scholarly journals Interactive effects of wind speed, vegetation coverage and soil moisture in controlling wind erosion in a temperate desert steppe, Inner Mongolia of China

2018 ◽  
Vol 10 (4) ◽  
pp. 534-547 ◽  
Author(s):  
Zhongju Meng ◽  
Xiaohong Dang ◽  
Yong Gao ◽  
Xiaomeng Ren ◽  
Yanlong Ding ◽  
...  
2014 ◽  
Vol 2014 ◽  
pp. 1-9 ◽  
Author(s):  
Yongsheng Yang ◽  
Chongfeng Bu ◽  
Xingmin Mu ◽  
Hongbo Shao ◽  
Kankan Zhang

To better understand the effects of biological soil crusts (BSCs) on soil moisture and wind erosion and study the necessity and feasibility of disturbance of BSCs in the Mu Us sandland, the effects of four treatments, including moss-dominated crusts alone,Artemisia ordosicaalone, bare sand, andArtemisia ordosicacombined with moss-dominated crusts, on rainwater infiltration, soil moisture, and annual wind erosion were observed. The major results are as follows. (1) The development of moss-dominated crusts exacerbated soil moisture consumption and had negative effects on soil moisture in the Mu Us sandland. (2) Moss-dominated crusts significantly increased soil resistance to wind erosion, and when combined withArtemisia ordosica, this effect became more significant. The contribution of moss-dominated crusts underArtemisia ordosicawas significantly lower than that of moss-dominated crusts alone in sites where vegetative coverage > 50%. (3) Finally, an appropriate disturbance of moss-dominated crusts in the rainy season in sites with high vegetative coverage improved soil water environment and vegetation succession, but disturbance in sites with little or no vegetative cover should be prohibited to avoid the exacerbation of wind erosion.


2014 ◽  
Vol 955-959 ◽  
pp. 3505-3508 ◽  
Author(s):  
Tian Ming Gao ◽  
Rui Qiang Zhang ◽  
Jian Ying Guo

In northern China, grassland has degraded severely and wind erosion occurs remarkably due to irrational land use in recent years. By employing sand sampler and mobile wind tunnel, an observation for 6 years was made to analyze the mechanisms of wind erosion in Xilamuren grassland, the central of Yinshan Mountains, Inner Mongolia. Results show that: (1) vegetation is the decisive factor for controlling wind erosion and the inhibiting effect of vegetation height on wind erosion is greater than that of vegetation coverage. (2) Wind erosion modulus in the initial period of enclosure reaches 1313.7 t km-2a-1 and with the improvement of the grassland vegetation, wind erosion decreases year by year. (3) For every 1000 kg soil eroded by wind, 15 kg organic matter, 227g available nitrogen, 262g available phosphorus and 120g available potassium lose in the region at the same time, being a tremendous fertility loss. Therefore, the protection of base grassland and restoration of degraded grassland are two fundamental approaches to control wind erosion on the grassland.


2012 ◽  
Vol 518-523 ◽  
pp. 4496-4503
Author(s):  
Jian Qiang Chen ◽  
Man Quan Zhao ◽  
Zhi Chen

The soil erosion test was carried out for the Zhao He grassland on the northern foothills of Yin Shan Mountain by the use of a portable wind erosion tunnel developed by Inner Mongolia Agricultural University, the variation low of soil wind erosion rate with the different wind speed and different arrangement in pairs of different soil moisture content and different vegetation coverage was obtained and the data analysis indicates that the anti-wind erosion characteristics of ground surface is most satisfactory when the vegetation coverage is 40%, soil moisture content 9.3% and the height of vegetation 50cm. The result of this study may provide a certain reference date for the application of prevention and control technology of soil wind erosion and be of vital significance to the implementation of sustainable development of livestock husbandry.


2011 ◽  
Vol 26 (3) ◽  
pp. 379-386 ◽  
Author(s):  
Feng Zhang ◽  
Guangsheng Zhou ◽  
Yu Wang ◽  
Fulin Yang ◽  
Christer Nilsson

2012 ◽  
Vol 32 (13) ◽  
pp. 4017-4024 ◽  
Author(s):  
颜亮 YAN Liang ◽  
周广胜 ZHOU Guangsheng ◽  
张峰 ZHANG Feng ◽  
隋兴华 SUI Xinghua ◽  
平晓燕 PING Xiaoyan

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