Combined effects of soil colloid and soil extracellular enzymes on nitrogen loss from sloping farmland

• Soil colloids and extracellular enzymes undergo co-transport during hydrological processes. • Extracellular enzyme of hydrological pathways have a powerful effect on nitrogen loss by controlled enzyme stoichiometric. • Soil colloids' and extracellular enzymes' synergistic transport have potential impact on nitrogen loss in hydrology path. The extracellular enzyme plays a crucial role in nitrogen (N) conversion. Soil colloid serves as an important transporter of N transport in hydrological processes. This study investigated soil colloid-mediated N loss co-transporting with soil extracellular enzymes. Five simulated rainfall experiments were conducted under four tillage treatments in a purple sloping farmland in Sichuan, China. The N concentrations, soil mineral colloids, and four carbon (C), N and phosphorus (P) acquisition extracellular enzymes (βG, AP, NAG, and LAP) in surface runoff and interflow were measured. The results showed that cross-slope tillage with straw returning practices significantly reduced the concentrations of TN, PN, NH 4 + , and DON in surface runoff. The activities of N and P acquisition enzymes in interflow were higher than in surface runoff, while C acquisition enzymes showed the opposite trend. The BG and AP enzymes dominated in surface runoff, while AP and NAG dominated in interflow. The concentrations of fine soil mineral colloids (SMC, φ<1 μm) and coarse mineral colloids (CMC, φ>1 μm) in interflow were higher than that in surface runoff. The extracellular enzymes were found to co-transport with soil colloid migration during the hydrologic process. The involvement of colloid in extracellular enzyme migration in surface runoff was primarily due to SMC, while in interflow, it was the joint action of SMC and CMC. Surface runoff is always in N and P limits, while interflow is only in the P limits. With a SEM combined model quantitatively analysis, we found the synergistic transport of soil colloid and extracellular enzymes significantly impacted TN loss, explaining 95 % and 55 % of the differences between surface runoff and interflow N loss pathways. This emphasizes the importance of understanding the co-transport mechanism between soil colloid and extracellular enzymes in N loss processes.

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Publication Details

Journal
Geoderma
Published
2024-09-21
DOI
https://doi.org/10.1016/j.geoderma.2024.117041
Citations
4
Primary Topic
Soil Carbon and Nitrogen Dynamics
Type
article
Field-Weighted Citation Impact
1.33

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article

Combined effects of soil colloid and soil extracellular enzymes on nitrogen loss from sloping farmland

Mingxiang Xu, Shanghong Chen, Dinghui Liu, Xuekai Jing et al.
4 citations
Geoderma
Soil Carbon and Nitrogen Dynamics
1.33
article

Combined effects of soil colloid and soil extracellular enzymes on nitrogen loss from sloping farmland

Mingxiang Xu, Shanghong Chen, Dinghui Liu, Xuekai Jing, Yulong Shi, Qingwen Zhang, Zheng Li
article en
4 citations

Abstract

• Soil colloids and extracellular enzymes undergo co-transport during hydrological processes. • Extracellular enzyme of hydrological pathways have a powerful effect on nitrogen loss by controlled enzyme stoichiometric. • Soil colloids' and extracellular enzymes' synergistic transport have potential impact on nitrogen loss in hydrology path. The extracellular enzyme plays a crucial role in nitrogen (N) conversion. Soil colloid serves as an important transporter of N transport in hydrological processes. This study investigated soil colloid-mediated N loss co-transporting with soil extracellular enzymes. Five simulated rainfall experiments were conducted under four tillage treatments in a purple sloping farmland in Sichuan, China. The N concentrations, soil mineral colloids, and four carbon (C), N and phosphorus (P) acquisition extracellular enzymes (βG, AP, NAG, and LAP) in surface runoff and interflow were measured. The results showed that cross-slope tillage with straw returning practices significantly reduced the concentrations of TN, PN, NH 4 + , and DON in surface runoff. The activities of N and P acquisition enzymes in interflow were higher than in surface runoff, while C acquisition enzymes showed the opposite trend. The BG and AP enzymes dominated in surface runoff, while AP and NAG dominated in interflow. The concentrations of fine soil mineral colloids (SMC, φ<1 μm) and coarse mineral colloids (CMC, φ>1 μm) in interflow were higher than that in surface runoff. The extracellular enzymes were found to co-transport with soil colloid migration during the hydrologic process. The involvement of colloid in extracellular enzyme migration in surface runoff was primarily due to SMC, while in interflow, it was the joint action of SMC and CMC. Surface runoff is always in N and P limits, while interflow is only in the P limits. With a SEM combined model quantitatively analysis, we found the synergistic transport of soil colloid and extracellular enzymes significantly impacted TN loss, explaining 95 % and 55 % of the differences between surface runoff and interflow N loss pathways. This emphasizes the importance of understanding the co-transport mechanism between soil colloid and extracellular enzymes in N loss processes.

GeodermaVol. 450
China Geological Survey (CN), Institute of Soil and Water Conservation (CN), Institute of Environment and Sustainable Development in Agriculture (CN), Northwest A&F University (CN)
National Natural Science Foundation of China
Zero hunger
Openalex Percentile: Top 19%
Soil Carbon and Nitrogen Dynamics
1.33
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