Dust Emission from Gobi under Different Dust Content Conditions: A Wind Tunnel Study atop the Mogao Grottoes

Dust emission from the Gobi desert is one of the major sources of global atmospheric aerosols. However, the main factors affecting dust emission from Gobi remain poorly understood. In this paper, field wind tunnel experiments were performed atop the Mogao Grottoes to determine the variation characte...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Linhao Liang, Weimin Zhang, Lihai Tan, Shuyi Chen
Formato: article
Lenguaje:EN
Publicado: MDPI AG 2021
Materias:
Acceso en línea:https://doaj.org/article/611203750f7a4f8b90ba71694c62fbaf
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:611203750f7a4f8b90ba71694c62fbaf
record_format dspace
spelling oai:doaj.org-article:611203750f7a4f8b90ba71694c62fbaf2021-11-25T16:45:35ZDust Emission from Gobi under Different Dust Content Conditions: A Wind Tunnel Study atop the Mogao Grottoes10.3390/atmos121114982073-4433https://doaj.org/article/611203750f7a4f8b90ba71694c62fbaf2021-11-01T00:00:00Zhttps://www.mdpi.com/2073-4433/12/11/1498https://doaj.org/toc/2073-4433Dust emission from the Gobi desert is one of the major sources of global atmospheric aerosols. However, the main factors affecting dust emission from Gobi remain poorly understood. In this paper, field wind tunnel experiments were performed atop the Mogao Grottoes to determine the variation characteristics of the vertical dust flux (<i>F</i>) of particulate matter less than 10 μm (PM10) for Gobi surfaces with different dust content and wind speeds under external sand supply. The results demonstrate that <i>F</i> obeyed a power function with increasing friction velocity (<inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><msub><mi>U</mi><mo>*</mo></msub></mrow></semantics></math></inline-formula>), and increased exponentially with the increasing surface dust content (<i>C</i>). The index of n-value in the formula <i>F</i>∝<inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><msup><msub><mi>U</mi><mo>*</mo></msub><mi>n</mi></msup></mrow></semantics></math></inline-formula> is taken in the range of 2.02–2.63 under the surface of 27.3–47.3% dust content (<100 µm), and the dust emission rate was significantly enhanced when the surface dust content exceeded approximately 37%. This study indicates that wind force is the primary dynamic condition affecting Gobi dust emission, and that surface dust content is a significant factor in determining the quantity of dust emission. Furthermore, the contribution of wind force to PM10 emission is greater than the surface dust content, and the higher the height, the greater the weight of friction velocity.Linhao LiangWeimin ZhangLihai TanShuyi ChenMDPI AGarticleGobiPM10vertical emission fluxwind tunnelMogao GrottoesMeteorology. ClimatologyQC851-999ENAtmosphere, Vol 12, Iss 1498, p 1498 (2021)
institution DOAJ
collection DOAJ
language EN
topic Gobi
PM10
vertical emission flux
wind tunnel
Mogao Grottoes
Meteorology. Climatology
QC851-999
spellingShingle Gobi
PM10
vertical emission flux
wind tunnel
Mogao Grottoes
Meteorology. Climatology
QC851-999
Linhao Liang
Weimin Zhang
Lihai Tan
Shuyi Chen
Dust Emission from Gobi under Different Dust Content Conditions: A Wind Tunnel Study atop the Mogao Grottoes
description Dust emission from the Gobi desert is one of the major sources of global atmospheric aerosols. However, the main factors affecting dust emission from Gobi remain poorly understood. In this paper, field wind tunnel experiments were performed atop the Mogao Grottoes to determine the variation characteristics of the vertical dust flux (<i>F</i>) of particulate matter less than 10 μm (PM10) for Gobi surfaces with different dust content and wind speeds under external sand supply. The results demonstrate that <i>F</i> obeyed a power function with increasing friction velocity (<inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><msub><mi>U</mi><mo>*</mo></msub></mrow></semantics></math></inline-formula>), and increased exponentially with the increasing surface dust content (<i>C</i>). The index of n-value in the formula <i>F</i>∝<inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><msup><msub><mi>U</mi><mo>*</mo></msub><mi>n</mi></msup></mrow></semantics></math></inline-formula> is taken in the range of 2.02–2.63 under the surface of 27.3–47.3% dust content (<100 µm), and the dust emission rate was significantly enhanced when the surface dust content exceeded approximately 37%. This study indicates that wind force is the primary dynamic condition affecting Gobi dust emission, and that surface dust content is a significant factor in determining the quantity of dust emission. Furthermore, the contribution of wind force to PM10 emission is greater than the surface dust content, and the higher the height, the greater the weight of friction velocity.
format article
author Linhao Liang
Weimin Zhang
Lihai Tan
Shuyi Chen
author_facet Linhao Liang
Weimin Zhang
Lihai Tan
Shuyi Chen
author_sort Linhao Liang
title Dust Emission from Gobi under Different Dust Content Conditions: A Wind Tunnel Study atop the Mogao Grottoes
title_short Dust Emission from Gobi under Different Dust Content Conditions: A Wind Tunnel Study atop the Mogao Grottoes
title_full Dust Emission from Gobi under Different Dust Content Conditions: A Wind Tunnel Study atop the Mogao Grottoes
title_fullStr Dust Emission from Gobi under Different Dust Content Conditions: A Wind Tunnel Study atop the Mogao Grottoes
title_full_unstemmed Dust Emission from Gobi under Different Dust Content Conditions: A Wind Tunnel Study atop the Mogao Grottoes
title_sort dust emission from gobi under different dust content conditions: a wind tunnel study atop the mogao grottoes
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/611203750f7a4f8b90ba71694c62fbaf
work_keys_str_mv AT linhaoliang dustemissionfromgobiunderdifferentdustcontentconditionsawindtunnelstudyatopthemogaogrottoes
AT weiminzhang dustemissionfromgobiunderdifferentdustcontentconditionsawindtunnelstudyatopthemogaogrottoes
AT lihaitan dustemissionfromgobiunderdifferentdustcontentconditionsawindtunnelstudyatopthemogaogrottoes
AT shuyichen dustemissionfromgobiunderdifferentdustcontentconditionsawindtunnelstudyatopthemogaogrottoes
_version_ 1718413020587098112