Transport Characteristics of Water and Nitrogen Under Bubbled-root Irrigation with Soil Initial Water Content[J]. 2017, 31(4): 118-126.
DOI:
Transport Characteristics of Water and Nitrogen Under Bubbled-root Irrigation with Soil Initial Water Content[J]. 2017, 31(4): 118-126. DOI: 10.13870/j.cnki.stbcxb.2017.04.020.
Transport Characteristics of Water and Nitrogen Under Bubbled-root Irrigation with Soil Initial Water Content
To explore the water and nitrogen transport characteristics under water and fertilizer integration of bubbled-root irrigation
through the indoor fertilizer infiltration test
the migration characteristics of wetting front migration
soil moisture
ammonium nitrogen and nitrate nitrogen were studied under different soil initial water content (4.13%
7.21%
11.06%
14.01%). The relationships between the cumulative infiltration amount
the wetting front migration distance and the soil initial water content of bubbled-root irrigation were established. An empirical model was proposed to calculate the cumulative infiltration volume and the wetting front migration distance under different initial water content. Results showed that: the cumulative infiltration
the wetting front migration distance
the moisture in the body
the distribution and transformation of nitrogen were all affected by the initial water content of soil. At the same time
the cumulative infiltration reduced with the increase of initial soil water content
while the wetting front migration distance increased with the increase of initial soil water content. The higher the initial water content of soil was
the larger volume of wetting body was
and the wilder water
ammonium nitrogen and nitrate nitrogen distributed. The closer to the emitter outlet
the contents of ammonium nitrogen and nitrate nitrogen in the soil were higher. The infiltration coefficient K decreased with the increase of initial soil water content
while the infiltration index α showed an opposite trend. The fitting parameters a and b of horizontal wetting front both increased with the increase of initial soil water content. The vertical downward wetting front migration index c increased with the increase of initial soil water content
while the infiltration index d decreased with the increase of initial soil water content. With the continuous redistribution of soil moisture distribution
the moisture distribution in the moist body was more uniform
and the uniformity of water distribution evaluated by Christiansen uniformity coefficient Cu
in moist body was 61.99%
74.27% and 83.60%
respectively
at the end of irrigation
redistribution of 1 day and 3 days. With the redistribution
the content of ammonium in the wetted body gradually decreased
but the distribution region of ammonium nitrogen was almost unchanged. With the redistribution
the distribution of nitrate nitrogen in the wetted area became larger
the average value of it increased
and the maximum value of it had a downward trend. The above research results can lay the foundation for further researches on water and nitrogen use efficient of bubbled-root irrigation technology.