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Journal of Arid Land  2022, Vol. 14 Issue (8): 877-893    DOI: 10.1007/s40333-022-0070-4
Research article     
Wind-proof and sand-fixing effects of Artemisia ordosica with different coverages in the Mu Us Sandy Land, northern China
PANG Yingjun1,2,3,4,*(), WU Bo1,2,3,*(), JIA Xiaohong1,2,3, XIE Shengbo5
1Institute of Desertification Studies, Chinese Academy of Forestry, Beijing 100091, China
2Institute of Ecological Conservation and Restoration, Chinese Academy of Forestry, Beijing 100091, China
3Key Laboratory of Desert Ecosystem and Global Change, National Forestry and Grassland Administration, Beijing 100091, China
4Kumtag Desert Ecosystem Research Station, National Forestry and Grassland Administration, Dunhuang 736200, China
5Key Laboratory of Desert and Desertification, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
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Abstract  

Wind erosion is a key global environmental problem and has many adverse effects. The Mu Us Sandy Land of northern China is characterized by an arid climate, where vegetation patches and bare sand patches are usually distributed mosaically, and aeolian activities occur frequently. Vegetation plays a significant role in controlling wind erosion. Artemisia ordosica is the most dominant native plant species in the Mu Us Sandy Land. It is urgent to study the wind-proof and sand-fixing effects of Artemisia ordosica in the Mu Us Sandy Land. This study analyzed the wind-proof and sand-fixing effects of Artemisia ordosica based on the field data of wind regimes, aeolian sediment transport, and surface change of Artemisia ordosica plots with four coverages (denoted as site A, site B, site C, and site D) in the Mu Us Sandy Land during the period from 1 June 2018 to 29 June 2019. The coverages of Artemisia ordosica at site A, site B, site C, and site D were 2%, 16%, 29%, and 69%, respectively. The annual average wind speeds at 2.0 m height above the ground for site A, site B, site C, and site D were 3.47, 2.77, 2.21, and 1.97 m/s, respectively. The annual drift potentials were 193.80, 69.72, 15.05, and 6.73 VU at site A, site B, site C, and site D, respectively. The total horizontal aeolian sediment fluxes during the period from 2-3 June 2018 to 6 June 2019 at site A, site B, site C, and site D were 4633.61, 896.80, 10.54, and 6.14 kg/m, respectively. Site A had the largest surface changes, and the surface changes at site B were significantly weaker than those at site A, whereas the surface changes at site C and site D were minimal. The results indicated that Artemisia ordosica significantly reduced the wind speed, drift potential, aeolian sediment transport, and surface changes. The higher the coverage of Artemisia ordosica is, the more obvious the effects of wind-proof and sand-fixing. Wind erosion would be effectively controlled in the Mu Us Sandy Land if the coverage of Artemisia ordosica is greater than 29%. These results provide a scientific basis for evaluating the ecosystem service function of Artemisia ordosica and the vegetation protection and construction projects in the Mu Us Sandy Land.



Key wordsArtemisia ordosica      wind-proof      sand-fixing      wind erosion      aeolian sediment flux      Mu Us Sandy Land     
Received: 14 February 2022      Published: 30 August 2022
Corresponding Authors: * PANG Yingjun (E-mail: pangyingjun@caf.ac.cn);WU Bo (E-mail: wubo@caf.ac.cn)
Cite this article:

PANG Yingjun, WU Bo, JIA Xiaohong, XIE Shengbo. Wind-proof and sand-fixing effects of Artemisia ordosica with different coverages in the Mu Us Sandy Land, northern China. Journal of Arid Land, 2022, 14(8): 877-893.

URL:

http://jal.xjegi.com/10.1007/s40333-022-0070-4     OR     http://jal.xjegi.com/Y2022/V14/I8/877

Fig. 1 Overview of the study area and distribution area of monitoring sites. Note that this map is based on the Google Earth images.
Fig. 2 Photographs of the monitoring sites with different coverages of Artemisia ordosica. (a), site A; (b), site B; (c), site C; (d), site D.
Location Artemisia ordosica
coverage (%)
Observation height of
wind (m)
Observation height of
sediment collection (m)
Site A 2 0.2, 0.5, 1.0, and 2.0 0.2, 0.5, 1.0, 1.5, and 2.0
Site B 16 2.0 0.2, 0.5, 1.0, and 2.0
Site C 29 0.2, 0.5, 1.0, and 2.0 0.2, 0.5, 1.0, 1.5, and 2.0
Site D 69 0.2, 0.5, 1.0, and 2.0 0.2, 0.5, 1.0, 1.5, and 2.0
Table 1 Description of the monitoring sites selected in this study
Direction Abbreviation Azimuth degree (°) Direction Abbreviation Azimuth degree (°)
North N 348.75-11.25 South S 168.75-191.25
North-northeast NNE 11.25-33.75 South-southwest SSW 191.25-213.75
Northeast NE 33.75-56.25 Southwest SW 213.75-236.25
East-northeast ENE 56.25-78.75 West-southwest WSW 236.25-258.75
East E 78.75-101.25 West W 258.75-281.25
East-southeast ESE 101.25-123.75 West-northwest WNW 281.25-303.75
Southeast SE 123.75-146.25 Northwest NW 303.75-326.25
South-southeast SSE 146.25-168.75 North-northwest NNW 326.25-348.75
Table 2 Description of the direction and azimuth degree
Fig. 3 Wind roses of the four monitoring sites at 2.0 m height above the ground during the period from 1 June 2018 to 31 May 2019. (a), site A; (b), site B; (c), site C; (d), site D. N, north; NNE, north-northeast; NE, northeast; ENE, east-northeast; E, east; ESE, east-southeast; SE, southeast; SSE, south-southeast; S, south; SSW, south-southwest; SW, southwest; WSW, west-southwest; W, west; WNW, west-northwest; NW, northwest; NNW, north-northwest.
Fig. 4 Monthly average wind speeds at a height of 2.0 m above the ground at the four monitoring sites during the period from 1 June 2018 to 31 May 2019
Fig. 5 Drift potential (DP) roses at the four monitoring sites during the period from 1 June 2018 to 31 May 2019. (a), site A; (b), site B; (c), site C; (d), site D. The arrow line segment represents the resultant drift potential (RDP), and the direction of the arrow represents the resultant drift direction (RDD). VU, vector units.
Fig. 6 Horizontal aeolian sediment fluxes at the four monitoring sites during the period from 2-3 June 2018 to 6 June 2019. (a), site A; (b), site B; (c), site C; (d), site D.
Location Sample Height above
the
ground
(m)
Percentage of grain size (%) Mean
grain
size
(μm)
Clay Silt Very fine sand Fine
sand
Medium
sand
Coarse
sand
Very coarse
sand
Gravel
(0-
2 μm)
(2-
63 μm)
(63-
125 μm)
(125-
250 μm)
(250-
500 μm)
(500-
1000 μm)
(1000-
2000 μm)
(>2000 μm)
Site A SSS 0.0 0.00 0.81 2.00 44.24 50.88 2.06 0.01 0.00 272.94
HASS 0.2 0.00 0.00 3.24 54.03 41.45 1.28 0.00 0.00 234.24
HASS 0.5 0.00 4.53 14.04 50.71 30.44 0.28 0.00 0.00 192.67
HASS 1.0 0.00 3.83 21.68 55.09 19.40 0.00 0.00 0.00 168.06
HASS 1.5 0.00 11.90 24.51 47.78 15.80 0.01 0.00 0.00 143.11
HASS 2.0 0.00 11.27 23.57 49.77 15.38 0.00 0.00 0.00 145.43
Site B SSS 0.0 0.05 2.38 1.82 36.27 52.71 6.77 0.00 0.00 293.79
HASS 0.2 0.00 0.00 2.39 43.25 49.29 5.06 0.00 0.00 261.83
HASS 0.5 0.00 1.23 6.24 52.53 38.58 1.43 0.00 0.00 224.38
HASS 1.0 0.00 6.20 9.89 50.24 33.11 0.57 0.00 0.00 201.48
HASS 2.0 0.01 45.99 25.45 20.82 7.59 0.15 0.00 0.00 73.06
Site C SSS 0.0 0.00 2.28 3.80 42.98 46.98 3.96 0.00 0.00 267.66
HASS 0.2 0.00 2.21 1.51 36.01 54.70 5.56 0.00 0.00 275.73
HASS 0.5 0.00 16.46 19.87 39.33 23.79 0.54 0.00 0.00 143.39
HASS 1.0 0.00 22.94 26.33 33.51 16.77 0.45 0.00 0.00 118.50
HASS 1.5 0.00 22.64 19.43 22.25 25.71 9.89 0.09 0.00 151.78
HASS 2.0 0.00 43.24 30.97 17.73 7.72 0.34 0.00 0.00 77.72
Site D SSS 0.0 0.15 21.07 10.68 34.85 31.25 2.00 0.00 0.00 150.81
HASS 0.2 0.00 19.63 19.97 34.27 23.46 2.66 0.02 0.00 138.16
HASS 0.5 0.00 47.30 25.65 17.51 8.55 0.99 0.00 0.00 71.02
HASS 1.0 0.01 64.01 23.85 9.32 2.80 0.01 0.00 0.00 45.94
HASS 1.5 0.01 62.36 24.36 9.36 3.45 0.46 0.00 0.00 49.00
HASS 2.0 0.00 50.74 28.81 12.90 6.05 1.49 0.00 0.00 66.47
Table 2 Grain size distributions of the surface sediment samples and horizontal aeolian sediment samples at different heights above the ground
Fig. 7 Grain size distributions of the surface sediment samples at the four monitoring sites
Fig. 8 Grain size distributions of the horizontal aeolian sediment samples at different heights at the four monitoring sites. (a), site A; (b), site B; (c), site C; (d), site D.
Fig. 9 Surface changes at the four monitoring sites during the period from 2 June 2018 to 29 June 2019. (a), site A; (b), site B; (c), site C; (d), site D. Positive values on y-axis represent surface deposition, while negative values represent surface erosion.
Fig. 10 Relationship between the DP and horizontal aeolian sediment flux at the four monitoring sites
Fig. 11 Relationship between Artemisia ordosica coverage and the total horizontal aeolian sediment flux during the period from 2-3 June 2018 to 6 June 2019
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