Scientia Agricultura Sinica ›› 2023, Vol. 56 ›› Issue (7): 1333-1343.doi: 10.3864/j.issn.0578-1752.2023.07.011

• SOIL & FERTILIZER·WATER-SAVING IRRIGATION·AGROECOLOGY & ENVIRONMENT • Previous Articles     Next Articles

Response of Carbon and Nitrogen Distribution in Organo-Mineral Complexes of Red Paddy Soil to Long-Term Fertilization

LI Hao1,2(), CHEN Jin3, WANG HongLiang2(), LIU KaiLou4, HAN TianFu1, DU JiangXue1, SHEN Zhe1, LIU LiSheng1,5, HUANG Jing1,5, ZHANG HuiMin1,5()   

  1. 1 Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences/Key Laboratory of Arable Land Quality Monitoring and Evaluation, Ministry of Agriculture and Rural Affairs, Beijing 100081
    2 School of Resources and Environment, Henan Institute of Science and Technology, Xinxiang 453003, Henan
    3 Soil and Fertilizer & Resources and Environment Institute, Jiangxi Academy of Agricultural Sciences/Key Laboratory of Crop Ecophysiology and Farming System for the Middle and Lower Reaches of the Yangtze River, Ministry of Agriculture and Rural Affairs/National Engineering and Technology Research Center for Red Soil Improvement, Nanchang 330200
    4 Jiangxi Institute of Red Soil/National Engineering and Technology Research Center for Red Soil Improvement/Scientific Observational and Experimental Station of Arable Land Conservation in Jiangxi, Ministry of Agriculture and Rural Affairs, Nanchang 330046
    5 Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences/Qiyang Farmland Ecosystem National Observation and Research Station, Qiyang 426182, Hunan
  • Received:2022-02-27 Accepted:2022-04-29 Online:2023-04-01 Published:2023-04-03

Abstract:

【Objective】 The effects of long-term fertilization on the distribution of organic carbon (OC) and total nitrogen (TNOIC) of organo-mineral complexes in red paddy soil were studied, so as to provide a basis for long-term management and cultivation of soil fertility in red paddy soil. 【Method】 The red paddy soils in long-term fertilization experiment were studied (Since 1984), which included four treatments: no fertilization (CK), inorganic P and K fertilizers (PK), inorganic N, P and K fertilizers (NPK), and NPK plus manure (NPKM, 70%NPK plus 30% manure). Soil samples of 0-20 cm soil layer were collected, and the distribution of organo-mineral complexes at each particle level (<2 μm, 2-10 μm, 10-20 μm, 20-50 μm, and 50-250 μm) was analyzed. The effects of fertilization on the content, storage of organic carbon and total nitrogen as well as the carbon-nitrogen ratio (C/N) were discussed. The effects of OC and TNOIC contents in organo-mineral complex on contribution rate of SOC and TN contents in red paddy soil were investigated too.【Result】 Compared with the CK treatment, the fertilization treatment significantly increased the particle size ratio of 20-50 μm and decreased the particle size ratio of <10 μm. Compared with other fertilization treatments, NPKM treatment increased the proportion of 50-250 μm grain size complex more significantly. Different fertilization treatments had different effects on the content of OC and TNOIC in grain size. Compared with PK, the content of OC and TNOIC in grain size from 50 μm to 250 μm under NPK treatment increased 36.3% and 80.6%, respectively. Compared with NPK, the content of OC and TNOIC in 50-250 μm granular complex increased by 35.4% and 19.5% under NPKM treatment, respectively. The OC and TNOIC storage of the organic and inorganic complexes were mainly distributed at the 10-20 μm particle level. And fertilization significantly reduced the storage of <2 μm particle-level complex OC and TNOIC, but increased the storage of OC and TNOIC at 20-50 μm particle-level. Compared with PK treatment, the OC storages of <2 μm and 50-250 μm particle-level complexes treated by NPK increased by 18.5% and 31.2%, respectively, and the storages of TNOIC increased by 18.8% and 73.7%, respectively. Compared with NPK, the NPKM treatment reduced the OC and TNOIC storages of the <2 μm particle-level complex by 25.6% and 27.4%, respectively, while OC and TNOIC storages of 50-250 μm particle-level complex increased by 56.3% and 38.6%, respectively. Fertilization significantly influenced the C/N ratio of 50-250 μm particles. Compared with PK, the C/N ratio of 50-250 μm fraction treated with NPK decreased by 24.6%; compared with NPK, the C/N ratio of 50-250 μm fraction treated with NPKM was increased by 13.4%. Fertilization significantly affected the contribution rate of organo-mineral complexes of each particle size to SOC and TN content. Compared with PK, the contribution rate of NPK treatment 50-250 μm particle-level complex to SOC and TN increased by 17.4% and 47.4%, respectively. Compared with NPK, the contribution rate of NPKM treatment 50-250 μm particle to SOC and TN were reduced by 39.5% and 32.8%, respectively.【Conclusion】 In red paddy soil, the long-term fertilization promoted the formation of large-grain organo-mineral complexes. The nitrogen input in the chemical fertilizers significantly increased the grain-level organic carbon, total nitrogen content and storage of the granular grade of 50-250 μm. The organo-mineral combined application was conducive to increasing the soil organic carbon content and the proportion of large-grain organo-mineral complexes, which was helping to preserve the inorganic nitrogen fertilizer application. Therefore, organic and inorganic compound application was an effective measure for long-term fertilization management of red paddy soils.

Key words: long-term fertilization, red paddy soil, organo-mineral complex, organic carbon, total nitrogen

Fig. 1

The distribution of different sizes of organo-mineral complex in soils Different letters above the bars indicate significant differences between different treatments at the same size of organo-mineral complexes (P<0.05)"

Table 1

The organic carbon contents of each size of organo-mineral complex under different fertilization regimes (g·kg-1)"

处理
Treatment
粒级Size (μm) Size
<2 2-10 10-20 20-50 50-250
CK 16.39±0.35cA 12.42±0.76cB 8.66±0.57bC 6.08±0.61cD 12.43±0.79cB **
PK 17.30±1.58bcA 13.29±1.00bcB 10.84±0.92aC 7.75±0.33abD 13.89±1.80cB
NPK 18.94±0.72bA 14.51±0.77bB 11.22±0.55aC 7.48±0.74bD 18.93±0.89bA
NPKM 21.06±1.00aB 16.45±0.42aC 12.07±0.42aD 8.73±0.31aE 25.64±0.44aA
Fertilization ** **

Fig. 2

Distribution of organic carbon storage in organo- mineral complex with different grain sizes F: Fertilization, S: Size, F×S: Fertilization×Size. Different letters above the bars indicate significant differences between different treatments at the same size of organo-mineral complexes (P<0.05).** Significant at the 0.01 probability levels. The same as Fig. 3"

Table 2

The total nitrogen contents of each size of organo-mineral complex under different fertilization regimes (g·kg-1)"

处理
Treatment
粒级Size (μm) Size
<2 2-10 10-20 20-50 50-250
CK 3.87±0.14cA 2.54±0.21bB 1.51±0.10bC 1.01±0.09cD 1.60±0.02cC **
PK 4.23±0.32bcA 2.63±0.20bB 1.99±0.17aC 1.28±0.08bD 1.65±0.23cC
NPK 4.63±0.07abA 2.85±0.16abB 2.07±0.12aC 1.26±0.15bD 2.98±0.15bB
NPKM 5.03±0.63aA 3.23±0.25aB 2.23±0.08aC 1.47±0.02aD 3.56±0.15aB
Fertilization ** **

Fig. 3

Distribution of total nitrogen storage in organo-mineral complex with different grain sizes"

Table 3

Effects of different fertilization on C/N ratio of organo-mineral complex in different grain sizes"

处理
Treatment
粒级Size (μm)
<2 2-10 10-20 20-50 50-250
CK 4.24±0.11aD 4.89±0.09aC 5.73±0.08aB 6.02±0.16aB 7.77±0.44cA
PK 4.09±0.07aE 5.05±0.15aD 5.45±0.07bC 6.05±0.14aB 8.42±0.08aA
NPK 4.09±0.09aC 5.09±0.19aB 5.42±0.16bB 5.94±0.13aA 6.35±0.38dA
NPKM 4.19±0.35aD 5.09±0.29aC 5.41±0.05bC 5.94±0.28aB 7.20±0.20bA

Fig. 4

Contribution rate of organo-mineral complexes of different grain sizes to organic carbon and total nitrogen"

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