Influence of Salinity and Sodicity on Soil Structural and Hydraulic Characteristics

• Published in: Soil Science Society of America journal Vol. 59; no. 6; pp. 1701 - 1708
• Main Authors: Crescimanno, Giuseppina, Iovino, Massimo, Provenzano, Giuseppe
• Format: Journal Article
• Language: English
• Published: Madison, WI Soil Science Society of America 01-11-1995; American Society of Agronomy
• Subjects: Agronomy; Agronomy. Soil science and plant productions; Biological and medical sciences; Fundamental and applied biological sciences. Psychology; Hydrology; Irrigation; Saline water; Soil degradation; Soil erosion, conservation, land management and development; Soil properties; Soil quality; Soil science; Soil testing; Water management; Laboratory study; Structure stability; Swelling; Soil structure; Hydraulic conductivity; Shrinkage; Inorganic element; Salinity; Soils; Vertisols; Soil water properties; Sodium; Soil analysis; Analysis; Exchangeable sodium percentage; Chemical properties; Aggregate
• ISSN: 0361-5995; 1435-0661
• DOI: 10.2136/sssaj1995.03615995005900060028x

An exchangeable sodium percentage (ESP) >15 is traditionally considered to affect soil structural and hydraulic characteristics. Recent investigations show that both this critical value and the concept of critical threshold need reconsideration, because soil degradation often takes place even at lower ESP in dilute solutions, and soil behavior at increasing ESP appears to be a continuum. This study was carried out to analyze the response of two Sicilian Typic Haploxererts to ESP values up to 15, at a low cationic concentration. The investigation was carried out on aggregate stability, rating of soil shrink‐swell potential, and both saturated and unsaturated hydraulic conductivity. The specific purpose was to verify if a critical ESP threshold exists, or if the hypothesis of a continuum behavior is more appropriate. The high‐energy moisture characteristic technique was used for determining aggregate stability, and Brasher's method for the shrinkage characteristic. The constant‐head method was used for determining saturated hydraulic conductivity, and the parameter estimation method based on one‐step outflow experiments for unsaturated hydraulic conductivity. Almost linear relationships were found between the investigated soil properties and ESP, indicating no critical ESP threshold; furthermore, the results obtained indicate that an effective hazard of soil quality degradation can be forecast even in a 2 to 5 ESP range at a low cationic concentration. This is a basic indication for irrigation management aimed to combat and prevent degradation of soil quality.