Presentation is loading. Please wait.

Presentation is loading. Please wait.

Dr. Selim KAPUR University of Çukurova Departments of Soil Science and Archaeometry Adana, TURKEY

Similar presentations

Presentation on theme: "Dr. Selim KAPUR University of Çukurova Departments of Soil Science and Archaeometry Adana, TURKEY"— Presentation transcript:

1 Dr. Selim KAPUR University of Çukurova Departments of Soil Science and Archaeometry Adana, TURKEY

2 Mineral Soils conditioned by Topography and Age The development of the profile is limited by the erosion exceeding soil formation or by the influence of topographic position The Reference Soil Group of the Leptosols accommodates very shallow soils over hard rock or highly calcareous material but also deeper soils that are extremely gravelly and/or stony. They are particularly common in mountain regions. Leptosols correlate with the `Lithosols' taxa of many international classification systems (USA, FAO) and with `Lithic' subgroups of other soils groupings. In many systems, Leptosols on calcareous rock are denoted `Rendzinas'; those on acid rock are also called `Rankers'.

3 Erosion, mass wasting, drought, flooding, poor drainage, and stoniness

4 Soils having continuous hard rock@ within 25 cm from the soil surface; or a mollic@ horizon with a thickness between 10 and 25 cm directly overlying material with a calcium carbonate equivalent of more than 40 percent, or less than 10 percent (by weight) fine earth from the soil surface down to a depth of 75 cm; and no diagnostic horizons other than a mollic@, ochric@, umbric@, or yermic@ horizon.

5 Mollic A-horizon, surface horizon with dark color due to organic matter; Base saturation exceeds 50%. Ochric A horizon, surface without stratification and lacking the characteristics of (A histic H-horizon, or) a mollic, umbric or fimic A-horizon Umbric, similar to a mollic A-horizon but base saturation lower than 50% Yermic, an A horizon with aridic properties and a pavement that is varnished or includes wind-shaped gravel or stones ("ventifacts"); or a pavement and a vesicular crust; or a vesicular crust above a platy A- horizon, without a pavement, or a biological crust, 1 -2 mm thick.

6 Black mollic epipedon

7 Yermic epipedon

8 Ochric epipedon BASALT LIMESTONE Lithic Leptosol Lithic (Chromic?) Leptosol

9 Calcaric Leptosols

10 Lithic, Hyperskeletic, Rendzic, Gelic, Vertic, Gleyic, Mollic, Umbric, Humic, Aridic, Gypsiric, Calcaric, Yermic, Dystric, Eutric, Haplic.

11 May be a shallow soil overlying calcareous material but a petrocalcic horizon integrates it to a Calcisol, NOT A LEPTOSOL CALCAREOUS ROCK PETROCALCIC HORIZON SOIL

12 Parent material Various kinds of rock or unconsolidated materials with less than 10 percent fine earth. Environment: High or medium altitude and with strongly dissected topography. Leptosols are found in all climatic zones, particularly in strongly eroding areas.

13 Profile development: A(B)R or A(B)C profiles with a thin A- horizon. Many Leptosols in calcareous weathering material have a mollic A-horizon that shows signs of intensive biological activity with a thin argic B.

14 From Tropics to the cold polar regions and from sea level to the highest mountains. Widespread in mountain areas, Can be found on hard rocks or where erosion has kept pace with soil formation or removed the top of the soil profile.


16 Associations with other Reference Soil Groups óShallow soils with continuous hard rock within 25 cm from the soil surface, excluding cemented layers such as a petrocalcic (laminar calcium carbonate on rock or sediment = 50% by weight, root penetration limited, extremely hard consistence when dry) or petroplinthic (Fe cementation, OC less 0.6%, limited restriction) horizon. óHowever, the definition includes also deeper soils, provided that these have less than 10% fine earth over a depth of at least 75 cm. óWHEN DISCUSSING LINKAGES BETWEEN (DIVERSE!) LEPTOSOLS AND OTHER REFERENCE SOIL GROUPS, ONE MIGHT MAKE A DISTINCTION BETWEEN LEPTIC SOIL UNITS OF OTHER REFERENCE SOIL GROUPS AND SOIL UNITS OF LEPTOSOLS.

17 Young soils, a thin A-horizon over an incipient B-horizon or directly over the unaltered rock. Presence of pedogenic differentiation despite the shallowness. Integration to other soils is common, thus they occur as associations ie undularting, mountainous, sloping soilscapes are composed of integrates of Leptosols to; I. Cambisols: with the development of a cambic horizon. II. Andosols: if tephric soil material is present in profile III. Podzols: The definition of the spodic horizon leaves the possibility open that a full-fledged Podzol exists within the depth limits of Leptosols. Such (mature!) soils are not Leptosols, despite the presence of hard rock within 25 cm from the surface, but are classified as (Leptic) Podzols. IV. Luvisols: The definition of the argic horizon (a relict Bt on the surface) precludes that an argic horizon can be present within the depth limits of Leptosols, unless there is an abrupt textural transition from the overlying horizon to the (more than 7.5 cm thick) argic horizon. In that case the soil is classified as a (Leptic) Luvisol (or Acrisol or Lixisol, depending on CEC, clay and base saturation).

18 V. Gleysols: "Gleyic properties" in Leptosols are exclusive to (deeper) soils that qualify as Leptosols because they have less than 10 percent (by weight) fine earth to a depth of at least 75 cm. "Stagnic properties" may have to be considered both in Leptosols with continuous hard rock within 25 cm of the surface and in Leptosols with less than 10 percent of fine earth to a depth of 75 cm, but Leptosols with stagnic properties have not been sufficiently documented so far. VI. Mollisols: A thin mollic epipedon overyling unalterned rock particulary at mountaionus conditions under dense natural pasture vegetation of Turkey most probably similar to the Rendzic units of Spain, Italy, France, Albania, and Crotia qualifying as Leptosols

19 an A(B)R or A(B)C sequence Rendzic (with white limestone fragments and abrupt boundary to the rock) & Mollic units more pronounced with dark brown color or black calcareous organo-mineral surface soil Stable granular structure + vermicular with earthworm activity Blocky structure with increasing smectite

20 Free-draining soils with exceptions of shallow groundwater. Shallowness, stoniness, low water holding capacity Earthworms and enchytraeid worms are the chief organisms important in carbon sequestration enchytraeid worms Earthworms

21 +A resource potential for wet-season grazing, olive orchards, and vineyard. Abandoned Roman Terraces inducing biodiversity and soil development

22 Terrace walls on karstic landscape for water harvesting +Human induced Erosion is the greatest threat. But natural erosion is almost nil beacuse of vegetation cover coupled with cracks with clay infills to retain water & inhibit movement on bare karstic surface +High population pressure (tourism), overexploitation and increasing environmental pollution lead to increasing deterioration of forests and threaten large areas of vulnerable Leptosols.

23 +Man-made terraces for SLM allocated for grazing, grain and vineyard, olive, carob, fig production on Chromic/Luvic Leptosols

Download ppt "Dr. Selim KAPUR University of Çukurova Departments of Soil Science and Archaeometry Adana, TURKEY"

Similar presentations

Ads by Google