{"title":"Responses of soil carbon, nitrogen, and phosphorus stoichiometry to afforestation of severely desertified land in northern China","authors":"Yuqiang Li , Wenjie Cao , Yun Chen , Libing Han","doi":"10.1016/j.ecolind.2025.113520","DOIUrl":null,"url":null,"abstract":"<div><div>Large-scale afforestation is being implemented globally to promote carbon sequestration in ecosystems, address climate change, and restore degraded ecosystems. However, the impacts of trees and shrubs on soil stoichiometry in severely desertified land remain unclear. We investigated the topsoil (0 − 20 cm) carbon, nitrogen, and phosphorus (C:N:P) stoichiometry of <em>Pinus sylvestris</em> var. <em>mongolica</em> and <em>Caragana microphylla</em> plantations established on mobile sand dunes in northern China. Soil organic carbon (SOC, 2.6 to 11.3 g kg<sup>−1</sup>) and total nitrogen (TN, 0.3 to 1.2 g kg<sup>−1</sup>) concentrations increased by 3.2 to 6.5 times the values in mobile dunes, on average, after 40 years of afforestation. Total phosphorus (TP, 0.1 to 0.2 g kg<sup>−1</sup>) in the 40-year-old <em>P. sylvestris</em> and <em>C</em>. <em>microphylla</em> plantations increased by 15.1 and 24.3 %, respectively. Well-constrained C:N ratios (7.7 to 10.1 on average) indicated strong coupling relationship between SOC and TN. The average C:P (7.2 to 43.8) and average N:P (0.8 to 4.4) ratios increased with increasing afforestation age due to disproportionate changes in the three elements, but the rate of increase under <em>C. microphylla</em> decreased. N:P ratios under <em>P. sylvestris</em> increased with increasing afforestation age, indicating that long-term <em>P. sylvestris</em> afforestation may become P-limited. Environmental factors explained 75 % of the total variation of soil C:N:P stoichiometry. The improved plant diversity, productivity, and soil physical properties after afforestation improved the soil C:N:P stoichiometry. Climate and terrain had negative impacts on this stoichiometry. We suggest combining multiple species for afforestation to improve species diversity and providing supplemental P in later stages of afforestation to counteract the future P limitation. Our findings provide new knowledge on the relationships between afforestation and soil stoichiometry in severely desertified areas, and provide a reference for optimizing afforestation.</div></div>","PeriodicalId":11459,"journal":{"name":"Ecological Indicators","volume":"175 ","pages":"Article 113520"},"PeriodicalIF":7.0000,"publicationDate":"2025-04-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Ecological Indicators","FirstCategoryId":"93","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1470160X25004509","RegionNum":2,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
引用次数: 0
Abstract
Large-scale afforestation is being implemented globally to promote carbon sequestration in ecosystems, address climate change, and restore degraded ecosystems. However, the impacts of trees and shrubs on soil stoichiometry in severely desertified land remain unclear. We investigated the topsoil (0 − 20 cm) carbon, nitrogen, and phosphorus (C:N:P) stoichiometry of Pinus sylvestris var. mongolica and Caragana microphylla plantations established on mobile sand dunes in northern China. Soil organic carbon (SOC, 2.6 to 11.3 g kg−1) and total nitrogen (TN, 0.3 to 1.2 g kg−1) concentrations increased by 3.2 to 6.5 times the values in mobile dunes, on average, after 40 years of afforestation. Total phosphorus (TP, 0.1 to 0.2 g kg−1) in the 40-year-old P. sylvestris and C. microphylla plantations increased by 15.1 and 24.3 %, respectively. Well-constrained C:N ratios (7.7 to 10.1 on average) indicated strong coupling relationship between SOC and TN. The average C:P (7.2 to 43.8) and average N:P (0.8 to 4.4) ratios increased with increasing afforestation age due to disproportionate changes in the three elements, but the rate of increase under C. microphylla decreased. N:P ratios under P. sylvestris increased with increasing afforestation age, indicating that long-term P. sylvestris afforestation may become P-limited. Environmental factors explained 75 % of the total variation of soil C:N:P stoichiometry. The improved plant diversity, productivity, and soil physical properties after afforestation improved the soil C:N:P stoichiometry. Climate and terrain had negative impacts on this stoichiometry. We suggest combining multiple species for afforestation to improve species diversity and providing supplemental P in later stages of afforestation to counteract the future P limitation. Our findings provide new knowledge on the relationships between afforestation and soil stoichiometry in severely desertified areas, and provide a reference for optimizing afforestation.
期刊介绍:
The ultimate aim of Ecological Indicators is to integrate the monitoring and assessment of ecological and environmental indicators with management practices. The journal provides a forum for the discussion of the applied scientific development and review of traditional indicator approaches as well as for theoretical, modelling and quantitative applications such as index development. Research into the following areas will be published.
• All aspects of ecological and environmental indicators and indices.
• New indicators, and new approaches and methods for indicator development, testing and use.
• Development and modelling of indices, e.g. application of indicator suites across multiple scales and resources.
• Analysis and research of resource, system- and scale-specific indicators.
• Methods for integration of social and other valuation metrics for the production of scientifically rigorous and politically-relevant assessments using indicator-based monitoring and assessment programs.
• How research indicators can be transformed into direct application for management purposes.
• Broader assessment objectives and methods, e.g. biodiversity, biological integrity, and sustainability, through the use of indicators.
• Resource-specific indicators such as landscape, agroecosystems, forests, wetlands, etc.