; Soils = soilscape = geopedological setting. OUTLINE INTRODUCTION THEORETICAL BACKGROUND AND...
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Transcript of ; Soils = soilscape = geopedological setting. OUTLINE INTRODUCTION THEORETICAL BACKGROUND AND...
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Soils = soilscape = geopedological setting
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OUTLINE
• INTRODUCTION
• THEORETICAL BACKGROUND AND ILLUSTRATIVE EXAMPLES
• CONCLUSION
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•INTRODUCTION: Soil definition
• “A natural body consisting of layers (or horizons) of mineral (and/or organic constituents) of variable thickness, which differ from the parent material in their morphological, physical, chemical, and mineralogical properties and their biological characteristics”
S = f (Cl, O, R, P, T,……M)
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Definition :A soil = “pedon” is the smallest volume with a surface extent which varies from
about 1 to 10 m²”
Soil sample Pedons/ polypedons in ‘soilscape’
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Definition:Pedon / polypedon
• For mapping purposes, similar pedons are pooled together, forming a polypedon, obviously associated with variability, depending on scale
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Functions:
What does soil do? 1- Soil provides the required setting for water, nutrient, air, and heat exchange for living organisms.
2- Soil controls the water distribution;affects the movement of soluble materials.
3- Soil regulates biological activity and molecular exchanges among solid, liquid, and gaseous phases.
4- Soil acts as a filter to protect the quality of water, air, and other resources.
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What does soil do? 5- Soil provides mechanical support for living organisms and their structures. People and wildlife depend on this function.
6- Soils act:- as an archive (=history book of the landscape), - as a guide, and - as a ‘predictor’
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Soils speak out; an account of
the past, present, and future
• THEORETICAL BACKGROUND AND ILLUSTRATIVE EXAMPLES
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An account of the past, present, and future
Past Paleoecology
Present Soil Management
Future Soil Degradation/ Conservation
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Past:
Paleoecology
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History book of the landscape (archive)
Examples of features revealing paleoecology:1. Pedogenic (horizons):
* Anthropic, * Plaggen, etc * Argillic, *Agric, etc2. Geomorphic (features):
* Glacis formation:Tunisia, Morocco
* Travertine (karstic): Iran
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1. Pedogenic (horizons)
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2. Geomorphic; glacis formation2.1 Tunisian example:
Pedimentation/ planation : in practice, erosional glacis – adjacent to the mountain front— is followed by an accumulation glacis. A fan distinguishes itself from the glacis by being associated with a distributary (dichotomic) drainage pattern .
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2. Geomorphic; glacis formation 2.2 Moroccan example
Erosional glacis terraces Accumulation glacis
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2. Geomorphic; glacis formation 2.3 Iranian example
Stereogram depicting glacis Pedostratigraphy (approving)
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2. Geomorphic featuresKarstic springs; Travertine
Karst spring (dried out) Travertine in scattered patches
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Microgram of travertine speciman
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Iran:
• A wetter climate, karstic springs where travertine is spread out;
• Once upon a time (27000 yr BP-13000 yr BP) the study area was subject to cycles of erosion and sedimention, also approved by the occurrence of Argillic and Petrocalcic horizon ;
• Aridification has never been as degrading as it is today
Morocco: • Occurrence of Ultisols and Plinthite implies a wetter
and hotter climatic condition• Different vegetation cover
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Present:Soil-
management
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Present: Soil Management
Guiding features:
*Soil properties (Physico-chemical): particle size class, depth, pH,…… *Position in landscape (Site)
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When well managed
Traditional wooden device for plowing; pulled by oxen
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When mis-managed
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Future:Prediction
”A soil survey describes the characteristics of the soils in a given area, classifies the soils according to a standard system of
classification, plots the boundaries of the soils on a map, and makes predictions
about the behavior of soils.”(SSM, 1993)
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Future : Predictionregarding (possible) land degradation
Guiding features:
• Pedon (individual soil body)
• Diagnostic soil characteristics- Abrupt textural change
- COLE (coefficient of Linear Extensibility)
- (Para-) Lithic contact,……..
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Change of erosion base-level: gully formation and landslide
Landslide
Bushes hold soils together
The gully
Gully running perpendicular
Landslide
It is clearly seen that the gullyin the bottom of the vale (fig c)is triggering; landslide has occurred once the slope hasbeen de-bushed (cleared)
Fig. c
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Gullies formed
Bush land
Cereals
Ploughed for Vine tree plantation
Gully
Gully
Boundary between 2 soil series
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Incision (gully) occurs in a joint, the weakest line between two pedons
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If you want to conserve the environment
Listen to what soils say
Prevention is better than cure
• CONCLUSION:
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Is check-dam solving the problem?!
Slump
Check-dam does not help
The first check dam
Second trial
Water goes like this; neglecting the dam
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Rferences
Rosa M.Poch (editor- in- Chief) and Kovda, Irnia and Curtis Monger (Guest editors). 2013.1st volume of the proceedings of the 14th IWMSM.Departament de Medi Ambient i Ciències del Sòl Universitat de Lleida Av. Rovira Roure 191, 25198 Lleida (Catalonia)
Buol, S.W., Hole, F.D., and R.J. McCracken. 1973. Soil Genesis and Classification. The Iowa State University Press, Ames.
Farshad, A. 2006. Introduction to Applied Geomorphology for Soil Scientists (Geopedologists). Lecture-notes, Department of Earth System Analysis (ESA), ITC, Enschede, The Netherlands.
USDA, 1975. Soil Taxonomy, A Basic System of Soil Classification for Making Interpreting Soil Surveys. Soil Survey Staff. Agricultural Handbook No. 436.
Zinck, G.A. 1988/89. Physiography and soils; soil survey courses (Lecture-notes), ITC, Enschede, The Netherlands.