The development and application of a wind erosion model for the assessment of fugitive dust emissions from mine tailings dumps

2007 ◽  
Vol 21 (3) ◽  
pp. 198-218 ◽  
Author(s):  
L. Chane Kon ◽  
S. Durucan ◽  
A. Korre
2009 ◽  
Vol 34 (13) ◽  
pp. 1743-1757 ◽  
Author(s):  
Gerardo Fratini ◽  
Monia Santini ◽  
Paolo Ciccioli ◽  
Riccardo Valentini

Author(s):  
Sandra Sorte ◽  
Myriam Lopes ◽  
Vera Rodrigues ◽  
Joana Leitão ◽  
Alexandra Monteiro ◽  
...  

Land ◽  
2020 ◽  
Vol 9 (12) ◽  
pp. 503
Author(s):  
Heleen Vos ◽  
Wolfgang Fister ◽  
Frank Eckardt ◽  
Anthony Palmer ◽  
Nikolaus Kuhn

The sandy croplands in the Free State have been identified as one of the main dust sources in South Africa. The aim of this study was to investigate the occurrence and strength of physical soil crusts on cropland soils in the Free State, to identify the rainfall required to form a stable crust, and to test their impact on dust emissions. Crust strength was measured using a fall cone penetrometer and a torvane, while laboratory rainfall simulations were used to form experimental crusts. Dust emissions were measured with a Portable In-Situ Wind Erosion Laboratory (PI-SWERL). The laboratory rainfall simulations showed that stable crusts could be formed by 15 mm of rainfall. The PI-SWERL experiments illustrated that the PM10 emission flux of such crusts is between 0.14% and 0.26% of that of a non-crusted Luvisol and Arenosol, respectively. The presence of abraders on the crust can increase the emissions up to 4% and 8% of the non-crusted dust flux. Overall, our study shows that crusts in the field are potentially strong enough to protect the soil surfaces against wind erosion during a phase of the cropping cycle when the soil surface is not protected by plants.


2015 ◽  
Vol 25 (5) ◽  
pp. 551-569 ◽  
Author(s):  
Eleftheria Chalvatzaki ◽  
Thodoros Glytsos ◽  
Mihalis Lazaridis

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