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We evaluated the deposition rate of atmospheric dust in a non urban area of the Granada Depression (SE of Iberian Peninsula). By using in part existing methodology, we determined a rate of 23.06 g&#194;&#183;m2&#194;&#183;yr-1 on the basis of weekly observations, that showed marked variations, partially controlled by Saharan winds. The components of the dust can indicate source area. Thus, southerly winds provide considerable allochthonous components from North Africa, while others are local. Despite the scarcity of industrial activity, signs of contamination were recorded. The employed methodology complements the work methods used by other researchers. The role of airborne sediments provides an illustration in soil genesis of the Mediterranean region. La Depresi&#243;n de Granada (SE de la Pen&#237;nsula Ib&#233;rica) presenta, en &#225;reas no urbanas y no industriales, una tasa anual de deposici&#243;n de polvo atmosf&#233;rico de 23,06 g&#194;&#183;m2&#194;&#183;a&#241;o-1 , obtenida a partir de observaciones semanales durante el a&#241;o 1992. Este dato es el resultado de una metodolog&#237;a propia, que complementa los m&#233;todos de trabajo seguidos por otros investigadores. Dada la ubicaci&#243;n de la estaci&#243;n, este valor es representativo del fondo regional de part&#237;culas s&#243;lidas en suspensi&#243;n. La distribuci&#243;n temporal de las tasas presenta importantes fluctuaciones, relacionadas con la direcci&#243;n predominante del viento, que tambi&#233;n parece tener influencia sobre los componentes del polvo. Estos datos se integran en el conocimiento de los procesos edafogen&#233;ticos de los suelos mediterr&#225;neos

Tasas de deposición de polvo atmosférico en un área semiárida del entorno mediterráneo occidental