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Quantitative Investigations of Water Balances of a Dune-Interdune Landscape during the Growing Season in the Horqin Sandy Land, Northeastern China

Author

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  • Xueya Zhou

    (Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China
    University of Chinese Academy of Sciences, Beijing 100049, China)

  • Dexin Guan

    (Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China)

  • Jiabing Wu

    (Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China)

  • Tingting Yang

    (Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China
    University of Chinese Academy of Sciences, Beijing 100049, China)

  • Fenghui Yuan

    (Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China)

  • Ala Musa

    (Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China)

  • Changjie Jin

    (Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China)

  • Anzhi Wang

    (Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China)

  • Yushu Zhang

    (Institute of Atmospheric Environment, China Meteorological Administration, Shenyang 110166, China)

Abstract

Dune-interdune is the main landscape pattern of desert areas, such as the Horqin sandy land of Northeastern China. Exploring the temporal and spatial variation of the water balance is crucial for efficient vegetation restoration at the micro-landform scale. The SWMS-2D model was used to estimate the seasonal variations of the water balance including evapotranspiration, soil water storage changes, lateral flow and drainage, and to examine the effects of micro-landforms (i.e., the top, upper, down, and bottom positions of the dune slope, and the interdune lowland area) on these components from May to October 2013 and 2015. Results showed that the soil water content was sensitive to rainfall pulses, particularly large precipitation events. Over 70% of the total evapotranspiration occurred from June to August, with a maximum daily value of 6.56 mm. At a monthly scale, evapotranspiration was not synchronous with precipitation. The ratio of evapotranspiration to precipitation was 1.84, 0.39, 2.49, 0.93, 2.26, and 1.14 in May, June, July, August, September, and October 2013 (a wet year), respectively; and 2.40, 1.11, 0.69, 2.14, 1.07, and 1.11 in 2015 (a dry year), respectively. The components of the water balance were significantly different among different micro-landforms. Evapotranspiration of a lowland area was greater than that in other micro-landforms, and the value in the wet year (2013) was significantly greater than that in the dry year (2015). However, water consumption in the lowland area was similar in both years. At the top, upper, down, and bottom positions of the dune slope, the ratio of evapotranspiration to precipitation in the wet year (2013) was 96%, 97%, 86%, and 96%, respectively; while in the dry year (2015), the ratio was 103%, 103%, 88%, and 104%. Therefore, in the dry year, evapotranspiration was generally larger than precipitation, indicating that almost all water from precipitation was evaporated. The lateral flow of the root zone from top to bottom accounted for only a small portion of water budget at the growing season scale. The results could be generalized to other similar region with corresponding model calibration, and would help to reveal seasonal variations of water balance components under the local topography, climate, soil, and vegetation conditions.

Suggested Citation

  • Xueya Zhou & Dexin Guan & Jiabing Wu & Tingting Yang & Fenghui Yuan & Ala Musa & Changjie Jin & Anzhi Wang & Yushu Zhang, 2017. "Quantitative Investigations of Water Balances of a Dune-Interdune Landscape during the Growing Season in the Horqin Sandy Land, Northeastern China," Sustainability, MDPI, vol. 9(6), pages 1-13, June.
    • Handle: RePEc:gam:jsusta:v:9:y:2017:i:6:p:1058-:d:101913
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    References listed on IDEAS

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    1. Liu, Wenzhao & Zhang, X.-C. & Dang, Tinghui & Ouyang, Zhu & Li, Zhi & Wang, Jun & Wang, Rui & Gao, Changqing, 2010. "Soil water dynamics and deep soil recharge in a record wet year in the southern Loess Plateau of China," Agricultural Water Management, Elsevier, vol. 97(8), pages 1133-1138, August.
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    Cited by:

    1. Xueya Zhou & Dexin Guan & Jiabing Wu & Fenghui Yuan & Anzhi Wang & Cangjie Jin & Yushu Zhang, 2019. "Soil water response to rainfall in a dune-interdune landscape in Horqin Sand Land, northern China," Soil and Water Research, Czech Academy of Agricultural Sciences, vol. 14(4), pages 229-239.
    2. Haorui Chen & Zhanyi Gao & Wenzhi Zeng & Jing Liu & Xiao Tan & Songjun Han & Shaoli Wang & Yongqing Zhao & Chengkun Yu, 2017. "Scale Effects of Water Saving on Irrigation Efficiency: Case Study of a Rice-Based Groundwater Irrigation System on the Sanjiang Plain, Northeast China," Sustainability, MDPI, vol. 10(1), pages 1-18, December.

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