Effects of initial soil moisture content on soil water and nitrogen transport under muddy water film hole infiltration

被引:6
|
作者
Liu, Lihua [1 ,2 ]
Fei, Liangjun [1 ,2 ]
Chen, Lin [1 ,2 ]
Hao, Kun [1 ,2 ]
Zhang, Quanju [1 ,2 ]
机构
[1] Xian Univ Technol, State Key Lab Ecohydraul Northwest Arid Reg, Xian 710048, Peoples R China
[2] Xian Univ Technol, Inst Water Resources & Hydroelect Engn, Xian 710048, Peoples R China
基金
中国国家自然科学基金;
关键词
film hole irrigation; muddy water; initial soil moisture content; water and nitrogen transport; water redistribution; IRRIGATION; MODEL;
D O I
10.25165/j.ijabe.20211404.6024
中图分类号
S2 [农业工程];
学科分类号
0828 ;
摘要
Film hole irrigation has been widely adopted as an effective water-saving irrigation technology in the arid and semiarid areas of China. To investigate the effects of initial soil moisture content (theta(0)) on soil water and nitrogen transport characteristics under muddy water film hole infiltration, the laboratory experiments were conducted with muddy water film hole infiltration, using five initial soil moisture content treatments. The models for describing the relationships between the cumulative infiltration (I(t)) and infiltration duration (t); the relationship among the horizontal and vertical migration distances of the wetting front (F-x, F-z), theta(0) and t, were established. The results showed that the initial soil moisture content had a significant effect on I(t), F-x, F-z and moisture content distribution in the wetted body. The change of I(t) over t conformed to Kostiakov model. With the increase of theta(0), the infiltration coefficient (K) gradually decreased. NO3--N was mainly distributed in the range of the wetting radius of 15 cm, while NH4+-N was mainly distributed in the range of the wetting radius of 8 cm. This study can provide a theoretical basis and technical support for film hole irrigation.
引用
收藏
页码:182 / 189
页数:8
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