Rare and Abundant <scp><i>phoD</i></scp>‐Harboring Bacteria Mediate the Mineralization of Organic Phosphorus Fractions in Soil Aggregates During Cut Slope Restoration

ABSTRACT Phosphorus (P) is the key nutritional element in the soil of cut road slopes undergoing ecological restoration, and the transformation of organic P (Po) is a crucial part of the P cycle. However, the role of phoD ‐harboring bacteria in driving the mineralization of Po fractions in road slope soil aggregates is unclear. This study analyzed road slope soils that had undergone 7, 11, and 14 years of restoration in the western Sichuan Plateau of China. We examined the differences and associations between the Po fraction content, alkaline phosphatase (ALP) activity, and community composition of rare and abundant phoD ‐harboring bacteria in soil aggregates of four particle sizes (0.053–0.25, 0.25–2, 0.053–0.25, and, &gt; 2 mm). The results showed that NaHCO 3 ‐extracted Po (NaHCO 3 ‐Po) content in soil aggregates increased with restoration years, while NaOH‐extracted Po (NaOH‐Po) content decreased. ALP activity in soil aggregates increased with restoration years, but there was no significant relationship between ALP activity with the phoD ‐harboring bacterial community. There were significant differences in the composition of rare and abundant phoD ‐harboring bacterial communities during slope restoration. Soil moisture, pH, organic carbon, and the C:P ratio in soil aggregates were the primary factors affecting the distribution of the Po fractions and the phoD ‐harboring bacterial community. NaHCO 3 ‐Po and NaOH‐Po in soil aggregates were likely the main substrates for ALP‐mediated Po mineralization. More genera were involved in Po mineralization in slope soils restored for 14 years than in soils restored for 7 and 11 years, and rare phoD ‐harboring genera were more actively involved in Po mineralization than abundant phoD ‐harboring genera. This study provides some theoretical basis for P effectiveness enhancement and P management during slope soil restoration.

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Publication Details

Journal
Land Degradation and Development
Published
2024-11-11
DOI
https://doi.org/10.1002/ldr.5371
Citations
3
Primary Topic
Microbial Community Ecology and Physiology
Type
article
Field-Weighted Citation Impact
1.38

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article

Rare and Abundant phoD‐Harboring Bacteria Mediate the Mineralization of Organic Phosphorus Fractions in Soil Aggregates During Cut Slope Restoration

Shenghao Ai, Zongyang Liu, Xiaoyan Ai, Meihua Sheng et al.
3 citations
Land Degradation and Development
Microbial Community Ecology and Physiology
1.38
article

Rare and Abundant phoD‐Harboring Bacteria Mediate the Mineralization of Organic Phosphorus Fractions in Soil Aggregates During Cut Slope Restoration

Shenghao Ai, Zongyang Liu, Xiaoyan Ai, Meihua Sheng, Jingyao Xiao, Yingwei Ai, Xue Jiang, Fuyun Pei
article en
3 citations

Abstract

ABSTRACT Phosphorus (P) is the key nutritional element in the soil of cut road slopes undergoing ecological restoration, and the transformation of organic P (Po) is a crucial part of the P cycle. However, the role of phoD ‐harboring bacteria in driving the mineralization of Po fractions in road slope soil aggregates is unclear. This study analyzed road slope soils that had undergone 7, 11, and 14 years of restoration in the western Sichuan Plateau of China. We examined the differences and associations between the Po fraction content, alkaline phosphatase (ALP) activity, and community composition of rare and abundant phoD ‐harboring bacteria in soil aggregates of four particle sizes (0.053–0.25, 0.25–2, 0.053–0.25, and, &gt; 2 mm). The results showed that NaHCO 3 ‐extracted Po (NaHCO 3 ‐Po) content in soil aggregates increased with restoration years, while NaOH‐extracted Po (NaOH‐Po) content decreased. ALP activity in soil aggregates increased with restoration years, but there was no significant relationship between ALP activity with the phoD ‐harboring bacterial community. There were significant differences in the composition of rare and abundant phoD ‐harboring bacterial communities during slope restoration. Soil moisture, pH, organic carbon, and the C:P ratio in soil aggregates were the primary factors affecting the distribution of the Po fractions and the phoD ‐harboring bacterial community. NaHCO 3 ‐Po and NaOH‐Po in soil aggregates were likely the main substrates for ALP‐mediated Po mineralization. More genera were involved in Po mineralization in slope soils restored for 14 years than in soils restored for 7 and 11 years, and rare phoD ‐harboring genera were more actively involved in Po mineralization than abundant phoD ‐harboring genera. This study provides some theoretical basis for P effectiveness enhancement and P management during slope soil restoration.

Land Degradation and DevelopmentVol. 36(2)
Chinese Academy of Sciences (CN), Sichuan University (CN), Mianyang Normal University (CN), Chengdu Organic Chemicals (China) (CN), University of Chinese Academy of Sciences (CN), State Key Laboratory of Hydraulics and Mountain River Engineering
National Natural Science Foundation of China, National Key Research and Development Program of China
Life in Land
Openalex Percentile: Top 17%
Microbial Community Ecology and Physiology
1.38
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