Analysis of soil moisture condition under different land uses in the arid region of Horqin sandy land, northern China

• Published in: Solid earth (Göttingen) 2015-10, Vol.6 (4), p.1157-1167
• Main Authors: Niu, C. Y, Musa, A, Liu, Y
• Format: Article
• Language: English
• Subjects: Agricultural land; Agricultural management; Analysis; Arid regions; Arid zones; Atmospheric precipitations; Crop growth; Depth indicators; Dynamics; Earth science; Environmental restoration; Evapotranspiration; Grasslands; Growing season; Infiltration; Infiltration (Hydrology); Infiltration rate; Land; Land cover; Land use; Moisture content; Moisture profiles; Poplar; Precipitation; Precipitation (Meteorology); Rain; Rainfall; Restoration; Root zone; Runoff; Sandy soils; Seasonal variation; Seasonal variations; Semi arid environments; Semiarid environments; Soil; Soil (material); Soil analysis; Soil classification; Soil conditions; Soil dynamics; Soil layers; Soil moisture; Soil profiles; Soil water; Temporal variations; Vegetation; Water depth; Water management
• ISSN: 1869-9529; 1869-9510; 1869-9529
• DOI: 10.5194/se-6-1157-2015

Land use plays an important role in controlling spatial and temporal variations of soil moisture by influencing infiltration rates, runoff and evapotranspiration, which is important to crop growth and vegetation restoration in semiarid environments, such as Horqin sandy land in north China. However, few studies have been conducted comparing differences of dynamics of soil water conditions and the responses of soil to infiltration under different land use types in semiarid area. Five different land use types were selected to analyze soil moisture variations in relation to land use patterns during the growing season of 2 years. Results showed that soil moisture condition was affected by different land uses in semi-arid sandy soils. The higher soil moisture content among different land uses was exhibited by the grassland, followed by cropland, poplar land, inter-dunes and shrub land. The temporal variations of soil moisture in different land uses were not always consistent with the rainfall due to the dry sequence. Moreover, soil water at the surface, in the root zone and at the deep soil layer indicated statistical differences for different types of land cover. Meanwhile, temporal variations of soil moisture profile changed with precipitation. However, in the deep soil layer, there was a clear lag in response to precipitation. In addition, seasonal variations of profile soil moisture were classified into two types: increasing and waving types. And the stable soil water layer was at 80-120 cm. Furthermore, the infiltration depth exhibited a positive correlation with precipitation under all land uses. This study provided an insight into the implications for land and agricultural water management in this area.