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Chinese Journal of Applied Ecology ›› 2018, Vol. 29 ›› Issue (4): 1249-1258.doi: 10.13287/j.1001-9332.201804.027

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Soil moisture variation under different water and fertilization managements in apple orchard of Weibei dryland, China

ZHAO Zhi-yuan1, ZHENG Wei1, LIU jie1, MA Peng-yi1, LI Zi-yan1, ZHAI Bing-nian1,2*, WANG Zhao-hui1   

  1. 1College of Natural Resources and Environment,Northwest A&F University/Ministry of Agriculture Key Laboratory of Plant Nutrition and Agri-environment of Northwest, Yangling 712100, Shaanxi, China;
    2Apple Experiment Station, Northwest A&F University, Baishui 715600, Shaanxi, China;
  • Received:2017-07-24 Online:2018-04-18 Published:2018-04-18
  • Contact: * E-mail: zhaibingnian@nwafu.edu.cn
  • Supported by:

    This work was supported by the Special Foundation of Public Welfare (Agriculture) Research of China (201303104, 201103005-9), the Project of Agricultural Science and Technology Innovation Transformation of Shaanxi Province, China (NYKJ-2015-17), the Agricultural Science & Technology Demonstration Foundation of Yangling, China (2015-TS-18,2015NY-05) and the Demonstration Base Foundation of Technology Achievement of Northwest A&F University (TGZX2014-16).

Abstract: To evaluate the variations of soil moisture under different water and fertilizer treatments in apple orchard in the Weibei dryland, a field experiment was carried out in 2013-2016 at Tianjiawa Village, Baishui County, Shaanxi Province. There were three treatments, i.e., farmers traditional model (only addition of NPK chemical fertilizer, FM), extension model (swine manure and NPK chemical fertilizer combined with black plastic film in tree row space, EM), and optimized model (swine manure and NPK chemical fertilizer combined with black plastic film in tree row space and planting rape in the inter-row of apple trees, OM). The results showed that OM treatment significantly increased soil water storage capacity in 0-200 cm soil layer. Water content of 0-100 cm soil layer was increased by 5.6% and 15.3% in the dry season compared with FM and EM treatment, respectively. Moreover, the soil water relative deficit index of OM was lower than that of EM in 200-300 cm soil layer. The rainfall infiltration in the dry year could reach 300 cm depth under OM. Meanwhile, OM stabilized soil water content and efficiently alleviated the desiccation in deep soil layer. Compared with FM and EM, the 4-year average yield of OM was increased by 36.6% and 22.5%, respectively. In summary, OM could increase water use efficiency through increasing the contents of available soil water and improving the soil water condition in shallow and deep layers, which help alleviate the soil deficit in deep layer and increase yield.