Abstract
Aeolian (wind) erosion is most common in arid regions. The resulted emission of PM10 (particulate matter that is smaller than 10 μm in diameter) from the soil has many environmental and socioeconomic consequences such as soil degradation and air pollution. Topsoil resistance to aeolian transport highly depends on the surface composition. The study aim was to examine variations in PM10 fluxes in a desert-dust source due to surface composition and topsoil disturbance. Aeolian field experiments using a boundary layer wind tunnel alongside soil composition analysis were integrated in this study. The results show variations in PM10 fluxes (ranging from 9.5 to 524.6 mg m−2 min−1) in the studied area. Higher wind velocity increased significantly the PM10 fluxes in all surface compositions. A short-term natural disturbance caused changes in the aggregate soil distribution (ASD) and increased significantly PM10 emissions. Considering that PM10 contains clays, organic matter, and absorbed elements, the recorded PM10 fluxes are indicative of the potential soil loss and degradation by wind erosion in such resource-limited ecosystems. The findings have implications in modeling dust emission from a source area with complex surfaces.
Similar content being viewed by others
References
Al-Dousari AM, Al-Awadhi J (2012) Dust fallout in northern Kuwait, major sources and characteristics. Kuwait Journal of Science and Engineering 39(2 A):171–187
Bacon SN, McDonald EV, Amit R, Enzel Y, Crouvi O, 2011. Total suspended particulate matter emissions at high friction velocities from desert landforms. Journal of Geophysics Research, 116, doi:10.1029/2011JF001965
Baddock MC, Zobeck TM, Van Pelt RS, Fredrickson EL (2011) Dust emissions from undisturbed and disturbed, crusted playa surfaces: cattle trampling effects. Aeolian Res 3(1):31–41
Bagnold RA (1941) The physics of wind blown sand and desert dunes. Methuen, London, 265
Belnap J, Gillette D (1998) Vulnerability of desert biological soil crusts to wind erosion: the influences of crust development, soil texture, and disturbance. J Arid Environ 39:133–142
Ganor E, Kronfeld J, Feldman HR, Rosenfeld A, Ilani S (2009) Environmental dust: a tool to study the patina of ancient artifacts. J Arid Environ 73(12):1170–1176
Gillies JA, Nickling WG, King J (2006) Aeolian sediment transport through large patches of roughness in the atmospheric inertial sublayer. J Geophys Res 111:F02006. doi:10.1029/2005JF000434
Hevia GG, Mendez M, Buschiazzo DE (2007) Tillage affects soil aggregation parameters linked with wind erosion. Geoderma 140(1):90–96
Hoffmann C, Funk R (2015) Diurnal changes of PM10-emission from arable soils in NE-Germany. Aeolian Res 17:117–127
Katra I, Lancaster N (2008) Surface-sediment dynamics in a dust source from spaceborne multispectral thermal infrared data. Remote Sens Environ. doi:10.1016/j.rse.2008.03.016
Katra I, Yizhaq H, Kok JF (2014) Mechanisms limiting the growth of aeolian megaripples. Geophys Res Lett. doi:10.1002/2013GL058665
Katra I, Gross A, Swet N, Tanner S, Krasnov H, Angert A (2016) Substantial dust loss of bioavailable phosphorus from agricultural soils. Scientific Reports 6:24736
King J, Nickling GW (2005) Representation of vegetation and other nonerodible elements in aeolian shear stress partitioning models for predicting transport threshold. Journal of Geophysics Research 110:F04015. doi:10.1029/2004JF000281
Klute A (1986) Methods of soil analysis. part 1. physical and mineralogical methods. American Society of Agronomy, Inc
Kok JF, Parteli EJ, Michaels TI, Karam DB (2012) The physics of wind-blown sand and dust. Rep Prog Phys 75(10):106901
Krasnov H, Katra I, Koutrakis P, Friger M (2014) Contribution of dust storms to PM10 levels in an urban arid environment. J Air Waste Manage Assoc 64:89–94
Langston G, McKenna Neuman C (2005) An experimental study on the susceptibility of crusted surfaces to wind erosion: a comparison of the strength properties of biotic and salt crusts. Geomorphology 72:40–53
Li F, Kang L, Zhang H, Zhao L, Shirato Y, Taniyama I (2005) Changes in intensity of wind erosion at different stages of degradation development in grasslands of Inner Mongolia, China. J Arid Environ 62(4):567–585
Li H, Tatarko J, Kucharski M, Dong Z (2015) PM2. 5 and PM10 emissions from agricultural soils by wind erosion. Aeolian Research
Pansu M, Gautheyrou J (2006) Handbook of soil analysis: mineralogical, organic and inorganic methods Springer
Rowell DL (1994) Soil science: methods and applications. Longman Group Limited, Longman Scientific & Technical
Shao Y (2008) Physics and modelling of wind erosion (Vol. 37). Springer Science & Business Media
Shao Y, Raupach MR, Findlater PA (1993) Effect of saltation bombardment on the entrainment of dust by wind. J Geophys Res 98:12719–12726
Sharratt B, Wendling L, Feng G (2010) Windblown dust affected by tillage intensity during summer fallow. Aeolian Res 2:129–134
Singh P, Sharratt B, Schillinger WF (2012) Wind erosion PM10 emission affected by tillage system in the world’s driest rainfed wheat region. Soil Tillage Res 124:219–225
Sweeney MR, Mason JA (2013) Mechanism of dust emission from Pleistocene loess deposits, Nebraska, USA. J Geophys Res 118:1460–1471
Sweeney MR, McDonald EV, Etyemezian V (2011) Quantifying dust emissions from desert landforms, eastern Mojave Desert, USA. Geomorphology 135:21–34
Swet N, Katra I (2016) Reduction in soil aggregation in response to dust emission processes. Geomorphology 268:177–183
Tanner S, Katra I, Haim A, Zaady E (2016) Short-term soil loss by aeolian erosion in response to conventional and organic agricultural practices. Soil Tillage Res 155:146–156
Tisdall J, Oades J (1982) Organic matter and water-stable aggregates in soils. J Soil Sci 33(2):141–163
Van Pelt RS, Baddock MC, Zobeck TM, Schlegel AJ, Vigil MF, Acosta Martinez V (2013) Field wind tunnel testing of two silt loam soils on the North America central high plains. Aeolian Res 10:53–59
Vodonos A, Friger M, Katra I, Avnon L, Krasnov H, Koutrakis P, Schwatz J, Lior O, Novack V (2014) The impact of desert dust exposures on hospitalizations due to exacerbation of chronic obstructive pulmonary disease. Air Quality, Atmosphere & Health 7(4):433–439
Wolfe SA, Nickling WG (1993) The protective role of sparse vegetation in wind erosion. Prog Phys Geogr 17:50–68
Yitshak-Sade M, Novack V, Katra I, Gorodischer R, Tal A, Novack L (2015) Non-anthropogenic dust exposure and asthma medication purchase in children. Eur Respir J 45(3):652–660
Zaady E, Katra I, Yizhaq H, Kinast S, Ashkenazy Y (2014) Inferring the impact of rainfall gradient on biocrusts’ developmental stage and thus on soil physical structures in sand dunes. Aeolian Res 13:81–89
Acknowledgments
The study was supported by grants from the Israel Science Foundation (1100/11) and the Nuclear Research Center-Negev Israel.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Edri, A., Dody, A., Tanner, S. et al. Variations in dust-related PM10 emission from an arid land due to surface composition and topsoil disturbance. Arab J Geosci 9, 607 (2016). https://doi.org/10.1007/s12517-016-2651-z
Received:
Accepted:
Published:
DOI: https://doi.org/10.1007/s12517-016-2651-z