Meteorological conditions during dust (PM10) emission from a tilled loam soil: Identifying variables and thresholds

Abstract Soil wind erosion and consequent PM 10 emission is a complex process that has been related to surface properties and meteorological conditions. Most of the studies have emphasized on the relationship between the surface conditions and the dust emission, in general on deserts and dry lakes or playas. Little is known about the influence of meteorological variables on PM 10 emission from agricultural soils. The objective of this study was to identify the most important meteorological variables involved in the emission of PM 10 , identify their threshold values, and to analyze their interaction with the soil surface conditions. Measurements were made on a loam soil (Entic Haplustoll) in the semiarid Argentinian Pampa. Horizontal mass transport (Q) and PM 10 emission were measured during two years on a bare and flat surface that was tilled periodically. The meteorological variables measured were: average and maximum wind speed, wind direction, air temperature, relative humidity and soil temperature. In 30% of the events, the PM 10 concentration at 1.8 m height exceeded the average values allowed by the World Health Organization (50 μg m −3 for a 24 h period). Maximum values exceeded 1000 μg m −3 . The slope of the PM 10 concentration gradient changed between spring − summer and autumn − winter periods. Threshold values of the studied variables were set when PM 10 concentration values at 1.8 m height were consistently above the 50 μg m −3 limit. The highest PM 10 emission rates were observed when relative humidity values were below 20% and the air temperature was higher than 30 °C. In addition when the wind speed exceeded 8 m s −1 , dust emission increased significantly. From a multiple regression analysis, results indicated that PM 10 emission was well correlated (p 10 emission in a synergistic way. However, the regression explained only 32% of the variability. Although higher average PM 10 emission values were measured during events with a crusted surface, lower average values of Q were measured during events with a crust. Field observations indicated that the complex interaction between the weather conditions and soil surface properties such as soil crusts, aggregate size distribution, soil moisture and even the soil condition when the tilling is done, can produce a high variability and unpredictability, of the PM 10 emission from bare agricultural soils.