新疆农业科学 ›› 2018, Vol. 55 ›› Issue (2): 319-327.DOI: 10.6048/j.issn.1001-4330.2018.02.015

• • 上一篇    下一篇

不同滴灌水温在灰漠土中水热耦合模拟与验证

吉恒莹1,李磐2,付彦博2,冯耀祖2   

  1. 1.新疆师范大学,乌鲁木齐 830054;
    2.新疆农业科学院土壤肥料与农业节水研究所,乌鲁木齐 830091
  • 收稿日期:2017-10-18 出版日期:2018-02-20 发布日期:2018-06-30
  • 通信作者: 冯耀祖(1973-),男,甘肃人,研究员,博士,研究方向为农艺节水,(E-mail)fengyaozu@sina.com
  • 作者简介:吉恒莹(1978-),女,河南人,讲师,博士,研究方向为土壤物理,(E-mail)jihengying@126.com
  • 基金资助:
    国家自然科学基金项目“滴灌灌溉水温对新疆灰漠土环境及棉花生长机制研究”(51169025);新疆高校科研启动基金“艾丁湖盆地植被斑块镶嵌格局与土壤特征的互馈效应研究”(XJEDU2013S26)

Simulation and Validation of Coupled Water-heat Transfer in the Grey Dessert Soil in Different Water Temperatures during Surface Drip Irrigation

JI Heng-ying1, LI Pan2, FU Yan-bo2, FENG Yao-zu2   

  1. 1.Xinjiang Normal University, Urumqi 830054,China;
    2. Research Institute of Soil, Fertilizer and Agricultural Water Conservation, Xinjiang Academy of Agricultural Sciences, Urumqi 830091, China
  • Received:2017-10-18 Online:2018-02-20 Published:2018-06-30
  • Correspondence author: Feng Yao-zu(1973-), Dr, Research Fellow, Engaged in the research agronomic water saving, (E-mail)fengyaozu@sina.com

摘要: 【目的】滴灌条件下不同灌溉水水热状况对土壤水热状况的影响规律,根据土壤水、热运动基本方程,建立了地表滴灌水、热运移数学模型。【方法】采用正交试验设计,设计不同滴灌水温水平及其组合,共计40个试验处理。利用 HYDRUS-1D 软件建立的数学模型进行了数值求解,与实测数据结果进行验证。【结果】建立新疆灰漠土土壤含水量与压力水头的模拟方程(1)公式;(2)eln0.328 9Q-0.063 81.560 5(h<0),确定土壤的水力学参数和热特性参数。【结论】利用该数学模型对地表滴灌条件下作物生长所需的土壤水、热环境条件模拟预测。从模型的数值模拟值和实测结果对比验证显示,地表滴灌条件下低水温(10℃)和高水温(30℃)对土壤表层影响比较大,而且在早春增加一定的灌水温度,有利于作物苗期的生长。

关键词: 灰漠土; 水热耦合; 滴灌; 模型; 温度

Abstract: 【Objective】 This project aims to study the influence of water and heat conditions of different irrigation water on soil water and heat conditions under drip irrigation conditions so as to establish the mathematical model of water and heat transfer of surface drip irrigation according to the fundamental equations of water thermal motion of soil.【Method】Orthogonal experiments were conducted to design different drip irrigation water temperature levels and their combinations, 40 treatments in total. The mathematical model set with HYDRUS-1D software was applied to solve the numerical results, which were compared with the indoor measured data.【Result】The simulation equations of soil moisture content and pressure head of Xinjiang gray desert soil were established: (1) 公式; (2) eln0.328 9Q-0.063 81.560 5 (h<0), Soil hydraulic parameters and thermal characteristic parameters were determined.【Conclusion】The soil water and thermal environment conditions for crop growth under the surface drip irrigation condition can be predicted with this mathematical model. In addition, both numerical simulation values and measured results indicate that low (10 ℃) and high (30 ℃) water temperature have great influences on soil surface under surface drip irrigation condition, and a certain increase of irrigation water temperature in early spring is beneficial to the growth of crops in the seedling stage.

Key words: gray desert soil; hydrothermal coupling; drip irrigation; models; temperature

中图分类号: 


ISSN 1001-4330 CN 65-1097/S
邮发代号:58-18
国外代号:BM3342
主管:新疆农业科学院
主办:新疆农业科学院 新疆农业大学 新疆农学会

出版单位:《新疆农业科学》编辑部
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