张子卓,张珂萌,牛文全,薛万来.微润带埋深对温室番茄生长和土壤水分动态的影响[J].干旱地区农业研究,2015,33(2):122~129
微润带埋深对温室番茄生长和土壤水分动态的影响
Effects of burying depth on growth of tomato and soil moisture dynamics by moistube-irrigation in green house
  
DOI:10.16302/j.cnki.1000-7601.2015.02.020
中文关键词:  微润灌溉  埋深  压力水头  番茄生长状况  土壤水分动态
英文关键词:Moistube-irrigation  burying depth  working pressure  growth characteristics of tomato  soil moisture dynamics
基金项目:国家高技术发展计划(863 计划)课题(2011AA100507)
作者单位
张子卓 西北农林科技大学水利与建筑工程学院 陕西 杨凌 712100 
张珂萌 西北农林科技大学水利与建筑工程学院 陕西 杨凌 712100 
牛文全 西北农林科技大学水土保持研究所 陕西 杨凌 712100中国科学院水利部水土保持研究所 陕西 杨凌 712100 
薛万来 中国科学院水利部水土保持研究所 陕西 杨凌 712100 
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中文摘要:
      为探明微润灌溉对番茄生长和土壤水分的影响,设置了3种不同埋深和2种不同工作压力,研究了微润带埋设深度和压力对番茄生长、产量及水分利用效率的影响。结果表明:定植后94天,微润带压力水头为180 cm、埋深为15 cm时的番茄株高分别比埋深10 cm和20 cm的处理增加9.17%和7.55%;此时番茄气孔导度最小,光合速率和水分利用效率最大,分别比埋深为10 cm和20 cm的处理增产3.24%和7.45%;不同埋深土壤含水率垂直分布随时间的变化存在差异,15 cm埋深时的土壤含水率最大。微润带埋深是影响土壤水分时空变化的主要因素;压力对土壤含水量时间变化影响不显著。
英文摘要:
      In order to verify the effects of moistube-irrigation on the growth of tomato and water condition of soil, three different buried depths and two different pressure heads were designed. In addition, the resulting the effects were further analyzed on the growth and yield of tomato and water use efficiency. The results showed that after 94 days of planting, the buried depth at 15 cm had the highest plants which were increased by 9.17% and 7.55% from the buried depths at 10 cm and 20 cm, respectively. At this time, tomatoes had the minimal stomata conductance and highest photosynthetic rate and WUE within all of the four treatments employed in this investigation, resulting in yield increases of 3.24% and 7.45% more at buried depth at 15cm than those at buried depths at 10 cm and 20 cm, respectively. The temporal variations of soil water content along vertical distribution were different under different buried depths, with the buried depth at 15 cm the highest. The buried depth of moistube was the main factor influencing the temporal variations of soil water content. However, the effects of temporal variations of soil water content under different pressures were secondary.
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