Pedosphere 25(4): 613--621, 2015
ISSN 1002-0160/CN 32-1315/P
©2015 Soil Science Society of China
Published by Elsevier B.V. and Science Press
Deposition of nutrients from Harmattan dust in Ghana, West Africa
H. BREUNING-MADSEN1, T. W. AWADZI2 and G. LYNGSIE1
1Institute of Geosciences and Natural Resource Management, University of Copenhagen, Oster Voldgade 10, 1350 Copenhagen K (Denmark)
2Department of Geography and Resource Development, University of Ghana, PO Box LG 59, Legon, Accra (Ghana)
ABSTRACT
      In order to measure dust’s nutrient input on farmland in different agro-ecological zones, Harmattan dust was sampled by mats with plastic straw in Ghana between 2002–2006. The inputs of total nutrients by Harmattan dust in Ghana per Harmattan period were about 1–2 kg Ca ha-1, 0.5–2 kg K ha-1, 0.5–1.5 kg Mg ha-1 and less than 0.5 kg P ha-1. Compared with the annual input of nutrients by precipitation, the dust accounted for 10% or less of Ca, Mg and K but approximately 20%–40% of P. The input of nutrients by dust was only valid for areas with vegetation, because in areas with none or sparse vegetation, loss of soil due to wind erosion and hereby loss of nutrients might be significant. In farmland areas with bare and vegetated fields there seemed to be an internal redistribution of the nutrients and not a net gain of nutrients from outside the area (long-range transported dust). The input of P by dust might be of some importance in the traditional shifting cultivation systems, while the inputs of other three nutrients of Ca, Mg and K were so low that they must be considered insignificant. In the intensive agriculture systems with huge inputs of manures and fertilizers the nutrient input by dust is insignificant and could be neglected.
Key Words:  deposition rate, dust deposition, input of nutrient, long-range transported dust, nutrient concentration, traditional agricultural system
Citation: Breuning-madsen, H., Awadzi, T. W. and Lyngsie, G. 2015. Deposition of nutrients from Harmattan dust in Ghana, West Africa. Pedosphere. 25(4): 613-621.
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