Trans-Disciplinary Soil Physics Research Critical to Synthesis and Modeling of Agricultural Systems

Total Page:16

File Type:pdf, Size:1020Kb

Trans-Disciplinary Soil Physics Research Critical to Synthesis and Modeling of Agricultural Systems Published online February 2, 2006 Trans-Disciplinary Soil Physics Research Critical to Synthesis and Modeling of Agricultural Systems Lajpat R. Ahuja,* Liwang Ma, and Dennis J. Timlin ABSTRACT global climate change are threatening economic viability Synthesis and quantification of disciplinary knowledge at the whole of the traditional agricultural systems, and require the system level, via the process models of agricultural systems, are critical development of new and dynamic production systems. to achieving improved and dynamic management and production Site-specific, optimal management of spatially variable systems that address the environmental concerns and global issues of soil, appropriately selected crops, and available water the 21st century. Soil physicists have made significant contributions in resources on the landscape can help achieve both envi- this area in the past, and are uniquely capable of making the much- ronmental and production objectives. Fortunately, the new needed and exciting new contributions. Most of the exciting new re- electronic technologies can provide a vast amount of real- search opportunities are trans-disciplinary, that is, lie on the interfacial time information about soil and crop conditions via re- boundaries of soil physics and other disciplines, especially in quanti- mote sensing with satellites or ground-based instruments, fying interactions among soil physical processes, plant and atmospheric processes, and agricultural management practices. Some important which, combined with near-term weather, can be utilized knowledge-gap and cutting-edge areas of such research are: (1) quan- to develop a whole new level of site-specific management. tification and modeling the effects of various management practices However, we need the means to assimilate this vast (e.g., tillage, no-tillage, crop residues, and rooting patterns) on soil amount of data. A synthesis and quantification of disci- properties and soil–plant–atmosphere processes; (2) the dynamics of plinary knowledge at the whole-system level, via process- soil structure, especially soil cracks and biochannels, and their effects based modeling of agricultural systems, is essential to on surface runoff of water and mass, and preferential water and chem- develop such means and the management systems that can ical transport to subsurface waters; (3) biophysics of changes in proper- be adapted to continual change. Interactions among dis- ties and processes at the soil–plant and plant–atmosphere interfaces; ciplinary components of the agricultural systems are gen- (4) modeling contributions of agricultural soils to climate change and erally very important. Models are the only way to find and effects of climate change on soil environment and agriculture; and (5) physical (cause-effect) quantification of spatial variability of soil understand these interactions in a system, integrate var- properties and their outcomes, new methods of parameterizing a ious experimental results and observations for different variable field for field-scale modeling, and new innovative methods conditions, and extrapolate limited experimental results to of aggregating output results from plots to fields to larger scales. The other soil and climate conditions. current status of the various aspects of these research areas is re- An agricultural system is complex (Fig. 1; also see viewed briefly. The future challenges are identified that will re- Fig. 3) and needs interdisciplinary field research and quire both experimental research and development of new concepts, quantification. Integration of system models with field theories, and models. research has the potential to raise agricultural research to the next higher level. It is also an essential first step to improve model integrity, reliability, and usability. The NDERSTANDING REAL-WORLD SITUATIONS and solving integration will benefit both field research and models in Usignificant agronomic, engineering, and environmen- the following ways: tal problems require process-based synthesis and quanti- fication of knowledge at the whole system level. In the 20th . Promote a systems approach to field research, which Century, we made tremendous advances in discovering looks at all component interactions fundamental principles in different scientific disciplines . Facilitate better understanding and quantification of using reduction methods, which created major break- research results throughs in management and technology for agricultural . Promote efficient and effective transfer of field re- systems. However, as we enter the 21st Century, agricul- search results to different soil and weather condi- tural research has more difficult and complex problems to tions, and to different cropping and management solve. The environmental consciousness of the general systems outside the experimental plots public is challenging producers to modify farm manage- . Help field researchers to focus on the identified ment to protect water, air, and soil quality, while staying fundamental knowledge gaps and make field re- economically profitable. At the same time, market-based search more efficient global competition in agricultural production and the . Provide the needed field test and improvement of the models before delivery to other potential L.R. Ahuja and L. Ma, USDA-ARS, Great Plains Systems Research users—agricultural consultants, farmers, ranchers, Unit, Fort Collins, CO 80526, USA; D.J. Timlin, USDA-ARS, Crop extension agencies, and action agencies (NRCS, Systems and Global Change Lab., Beltsville, MD 20705. Received 29 EPA, and others). June 2005. *Corresponding author ([email protected]). Field-tested models can be used as decision aids or Published in Soil Sci. Soc. Am. J. 70:311–326 (2006). Reproduced from Soil Science Society of America Journal.Reviews Published by Soil Science Society of America. All copyrights reserved. and Analyses and Soil Physics guides for best management practices, including site- doi:10.2136/sssaj2005.0207 specific management or precision agriculture (Ahuja ª Soil Science Society of America 677 S. Segoe Rd., Madison, WI 53711 USA Abbreviations: DSS, decision support system. 311 312 SOIL SCI. SOC. AM. J., VOL. 70, MARCH–APRIL 2006 a lot more work is needed to bring them to the level of physics, engineering, and hydraulic system models. In particular, we need to improve on the methods and structure of building models so that: (1) the models are modular, with each model component (module) clearly defined, documented, and assigned a degree of uncer- tainty; (2) each model component can be independently tested and improved, and can be easily substituted; (3) the whole world community can contribute to developing, testing, and improving components; (4) the components may vary with the scale of application; (5) hierarchical parameter estimation from varying degree of input infor- mation is a component of the model; (6) the assembled models of the system are kept compact and easy to use by Fig. 1. Complex nature of an agriculture system, illustrated by the C-N customizing them to agroecosystem regions; (7) a user- cycle. Also see Fig. 3. friendly interface is provided for easy input of data and output of results; and (8) a well-illustrated user manual and Ma, 2002), as tools for in-depth analyses of problems is provided to illustrate a step-by-step procedure for run- in management, environmental quality, global climate ning the model and some examples of model application change effects, and other emerging issues, and as guides that demonstrate the benefits of using the model as well as for planning and policymaking (Ahuja et al., 2002). the uncertainty in results. An Object Modeling System, Models can be used to explore new ideas and strategies with a library of components (modules), being developed under different weather and climatic conditions before by the USDA-ARS (Ahuja et al., 2005), will hopefully in- testing them in expensive field experiments. The most corporate all the above features. desirable vision for agricultural research and technology transfer is to have a continual two-way interaction among SOIL PHYSICISTS CAN MAKE the cutting-edge field research, process-based models of A GREAT IMPACT agricultural systems, and management decision support systems (Fig. 2). Field research can certainly benefit from Variation of soil physical properties and their effects process models as described above, but also a great deal on soil water movement and retention, heat movement, from the feedbacks from the management decision soil temperature, chemical transport, root activity, and support systems (DSSs). On the other hand, field research soil biota functioning, involving both measurements and forms the basis for models and DSSs. theory, have been the core of soil physics research. System modeling has been a vital step in many sci- However, the scope of soil physics has gradually ex- entific disciplines. We would not have gone to the moon panded toward interdisciplinary boundaries (trans- successfully without the combined use of good data and disciplinary) because of the central role of soil water in models. In automobile designing, computer models of agricultural systems (Fig. 3). Examples of soil physics the system are increasingly replacing the scaled physical research in the interfacial areas include: modeling the models of the past. Models have also been used ex- linkage of transpiration and photosynthesis (Tanner, tensively in designing and managing water resource 1981; Tanner and Sinclaire,
Recommended publications
  • Soil Physics and Agricultural Production
    Conference reports Soil physics and agricultural production by K. Reichardt* Agricultural production depends very much on the behaviour of field soils in relation to crop production, physical properties of the soil, and mainly on those and to develop effective management practices that related to the soil's water holding and transmission improve and conserve the quality and quantity of capacities. These properties affect the availability of agricultural lands. Emphasis is being given to field- water to crops and may, therefore, be responsible for measured soil-water properties that characterize the crop yields. The knowledge of the physical properties water economy of a field, as well as to those that bear of soil is essential in defining and/or improving soil on the quality of the soil solution within the profile water management practices to achieve optimal and that water which leaches below the reach of plant productivity for each soil/climatic condition. In many roots and eventually into ground and surface waters. The parts of the world, crop production is also severely fundamental principles and processes that govern limited by the high salt content of soils and water. the reactions of water and its solutes within soil profiles •Such soils, classified either as saline or sodic/saline are generally well understood. On the other hand, depending on their alkalinity, are capable of supporting the technology to monitor the behaviour of field soils very little vegetative growth. remains poorly defined primarily because of the heterogeneous nature of the landscape. Note was According to statistics released by the Food and taken of the concept of representative elementary soil Agriculture Organization (FAO), the world population volume in defining soil properties, in making soil physical is expected to double by the year 2000 at its current measurements, and in using physical theory in soil-water rate of growth.
    [Show full text]
  • Fundamentals of Geoenvironmental Engineering
    NPTEL – Civil – Geoenvironmental Engineering Module 1 FUNDAMENTALS OF GEOENVIRONMENTAL ENGINEERING A) Scope of geoenvironmental engineering Any project that deals with the interrelationship among environment, ground surface and subsurface (soil, rock and groundwater) falls under the purview of geoenvironmental engineering (Fang and Daniels 2006). The scope is vast and requires the knowledge of different branches of engineering and science put together to solve the multi-disciplinary problems. A geoenvironmental engineer should work in an open domain of knowledge and should be willing to use any concepts of engineering and science to effectively solve the problem at hand. The most challenging aspect is to identify the unconventional nature of the problem, which may have its bearing on multiple factors. For example, an underground pipe leakage may not be due to the faulty construction of the pipe but caused due to the highly corrosive soil surrounding it. The reason for high corrosiveness may be attributed to single or multiple manmade factors, which need to be clearly identified for the holistic solution of the problem. The conventional approach of assessing the material strength of the pipe alone will not solve the problem at hand. A lot of emphasis has been laid for achieving a “green environment”. Despite a lot of effort, it is very difficult to cut off the harmful effects of pollutants disposed off into the geoenvironment. The damage has already been done to the subsurface and ground water resources, which is precious. An effective waste containment system is one of the solutions to this problem. However, such a project has different socio-economic and technical perspectives.
    [Show full text]
  • Introduction to Soil Physics - S.W
    AGRICULTURAL SCIENCES – Vol. I - Introduction to Soil Physics - S.W. Duiker and D.D. Fritton INTRODUCTION TO SOIL PHYSICS S.W. Duiker and D.D. Fritton The Department of Crop and Soil Sciences, Pennsylvania State University, Pennsylvania, USA. Keywords: Soil physics, soil texture, organic matter, bulk density, porosity, infiltration, water holding capacity, soil temperature, erosion, compaction, irrigation, drainage, water use efficiency, systems approach, interdisciplinary Contents 1. The beginning of soil physics 2. Contemporary soil physics 2.1. Theory of soil physics 2.1.1. Solid phase 2.1.2. Liquid phase 2.1.3. Gaseous phase 2.1.4. Heat flow and temperature 2.2. Applications of soil physics 2.2.1. Soil erosion 2.2.2. Soil organic matter management 2.2.3. Soil compaction 2.2.4. Irrigation 2.2.5. Drainage 2.2.6. Water use efficiency 3. The future of soil physics Glossary Bibliography Biographical Sketches Summary Soil physics is the study of the solid, liquid, and gaseous phases of soils and of fluxes of fluids and energy in soils. The solid phase consists of mineral and organic matter. The dominantUNESCO liquid in soils is water, and the– dominant EOLSS gases are similar to those in the atmosphere, except that soils contain more CO2 and water vapor and less O2. Interactions between the three phases in soils determine the movement of fluids and energy. Soil physicsSAMPLE established itself as a scientific CHAPTERS discipline in the early 20th century. Much progress has been made since then in the characterization of the physical properties and processes in soils.
    [Show full text]
  • Effect of Environmental Factors on Pore Water Pressure
    Examensarbete vid Institutionen för geovetenskaper Degree Project at the Department of Earth Sciences ISSN 1650-6553 Nr 416 Effect of Environmental Factors on Pore Water Pressure in River Bank Sediments, Sollefteå, Sweden Påverkan av miljöfaktorer på porvattentryck i flodbanksediment, Sollefteå, Sverige Hanna Fritzson INSTITUTIONEN FÖR GEOVETENSKAPER DEPARTMENT OF EARTH SCIENCES Examensarbete vid Institutionen för geovetenskaper Degree Project at the Department of Earth Sciences ISSN 1650-6553 Nr 416 Effect of Environmental Factors on Pore Water Pressure in River Bank Sediments, Sollefteå, Sweden Påverkan av miljöfaktorer på porvattentryck i flodbanksediment, Sollefteå, Sverige Hanna Fritzson ISSN 1650-6553 Copyright © Hanna Fritzson Published at Department of Earth Sciences, Uppsala University (www.geo.uu.se), Uppsala, 2017 Abstract Effect of Environmental Factors on Pore Water Pressure in River Bank Sediments, Sollefteå, Sweden Hanna Fritzson Pore water pressure in a silt slope in Sollefteå, Sweden, was measured from 2009-2016. The results from 2009-2012 were presented and evaluated in a publication by Westerberg et al. (2014) and this report is an extension of that project. In a silt slope the pore water pressures are generally negative, contributing to the stability of the slope. In this report the pore water pressure variations are analyzed using basic statistics and a connection between the pore water pressure variations, the geology and parameters such as temperature, precipitation and soil moisture are discussed. The soils in the slope at Nipuddsvägen consists of sandy silt, silt, clayey silt and silty clay. The main findings were that at 2, 4 and 6 m depth there are significant increases and decreases in the pore water pressure that can be linked with the changing of the seasons, for example there is a significant increase in the spring when the ground frost melts.
    [Show full text]
  • Part 533 – Geotechnical Engineering
    Title 210 – National Engineering Manual Part 533 – Geotechnical Engineering Subpart C – Operations 533.20 General A. Soil mechanics is a branch of soil physics and engineering mechanics that describes the behavior of soils and provides the theoretical basis for analysis in geotechnical engineering. Soil mechanics is the application of the laws and principles of mechanics and hydraulics to engineering problems dealing with soil as an engineering material. The testing of soil’s properties are typically done at a testing laboratory with specialized equipment or can be measured or correlated in the field. Soil mechanics is a subdivision of civil engineering and engineering geology that evaluates the action of forces within a soil mass for natural or artificial structures that are supported on or made of soil. B. Collection and analysis of geotechnical engineering data are essential in the investigation and design of engineering structures. The examination and verification of soil properties during construction are critical. Specialized training and experience in geotechnical engineering are needed due to the many factors which depend on interpretation and judgment of soil related issues. Close coordination is needed between the investigation, soil testing, design, and construction functions. C. Soil mechanics testing provides data for evaluating soil and rock as engineering materials for planning, design, and construction. Test results identify the index, chemical, and engineering properties used in the analysis and design of foundations and earth or earth-supported structures such as dams, buildings, bridge foundations, retaining walls, as well as the support structure of buried pipeline systems. 533.21 Data Collection A. The engineering staff or team that prepares the final design will assist in planning of the geotechnical site investigation, sample selection, and final soil testing program.
    [Show full text]
  • Soil Science 1
    Soil Science 1 Soil Chemistry and Plant Nutrition: Nutrient cycling; nutrient recovery from wastewater; molecular visualization of soil minerals SOIL SCIENCE and molecules; soil acidification. The Department of Soil Science provides undergraduate and graduate Professor William Bleam education in the environmental, agricultural, and natural resource Surface and Colloid Chemistry: Physical chemistry of soil aspects of soils. Areas of emphasis include soil ecology; soil erosion colloids and sorption processes, chemistry of humic substances, management; soil fertility and plant nutrition; soil physical and chemical factors controlling biological availability of contaminants to characterization; biogeochemistry; urban soils; soil carbon; soil health; microorganisms, magnetic resonance and synchrotron studies of soil contaminants; waste management; pedology; and land-use analysis. adsorption and precipitation. Soils are a critical natural resource in environmental protection, food Assistant Professor Zachary Freedman and fiber production, turf and grounds management, rural and urban planning, and waste disposal. All of these facets are integrated into the Soil microbiology, ecology and sustainability: Effects of environmental department's course offerings and research programs. Soil Science change on biogeochemical cycles; community ecology and trophic majors prepare for professional, technical, consulting, and project dynamics; forest soil ecology; soil organic matter dynamics; sustainable positions in environmental sciences, ecology and restoration, crop and agroecosystems; bio-based product crop production on marginal lands. timber production, soil informatics, soil conservation, environmental pollution control, turf and grounds management, and land-use planning. Professor Alfred Hartemink Please contact the department for further information on career Pedology and Digital Soil Mapping: Pedology, soil carbon; digital soil opportunities. mapping; tropical soils; history and philosophy of soil science.
    [Show full text]
  • Sos 314 Course Title: Introduction to Pedology and Soil Physics Number of Units
    http://www.unaab.edu.ng COURSE CODE: SOS 314 COURSE TITLE: INTRODUCTION TO PEDOLOGY AND SOIL PHYSICS NUMBER OF UNITS: 3 Units COURSE DURATION: Two hours per week COURSECOURSE DETAILS:DETAILS: Course Coordinator: Dr. J. K. Adesodun BSc., MSc., PhD Email: [email protected] Office Location: Room 233, COLPLANT Other Lecturers: Dr. B.A Senjobi., Dr. G.A. Ajiboye; Dr. S.J. Akinsete; and Dr. M.A. Busari COURSE CONTENT: Factors and processes of soil formation; rock weathering and common minerals in soil; soil morphological characteristics and profile description; characterization of soils using diagnostic properties; soil survey, mapping and classification. Soil texture and surface area of particles; volume-mass relationships in soil; bulk density; porosity; soil water; hydrological cycle; water balance; water content and water retention; field capacity and permanent wilting point; water flow in soils; energy balance; soil erosion and its control; conservation tillage. Practical: Field: Soil profile description; morphology; texture by feel; colour; horizon designation; sampling soil profile for water content and bulk density determination; comparing soil texture by feel wit texture by particle size distribution, soil temperature measurement in the field COURSE REQUIREMENTS: This is a compulsory course for all students in 300 level of B. Agric program in the University. In view of this, students are expected to participate in all the course activities and have a minimum of 70 % attendance to be able to write the final examination. READING LIST: 1. Fitzpatrick, E.A., 1980. Soils – Their Formation, Classification and Distribution. London: Longman, 353 pp. 2. Fitz Patrick, E.A., 1986. An Introduction to Soil Science, 2nd edn.
    [Show full text]
  • Miroslav Kutílek Professor of Soil Science, Soil Physics and Soil Hydrology
    Soil & Water Res., 3, 2008 (Special Issue 1): S5–S6 Miroslav KUTÍLEK Professor of Soil Science, Soil Physics and Soil Hydrology This thematic issue of Soil and Water Research is dedicated to Prof. Miroslav Kutílek, who cel- ebrated his 80th birthday in the past year. Prof. Kutílek has been internationally recognised for his expertise in soil science, physics and hydrology not only in the former Czechoslovakia, but worldwide. I am delighted to recapitulate here briefly his personal professional highlights as a preface to this special issue in his honour. Prof. Kutílek was born on October 8th, 1927, in Trutnov in the Czech Republic. In 1951, he was graduated at the Faculty of Civil Engineering, the Czech Technical University in Prague (Ing. degree). In 1956, he defended his Ph.D. work (CSc. degree), and in 1966, he was awarded DrSc. degree, also by CTU Prague. He entered the faculty there as an associate professor and held this post from 1962 to 1965 and again from 1968 to1973, and later served as a professor (1973–1990 and 1992–1993). He had also several long-term running lecturing and research contracts at many universities abroad: Baghdad University in 1960; the University of Khartoum, Faculty of Agriculture, Sudan, from 1965 to 1968; Bayreuth University, Fachbereich Geoökologie, Bayreuth, Germany, from 1990 to 1992; L’Institut de Mécanique, Université Grenoble, France, for many years (1979–1980, 1985, 1991); the University of California, Davis, USA, 1981–1982, and Die Technische Universität, Braunschweig, Germany, in 1989. Prof. Kutílek played a key role in the development of physical and mathematical methods aimed at replacing the empirical methods originally used in the soil science.
    [Show full text]
  • Soil Physics - Willy R
    LAND USE, LAND COVER AND SOIL SCIENCES – Vol. VI - Soil Physics - Willy R. Dierickx SOIL PHYSICS Willy R. Dierickx Retired from Ministry of the Flemish Community, Institute for Agricultural and Fisheries Research, Technology and Food Unit, Agricultural Engineering, Merelbeke, Belgium Keywords: Aggregate stability, bulk density, Darcy’s law, hydraulic conductivity, particle size distribution, porosity, Stokes’ law, water retention, soil texture, soil structure. Contents 1. Introduction 2. Soil Texture 2.1. Mineral Soil Fractions 2.1.1. Sand 2.1.2. Silt 2.1.3. Clay 2.2. Organic Soil Fraction 2.3. Particle Size Distribution 2.3.1. Particle Size Analysis 2.3.2. Cumulative Particle Size Distribution Curve 2.3.3. Textural Triangle 3. Soil Structure 3.1. Soil Structure Classification 3.2. Soil Structure Characterization 3.3. Aggregate Stability 4. Soil Physical Properties 4.1. Specific Soil Surface 4.2. Soil Density 4.2.1. Particle Density 4.2.2. Bulk Density 4.3. Porosity and Void Ratio 4.3.1. Porosity 4.3.2. Void Ratio 4.4. WaterUNESCO Content – EOLSS 4.5. Plasticity Index 5. Soil HydraulicSAMPLE Properties CHAPTERS 5.1. Saturated Hydraulic Conductivity 5.2. Unsaturated Hydraulic Conductivity 6. Agricultural Significance 6.1. Importance of Texture 6.2. Importance of Structure 6.3. Importance of Other Soil Physical Characteristics 7. Conclusions Glossary Bibliography ©Encyclopedia of Life Support Systems (EOLSS) LAND USE, LAND COVER AND SOIL SCIENCES – Vol. VI - Soil Physics - Willy R. Dierickx Biographical Sketch Summary Soil physics deals with the physical properties of the soil and their measurement, and the physical processes taking place in and through the soil.
    [Show full text]
  • Vadose Zone Characterization and Monitoring Current Technologies, Applications, and Future Developments
    3 Vadose Zone Characterization and Monitoring Current Technologies, Applications, and Future Developments Boris Faybishenko Contributors: M. Bandurraga, M. Conrad, P. Cook, C. Eddy-Dilek, L. Everett, FRx Inc. of Cincinnati, T. Hazen, S. Hubbard, A.R. Hutter, P. Jordan, C. Keller, F.J. Leij, N. Loaiciga, E.L. Majer, L. Murdoch, S. Renehan, B. Riha, J. Rossabi, Y. Rubin, A. Simmons, S. Weeks, C.V. Williams INTRODUCTION NEEDS FOR VADOSE ZONE CHARACTERIZATION AND MONITORING Vadose zone characterization and monitoring are essential for: • Development of a complete and accurate assessment of the inven- tory, distribution, and movement of contaminants in unsaturated- saturated soils and rocks. • Development of improved predictive methods for liquid flow and contaminant transport. • Design of remediation systems (barrier systems, stabilization of buried wastes in situ, cover systems for waste isolation, in situ treat- ment barriers of dispersed contaminant plumes, bioreactive treat- ment methods of organic solvents in sediments and groundwater). • Design of chemical treatment technologies to destroy or immobilize highly concentrated contaminant sources (metals, radionuclides, explosive residues, and solvents) accumulated in the subsurface. 133 134 VADOSE ZONE SCIENCE AND TECHNOLOGY SOLUTIONS Development of appropriate conceptual models of water flow and chemical transport in the vadose zone soil-rock formation is critical for developing adequate predictive modeling methods and designing cost- effective remediation techniques. These conceptual models of unsatu- rated heterogeneous soils must take into account the processes of preferential and fast water seepage and contaminant transport toward the underlying aquifer. Such processes are enhanced under episodic natural precipitation, snowmelt, and extreme chemistry of waste leaks from tanks, cribs, and other surface sources.
    [Show full text]
  • The Impact of Landscape Evolution on Soil Physics: Evolution of Soil Physical and Hydraulic Properties Along Two Chronosequences of Proglacial Moraines
    Earth Syst. Sci. Data, 12, 3189–3204, 2020 https://doi.org/10.5194/essd-12-3189-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. The impact of landscape evolution on soil physics: evolution of soil physical and hydraulic properties along two chronosequences of proglacial moraines Anne Hartmann1, Markus Weiler2, and Theresa Blume1 1GFZ German Research Centre for Geosciences, Section Hydrology, Potsdam, Germany 2Faculty of Environment and Natural Resources, University of Freiburg, Freiburg, Germany Correspondence: Anne Hartmann ([email protected]) Received: 30 April 2020 – Discussion started: 9 June 2020 Revised: 5 October 2020 – Accepted: 22 October 2020 – Published: 4 December 2020 Abstract. Soil physical properties highly influence soil hydraulic properties, which define the soil hydraulic behavior. Thus, changes within these properties affect water flow paths and the soil water and matter balance. Most often these soil physical properties are assumed to be constant in time, and little is known about their natural evolution. Therefore, we studied the evolution of physical and hydraulic soil properties along two soil chronosequences in proglacial forefields in the Central Alps, Switzerland: one soil chronosequence developed on silicate and the other on calcareous parent material. Each soil chronosequence consisted of four moraines with the ages of 30, 160, 3000, and 10 000 years at the silicate forefield and 110, 160, 4900, and 13 500 years at the calcareous forefield. We investigated bulk density, porosity, loss on ignition, and hydraulic properties in the form of retention curves and hydraulic conductivity curves as well as the content of clay, silt, sand, and gravel.
    [Show full text]
  • Pressures Recorded During Laboratory Freezing and Thawing of a Natural Silt-Rich Soil
    PRESSURES RECORDED DURING LABORATORY FREEZING AND THAWING OF A NATURAL SILT-RICH SOIL Charles Harris1, Michael C.R. Davies2 1. Department of Earth Sciences, Cardiff University, P.O. Box 914, Cardiff CF1 3YE UK e-mail: [email protected] 2. Department of Civil Engineering, University of Dundee, Dundee DH1 4HN, UK Abstract Porewater pressures in a natural silty soil were measured during seven cycles of downward soil freezing and thawing using Druck electronic pore pressure transducers placed at 50,150 and 250 mm below the surface. Surface frost heave/thaw settlement was monitored using LVDTs, and soil temperatures recorded using semi- conductor temperature sensors. A pronounced Òzero curtainÓ was observed during both soil freezing and thaw- ing, and pore pressure change followed a consistent pattern through each freeze/thaw cycle. Arrival of the freezing front led to a gradual fall in pressure to between -5 kPa and -15kPa. Just before the end of the Òzero curtainÓ period pressures rose rapidly to between 15 kPa and 40 kPa, with higher pressures at greater depths. These high pressures were maintained as the soil cooled but fell when soil warming began. Warming ahead of the thaw front progressed rapidly through the frozen soil, leading to an accelerating fall in pressure. With the arrival of the thaw Òzero curtainÓ, pore pressures became strongly negative, then rose, and became positive again when soil thawing adjacent to the transducer was complete. Freezing processes responsible for these observed pressure changes are discussed in the context of the mechanisms of soil phase change and associated frost heaving and thaw consolidation.
    [Show full text]