SciELO - Scientific Electronic Library Online

 
vol.37 issue2Changes in soil use: infiltration capacity in the center of Córdoba (Argentina)Bacterial groups in a typical argiudol with application of glyphosate: influence on bacteria of nitrogen author indexsubject indexarticles search
Home Pagealphabetic serial listing  

Services on Demand

Journal

Article

Indicators

  • Have no cited articlesCited by SciELO

Related links

  • Have no similar articlesSimilars in SciELO

Share


Ciencia del suelo

On-line version ISSN 1850-2067

Abstract

AVECILLA, Fernando; PANEBIANCO, Juan Esteban  and  BUSCHIAZZO, Daniel Eduardo. Wind erosion and pm10 emission in two agricultural soils of La Pampa province, Argentina. Cienc. suelo [online]. 2019, vol.37, n.2, pp.209-224. ISSN 1850-2067.

The objective of this study was to evaluate the wind erosion and emission of fine particles (PM10) on two agricultural soils: a loam soil (F) and sandy loam soil (AF). Measurements were made during two consecutive years at two experimental plots of 80 x 200m oriented north-south. The horizontal mass transport (Q) and the PM10 emission were quantified. The average Q in F (6.955E-05 kg m-2 s-1) was higher than in AF (4.19E-06 kg m-2 s-1) due to the higher wind speeds and lower vegetation cover in F. In F the mass transport increased linearly with distance, while in AF it stabilized between 100 and 150m, indicating that on fine-textured soils the maximum Q could be reached at greater distances than at coarser textured soils. The PM10 emission was higher in F (5.05E- 09 kg m-2 s-1) than in AF (6.64E-10 kg m-2 s-1), probably on one hand due to the high Q occurred in F and on the other hand, to the different composition of the material transported by saltation, composed predominantly by aggregated fine particles that were progressively fragmented, emitting PM10. On the contrary, in AF the material transported by saltation is predominantly composed of individual particles that are fragmented to a lesser extent. For this reason, the emission efficiency was also higher in F for all the wind-erosion events. However, we found that this parameter changes depending on the weather (average wind speed) and soil conditions (aggregates size distribution of topsoil) that prevail during each erosive event, even on the same soil.

Keywords : Wind erosion; Soil; PM10; Mineral dust.

        · abstract in Spanish     · text in Spanish

 

Creative Commons License All the contents of this journal, except where otherwise noted, is licensed under a Creative Commons Attribution License