Knowledge gaps in soil carbon and nitrogen interactions - From molecular to global scale

被引:182
作者
Gardenas, Annemieke I. [1 ]
Agren, Goran I. [2 ]
Bird, Jeffrey A. [3 ]
Clarholm, Marianne [4 ]
Hallin, Sara [5 ]
Ineson, Phil [6 ]
Katterer, Thomas [1 ]
Knicker, Heike [7 ]
Nilsson, S. Ingvar [1 ]
Nasholm, Torgny [8 ]
Ogle, Stephen [9 ]
Paustian, Keith [9 ]
Persson, Tryggve [2 ]
Stendahl, Johan [1 ]
机构
[1] Swedish Univ Agr Sci, Dept Soil & Environm, SE-75007 Uppsala, Sweden
[2] Swedish Univ Agr Sci, Dept Ecol, SE-75007 Uppsala, Sweden
[3] CUNY, Queens Coll, Sch Earth & Environm Sci, New York, NY 11367 USA
[4] Swedish Univ Agr Sci, Dept Forest Mycol & Pathol, SE-75007 Uppsala, Sweden
[5] Swedish Univ Agr Sci, Dept Microbiol, SE-75007 Uppsala, Sweden
[6] Univ York, Dept Biol, York YO10 5YW, N Yorkshire, England
[7] Inst Nat Resources & Agrobiol IRNAS CSIC, Dept Geoecol & Biogeochem, Seville 41012, Spain
[8] Swedish Univ Agr Sci, Dept Forest Ecol & Management, SE-90183 Umea, Sweden
[9] Colorado State Univ, Nat Resource Ecol Lab, Ft Collins, CO 80523 USA
关键词
Soil-climate interactions; Carbon-nitrogen interactions; SOM; Rhizosphere; Priming; Greenhouse gases; Black nitrogen; Organic nitrogen; Model; Climate change; GCM; Uncertainties; Scaling; AMINO-ACID-UPTAKE; SOLID-STATE C-13; ORGANIC-MATTER DECOMPOSITION; FIRE-INDUCED TRANSFORMATION; AMMONIA-OXIDIZING ARCHAEA; BOREAL FOREST PLANTS; TEMPERATURE SENSITIVITY; METHANE OXIDATION; ELEVATED CO2; INORGANIC NITROGEN;
D O I
10.1016/j.soilbio.2010.04.006
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The objective of this review was to identify, address and rank knowledge gaps in our understanding of five major soil C and N interactions across a range of scales from molecular to global. The studied five soil C and N interactions are: i) N controls on the soil emissions of greenhouse gases, ii) plant utilisation of organic N, iii) impact of rhizosphere priming on C and N cycling, iv) impact of black N on the stabilisation of soil organic matter (SUM) and v) representation of fractions of SUM in simulation models. We ranked the identified knowledge gaps according to the importance we attached to them for functional descriptions of soil climate interactions at the global scale, for instance in general circulation models (GCMs). Both the direct and indirect influences on soil climate interactions were included. We found that the level of understanding declined as the scale increased from molecular to global for four of the five topics. By contrast, the knowledge level for SUM simulation models appeared to be highest when considered at the ecosystem scale. The largest discrepancy between knowledge level and importance was found at the global modelling scale. We concluded that a reliable quantification of greenhouse gas emissions at the ecosystem scale is of utmost importance for improving soil climate representation in GCMs. We see as key questions the identification of the role of different N species for the temperature sensitivity of SUM decomposition rates and its consequences for plant available N. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:702 / 717
页数:16
相关论文
共 240 条
[1]  
Agren G.I., 1998, THEORETICAL ECOSYSTE
[2]   Reconciling differences in predictions of temperature response of soil organic matter [J].
Ågren, GI ;
Bosatta, E .
SOIL BIOLOGY & BIOCHEMISTRY, 2002, 34 (01) :129-132
[3]   CLIMATE CHANGE Microbial mitigation [J].
Agren, Goran I. .
NATURE GEOSCIENCE, 2010, 3 (05) :303-304
[4]   Soil-carbon response to warming dependent on microbial physiology [J].
Allison, Steven D. ;
Wallenstein, Matthew D. ;
Bradford, Mark A. .
NATURE GEOSCIENCE, 2010, 3 (05) :336-340
[5]   Rearrangement of carbon and nitrogen forms in peat after progressive thermal oxidation as determined by solid-state 13C and 15N-NMR spectroscopy [J].
Almendros, G ;
Knicker, H ;
González-Vila, FJ .
ORGANIC GEOCHEMISTRY, 2003, 34 (11) :1559-1568
[6]   FIRE-INDUCED TRANSFORMATION OF SOIL ORGANIC-MATTER FROM AN OAK FOREST - AN EXPERIMENTAL APPROACH TO THE EFFECTS OF FIRE ON HUMIC SUBSTANCES [J].
ALMENDROS, G ;
GONZALEZVILA, FJ ;
MARTIN, F .
SOIL SCIENCE, 1990, 149 (03) :158-168
[7]   Amino acids, total organic and inorganic nitrogen in forest floor soil solution at low and high nitrogen input [J].
Andersson, P ;
Berggren, D .
WATER AIR AND SOIL POLLUTION, 2005, 162 (1-4) :369-384
[8]  
Andren O, 1997, ECOL APPL, V7, P1226, DOI 10.1890/1051-0761(1997)007[1226:ITICBM]2.0.CO
[9]  
2
[10]   THE PARTITIONING OF NITRATE ASSIMILATION BETWEEN ROOT AND SHOOT OF HIGHER-PLANTS [J].
ANDREWS, M .
PLANT CELL AND ENVIRONMENT, 1986, 9 (07) :511-519