Biogeochemical interfaces in soil: The interdisciplinary challenge for soil science

被引:138
作者
Totsche, Kai U. [1 ]
Rennert, Thilo [1 ]
Gerzabek, Martin H. [2 ]
Koegel-Knabner, Ingrid [3 ]
Smalla, Kornelia [4 ]
Spiteller, Michael [5 ]
Vogel, Hans-Joerg [6 ]
机构
[1] Univ Jena, Lehrstuhl Hydrogeol, Inst Geowissensch, D-07749 Jena, Germany
[2] Univ Bodenkultur Wien, Inst Bodenforsch, A-1190 Vienna, Austria
[3] Tech Univ Munich, Lehrstuhl Bodenkunde, D-85350 Freising Weihenstephan, Germany
[4] Bundesforsch Inst Kulturpflanzen, Julius Kuhn Inst, D-38104 Braunschweig, Germany
[5] TU Dortmund, Inst Umweltforsch, D-44227 Dortmund, Germany
[6] UFZ Helmholtz Ctr Environm Res, Dept Bodenphys, D-06120 Halle, Germany
关键词
soil function; soil architecture; spectro-microscopy; tomography; SOM; soil microbial ecology; organic chemicals; POLYCYCLIC AROMATIC-HYDROCARBONS; ATOMIC-FORCE MICROSCOPY; PERSISTENT ORGANIC POLLUTANTS; IONIZATION MASS-SPECTROMETRY; LASER-SCANNING MICROSCOPY; BOUND PESTICIDE-RESIDUES; TERM FIELD EXPERIMENT; X-RAY-FLUORESCENCE; HUMIC SUBSTANCES; SPECTROSCOPIC EVIDENCE;
D O I
10.1002/jpln.200900105
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Soil, the "Earth's thin skin" serves as the delicate interface between the biosphere, hydrosphere, atmosphere, and lithosphere. It is a dynamic and hierarchically organized system of various 7 organic and inorganic constituents and organisms, the spatial structure of which defines a large, complex, and heterogeneous interface. Biogeochemical processes at soil interfaces are fundamental for the overall soil development, and they are the primary driving force for key ecosystem functions such as plant productivity and water quality. Ultimately, these processes control the fate and transport of contaminants and nutrients into the vadose zone and as such their biogeochemical cycling. The definite objective in biogeochemical-interface research is to gain a mechanistic understanding of the architecture of these biogeochemical interfaces in soils and of the complex interplay and interdependencies of the physical, chemical, and biological processes acting at and within these dynamic interfaces in soil. The major challenges are (1) to identify the factors controlling the architecture of biogeochemical interfaces, (2) to link the processes operative at the individual molecular and/or organism scale to the phenomena active at the aggregate scale in a mechanistic way, and (3) to explain the behavior of organic chemicals in soil within a general mechanistic framework. To put this in action, integration of soil physical, chemical, and biological disciplines is mandatory. Indispensably, it requires the adaption and development of characterization and probing techniques adapted from the neighboring fields of molecular biology, analytical and computational chemistry as well as materials and nano-sciences. To shape this field of fundamental soil research, the German Research Foundation (DFG) has granted the Priority Program "Biogeochemical Interfaces in Soil", in which 22 individual research projects are involved.
引用
收藏
页码:88 / 99
页数:12
相关论文
共 141 条
[21]   Differences in sequestration and bioavailability of organic compounds aged in dissimilar soils [J].
Chung, NH ;
Alexander, M .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1998, 32 (07) :855-860
[22]   Extensive sorption of organic compounds to black carbon, coal, and kerogen in sediments and soils:: Mechanisms and consequences for distribution, bioaccumulation, and biodegradation [J].
Cornelissen, G ;
Gustafsson, Ö ;
Bucheli, TD ;
Jonker, MTO ;
Koelmans, AA ;
Van Noort, PCM .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2005, 39 (18) :6881-6895
[23]   Sorption of imidacloprid on soil clay mineral and organic components [J].
Cox, L ;
Koskinen, WC ;
Celis, R ;
Yen, PY ;
Hermosin, MC ;
Cornejo, J .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1998, 62 (04) :911-915
[24]   Exploring microbial diversity - A vast below [J].
Curtis, TP ;
Sloan, WT .
SCIENCE, 2005, 309 (5739) :1331-1333
[25]   Methods for speciation of metals in soils: A review [J].
D'Amore, JJ ;
Al-Abed, SR ;
Scheckel, KG ;
Ryan, JA .
JOURNAL OF ENVIRONMENTAL QUALITY, 2005, 34 (05) :1707-1745
[26]   Use of field-based stable isotope probing to identify adapted populations and track carbon flow through a phenol-degrading soil microbial community [J].
DeRito, CM ;
Pumphrey, GM ;
Madsen, EL .
APPLIED AND ENVIRONMENTAL MICROBIOLOGY, 2005, 71 (12) :7858-7865
[27]   Long-term fate of polychlorinated biphenyls and polycyclic aromatic hydrocarbons in an agricultural soil [J].
Doick, KJ ;
Klingelmann, E ;
Burauel, P ;
Jones, KC ;
Semple, KT .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2005, 39 (10) :3663-3670
[28]   Empirical and theoretical bacterial diversity in four Arizona soils [J].
Dunbar, J ;
Barns, SM ;
Ticknor, LO ;
Kuske, CR .
APPLIED AND ENVIRONMENTAL MICROBIOLOGY, 2002, 68 (06) :3035-3045
[29]   Composition of organic matter fractions for explaining wettability of three forest soils [J].
Ellerbrock, RH ;
Gerke, HH ;
Bachmann, J ;
Goebel, MO .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 2005, 69 (01) :57-66
[30]   Boundaries for biofilm formation: Humidity and temperature [J].
Else, TA ;
Pantle, CR ;
Amy, PS .
APPLIED AND ENVIRONMENTAL MICROBIOLOGY, 2003, 69 (08) :5006-5010