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土壤容重对一维垂直浑水肥液入渗水氮运移特性影响
引用本文:白瑞,费良军,陈琳,刘乐,钟韵,李巧丽. 土壤容重对一维垂直浑水肥液入渗水氮运移特性影响[J]. 排灌机械工程学报, 2021, 39(3): 306-311. DOI: 10.3969/j.issn.1674-8530.19.0100
作者姓名:白瑞  费良军  陈琳  刘乐  钟韵  李巧丽
作者单位:西安理工大学水利水电学院,陕西 西安 710048;陕西省水利电力勘测设计研究院,陕西 西安710048;西安理工大学水利水电学院,陕西 西安 710048
基金项目:国家自然科学基金资助项目(51779205,51479161);陕西省水利科技项目(2014slkj-02)。
摘    要:为了揭示土壤容重对浑水肥液入渗水氮运移特性的影响,通过室内土柱试验,研究不同土壤容重(1.30,1.35,1.40,1.45 g/cm3)累积入渗量、湿润锋运移距离、土壤含水率分布规律以及土壤硝态氮运移特性,采用Philip入渗模型和电容充电经验模型对累积入渗量进行了拟合,建立了累积入渗量、湿润锋运移距离与土壤容重之间...

关 键 词:浑水入渗  土壤容重  水分分布  硝态氮
收稿时间:2019-04-25

Effects of soil bulk density on water and nitrogen transport characteristics under one-dimensional vertical infiltration of muddy water and fertilizer
BAI Rui,FEI Liangjun,CHEN Lin,LIU Le,ZHONG Yun,LI Qiaoli. Effects of soil bulk density on water and nitrogen transport characteristics under one-dimensional vertical infiltration of muddy water and fertilizer[J]. Journal of Drainage and Irrigation Machinery Engineering, 2021, 39(3): 306-311. DOI: 10.3969/j.issn.1674-8530.19.0100
Authors:BAI Rui  FEI Liangjun  CHEN Lin  LIU Le  ZHONG Yun  LI Qiaoli
Affiliation:1. Institute of Water Resources and Hydro-electric Engineering, Xi′an University of Technology, Xi′an, Shaanxi 710048, China; 2. Shaanxi Province Institute of Water Resources and Electric Power Investigation and Design, Xi′an, Shaanxi 710001, China
Abstract:In order to reveal the effect of soil bulk density on water and nitrogen transport characteristics of muddy water and fertilizer infiltration,through the indoor soil column infiltration test,the cumulative infiltration,the wetting front migration distance,soil water content distribution and soil nitrate nitrogen transport characteristics were studied under different soil bulk densities(1.30,1.35,1.40,1.45 g/cm3).The cumulative infiltration was fitted using the Philip infiltration model and capacitive charging empirical model.The relationships of cumulative infiltration and wetting front migration distance with soil bulk density were established,respectively.The results showed that for the same infiltration time the cumulative infiltration reduced with increasing soil bulk density,the higher the soil bulk density,the smaller the wetting front migration distance,and the narrower the distribution range of water and nitrate nitrogen in the wetted body.The cumulative infiltration of muddy water and fertili-zer infiltration conformed to the Philip infiltration model and capacitive charging empirical model.There was a significant power function relationship between wetting front migration distance and infiltration time.After the water supply was stopped,both of the soil water content and nitrate decreased with increasing infiltration depth.As the soil moisture was redistributed,the nitrate nitrogen content in the upper layer gradually decreased,but that in the lower layer gradually increased.After a redistribution for two days,the nitrate nitrogen content peaked near the wetting front,and the distribution of nitrate nitrogen content in the whole wetted body tended to be uniform.The results provide a basic reference for further study on nitrogen transport in the infiltration of muddy water and fertilizer.
Keywords:muddy water infiltration  soil bulk density  water distribution  nitrate nitrogen
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