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[中国西北黄土高原苹果园土壤水分与水分生产率模拟]

[Simulation on soil moisture and water productivity of apple orchard on the Loess Plateau, Northwest China].

作者信息

Wang Xian-Zhi, Zhao Xi-Ning, Gao Xiao-Dong, Wei Wei, Wang Shao-Fei, Yu Liu-Yang, Wang Jia-Xin, Shao Zhu-En

机构信息

Ministry of Education Key Laboratory of Agricultural Soil and Water Engineering in Arid and Semiarid Areas, Northwest A&F University, Yangling 712100, Shaanxi, China.

College of Water Resources and Architectural Engineering, Northwest A&F University, Yangling 712100, Shaanxi, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2021 Jan;32(1):201-210. doi: 10.13287/j.1001-9332.202101.012.

DOI:10.13287/j.1001-9332.202101.012
PMID:33477228
Abstract

The WinEPIC model was used to simulate the dynamics of soil moisture and water productivity in the deep layer of the dry farm apple orchard of Changwu in the Loess Plateau from 1980 to 2018, aiming to provide a scientific basis for the sustainable development of apple production in the area. The results showed that the average annual yield of apple orchards in Changwu area was 27.37 t·hm, the average annual evapotranspiration was 673.66 mm, and the average annual water productivity was 4.07 kg·m. The number of water stress days in adult apple trees was mainly affected by rainfall. The average number of stress days in the late stage of apple tree growth was 46.46 d. The soil water content in deep layer began to approach withering humidity as early as 9-year-old apple trees. Water supply in the whole growing season of Changwu area was the dominant factor impacting the yield of orchards. The reduction of effective soil water content in deep soil was the main factor restricting yield enhancement in the middle and late growth stages of apple trees. When there was no sufficient precipitation, apple trees would use soil water from deeper soil layer. Excessive precipitation could not be used by apple trees but could be converted into shallow soil moisture and evaporation if the deep layer had less available water. For the mature apple trees, less than 500 mm or higher than 700 mm of annual water supply would cause a decline in production. For apple orchard at different growth periods, water management strategy should be adjusted according to rainfall conditions in different years. Supplementary irrigation, rainwater retention, covering, and pruning of branches could be used to reduce the unproductive and luxury water consumption of apple trees, delay the appearance of deep dry layer of soil, and avoid the waste of water resources while ensuring the growth of apple trees.

摘要

利用WinEPIC模型模拟了黄土高原长武旱作苹果园1980—2018年深层土壤水分动态及水分生产率,旨在为该地区苹果生产可持续发展提供科学依据。结果表明,长武地区苹果园平均年产量为27.37t·hm,年均蒸发散量为673.66mm,年均水分生产率为4.07kg·m。成年苹果树水分胁迫天数主要受降雨影响,苹果树生长后期平均胁迫天数为46.46d。早在9年生苹果树时,深层土壤含水量就开始接近凋萎湿度。长武地区整个生长季的水分供应是影响果园产量的主导因素,深层土壤有效含水量减少是制约苹果树生长中后期产量提高的主要因素。在降水不足时,苹果树会利用更深土层的土壤水分;若深层土壤有效水分较少,过多降水苹果树无法利用,会转化为浅层土壤水分并蒸发。对于成年苹果树,年供水量小于500mm或大于700mm均会导致产量下降。针对不同生长时期的苹果园,应根据不同年份降雨情况调整水分管理策略,可采用补充灌溉、雨水集蓄、覆盖及枝条修剪等措施,减少苹果树无效和奢侈性水分消耗,延缓土壤深层干层出现,在保证苹果树生长的同时避免水资源浪费。

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