Movement and paths of dust phenomena affecting Najaf Governorate

The ability of the air to carry large quantities of sand and dust depends on the wind speed, the size of the sand or dust grains, the degree of soil cohesion, the stability of the atmosphere, and the intensity of the vertical air currents. In general, the movement of dust particles is a function of...

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Main Authors: عبد الحسن أبو رحيل, محمد محمد
Format: Article
Language:Arabic
Published: Unviversity of Kufa, Faculty of Arts 2015-05-01
Series:آداب الكوفة
Subjects:
Online Access:https://www.journal.uokufa.edu.iq/index.php/kufa_arts/article/view/6494
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author عبد الحسن أبو رحيل
محمد محمد
author_facet عبد الحسن أبو رحيل
محمد محمد
author_sort عبد الحسن أبو رحيل
collection DOAJ
description The ability of the air to carry large quantities of sand and dust depends on the wind speed, the size of the sand or dust grains, the degree of soil cohesion, the stability of the atmosphere, and the intensity of the vertical air currents. In general, the movement of dust particles is a function of both the strength of the wind and the characteristics of the granules that carry it from its place. Dust storms are generated when the wind speed exceeds 7 m / s, as the soil atoms attached to the surface of the earth will lose their bonding strength with their molecules. These atoms begin to move when the wind speed increases, which overcomes the force of friction of the atom with the surface of the earth and the weight of the atom itself. The phenomenon of rising dust occurs during the day or night, especially in the summer season, as a result of the intense heating of the earth’s surface and the surface air in contact with it, which results in a sharp instability of the surface air layer.
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spelling doaj.art-22ac47d8cafe4ea4bc9185855261ff442023-10-24T14:13:15ZaraUnviversity of Kufa, Faculty of Artsآداب الكوفة1994-89992664-469X2015-05-0112210.36317/kaj/2014/v1.i22.6494Movement and paths of dust phenomena affecting Najaf Governorateعبد الحسن أبو رحيل0محمد محمد1University of Kufa- College of ArtsUniversity of Kufa- College of Arts The ability of the air to carry large quantities of sand and dust depends on the wind speed, the size of the sand or dust grains, the degree of soil cohesion, the stability of the atmosphere, and the intensity of the vertical air currents. In general, the movement of dust particles is a function of both the strength of the wind and the characteristics of the granules that carry it from its place. Dust storms are generated when the wind speed exceeds 7 m / s, as the soil atoms attached to the surface of the earth will lose their bonding strength with their molecules. These atoms begin to move when the wind speed increases, which overcomes the force of friction of the atom with the surface of the earth and the weight of the atom itself. The phenomenon of rising dust occurs during the day or night, especially in the summer season, as a result of the intense heating of the earth’s surface and the surface air in contact with it, which results in a sharp instability of the surface air layer. https://www.journal.uokufa.edu.iq/index.php/kufa_arts/article/view/6494حركة ومسالك الظواهر الغبارية
spellingShingle عبد الحسن أبو رحيل
محمد محمد
Movement and paths of dust phenomena affecting Najaf Governorate
آداب الكوفة
حركة ومسالك الظواهر الغبارية
title Movement and paths of dust phenomena affecting Najaf Governorate
title_full Movement and paths of dust phenomena affecting Najaf Governorate
title_fullStr Movement and paths of dust phenomena affecting Najaf Governorate
title_full_unstemmed Movement and paths of dust phenomena affecting Najaf Governorate
title_short Movement and paths of dust phenomena affecting Najaf Governorate
title_sort movement and paths of dust phenomena affecting najaf governorate
topic حركة ومسالك الظواهر الغبارية
url https://www.journal.uokufa.edu.iq/index.php/kufa_arts/article/view/6494
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