An interdisciplinary approach towards improved understanding of soil deformation during compaction

被引:75
|
作者
Keller, T. [1 ,2 ]
Lamande, M. [3 ]
Peth, S. [4 ,5 ]
Berli, M. [6 ]
Delenne, J. -Y. [7 ]
Baumgarten, W. [4 ]
Rabbel, W. [8 ]
Radjai, F. [7 ]
Rajchenbach, J. [9 ]
Selvadurai, A. P. S. [10 ]
Or, D. [11 ]
机构
[1] Agroscope Reckenholz Tanikon Res Stn ART, Dept Nat Resources & Agr, CH-8046 Zurich, Switzerland
[2] Swedish Univ Agr Sci, Dept Soil & Environm, SE-75007 Uppsala, Sweden
[3] Aarhus Univ, Dept Agroecol & Environm, Res Ctr Foulum, DK-8830 Tjele, Denmark
[4] Univ Kiel, Inst Plant Nutr & Soil Sci, D-24118 Kiel, Germany
[5] Univ Kassel, Fac 11, Grp Soil Sci, D-37213 Witzenhausen, Germany
[6] Desert Res Inst, Div Hydrol Sci, Las Vegas, NV USA
[7] Univ Montpellier 2, Cc 048, F-34095 Montpellier 5, France
[8] Univ Kiel, Inst Geosci, D-24118 Kiel, Germany
[9] Univ Nice, Phys Mat Condensee Lab, F-06108 Nice 2, France
[10] McGill Univ, Dept Civil Engn & Appl Mech, Montreal, PQ H3A 2K6, Canada
[11] Swiss Fed Inst Technol, CH-8092 Zurich, Switzerland
来源
SOIL & TILLAGE RESEARCH | 2013年 / 128卷
基金
瑞典研究理事会;
关键词
Soil compaction; Continuum mechanics; Granular media; Seismic methods; Modelling; X-ray computed tomography; RAY-COMPUTED-TOMOGRAPHY; WAVE VELOCITY-MEASUREMENTS; EARTHWORM BURROW SYSTEMS; UNIAXIAL COMPRESSION; STRESS TRANSMISSION; STRUCTURAL-CHANGES; EUTRIC CAMBISOL; BULK-DENSITY; MACRO-PORES; MODEL;
D O I
10.1016/j.still.2012.10.004
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Soil compaction not only reduces available pore volume in which fluids are stored, but it alters the arrangement of soil constituents and pore geometry, thereby adversely impacting fluid transport and a range of soil ecological functions. Quantitative understanding of stress transmission and deformation processes in arable soils remains limited. Yet such knowledge is essential for better predictions of effects of soil management practices such as agricultural field traffic on soil functioning. Concepts and theory used in agricultural soil mechanics (soil compaction and soil tillage) are often adopted from conventional soil mechanics (e.g. foundation engineering). However, in contrast with standard geotechnical applications, undesired stresses applied by agricultural tyres/tracks are highly dynamic and last for very short times. Moreover, arable soils are typically unsaturated and contain important secondary structures (e.g. aggregates), factors important for affecting their soil mechanical behaviour. Mechanical processes in porous media are not only of concern in soil mechanics, but also in other fields including geophysics and granular material science. Despite similarity of basic mechanical processes, theoretical frameworks often differ and reflect disciplinary focus. We review concepts from different but complementary fields concerned with porous media mechanics and highlight opportunities for synergistic advances in understanding deformation and compaction of arable soils. We highlight the important role of technological advances in non-destructive measurement methods at pore (X-ray tomography) and soil profile (seismic) scales that not only offer new insights into soil architecture and enable visualization of soil deformation, but are becoming instrumental in the development and validation of new soil compaction models. The integration of concepts underlying dynamic processes that modify soil pore spaces and bulk properties will improve the understanding of how soil management affect vital soil mechanical, hydraulic and ecological functions supporting plant growth. (c) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:61 / 80
页数:20
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