WANG Meirong, SHI Haibin, YAN Jianwen, et al. Effects of Water and Nitrogen Regulation on Soil Nutrient Transfer During Fallow Period and Soil Fertility in the Following Year[J]. 2019, 33(2): 146-154.
DOI:
WANG Meirong, SHI Haibin, YAN Jianwen, et al. Effects of Water and Nitrogen Regulation on Soil Nutrient Transfer During Fallow Period and Soil Fertility in the Following Year[J]. 2019, 33(2): 146-154. DOI: 10.13870/j.cnki.stbcxb.2019.02.024.
Effects of Water and Nitrogen Regulation on Soil Nutrient Transfer During Fallow Period and Soil Fertility in the Following Year
Studying the effects of different nitrogen application amount on soil fertility before spring sowing could help determine the suitable nitrogen application amount in Hetao Irrigation Area. In this study
four nitrogen application levels (high-nitrogen N3:325 kg/hm2
medium-nitrogen N2:225 kg/hm2
low-nitrogen N1:125 kg/hm2
and no nitrogen application N0) were set up in the field experiment. The spatial and temporal distribution of water and salt and the changes of total nitrogen
alkali-hydrolysis nitrogen and organic matter contents were studied during freezing-thawing period. Then the soil fertility was evaluated by principal component analysis. The results showed:Firstly
after autumn water application
soil moisture content was significantly higher than before. The surface soil moisture content increased. When it just began to freeze
soil water accumulated to surface layer
and then froze to the deeper layer as the temperature reduced. The irrigation rates were the same in different treatments. The impacts of different nitrogen treatments on the soil moisture content was not significant. The soil moisture could meet the crop water demand. The soil salinities increased with the increasing nitrogen application rates during the growth period. A large amount of salt was leaching when water was applied in autumn. Soil salt was subjected to the combined effects of infiltration and evaporation during the water thawing
resulting in that the surface soil salinities were N0(0.14%) < N1(0.17%) < N2(0.19%) < N3 (0.45%). Secondly
during freeze-thaw period
soil nutrients were mainly concentrated in the surface soil layer of 0-20 cm. During the freeze-thaw period
the contents of total nitrogen
alkali-hydrolysis and organic matter in the soil showed a change pattern of first increasing and then decreasing. The maximum value occurred in the maximum freeze-thaw period
indicating that freezing helped the accumulation of total nitrogen
alkali-hydrolysis and organic matter. The last
soil fertility was comprehensively evaluated before the next spring sowing. Organic matter
organic carbon and total phosphorus on PC1 and PC2 had higher factor loads
contributing to soil fertility. Considering from the composite scores (N3 < N0 < N1 < N2)
high nitrogen treatment led to the low soil fertility
and the highest scores were given in the medium nitrogen treatment
resulting in the highest soil fertility. Therefore
it is
recommended that the nitrogen application rate should be around 225 kg/hm2 for the maize growth
and 20% for the basal
40% for the jointing stage and 40% for the tasseling stage respectively. This fertilization will be beneficial for the improvement of the soil fertility in the following spring sowing and also for the agricultural sustainable development.
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Related Author
YU Wu
TIAN Fangxiao
SHI Bohao
ZHOU Jinlong
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ZHOU Jinlong
WAN Dan
ZHAO Hongbo
Related Institution
College of Resources and Environment, Xizang Agricultural and Animal Husbandry University, Linzhi, Xizang
Alpine Soil and Water Conservation Research Center, Xizang Agriculture and Animal Husbandry University, Linzhi, Xizang
State Key Laboratory of Soil Erosion and Dryland Farming in Loess Plateau, Institute of Soil and WaterConservation, Northwest A&F University, Yangling, Shannxi
Institute of Soil and Water Conservation, CAS & MWR, Yangling