Depth‐Dependent Soil C:N:P Stoichiometry in <i>Robinia pseudoacacia</i> Mixed Versus Pure Stands and Its Drivers in the Chinese Loess Hilly Region

ABSTRACT Soil carbon (C): nitrogen (N): phosphorus (P) stoichiometry, which reflects nutrient availability, responds species‐specifically to mixed‐species afforestation. However, how mixed species affect soil C:N:P stoichiometry with depth remains poorly understood. This knowledge gap is critical in the Loess Hilly Region, where understanding depth‐dependent nutrient dynamics is essential for ecological restoration and sustainable management. Here, we investigated C:N:P dynamics across soil depths (0–20, 20–40, and 40–60 cm) and associated influencing factors (i.e., afforestation measures and soil physicochemical properties) in mixed stands ( Robinia pseudoacacia/Prunus davidiana ; R. pse/Prunus sibirica ), pure Robinia ( R. pse ), and Prunus ( P. dav ; P. sib ). The results showed that stand type significantly influenced the vertical migration of N and P elements in soil profiles ( p &lt; 0.05). Compared to pure Robinia, mixed stands ( R. pse/P. dav ) enhanced N cycling, while mixtures with P. sib demonstrated N complementarity. In contrast, P . dav and P . sib mixtures promoted P cycling due to contrasting soil organic matter (SOM) decomposition effects between R. pse (inhibitory) and the other two species (enhancing). Soil organic C and total N (TN) across soil depths primarily derived from SOM, whereas soil total P originated predominantly from mineral sources. The nodule bacteria of R. pse enhanced TN concentrations, whereas mixed planting accelerated P release from SOM and minerals. Soil C:N:P stoichiometry at 20–40 cm depth was more influenced by the proportion of clay, associated with improved microenvironment, for example, soil water content. These findings demonstrate that mixing R. pse and P . dav enhances soil nutrient cycles through soil physical‐dominated properties, which provides new insights for optimizing mixed afforestation strategies in arid land ecosystems.

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Journal
Land Degradation and Development
Published
2025-12-23
DOI
https://doi.org/10.1002/ldr.70185
Primary Topic
Soil Carbon and Nitrogen Dynamics
Type
article
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article

Depth‐Dependent Soil C:N:P Stoichiometry in Robinia pseudoacacia Mixed Versus Pure Stands and Its Drivers in the Chinese Loess Hilly Region

Jordi Sardans, Josep Penuelas, Senbao Lu, Yarong Sun et al.
Land Degradation and Development
Soil Carbon and Nitrogen Dynamics
article

Depth‐Dependent Soil C:N:P Stoichiometry in Robinia pseudoacacia Mixed Versus Pure Stands and Its Drivers in the Chinese Loess Hilly Region

Jordi Sardans, Josep Penuelas, Senbao Lu, Yarong Sun, Yunming Chen
article en

Abstract

ABSTRACT Soil carbon (C): nitrogen (N): phosphorus (P) stoichiometry, which reflects nutrient availability, responds species‐specifically to mixed‐species afforestation. However, how mixed species affect soil C:N:P stoichiometry with depth remains poorly understood. This knowledge gap is critical in the Loess Hilly Region, where understanding depth‐dependent nutrient dynamics is essential for ecological restoration and sustainable management. Here, we investigated C:N:P dynamics across soil depths (0–20, 20–40, and 40–60 cm) and associated influencing factors (i.e., afforestation measures and soil physicochemical properties) in mixed stands ( Robinia pseudoacacia/Prunus davidiana ; R. pse/Prunus sibirica ), pure Robinia ( R. pse ), and Prunus ( P. dav ; P. sib ). The results showed that stand type significantly influenced the vertical migration of N and P elements in soil profiles ( p &lt; 0.05). Compared to pure Robinia, mixed stands ( R. pse/P. dav ) enhanced N cycling, while mixtures with P. sib demonstrated N complementarity. In contrast, P . dav and P . sib mixtures promoted P cycling due to contrasting soil organic matter (SOM) decomposition effects between R. pse (inhibitory) and the other two species (enhancing). Soil organic C and total N (TN) across soil depths primarily derived from SOM, whereas soil total P originated predominantly from mineral sources. The nodule bacteria of R. pse enhanced TN concentrations, whereas mixed planting accelerated P release from SOM and minerals. Soil C:N:P stoichiometry at 20–40 cm depth was more influenced by the proportion of clay, associated with improved microenvironment, for example, soil water content. These findings demonstrate that mixing R. pse and P . dav enhances soil nutrient cycles through soil physical‐dominated properties, which provides new insights for optimizing mixed afforestation strategies in arid land ecosystems.

Land Degradation and DevelopmentVol. 37(4)
Shanxi Agricultural University (CN), Institute of Soil and Water Conservation (CN), Centre for Research on Ecology and Forestry Applications (ES), Ministry of Water Resources of the People's Republic of China (CN), Shanxi Academy of Agricultural Sciences (CN), University of Chinese Academy of Sciences (CN), Global Ecology Unit CREAF-CSIC-UAB
Life in Land
Openalex Percentile: Top 34%
Soil Carbon and Nitrogen Dynamics
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