The Impact of Agriculture on Soil Texture Due to Wind Erosion. (31st July 2014)

• Record Type: Journal Article
• Authors: Colazo, Juan Cruz; Buschiazzo, Daniel
• Is Part Of: Land degradation & development. Volume 26:Number 1(2015)
• Page Start: 62
• Page End: 70
• Publication Date: 2014-07-31
• Subjects: Land degradation -- Periodicals; Soil conservation -- Periodicals; Reclamation of land -- Periodicals; Land use -- Periodicals; Economic development -- Environmental aspects -- Periodicals; 333.7315
• DOI: 10.1002/ldr.2297
• Languages: English
• ISSNs: 1085-3278

Abstract

<abstract abstract-type="main"> <title>Abstract</title> <p>Wind erosion produces textural changes on topsoil of semiarid and arid environments; however, the selection of particles on different textured soils is unclear. Our objectives were to evaluate textural changes induced by wind erosion on cultivated soils of different granulometry and to asses if textural changes produced by wind erosion are linked to aggregation of granulometric particles into different sizes of aggregates formed in contrasting textured soils. Considering this, we studied the particle size distribution (PSD) with full dispersion (PSD<sub>F</sub>) of 14 cultivated (CULT) and uncultivated (UNCULT) paired soils and, on selected sites, the PSD with minimum dispersion (PSD<sub>MIN</sub>) and the quotient PSD<sub>MIN/F</sub>. Results showed that the content of silt plus clay was lower in CULT than in UNCULT in most of the sites. The highest removal of silt was produced in soils with low sand and high silt content; meanwhile, the highest removal of clay was observed in soils with medium sand content. According to PSD<sub>MIN</sub>, particles of 250–2, 000 μm predominated in the sandy soil, in the loamy soil particles between 50 and 250 μm and in the silty loam soil particles between 2 and 50 μm. For clay sized particles, PSD<sub>MIN/F</sub> was lower than 1 in all soils and managements, but this quotient was higher in CULT compared with UNCULT only in the loamy soil. This means a decrease of clay accumulation in aggregates of larger sizes produced by agriculture, which indicates an increase in the risk of removal of these particles by wind in loamy soils. Copyright © 2014 John Wiley & Sons, Ltd.</p> </abstract>