Interdisciplinarity of hydropedology
A new interdisciplinary subject hydropedology is developing owing to the necessity of sustaining optimal environments. Hydropedology provides the bridge between the disciplines of pedology, including soil macro- and micromorphology and vadose zone hydrology together with other disciplines dealing wi...
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| Published in | Geoderma Vol. 138; no. 3; pp. 252 - 260 |
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| Main Authors | , |
| Format | Journal Article |
| Language | English |
| Published |
Amsterdam
Elsevier B.V
15.03.2007
Elsevier |
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| Online Access | Get full text |
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| Abstract | A new interdisciplinary subject hydropedology is developing owing to the necessity of sustaining optimal environments. Hydropedology provides the bridge between the disciplines of pedology, including soil macro- and micromorphology and vadose zone hydrology together with other disciplines dealing with land, air and water interfaces. Soil taxons and soil-forming processes are defined phenomenologically. Soil-forming processes which are usually linked have rates that differ by orders of magnitude. And, if soil polygenesis is considered, too, the equilibrium concept between the properties of soil taxons and soil forming factors is not applicable. The coupling of such processes on various tensorial orders leads to the conclusion that anisotropy is a general characteristic of soils. In order to ascertain the links between pedology and hydropedology, the formulation of physically meaningful transport parameters from a quantified knowledge of soil micromorphology is required. This linkage is achieved when the pore size distribution is reflected by the soil hydraulic functions, i.e. by the soil water retention equation and by the unsaturated hydraulic conductivity function. In future research, parameters of such functions must be related to quantified soil micromorphologic characteristics. The first attempt evaluating both functions is presented for soils manifesting a distinct bi-modal pore size distribution. A close cooperation of hydropedology with soil chemistry and microbiology will produce an insight into the role of organic substances upon the change of soil hydraulic parameters. The substances appear either as a consequence of soil pollution, or due to soil organic matter transformation. An example is presented on the change of saturated hydraulic conductivity caused by the adsorption of organic cations. Similar linkages are expected from the cooperation of hydropedology with plant physiology when the role of plant exudates upon the change of soil hydraulic functions is studied. |
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| AbstractList | A new interdisciplinary subject hydropedology is developing owing to the necessity of sustaining optimal environments. Hydropedology provides the bridge between the disciplines of pedology, including soil macro- and micromorphology and vadose zone hydrology together with other disciplines dealing with land, air and water interfaces. Soil taxons and soil-forming processes are defined phenomenologically. Soil-forming processes which are usually linked have rates that differ by orders of magnitude. And, if soil polygenesis is considered, too, the equilibrium concept between the properties of soil taxons and soil forming factors is not applicable. The coupling of such processes on various tensorial orders leads to the conclusion that anisotropy is a general characteristic of soils. In order to ascertain the links between pedology and hydropedology, the formulation of physically meaningful transport parameters from a quantified knowledge of soil micromorphology is required. This linkage is achieved when the pore size distribution is reflected by the soil hydraulic functions, i.e. by the soil water retention equation and by the unsaturated hydraulic conductivity function. In future research, parameters of such functions must be related to quantified soil micromorphologic characteristics. The first attempt evaluating both functions is presented for soils manifesting a distinct bi-modal pore size distribution. A close cooperation of hydropedology with soil chemistry and microbiology will produce an insight into the role of organic substances upon the change of soil hydraulic parameters. The substances appear either as a consequence of soil pollution, or due to soil organic matter transformation. An example is presented on the change of saturated hydraulic conductivity caused by the adsorption of organic cations. Similar linkages are expected from the cooperation of hydropedology with plant physiology when the role of plant exudates upon the change of soil hydraulic functions is studied. |
| Author | Kutílek, Miroslav Nielsen, Donald R. |
| Author_xml | – sequence: 1 givenname: Miroslav surname: Kutílek fullname: Kutílek, Miroslav email: miroslav.kutilek@volny.cz organization: Emeritus Professor, Nad Patankou 34, 160 00 Prague 6, Czech Republic – sequence: 2 givenname: Donald R. surname: Nielsen fullname: Nielsen, Donald R. organization: Department of Land, Air and Water Resources, University of California, Davis, California 95616, USA |
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| Keywords | Soil genesis Soil hydraulic functions Pedology Soil hydrology Soil micromorphology anisotropy soil sciences air Knowledge Pore size magnitude size distribution interfaces processes hydrology Property of soil bridges transport micromorphology water unsaturated zone Optimum concepts Characteristics Environment Parameter equilibrium Unsaturated soil Interdisciplinary field |
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| SubjectTerms | Agronomy. Soil science and plant productions Biological and medical sciences Earth sciences Earth, ocean, space Exact sciences and technology Fundamental and applied biological sciences. Psychology Pedology Soil genesis Soil hydraulic functions Soil hydrology Soil micromorphology Soils Surficial geology |
| Title | Interdisciplinarity of hydropedology |
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