stabilization: do labile plant inputs form stable soil organic matter? [J].
Cotrufo, M. Francesca ;
Wallenstein, Matthew D. ;
Boot, Claudia M. ;
Denef, Karolien ;
Paul, Eldor .
GLOBAL CHANGE BIOLOGY, 2013, 19 (04) :988-995
[7]   Soil organic matter turnover is governed by accessibility not recalcitrance [J].
Dungait, Jennifer A. J. ;
Hopkins, David W. ;
Gregory, Andrew S. ;
Whitmore, Andrew P. .
GLOBAL CHANGE BIOLOGY, 2012, 18 (06) :1781-1796
[8]   Stabilisation of soil organic matter by interactions with minerals as revealed by mineral dissolution and oxidative degradation [J].
Eusterhues, K ;
Rumpel, C ;
Kleber, M ;
Kögel-Knabner, I .
ORGANIC GEOCHEMISTRY, 2003, 34 (12) :1591-1600
[9]   Stability of organic carbon in deep soil layers controlled by fresh carbon supply [J].
Fontaine, Sebastien ;
Barot, Sebastien ;
Barre, Pierre ;
Bdioui, Nadia ;
Mary, Bruno ;
Rumpel, Cornelia .
NATURE, 2007, 450 (7167) :277-U10
[10]   Molecular Trickery in Soil Organic Matter: Hidden Lignin [J].
Hernes, Peter J. ;
Kaiser, Klaus ;
Dyda, Rachael Y. ;
Cerli, Chiara .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2013, 47 (16) :9077-9085