Soil aggregate stability under different Mediterranean vegetation types

The influence of vegetation type on soil erodibility was studied by means of aggregate stability measurements using the Modified Emerson Water Dispersion Test (MEWDT), water-drop impacts (CND and TDI) and Ultrasonic Disruption (UD) methods on soils from north-facing slopes of the mountain range of La Serra Grossa in the eastern Iberian Peninsula. Soils with similar characteristics but covered by the main plant species at the study area were selected. Quercus ilex woodland showed the most resistant soil aggregates followed by Q. coccifera and Pistacea lentiscus scrubland, Brachypodium retusum grassland and Pinus halepensis woodland. Aggregates developed beneath dwarf shrubs like Rosmarinus officinalis, Thymus vulgaris, Ulex parviflorus and Anthyllis cystisoides were least resistant. The different methods and tests applied are useful to study the soil aggregate stability. The MEWDT and TDI tests showed only minor differences between samples due to the high aggregate resistance and the low energy applied by these tests. CND and UD tests are considered to be more suitable for resistant Mediterranean soil developed on limestone due to the greater energy applied. Aggregates tested from an initially moist (pF1) condition were always more stable than air dried aggregates. Rangeland management after disturbances by fire, agriculture or grazing, etc. should try to establish natural woodland (Q. ilex) in order to get the most stable soil. Alternative vegetation cover to the climax vegetation that give high aggregate stability are Q. coccifera and P. lentiscus scrublands. Immediately after disturbance, B. retusum grassland seems to be the best option for soil protection.

[1]  John Doe,et al.  Soil Map of the World , 1962 .

[2]  Isric FAO - Unesco Soil map of the world : revised legend with corrections and updates , 1997 .

[3]  A. J. Low THE STUDY OF SOIL STRUCTURE IN THE FIELD AND THE LABORATORY , 1954 .

[4]  Manuel Costa La Vegetación en el País Valenciano , 1986 .

[5]  W. Emerson,et al.  A Classification of Soil Aggregates Based on Their Coherence in Water , 1967 .

[6]  M. Wood,et al.  Flash grazing and trampling: effects on infiltration rates and sediment yield on a selected New Mexico range site , 1989 .

[7]  W. H. Blackburn,et al.  Sediment production as influenced by livestock grazing in the Texas rolling plains. , 1981 .

[8]  Artemi Cerdà,et al.  Fire and aspect induced differences on the erodibility and hydrology of soils at La Costera, Valencia, southeast Spain , 1995 .

[9]  A. Imeson,et al.  Aggregate Stability Dynamics as Affected by Soil Temperature and Moisture Regimes , 1996 .

[10]  T. McCalla WATER‐DROP METHOD OF DETERMINING STABILITY OF SOIL STRUCTURE , 1944 .

[11]  F. D. Whisler,et al.  Surface sealing and infiltration. , 1990 .

[12]  F. di Castri,et al.  Ecosystems of the world [Vol.] 11. Mediterranean-type shrublands. , 1981 .

[13]  J. M. Bremner,et al.  Effect of Probe Condition on Ultrasonic Dispersion of Soils by Probe-Type Ultrasonic Vibrators 1 , 1972 .

[14]  A. Imeson An Eco-Geomorphological Approach to the Soil Degradation and Erosion Problem , 1986 .

[15]  J. Verstraten,et al.  The erodibility of highly calcareous soil material from southern Spain , 1985 .

[16]  R. Morgan Soil Erosion and Conservation , 1988 .

[17]  Philippe Duchaufour Manual de edafología , 1987 .

[18]  E. Bergsma,et al.  Drop testing aggregate stability of some soils near Merida, Spain , 1981 .

[19]  A. Imeson,et al.  Climatic and altitudinal effects on soil aggregation in slopes of mediterranean environment , 1995 .

[20]  Haiquan Zhang Organic matter incorporation affects mechanical properties of soil aggregates , 1994 .

[21]  T. Dunne,et al.  Effects of Rainfall, Vegetation, and Microtopography on Infiltration and Runoff , 1991 .

[22]  J. M. Bremner,et al.  MICROAGGREGATES IN SOILS1 , 1967 .

[23]  J. L. Ternan,et al.  A field study of the influence of land management and soil properties on runoff and soil loss in central Spain , 1995, Environmental monitoring and assessment.

[24]  A. Parsons,et al.  Hydrologic and sediment responses to simulated rainfall on desert hillslopes in southern Arizona , 1988 .

[25]  A. Imeson,et al.  Assessing soil aggregate stability by water-drop impact and ultrasonic dispersion , 1984 .

[26]  F. E. Egler Ecosystems of the World , 1960 .

[27]  Rattan Lal,et al.  Soil Erosion Research Methods , 1994 .

[28]  A. Williams,et al.  AGGREGATE STABILITY OF SOILS IN CENTRAL SPAIN AND THE ROLE OF LAND MANAGEMENT , 1996 .

[29]  R. Evans Some soil factors influencing accelerated water erosion of arable land , 1996 .

[30]  A. Walkley,et al.  AN EXAMINATION OF THE DEGTJAREFF METHOD FOR DETERMINING SOIL ORGANIC MATTER, AND A PROPOSED MODIFICATION OF THE CHROMIC ACID TITRATION METHOD , 1934 .

[31]  J. Oades,et al.  The retention of organic matter in soils , 1988 .

[32]  J. Oades The role of biology in the formation, stabilization and degradation of soil structure , 1993 .

[33]  A. Cerda,et al.  Soil aggregate stability in three Mediterranean environments , 1996 .