Over recent decades, the Chinese government has instigated large-scale vegetation restoration projects across the Loess Plateau to control soil erosion. Yet, this project coupling effect with associative interannual variations and magnitudinous decreases during vegetation species’ developmental stages have rarely been explored. Therefore, we conducted experiments to explore the water budget characteristics under different stand ages of Robinia pseudoacacia.
Methods
We selected five R. pseudoacacia stand ages (i.e., 6 yr, 16 yr, 20 yr, 35 yr, and 45 yr) to investigate their individual interannual water budgets over four consecutive years (2019–2022).
Results
Compared with grassland, the significant soil water amounts were consumed within the deep soil layers (> 200 cm) of all R. pseudoacacia stand ages. The soil water storage (SWS) deficit gradually worsened between 6–20 yr but then improved between 35–45 yr. Also, SWS values of all five R. pseudoacacia stands significantly differed (p < 0.05). Interestingly, as the stands aged, the increasing rate of actual evapotranspiration (AET) largely decreased from 125 mm yr−1 to 29 mm yr−1. The relationship between cumulative precipitation and AET further revealed that the water equilibrium input–output state reached at the stand’s middle age (~ 20 yr), after which the positive water input feedback occurred.
Conclusions
These findings highlight that the water consumption process turning point for R. pseudoacacia occurs at the stand’s middle stage, indicating its role in SWS recovery. Our experimental evidence will benefit both researchers and policymakers, helping them to better regulate water resources and to optimize forest management alternatives.
{"title":"Water consumption turning point for Robinia pseudoacacia occurs at its middle stand age","authors":"Yali Zhao, Yunqiang Wang, Ruijie Li, Lijun Qi, Hui Sun, Pingping Zhang, Zimin Li","doi":"10.1007/s11104-025-07231-x","DOIUrl":"https://doi.org/10.1007/s11104-025-07231-x","url":null,"abstract":"<h3 data-test=\"abstract-sub-heading\">Aims</h3><p>Over recent decades, the Chinese government has instigated large-scale vegetation restoration projects across the Loess Plateau to control soil erosion. Yet, this project coupling effect with associative interannual variations and magnitudinous decreases during vegetation species’ developmental stages have rarely been explored. Therefore, we conducted experiments to explore the water budget characteristics under different stand ages of <i>Robinia pseudoacacia.</i></p><h3 data-test=\"abstract-sub-heading\">Methods</h3><p>We selected five <i>R. pseudoacacia</i> stand ages (i.e., 6 yr, 16 yr, 20 yr, 35 yr, and 45 yr) to investigate their individual interannual water budgets over four consecutive years (2019–2022).</p><h3 data-test=\"abstract-sub-heading\">Results</h3><p>Compared with grassland, the significant soil water amounts were consumed within the deep soil layers (> 200 cm) of all <i>R. pseudoacacia</i> stand ages. The soil water storage (SWS) deficit gradually worsened between 6–20 yr but then improved between 35–45 yr. Also, SWS values of all five <i>R. pseudoacacia</i> stands significantly differed (<i>p</i> < 0.05). Interestingly, as the stands aged, the increasing rate of actual evapotranspiration (AET) largely decreased from 125 mm yr<sup>−1</sup> to 29 mm yr<sup>−1</sup>. The relationship between cumulative precipitation and AET further revealed that the water equilibrium input–output state reached at the stand’s middle age (~ 20 yr), after which the positive water input feedback occurred.</p><h3 data-test=\"abstract-sub-heading\">Conclusions</h3><p>These findings highlight that the water consumption process turning point for <i>R. pseudoacacia</i> occurs at the stand’s middle stage, indicating its role in SWS recovery. Our experimental evidence will benefit both researchers and policymakers, helping them to better regulate water resources and to optimize forest management alternatives.</p>","PeriodicalId":20223,"journal":{"name":"Plant and Soil","volume":"20 1","pages":""},"PeriodicalIF":4.9,"publicationDate":"2025-01-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143031341","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Plant roots can induced changes in soil nitrogen (N) transformation, which is critical for plant N utilization in N-limited ecosystems. However, the linkage between plant N preference and the rhizosphere effects on soil N transformation is rarely explored.
Methods
We determined the relationship between plant N preference (15N labeling) and the rhizosphere effects on soil net ammonification/nitrification rates of three dominant shrub species (Artemisia ordosica, Salix psammophila, and Caragana korshinskii) in the Mu Us Desert, as well as root traits, rhizosphere and bulk soil microbiomes, functional genes and enzyme activities.
Results
S. psammophila and C. korshinskii with preference for NO3− had higher rhizosphere nitrification rates, while A. ordosica with preference for NH4+ had higher rhizosphere ammonification rates. The plant N preference was also positively linked to the rhizosphere effects on soil N transformation, indicating that rhizosphere process provided positive feedback to plant N demands. Furthermore, root exudation rates and morphological traits explained the interspecific variations in rhizosphere effects on net ammonification and nitrification rates, respectively. The rhizosphere nifH gene copies and nitrogenase activity contributed to the increasing rhizosphere effect on ammonification rates, while rhizosphere ammonia-oxidizing archaea gene abundance was responsible for the rhizosphere effect on soil net nitrification rates.
Conclusion
We conclude that the linkage between plant N preference and rhizosphere effects on N transformation is driven by specific rhizosphere physical, physiological and microbial environments. This positive plant-soil feedback may promote species establishment in N-limited soils, which is insightful for understanding plant adaption from a rhizosphere perspective.
{"title":"Linkage between plant nitrogen preference and rhizosphere effects on soil nitrogen transformation reveals a plant resource adaptive strategies in nitrogen-limited soils","authors":"Xinyue Yuan, Weiwei She, Yanpei Guo, Yangui Qiao, Liang Liu, Chunyang Song, Shugao Qin, Yuqing Zhang","doi":"10.1007/s11104-025-07220-0","DOIUrl":"https://doi.org/10.1007/s11104-025-07220-0","url":null,"abstract":"<h3 data-test=\"abstract-sub-heading\">Background and aims</h3><p>Plant roots can induced changes in soil nitrogen (N) transformation, which is critical for plant N utilization in N-limited ecosystems. However, the linkage between plant N preference and the rhizosphere effects on soil N transformation is rarely explored.</p><h3 data-test=\"abstract-sub-heading\">Methods</h3><p>We determined the relationship between plant N preference (<sup>15</sup>N labeling) and the rhizosphere effects on soil net ammonification/nitrification rates of three dominant shrub species (<i>Artemisia ordosica</i>, <i>Salix psammophila</i>, and <i>Caragana korshinskii</i>) in the Mu Us Desert, as well as root traits, rhizosphere and bulk soil microbiomes, functional genes and enzyme activities.</p><h3 data-test=\"abstract-sub-heading\">Results</h3><p><i>S. psammophila</i> and <i>C. korshinskii</i> with preference for NO<sub>3</sub><sup>−</sup> had higher rhizosphere nitrification rates, while <i>A. ordosica</i> with preference for NH<sub>4</sub><sup>+</sup> had higher rhizosphere ammonification rates. The plant N preference was also positively linked to the rhizosphere effects on soil N transformation, indicating that rhizosphere process provided positive feedback to plant N demands. Furthermore, root exudation rates and morphological traits explained the interspecific variations in rhizosphere effects on net ammonification and nitrification rates, respectively. The rhizosphere <i>nifH</i> gene copies and nitrogenase activity contributed to the increasing rhizosphere effect on ammonification rates, while rhizosphere ammonia-oxidizing archaea gene abundance was responsible for the rhizosphere effect on soil net nitrification rates.</p><h3 data-test=\"abstract-sub-heading\">Conclusion</h3><p>We conclude that the linkage between plant N preference and rhizosphere effects on N transformation is driven by specific rhizosphere physical, physiological and microbial environments. This positive plant-soil feedback may promote species establishment in N-limited soils, which is insightful for understanding plant adaption from a rhizosphere perspective.</p>","PeriodicalId":20223,"journal":{"name":"Plant and Soil","volume":"25 1","pages":""},"PeriodicalIF":4.9,"publicationDate":"2025-01-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143031097","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Different legumes are distributed across low phosphorus (P) steppe of Inner Mongolia from west to east, this study aimed to investigate the adaptation strategies of different legumes to soil P availability in steppe regions.
Methods
Three legumes (Caragana microphylla, Melissitus ruthenica and Medicago falcata) were grown in pots with soil P additions ranging from 0 to 300 mg P kg−1 soil. Nitrogen (N) and P uptake, growth, rhizosphere processes, and N fixation were determined at harvest.
Results
C. microphylla and M. falcata exhibited increased biomass in response to P addition, with M. falcata demonstrating a more pronounced effect. M. ruthenica responded positively to P addition at 25 mg P kg−1 soil, but P levels above 50 mg P kg−1 soil significantly suppressed its growth and resulted in lower P utilization efficiency compared to M. falcata and C. microphylla. C. microphylla had higher acid phosphatase activity (APase) than the other species, and highest P absorption rate at P addition below 150 mg P kg−1 soil. Low P enhanced succinate exudation in M. ruthenica but not in the other species. P addition promoted P uptake of M. falcata by increasing root length, area and rhizosphere acidification. Low-P deficiency reduced nodulation and N fixation of three legumes in treatments without P addition.
Conclusions
C. microphylla’s higher P absorption rate and APase activity are main adaptive traits for tolerating and adapting to low-P desert steppe soils. Due to M. ruthenica tolerating low-P with high P utilization efficiency traits, it exhibits a fast relative growth rate. M. falcata thrives in high available P soils with accelerated growth. These findings highlight each species’ distinct strategies for nutrient acquisition and adaptation to varying soil P levels, providing scientific insights for sustainable grassland management.
{"title":"Adaptation strategies of three legumes to soil phosphorus availability in steppes of Inner Mongolia","authors":"Qian Liu, Weifan Wan, Weiwei Chen, Caihong Zhang, Hui Gao, Junling Zhang, Zhi Sun, Haigang Li","doi":"10.1007/s11104-025-07232-w","DOIUrl":"https://doi.org/10.1007/s11104-025-07232-w","url":null,"abstract":"<h3 data-test=\"abstract-sub-heading\">Aims</h3><p>Different legumes are distributed across low phosphorus (P) steppe of Inner Mongolia from west to east, this study aimed to investigate the adaptation strategies of different legumes to soil P availability in steppe regions.</p><h3 data-test=\"abstract-sub-heading\">Methods</h3><p>Three legumes (<i>Caragana microphylla</i>, <i>Melissitus ruthenica</i> and <i>Medicago falcata</i>) were grown in pots with soil P additions ranging from 0 to 300 mg P kg<sup>−1</sup> soil. Nitrogen (N) and P uptake, growth, rhizosphere processes, and N fixation were determined at harvest.</p><h3 data-test=\"abstract-sub-heading\">Results</h3><p><i>C</i>. <i>microphylla</i> and <i>M. falcata</i> exhibited increased biomass in response to P addition, with <i>M. falcata</i> demonstrating a more pronounced effect. <i>M. ruthenica</i> responded positively to P addition at 25 mg P kg<sup>−1</sup> soil, but P levels above 50 mg P kg<sup>−1</sup> soil significantly suppressed its growth and resulted in lower P utilization efficiency compared to <i>M. falcata</i> and <i>C</i>. <i>microphylla</i>. <i>C</i>. <i>microphylla</i> had higher acid phosphatase activity (APase) than the other species, and highest P absorption rate at P addition below 150 mg P kg<sup>−1</sup> soil. Low P enhanced succinate exudation in <i>M</i>. <i>ruthenica</i> but not in the other species. P addition promoted P uptake of <i>M. falcata</i> by increasing root length, area and rhizosphere acidification. Low-P deficiency reduced nodulation and N fixation of three legumes in treatments without P addition.</p><h3 data-test=\"abstract-sub-heading\">Conclusions</h3><p><i>C</i>. <i>microphylla</i>’s higher P absorption rate and APase activity are main adaptive traits for tolerating and adapting to low-P desert steppe soils. Due to<i> M</i>. <i>ruthenica</i> tolerating low-P with high P utilization efficiency traits, it exhibits a fast relative growth rate. <i>M. falcata</i> thrives in high available P soils with accelerated growth. These findings highlight each species’ distinct strategies for nutrient acquisition and adaptation to varying soil P levels, providing scientific insights for sustainable grassland management.</p>","PeriodicalId":20223,"journal":{"name":"Plant and Soil","volume":"38 1","pages":""},"PeriodicalIF":4.9,"publicationDate":"2025-01-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143031096","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Grassland ecosystems consist of different grassland types and provide multiple ecosystem services and functions simultaneously. However, the relative importance of plant community characteristics and soil properties in promoting the ecosystem multifunctionality (EMF) among different grassland types is unclear.
Methods
A field study was conducted to investigate the effects of multidimensional plant diversity, plant coverage, and soil properties on EMF in alpine steppe (AS), alpine meadow (AM), and alpine swamp meadow (ASM).
Results
Environmental filtration resulted in a gradual decrease in plant species diversity and Faith’ s phylogenetic diversity (PD) from AS to ASM. Plant species in AM with high functional diversity and mean phylogenetic pairwise distance (MPD). There was no significant difference in EMF among grassland types. Importantly, phylogenetic diversity and plant coverage had a direct positive effect on EMF in AS and AM, respectively. Additionally, soil moisture also played a crucial role in maintaining EMF in AS. Functional richness index (FRic) was positively correlated with EMF, while soil moisture was the key to maintaining EMF in ASM, followed by soil bulk density.
Conclusion
Our research highlighted the importance of plant community characteristics in maintaining the EMF of AS and AM. Additionally, EMF in ASM was mainly regulated by soil properties. We suggest that management measures should be established based on the specific characteristics of each grassland type, which is essential for maintaining ecosystem multifunctionality.
{"title":"Driving factors of plant and soil properties on ecosystem multifunctionality vary among grassland types in the Qinghai-Tibetan Plateau","authors":"Zeying Yao, Meng-ai Hu, Lina Shi, Qiong Wu, Degang Zhang, Guihe Liu, Xinqing Shao, Dongxia Liu","doi":"10.1007/s11104-025-07229-5","DOIUrl":"https://doi.org/10.1007/s11104-025-07229-5","url":null,"abstract":"<h3 data-test=\"abstract-sub-heading\">Backgrounds</h3><p>Grassland ecosystems consist of different grassland types and provide multiple ecosystem services and functions simultaneously. However, the relative importance of plant community characteristics and soil properties in promoting the ecosystem multifunctionality (EMF) among different grassland types is unclear.</p><h3 data-test=\"abstract-sub-heading\">Methods</h3><p>A field study was conducted to investigate the effects of multidimensional plant diversity, plant coverage, and soil properties on EMF in alpine steppe (AS), alpine meadow (AM), and alpine swamp meadow (ASM).</p><h3 data-test=\"abstract-sub-heading\">Results</h3><p>Environmental filtration resulted in a gradual decrease in plant species diversity and Faith’ s phylogenetic diversity (PD) from AS to ASM. Plant species in AM with high functional diversity and mean phylogenetic pairwise distance (MPD). There was no significant difference in EMF among grassland types. Importantly, phylogenetic diversity and plant coverage had a direct positive effect on EMF in AS and AM, respectively. Additionally, soil moisture also played a crucial role in maintaining EMF in AS. Functional richness index (FRic) was positively correlated with EMF, while soil moisture was the key to maintaining EMF in ASM, followed by soil bulk density.</p><h3 data-test=\"abstract-sub-heading\">Conclusion</h3><p>Our research highlighted the importance of plant community characteristics in maintaining the EMF of AS and AM. Additionally, EMF in ASM was mainly regulated by soil properties. We suggest that management measures should be established based on the specific characteristics of each grassland type, which is essential for maintaining ecosystem multifunctionality.</p>","PeriodicalId":20223,"journal":{"name":"Plant and Soil","volume":"35 1","pages":""},"PeriodicalIF":4.9,"publicationDate":"2025-01-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143031095","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-01-24DOI: 10.1007/s11104-025-07212-0
Yingjie Li, Meng Wang, Qian Li, Lei Zhang, Bo Sun, Yubo Qin, Yuhan Yuan, Cuilan Li, Jinjing Zhang, Hang Liu
Background and aims
Mulching drip fertigation can effectively increases crop yields. However, with the insufficient recycling rate of mulch films and the continuous accumulation of film residues in the soil, mulch film residues and antibiotic resistance genes (ARGs) coexist in farmland. The impact of biodegradable mulch films on the reduction of soil ARGs remains uncertain.
Methods
This study employed high-throughput sequencing and high-throughput quantitative PCR (HT-qPCR) to examine the effects of three drip fertigation systems (drip fertigation without film (DI), drip fertigation with biodegradable film (DF), and drip fertigation with plastic film (PF) on bacteria and ARGs in farmland soils.
Results
The results indicated that compared with DI, mulched drip irrigation significantly reduced bacterial abundance and diversity (DI > DF > PF) but increased the abundance of ARGs and mobile genetic elements (MGEs) (PF > DF > DI). The ARG network structure in PF was more complex compared to DI and DF, whereas in DF, the ARG network structure was more stable compared to DI and PF. The abundance of MGEs directly influenced the abundance of ARGs, and the MGEs abundance was directly affected by the bacterial Shannon index, which also indirectly affected ARG abundance. Special attention was given to the impact of drip irrigation with different mulch films on ARG dissemination, emphasizing that biodegradable mulch films effectively reduce ecological risks compared to traditional plastic films.
Conclusions
In summary, although DF showed higher bacterial diversity than PF, it also reduced both the diversity and abundance of ARGs, thereby further decreasing soil ARG levels. This study provides new perspectives and scientific evidence for understanding the environmental dissemination mechanisms of ARGs and offers actionable recommendations for sustainable agricultural management, such as reducing mulch residue pollution and optimizing drip fertigation practices.