Simulating microbial degradation of organic matter in a simple porous system using the 3-D diffusion-based model MOSAIC

被引:38
作者
Monga, O. [1 ]
Garnier, P. [2 ]
Pot, V. [2 ]
Coucheney, E. [3 ]
Nunan, N. [3 ]
Otten, W. [4 ]
Chenu, C. [5 ]
机构
[1] Univ Paris 06, UMMISCO Cameroun, Unite Mixte Int Rech UMMISCO, Univ Yaounde 1 Cameroun,IRD, Paris, France
[2] AgroParisTech, INRA, EGC UMR1091, F-78850 Thiverval Grignon, France
[3] CNRS, Biogeochim & Ecol Milieux Continentaux UMR7618, F-78850 Thiverval Grignon, France
[4] Univ Abertay Dundee, SIMBIOS Ctr, Dundee DD1 1HG, Scotland
[5] AgroParisTech, Biogeochim & Ecol Milieux Continentaux UMR7618, F-8850 Thiverval Grignon, France
关键词
SOIL HETEROTROPHIC RESPIRATION; PORE-SPACE; GEOMETRIC STRUCTURES; BIOLOGICAL-ACTIVITY; CARBON TURNOVER; DECOMPOSITION; GROWTH; WATER; QUANTIFICATION; COMMUNITIES;
D O I
10.5194/bg-11-2201-2014
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
This paper deals with the simulation of microbial degradation of organic matter in soil within the pore space at a microscopic scale. Pore space was analysed with micro-computed tomography and described using a sphere network coming from a geometrical modelling algorithm. The biological model was improved regarding previous work in order to include the transformation of dissolved organic compounds and diffusion processes. We tested our model using experimental results of a simple substrate decomposition experiment (fructose) within a simple medium (sand) in the presence of different bacterial strains. Separate incubations were carried out in microcosms using five different bacterial communities at two different water potentials of -10 and -100 cm of water. We calibrated the biological parameters by means of experimental data obtained at high water content, and we tested the model without changing any parameters at low water content. Same as for the experimental data, our simulation results showed that the decrease in water content caused a decrease of mineralization rate. The model was able to simulate the decrease of connectivity between substrate and microorganism due the decrease of water content.
引用
收藏
页码:2201 / 2209
页数:9
相关论文
共 37 条
[1]  
[Anonymous], 1989, Molecular Cloning: A Laboratory
[2]   Microbial growth in soil and nitrogen turnover: Model calibration with laboratory data [J].
Blagodatsky, SA ;
Yevdokimov, IV ;
Larionova, AA ;
Richter, J .
SOIL BIOLOGY & BIOCHEMISTRY, 1998, 30 (13) :1757-1764
[3]  
Chenu C, 2002, IUPAC S ANAL PHYS CH, V8, P3
[4]   Simulating trends in soil organic carbon in long-term experiments using RothC-26.3 [J].
Coleman, K ;
Jenkinson, DS ;
Crocker, GJ ;
Grace, PR ;
Klir, J ;
Korschens, M ;
Poulton, PR ;
Richter, DD .
GEODERMA, 1997, 81 (1-2) :29-44
[5]  
Coucheney E., 2009, IMPACT BACTERIAL DIV, V6
[6]   Biodegradation in a Partially Saturated Sand Matrix: Compounding Effects of Water Content, Bacterial Spatial Distribution, and Motility [J].
Dechesne, Arnaud ;
Owsianiak, Mikolaj ;
Bazire, Alexis ;
Grundmann, Genevieve L. ;
Binning, Philip J. ;
Smets, Barth F. .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2010, 44 (07) :2386-2392
[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]  
Falloon P., 2011, GB3010
[9]   Modelling carbon and nitrogen dynamics in a bare soil with and without straw incorporation [J].
Garnier, P ;
Néel, C ;
Aita, C ;
Recous, S ;
Lafolie, F ;
Mary, B .
EUROPEAN JOURNAL OF SOIL SCIENCE, 2003, 54 (03) :555-568
[10]   A reactive transport modeling approach to simulate biogeochemical processes in pore structures with pore-scale heterogeneities [J].
Gharasoo, Mehdi ;
Centler, Florian ;
Regnier, Pierre ;
Harms, Hauke ;
Thullner, Martin .
ENVIRONMENTAL MODELLING & SOFTWARE, 2012, 30 :102-114