Book contents
- Frontmatter
- Contents
- List of contributors
- Preface
- Acknowledgements
- 1 Concepts of soils
- 2 Pedogenic processes and pathways of horizon differentiation
- 3 Soil phases: the inorganic solid phase
- 4 Soil phases: the organic solid phase
- 5 Soil phases: the liquid phase
- 6 Soil phases: the gaseous phase
- 7 Soil phases: the living phase
- 8 The State Factor theory of soil formation
- 9 Factors of soil formation: parent material. As exemplified by a comparison of granitic and basaltic soils
- 10 Factors of soil formation: climate. As exemplified by volcanic ash soils
- 11 Factors of soil formation: topography
- 12 Factors of soil formation: biota. As exemplified by case studies on the direct imprint of trees on trace metal concentrations in soils
- 13 Factors of soil formation: time
- 14 Soil formation on Earth and beyond: the role of additional soil-forming factors
- 15 Soil functions and land use
- 16 Physical degradation of soils
- 17 Chemical degradation of soils
- 18 The future of soil research
- Appendix: Naming soils and soil horizons
- References
- Index
13 - Factors of soil formation: time
Published online by Cambridge University Press: 11 November 2009
- Frontmatter
- Contents
- List of contributors
- Preface
- Acknowledgements
- 1 Concepts of soils
- 2 Pedogenic processes and pathways of horizon differentiation
- 3 Soil phases: the inorganic solid phase
- 4 Soil phases: the organic solid phase
- 5 Soil phases: the liquid phase
- 6 Soil phases: the gaseous phase
- 7 Soil phases: the living phase
- 8 The State Factor theory of soil formation
- 9 Factors of soil formation: parent material. As exemplified by a comparison of granitic and basaltic soils
- 10 Factors of soil formation: climate. As exemplified by volcanic ash soils
- 11 Factors of soil formation: topography
- 12 Factors of soil formation: biota. As exemplified by case studies on the direct imprint of trees on trace metal concentrations in soils
- 13 Factors of soil formation: time
- 14 Soil formation on Earth and beyond: the role of additional soil-forming factors
- 15 Soil functions and land use
- 16 Physical degradation of soils
- 17 Chemical degradation of soils
- 18 The future of soil research
- Appendix: Naming soils and soil horizons
- References
- Index
Summary
The factors of parent material, climate, topography and organisms are tangible and can be seen and/or touched. By contrast, time is intangible and progressive as the others interact with each other (Fig. 13.1). Time is presented within the Newtonian philosophy which deals with absolute time and space considered as a world framework. Alternatively time can itself be considered as an infinite and ever-increasing universe in which the other factors interact to produce an infinite number of soils, or more precisely soil horizons, the infinite composites of which comprise soils. Perhaps within this context there should be a consideration of the energy in soils (Blum, 1997). There are four main sources of energy – gravity, mineral energy, solar and capillarity (anti-gravity). All processes in soils are dependent upon energy; for example translocation is largely dependent on gravity, while climatic change is largely dependent upon variations of solar radiation.
Climate is not constant and may change to induce different processes, or there may be a change in vegetation as a result of human activity, natural successions or events such as fire. Thus although the progression through time is uninterrupted, the processes may change, leading to a different situation which will show a combination of the properties acquired by the first progression with the imprint of the new properties acquired by the new set of processes. The result will depend upon the strength of the two or more sets of properties.
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- Soils: Basic Concepts and Future Challenges , pp. 181 - 192Publisher: Cambridge University PressPrint publication year: 2006
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