{"title":"长期加磷增加了稻麦轮作中植物木质素和微生物坏死团对土壤有机碳的贡献","authors":"Zhaoming Chen, Jinchuan Ma, Feng Wang, Junwei Ma, Ping Zou, Wanchun Sun, Qiaogang Yu, Qiang Wang","doi":"10.1016/j.apsoil.2025.106010","DOIUrl":null,"url":null,"abstract":"<div><div>Plant-derived compound (PDC) and microbial necromass carbon (MNC) are the two most important drivers in soil organic carbon (SOC) formation and accrual. Continuous phosphorus (P) addition affects SOC accumulation in paddy soils. However, the underlying mechanisms by which P addition affect the contributions of PDC and MNC to the accrual of SOC remain unclear. Here, a 12-year P addition experiment with four rates (0, 75, 150, and 300 kg P<sub>2</sub>O<sub>5</sub> ha<sup>−2</sup> crop season<sup>−1</sup>) was conducted in paddy soils with rice–wheat rotation. Our findings showed that particulate organic carbon (POC) increased by P addition (<em>P</em> < 0.05), but mineral-associated organic carbon (MAOC) was not affected (<em>P ></em> 0.05). P addition enhanced the content and SOC-normalized content of lignin phenols by 40.1–71.8 % and 34.2–49.5 %, respectively, which were coincided with a decrease in lignin degradation. P addition enhanced the MNC content because of higher microbial biomass and lower nitrogen (N) acquisition enzyme activity. Moreover, P addition promoted the MNC contribution to the accrual of SOC, primarily from the increased contribution of fungal necromass carbon (FNC). The decrease in amino sugars to lignin phenols ratio and increase in POC to MAOC ratio implied that P addition might reduce SOC stability and enhance SOC loss potential. Long-term P addition increased bacterial richness but decreased fungal richness compared to that of the control. Moreover, bacterial and fungal richness: biomass ratios significantly reduced by P addition. Random forest and structural equation modelling analysis revealed that fungal richness played a significant role in controlling the contributions of PDC and MNC to SOC in paddy soils. Furthermore, microbial richness: biomass ratio was another non-negligible factor regulating PDC and MNC accumulation. Overall, our findings suggest that long-term P addition increases plant- and microbial-derived compounds but the increase in PDC is greater than in MNC, indicating that plant-derived SOC plays a more key role in SOC sequestration in paddy soils under continuous P addition.</div></div>","PeriodicalId":8099,"journal":{"name":"Applied Soil Ecology","volume":"209 ","pages":"Article 106010"},"PeriodicalIF":4.8000,"publicationDate":"2025-03-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Long-term phosphorus addition enhances the contributions of plant lignin and microbial necromass to soil organic carbon in a rice–wheat rotation\",\"authors\":\"Zhaoming Chen, Jinchuan Ma, Feng Wang, Junwei Ma, Ping Zou, Wanchun Sun, Qiaogang Yu, Qiang Wang\",\"doi\":\"10.1016/j.apsoil.2025.106010\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Plant-derived compound (PDC) and microbial necromass carbon (MNC) are the two most important drivers in soil organic carbon (SOC) formation and accrual. Continuous phosphorus (P) addition affects SOC accumulation in paddy soils. However, the underlying mechanisms by which P addition affect the contributions of PDC and MNC to the accrual of SOC remain unclear. Here, a 12-year P addition experiment with four rates (0, 75, 150, and 300 kg P<sub>2</sub>O<sub>5</sub> ha<sup>−2</sup> crop season<sup>−1</sup>) was conducted in paddy soils with rice–wheat rotation. Our findings showed that particulate organic carbon (POC) increased by P addition (<em>P</em> < 0.05), but mineral-associated organic carbon (MAOC) was not affected (<em>P ></em> 0.05). P addition enhanced the content and SOC-normalized content of lignin phenols by 40.1–71.8 % and 34.2–49.5 %, respectively, which were coincided with a decrease in lignin degradation. P addition enhanced the MNC content because of higher microbial biomass and lower nitrogen (N) acquisition enzyme activity. Moreover, P addition promoted the MNC contribution to the accrual of SOC, primarily from the increased contribution of fungal necromass carbon (FNC). The decrease in amino sugars to lignin phenols ratio and increase in POC to MAOC ratio implied that P addition might reduce SOC stability and enhance SOC loss potential. Long-term P addition increased bacterial richness but decreased fungal richness compared to that of the control. Moreover, bacterial and fungal richness: biomass ratios significantly reduced by P addition. Random forest and structural equation modelling analysis revealed that fungal richness played a significant role in controlling the contributions of PDC and MNC to SOC in paddy soils. Furthermore, microbial richness: biomass ratio was another non-negligible factor regulating PDC and MNC accumulation. Overall, our findings suggest that long-term P addition increases plant- and microbial-derived compounds but the increase in PDC is greater than in MNC, indicating that plant-derived SOC plays a more key role in SOC sequestration in paddy soils under continuous P addition.</div></div>\",\"PeriodicalId\":8099,\"journal\":{\"name\":\"Applied Soil Ecology\",\"volume\":\"209 \",\"pages\":\"Article 106010\"},\"PeriodicalIF\":4.8000,\"publicationDate\":\"2025-03-10\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Applied Soil Ecology\",\"FirstCategoryId\":\"97\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0929139325001489\",\"RegionNum\":2,\"RegionCategory\":\"农林科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"SOIL SCIENCE\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Applied Soil Ecology","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0929139325001489","RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"SOIL SCIENCE","Score":null,"Total":0}
引用次数: 0
摘要
植物源化合物(PDC)和微生物坏死块碳(MNC)是土壤有机碳(SOC)形成和积累的两个最重要的驱动因素。连续添加磷对水稻土有机碳积累有影响。然而,P添加影响PDC和MNC对土壤有机碳积累贡献的潜在机制尚不清楚。本研究在水稻-小麦轮作的水稻土上进行了为期12年的4种施磷量(0、75、150和300 kg P2O5 ha - 2作物季- 1)施磷试验。结果表明,磷的添加增加了土壤颗粒有机碳(POC)的含量(P <;0.05),但矿物相关有机碳(MAOC)不受影响(P >;0.05)。P的添加使木质素酚含量和soc标准化含量分别提高了40.1 ~ 71.8%和34.2 ~ 49.5%,与此同时木质素降解降低。添加磷提高了微生物量,降低了氮素获取酶活性,提高了MNC含量。此外,磷的添加促进了真菌坏死团碳(FNC)对土壤有机碳积累的贡献,主要来自真菌坏死团碳(FNC)贡献的增加。氨基糖与木质素酚的比值降低,POC与MAOC的比值升高,表明P的加入可能降低有机碳稳定性,增加有机碳损失潜力。与对照相比,长期添加磷增加了细菌丰富度,但降低了真菌丰富度。此外,添加磷显著降低了细菌和真菌丰富度:生物量比。随机森林和结构方程模型分析表明,真菌丰富度对水稻土中PDC和MNC对有机碳的贡献具有重要控制作用。微生物丰富度:生物量比是调节PDC和MNC积累的另一个不可忽视的因素。综上所述,长期加磷增加了水稻土中植物源性有机碳和微生物源性有机碳的含量,但PDC含量的增加幅度大于不加磷,表明在连续加磷条件下,水稻土中植物源性有机碳在固碳中起着更为关键的作用。
Long-term phosphorus addition enhances the contributions of plant lignin and microbial necromass to soil organic carbon in a rice–wheat rotation
Plant-derived compound (PDC) and microbial necromass carbon (MNC) are the two most important drivers in soil organic carbon (SOC) formation and accrual. Continuous phosphorus (P) addition affects SOC accumulation in paddy soils. However, the underlying mechanisms by which P addition affect the contributions of PDC and MNC to the accrual of SOC remain unclear. Here, a 12-year P addition experiment with four rates (0, 75, 150, and 300 kg P2O5 ha−2 crop season−1) was conducted in paddy soils with rice–wheat rotation. Our findings showed that particulate organic carbon (POC) increased by P addition (P < 0.05), but mineral-associated organic carbon (MAOC) was not affected (P > 0.05). P addition enhanced the content and SOC-normalized content of lignin phenols by 40.1–71.8 % and 34.2–49.5 %, respectively, which were coincided with a decrease in lignin degradation. P addition enhanced the MNC content because of higher microbial biomass and lower nitrogen (N) acquisition enzyme activity. Moreover, P addition promoted the MNC contribution to the accrual of SOC, primarily from the increased contribution of fungal necromass carbon (FNC). The decrease in amino sugars to lignin phenols ratio and increase in POC to MAOC ratio implied that P addition might reduce SOC stability and enhance SOC loss potential. Long-term P addition increased bacterial richness but decreased fungal richness compared to that of the control. Moreover, bacterial and fungal richness: biomass ratios significantly reduced by P addition. Random forest and structural equation modelling analysis revealed that fungal richness played a significant role in controlling the contributions of PDC and MNC to SOC in paddy soils. Furthermore, microbial richness: biomass ratio was another non-negligible factor regulating PDC and MNC accumulation. Overall, our findings suggest that long-term P addition increases plant- and microbial-derived compounds but the increase in PDC is greater than in MNC, indicating that plant-derived SOC plays a more key role in SOC sequestration in paddy soils under continuous P addition.
期刊介绍:
Applied Soil Ecology addresses the role of soil organisms and their interactions in relation to: sustainability and productivity, nutrient cycling and other soil processes, the maintenance of soil functions, the impact of human activities on soil ecosystems and bio(techno)logical control of soil-inhabiting pests, diseases and weeds.