Scientia Agricultura Sinica ›› 2025, Vol. 58 ›› Issue (8): 1579-1590.doi: 10.3864/j.issn.0578-1752.2025.08.009

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

Eeffects of Long-Term Fertilization on Bacterial Community Structure and Carbon Metabolic Functions in Brown Soil

BAI YuXin1,2,3(), LIU LingZhi1(), AN TingTing1, LI ShuangYi1, WANG JingKuan1   

  1. 1 College of Land and Environment, Shenyang Agricultural University/National Engineering Laboratory for Efficient Utilization of Soil and Fertilizer Resources/Key Laboratory of Arable Land Conservation in Northeast China, Ministry of Agriculture and Rural Affairs, Shenyang 110866
    2 Shenyang Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016
    3 University of Chinese Academy of Sciences, Beijing 101400
  • Received:2024-07-18 Accepted:2024-11-15 Online:2025-04-16 Published:2025-04-21
  • Contact: LIU LingZhi

Abstract:

【Objective】 This study aimed to elucidate the relationships among bacterial population structure, key species, carbon metabolic functions, and variations in soil physicochemical and biological properties resulting from long-term different fertilization treatments in agricultural soils. 【Method】 The amplicon sequencing technology based on the molecular marker of bacterial 16S rRNA were employed to analyze soil bacterial community structure, ecological networks, potential carbon metabolic functions, and their correlations with soil physicochemical and biological properties after 29 years of continuous application of various fertilization treatments (no fertilization as control, CK; chemical fertilizers, N4; and reduced application of chemical fertilizer combined with organic manure, M2N2) at the Long-term Positioning Experimental Station at Shenyang Agricultural University. 【Result】Different fertilization treatments significantly altered soil physicochemical and biological properties, and bacterial populations, diversity, and abundance of potential carbon metabolic genes. Compared with CK treatment, N4 treatment significantly decreased soil pH value, bacterial abundance and community diversity, which indicated that M2N2 treatment demonstrated a beneficial maintenance effect. Although long-term fertilization practices (both N4 and M2N2) significantly increased soil respiration rates, they also markedly reduced net nitrogen (N) mineralization rates at 0-20 cm soil layer. Furthermore, compared with N4 treatment, M2N2 treatment significantly enhanced soil net N mineralization rates. Soil ammonium N content, net N mineralization rate and pH value were the critical environmental factors influencing soil bacterial populations. Network co-occurrence analysis revealed that Bradyrhizobium elkanii and beta proteobacterium WWH154 were the key bacterial species that maintained the stability of bacterial ecological networks, and about 100 dominant bacterial species co-occurred fully with beta proteobacterium WWH154 and 54% of the species co-occurred with Bradyrhizobium elkanii. Long-term fertilization (N4 and M2N2) increased the relative abundance of two key species by 61.9%-169.4%, especially the M2N2 treatment. The function prediction of carbon metabolic genes showed that N4 treatment reduced the abundance of various carbon metabolism-related genes, such as carbon fixation pathways in prokaryotes, Aminoacyl tRNA biosynthesis and Amino acid related enzymes in soil bacteria, and M2N2 treatment significantly stabilized the carbon metabolic pathways. 【Conclusion】In summary, long-term fertilization altered the physicochemical and biological properties of agricultural soil. Reduced application of chemical fertilizer combined with organic manure enriched key bacterial species and increased the complexity of microbial networks, which would be beneficial to coping with environmental changes, thus maintaining soil ecological functions and increasing crop yield.

Key words: long-term fertilization, brown soil, key bacterial species, bacterial diversity, network co-occurrence

Table 1

Soil physical, chemical, and biological properties under different fertilization treatments"

土层
Soil layer (cm)
处理
Treatment
酸碱性
pH
总氮
TN
(mg·kg-1)
铵态氮
NH4+-N
(mg·kg-1)
硝态氮
NO3--N
(mg·kg-1)
有效磷
AP
(mg·kg-1)
有机质
SOM
(mg·kg-1)
16S rDNA
基因丰度
16S rDNA
gene abundance
(log copies·g-1)
氮矿化速率
Nitrogen
mineralization rate
(mg·kg-1·d-1)
土壤呼吸
Soil respiration
(μg·g-1·h-1)
0-20 CK 6.30±0.11Aa 1.04±0.01Ab 0.62±0.01Ac 9.34±0.04Ac 33.75±0.13Ab 18.57±0.36Ab 11.99±0.06Aa 30.00±4.29Aa 9.81±0.88Ab
N4 4.91±0.09Ac 0.93±0.01Ac 2.08±0.03Aa 11.59±0.02Ab 24.25±0.31Ac 16.33±0.11Ac 11.88±0.12Aa 22.93±3.28Ac 12.51±0.80Aa
M2N2 5.92±0.01Ab 1.35±0.003Aa 1.61±0.03Ab 12.64±0.12Aa 181.71±0.19Aa 22.37±0.17Aa 12.16±0.05Aa 29.45±4.21Ab 13.89±0.24Aa
20-40 CK 6.52±0.01Aa 0.69±0.02Ba 0.71±0.01Bb 7.15±0.01Ac 12.46±0.13Bb 12.03±0.36Ba 11.61±0.04Aa 18.57±2.65Ac 9.06±0.69Ab
N4 5.40±0.06Ac 0.65±0.01Ba 0.73±0.05Bab 9.89±0.05Ab 6.64±0.15Bc 11.69±0.25Ba 10.95±0.01Ac 23.61±3.37Ab 11.55±0.37Aa
M2N2 5.91±0.09Ab 0.66±0.01Ba 0.83±0.02Ba 11.24±0.07Aa 104.64±0.19Ba 11.26±0.21Ba 11.37±0.04Ab 31.53±4.50Aa 11.41±0.64Aa

Fig. 1

Changes in soil bacterial abundance, community differences, and the number of unique species under different fertilization treatments In the figure, uppercase letters indicate significant differences between soil layers within the same treatment at the P<0.05 level, while lowercase letters indicate significant differences between treatments within the same soil layer at the P<0.05 level. CK20、N420、M2N220: Treatment in 0-20 cm soil layer, CK40、N440、M2N240: Treatment in 20-40 cm soil layer. The same as below"

Fig. 2

Differences in the phylum-level community composition of soil bacteria under various fertilization treatments"

Fig. 3

Ecological network analysis and distribution of key bacterial species in soil under different fertilization treatments A: Bacterial ecological network analysis, where different colors represent different bacterial species-level OTU classifications, and the thickness of the gray lines indicates the degree of correlation; B: Distribution of keystone species in 0-20 cm soil layer"

Fig. 4

Redundancy analysis (RDA) of soil fungal communities and environmental factors under different fertilization regimes"

Fig. 5

Predicted functional genes of soil bacterial communities under different fertilization regimes"

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