Scientia Agricultura Sinica ›› 2026, Vol. 59 ›› Issue (21): 4854-4864.doi: 10.3864/j.issn.0578-1752.2026.21.011

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

Spatial Variation Characteristics and Influencing Factors of Soil Organic Matter Fractions in Drylands of the Songnen Plain

YAO Yi1(), ZHANG SiYu1, HAO SiQi1, LI ShuangYi1, SUN LiangJie1, CHEN JingYu2, AN TingTing1(), WANG JingKuan1   

  1. 1 College of Land and Environment, Shenyang Agricultural University/Key Laboratory of Northeast Land Conservation, Ministry of Agriculture and Rural Affairs/National Engineering Laboratory for Efficient Utilization of Soil and Fertilizer Resources, Shenyang 110866
    2 Grain Storage of North Agricultural Development Company, Nenjiang 161499, Heilongjiang
  • Received:2025-12-31 Accepted:2026-04-03 Online:2026-11-01 Published:2026-11-06
  • Contact: AN TingTing

Abstract:

【Objective】 This study explored the spatial distribution characteristics and influencing factors of soil organic matter (SOM) fractions in the drylands of the Songnen Plain, so as to provide a basis for SOM improvement and black soil protection in Northeast China. 【Method】Taking the dryland soil as the research object, 200 surface soil samples (0-20 cm) were collected in the Songnen Plain in June 2023. Then, soil samples were separated into particulate organic matter (POM) and mineral-associated organic matter (MAOM) fractions by the particle size fractionation method. Combined with classical statistical methods and the Random Forest model, this study investigated the distribution characteristics of SOM fractions and explored the influences of climate, topography, soil properties and vegetation factors on them. 【Result】The average content of MAOM and POM was 24.7 and 5.71 g·kg-1, respectively, accounting for an average of 70.9% and 17.1% of the total SOM content, respectively. In the Songnen Plain region, both fractions exhibited a decreasing trend from the northeast to the southwest regions. MAOM content (r=0.93, 0.66, and 0.51, respectively) and POM content (r=0.75, 0.25, and 0.36, respectively) were extremely significantly (P<0.01) positively correlated with SOM, clay content, and altitude. MAOM (r=-0.33, -0.57, -0.79, -0.73, and -0.40, respectively) and POM (r=-0.21, -0.26, -0.55, -0.58, and -0.24, respectively) were extremely significantly (P<0.01) negatively correlated with pH, bulk density, annual mean temperature, effective accumulated temperature, and normalized difference vegetation index. Random Forest model analysis showed that effective accumulated temperature, annual mean temperature, and clay content extremely significantly (P<0.01) affected the spatial variation of MAOM fraction, with explanation degrees of 33.7%, 32.7%, and 23.8%, respectively; effective accumulated temperature, annual mean temperature, and available phosphorus extremely significantly (P<0.01) affected the spatial variation of POM fractions, with explanation degrees of 26.1%, 25.2%, and 22.8%, respectively. 【Conclusion】 The soil organic matter fractions in the drylands of the Songnen Plain showed an obvious spatial distribution pattern of being higher in the northeast and lower in the southwest, and annual mean temperature and effective accumulated temperature were the key factors driving their spatial distribution.

Key words: dryland soil, particulate organic matter, mineral-associated organic matter, spatial distribution, influencing factors, dryland soil of the Songnen Plain

Fig. 1

Location of the study area and distribution map of sampling sites"

Table 1

Descriptive analysis of soil organic matter fractions in the Songnen Plain"

指标
Indicator
最小值
Minimum
最大值
Maximum
平均值
Mean
标准差
Standard deviation
变异系数
Coefficient of variation (%)
土壤有机质SOM (g·kg-1) 6.31 82.8 34.50 14.8 43.0
矿物结合态有机质MAOM (g·kg-1) 3.96 49.8 24.70 11.3 46.0
颗粒有机质POM (g·kg-1) 1.04 25.8 5.71 3.26 57.1
矿物结合态有机质占有机质比例MAOM/SOM (%) 47.00 92.0 70.90 11.00 15.6
颗粒有机质占有机质比例POM/SOM (%) 5.00 34.0 17.10 6.16 35.9

Fig. 2

Distribution of soil organic matter and its fractions contents in the Songnen Plain SOM: Soil organic matter; POM: Particulate organic matter; MAOM: Mineral-associated organic matter"

Fig. 3

Spatial distribution of soil organic matter fractions contents in the Songnen Plain"

Fig. 4

Correlation analysis between soil organic matter fractions and influencing factors in the Songnen Plain AK: Available potassium; AP: Available phosphorus; BD: Bulk density; MAT: Annual mean temperature; MAP: Annual mean precipitation; EAT: Effective accumulated temperature; ALT: Altitude; PX: Slope aspect; PD: Slope gradient; NDVI: Normalized difference vegetation index. Pearson correlation coefficient was used to evaluate the correlation between variables. * and ** denote significance levels of P<0.05 and P<0.01, respectively. The same as below"

Fig. 5

Relative importance of environmental variables affecting soil organic matter fractions in the Songnen Plain Panels a and b represent the relative importance of environmental variables in mineral associated organic matter and particulate organic matter, respectively"

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