ZHANG Quanju, FEI Liangjun, LIU Lihua, et al. Soil Water Movement Characteristics in Muddy and Fertilizer Water Solution Infiltration Under Film Hole Irrigation Affected by Multiple Factors[J]. 2021, 35(1): 265-270.
DOI:
ZHANG Quanju, FEI Liangjun, LIU Lihua, et al. Soil Water Movement Characteristics in Muddy and Fertilizer Water Solution Infiltration Under Film Hole Irrigation Affected by Multiple Factors[J]. 2021, 35(1): 265-270. DOI: 10.13870/j.cnki.stbcxb.2021.01.038.
Soil Water Movement Characteristics in Muddy and Fertilizer Water Solution Infiltration Under Film Hole Irrigation Affected by Multiple Factors
In order to study the influence of multiple factors on soil water movement characteristics of muddy water film hole fertilizer solution infiltration
indoor soil box infiltration test was carried out. Four experimental factors including initial soil moisture content
soil bulk density
sediment concentration of muddy water and fertilizer solution concentration
3 levels for each factor
and 12 groups of experiments (9 of orthogonal experiments and 3 of validation experiments). The effects of each factor on cumulative infiltration volume per unit membrane hole area
infiltration rate and average volume water content increment of muddy water membrane hole irrigation fertilizer solution were analyzed. The empirical model and model parameters of cumulative infiltration per unit membrane pore and average volume moisture content increment of wetting body with experimental factors were deduced and verified by multiple regression. The results showed that the initial moisture content of the soil
soil bulk density and sand content and fertilizer concentration had a significant effect on the cumulative inlet of the unit membrane hole (P<0.01). The degree of influence from large to small was the sand content
soil bulk density
the initial soil moisture content
the concentration of fertilizer. The increase in the average moisture content of the wet body was almost independent of the permeation time. The initial moisture content
sand content and fertilizer concentration of the soil were significantly related to it (P<0.01)
and the soil weight was significantly related to it (P<0.05)
and the degree of influence from large to small was the initial moisture content of the soil
fertilizer concentration
sand content
soil bulk density. The empirical model and model coefficient established were qualified. The error between the predicted and the measured values was within ±10%
and the precision was good
which could be used to predict the soil moisture infiltration situation when the experimental factors were different.
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Soil Moisture Migration Characteristics of Typical Small Watershed in Rain Feed Region Under Individual Rainfall Events
Effect of Film Hole Diameter on Transport Characteristics of Water and Nitrogen in Soil Under Film Hole Irrigation with Muddy Water
Soil Water Isotope Characteristics of the Vadose in a Typical Small Watershed on the Loess Plateau of China
Effects of Silt Content and Clay and Sand Grade on Freedom Infiltration Characteristics of Muddy Water Film Hole Irrigation
Related Author
CHEN Lin
ZHONG Yun
WANG Jinhui
FU Yuliang
FEI Liangjun
JIN Shijie
KE Haocheng1
MA Tiantian1
Related Institution
Institute of Water Resources and Hydro-electric Engineering, Xi’an University of Technology
State Key Laboratory Base of Eco-hydraulic Engineering in Arid Area, Xi’an University of Technology
State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling
Institute of Water Resources and Hydro-electric Engineering, Xian University of Technology, Xian
State Key Laboratory Base of Eco-hydraulic Engineering in Arid Area, Xi’an University of Technology