Effect of sand mulching on spatiotemporal variation of soil water content during the seasonal freezing-thawing period
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DOI:10.7606/j.issn.1000-7601.2019.05.07
Key Words: seasonal freezing-thawing period  sand mulching  soil water content in farmland  dynamic change
Author NameAffiliation
FENG Hui-jun College of Water Resources Science and Engineering, Taiyuan University of Technology, Taiyuan, Shanxi 030024, China 
ZHAO Hao-ran College of Water Resources Science and Engineering, Taiyuan University of Technology, Taiyuan, Shanxi 030024, China 
ZHENG Xiu-qing College of Water Resources Science and Engineering, Taiyuan University of Technology, Taiyuan, Shanxi 030024, China 
CHEN Jun-feng College of Water Resources Science and Engineering, Taiyuan University of Technology, Taiyuan, Shanxi 030024, China 
MIAO Chun-yan College of Water Resources Science and Engineering, Taiyuan University of Technology, Taiyuan, Shanxi 030024, China
First Hydrogeology and Engineering Geological Team of Shanxi Province, Taiyuan, Shanxi 030024, China 
XUE Jing College of Water Resources Science and Engineering, Taiyuan University of Technology, Taiyuan, Shanxi 030024, China 
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Abstract:
      The effect of sand mulching on soil water content was studied during the seasonal freezing-thawing period. A field experiment, involving bare plot (LD), sand mulches of particle size of 0.5~1.5 mm (XS) and 1.5~2.0 mm (CS), was set up in Taigu Water Balance Experimental Field to monitor soil water content in the soil layer of 0~100 cm. The results showed that, two higher-soil-moisture areas were formed with sand mulching treatments, which located at the near-surface of 20~40 cm. Soil water content on surface varied from 15.40% to 21.79% and ranged from 15.99% to 19.94% in the layer of 20~40 cm. Sand mulches had a significant effect on storing water, and the effect decreased with increasing soil depth. Sand mulching treatments resulted in more stored water in surface soil with value-added ranging from 8.45% to 10.94% of soil water content. Sand mulching treatments resulted less water storage in the layer of 0~40 cm with value-added varying from 1.56% to 1.62%. The differences of soil water content between the three treatments in the layer of 40~100 cm were slight, ranging from 0.09% to 0.40%. In addition, the effect of sand mulching on water storage was related to the particles size of sand. The water storage of XS treatment in the 0~5 cm layer was better than that of CS treatment. Soil water content of XS treatment in the layer of 0~5 cm was 0.57%~2.39% higher than that of CS treatment. Sand mulching resulted in a reduction of variations on surface soil water content, which reduced variations about 4.42%.