氮磷添加对土壤有机碳的影响: 进展与展望

doi:10.17521/cjpe.2021.0358

植物生态学报 ›› 2022, Vol. 46 ›› Issue (8): 855-870.DOI: 10.17521/cjpe.2021.0358

• 综述 • 下一篇

氮磷添加对土壤有机碳的影响: 进展与展望

冯继广¹, 张秋芳¹, 袁霞², 朱彪¹^,^*()

¹北京大学城市与环境学院, 生态研究中心, 地表过程分析与模拟教育部重点实验室, 北京 100871
²杭州师范大学生命与环境科学学院, 杭州 311121

收稿日期:2021-10-11 接受日期:2022-01-08 出版日期:2022-08-20 发布日期:2022-06-09
通讯作者: *朱彪 ORCID:0000-0001-9858-7943 (biaozhu@pku.edu.cn)
作者简介:冯继广 ORCID:0000-0002-7342-9313
基金资助:
国家自然科学基金(31988102);国家自然科学基金(31800437)

Effects of nitrogen and phosphorus addition on soil organic carbon: review and prospects

FENG Ji-Guang¹, ZHANG Qiu-Fang¹, YUAN Xia², ZHU Biao¹^,^*()

¹College of Urban and Environmental Sciences, Institute of Ecology, Key Laboratory for Earth Surface Processes of the Ministry of Education, Peking University, Beijing 100871, China
²College of Life and Environmental Sciences, Hangzhou Normal University, Hangzhou 311121, China

Received:2021-10-11 Accepted:2022-01-08 Online:2022-08-20 Published:2022-06-09
Contact: *ZHU Biao ORCID:0000-0001-9858-7943 (biaozhu@pku.edu.cn)
Supported by:
National Natural Science Foundation of China(31988102);National Natural Science Foundation of China(31800437)

摘要/Abstract

摘要：

土壤有机碳库是陆地生态系统最大的碳库, 在调控全球碳循环和气候变化中起着重要的作用。人为活动所导致的氮、磷输入和大气氮、磷沉降提高了陆地生态系统的氮、磷可利用性, 进而会通过调控植物生长和微生物活性对土壤有机碳动态产生重要影响。目前, 在全球范围内已经开展了很多氮磷添加调控土壤有机碳动态的野外控制实验, 并取得了一些突破和进展, 但还缺乏较为系统全面的梳理与总结。该文以氮磷添加对土壤碳输入和输出的影响为切入点, 从土壤有机碳的碳库大小、组分和分子组成3个方面系统阐述了氮磷添加对土壤有机碳的影响及其潜在机制。根据以往的研究结果, 氮添加、磷添加和氮磷共同添加对土壤有机碳库的影响总体上表现为促进作用。其中, 氮添加引起的促进作用是微生物对土壤有机碳的分解输出降低和/或植物碳输入增加所致, 而磷添加引起的促进作用可能主要是由于植物碳输入的增加。对于土壤有机碳组分(粒径分组或密度分组)而言, 氮添加虽然同时促进了活性有机碳组分(颗粒态有机碳或轻组分有机碳)和稳定性有机碳组分(矿物结合态有机碳或重组分有机碳), 但降低了稳定性碳组分占土壤总有机碳的比例。此外, 氮添加对土壤有机碳分子组成的影响较为复杂, 受到土壤氮有效性、氮添加量和氮形态等因素的调节。与氮添加相比, 磷添加和氮磷共同添加对土壤有机碳组分和分子组成影响的研究十分有限, 其影响机制尚不清楚。基于已有研究中存在的不足, 该文提出了未来需要加强的4个方面的研究内容: 磷添加对不同类型生态系统尤其是热带森林土壤有机碳的影响, 氮磷添加下植物和微生物在调控土壤有机碳及其组分变化中的作用与相对贡献, 长期氮磷添加及其交互作用对土壤有机碳的影响, 氮磷添加对深层土壤有机碳的影响。

关键词: 土壤有机碳, 矿物结合态有机碳, 颗粒态有机碳, 分子组成, 微生物群落结构, 密度分组, 氮沉降, 磷沉降

Abstract:

Soil organic carbon (SOC) pool is the largest carbon pool in terrestrial ecosystems and plays an important role in regulating the global carbon cycle and climate change. The inputs of nitrogen (N) and phosphorus (P) induced by anthropogenic activities and atmospheric deposition of N and P increase the availabilities of N and P in terrestrial ecosystems, which in turn will have important impacts on SOC dynamics via regulating plant growth and microbial activity. At present, many field-manipulation experiments regarding the effects of N addition and/or P addition on the dynamics of SOC have been conducted worldwide, and some breakthroughs and progress have been made, but a systematic and comprehensive review and summary of them is still lacking. By taking the effects of N addition and/or P addition on the inputs and outputs of soil carbon as the starting point, we systematically reviewed the effects of N addition and/or P addition on SOC and the potential mechanisms from three aspects: the size, fraction and molecular composition of SOC. According to the results of previous studies, N addition, P addition, and combined N and P (N + P) addition generally stimulate the size of SOC pool. The stimulation effect of N is caused by the decreased carbon outputs from microbial decomposition and/or the enhanced carbon inputs of plant above- and/or below-ground under N addition. However, the stimulation effect of P may be dominated by the enhanced carbon inputs of plant above- and/or below-ground under P addition. As for the fractions of SOC separated by particle-size or density fractionation, N addition promotes both labile fractions (particulate organic carbon or light fraction carbon) and stable fractions (mineral-associated organic carbon or heavy fraction carbon) of SOC, but reduces the proportion of stable carbon fractions to total SOC. In addition, the effects of N addition on the molecular composition of SOC are complex and diverse, and are regulated by environmental and experimental factors such as soil N availability, N addition rate, and N fertilizer form. Compared with N addition, studies on the effects of P addition and N + P addition on the fraction and molecular composition of SOC are very limited, and the associated mechanisms for the effects of P addition and N + P addition on these variables are still unclear. To improve our understanding, we propose four aspects of studies that need to be strengthened in the future, including the effects of P addition on SOC in different types of ecosystems (especially tropical forests), the role and relative contribution of plants and microorganisms in regulating the changes of SOC and its fractions under N addition and/or P addition, the effects of long-term N addition and/or P addition and their interactions on SOC, and the effects of N addition and/or P addition on SOC in deep soils (below 20 cm).

Key words: soil organic carbon, mineral-associated organic carbon, particulate organic carbon, molecular composition, microbial community structure, density fractionation, nitrogen deposition, phosphorus deposition

冯继广, 张秋芳, 袁霞, 朱彪. 氮磷添加对土壤有机碳的影响: 进展与展望. 植物生态学报, 2022, 46(8): 855-870. DOI: 10.17521/cjpe.2021.0358

FENG Ji-Guang, ZHANG Qiu-Fang, YUAN Xia, ZHU Biao. Effects of nitrogen and phosphorus addition on soil organic carbon: review and prospects. Chinese Journal of Plant Ecology, 2022, 46(8): 855-870. DOI: 10.17521/cjpe.2021.0358

导出引用管理器 EndNote|Ris|BibTeX

链接本文: https://www.plant-ecology.com/CN/10.17521/cjpe.2021.0358

https://www.plant-ecology.com/CN/Y2022/V46/I8/855

图/表 4

参考文献 131

[1]	Averill C, Waring B (2018). Nitrogen limitation of decomposition and decay: How can it occur? Global Change Biology, 24, 1417-1427. DOI PMID
[2]	Baldock JA, Masiello CA, Gélinas Y, Hedges JI (2004). Cycling and composition of organic matter in terrestrial and marine ecosystems. Marine Chemistry, 92, 39-64. DOI URL
[3]	Baldock JA, Oades JM, Nelson PN, Skene TM, Golchin A, Clarke P (1997). Assessing the extent of decomposition of natural organic materials using solid-state ¹³C NMR spectroscopy. Australian Journal of Soil Research, 35, 1061-1084.
[4]	Baldock JA, Oades JM, Waters AG, Peng X, Vassallo AM, Wilson MA (1992). Aspects of the chemical structure of soil organic materials as revealed by solid-state ¹³C NMR spectroscopy. Biogeochemistry, 16, 1-42. DOI URL
[5]	Camenzind T, Hättenschwiler S, Treseder KK, Lehmann A, Rillig MC (2018). Nutrient limitation of soil microbial processes in tropical forests. Ecological Monographs, 88, 4-21. DOI URL
[6]	Čapek P, Manzoni S, Kaštovská E, Wild B, Diáková K, Bárta J, Schnecker J, Biasi C, Martikainen PJ, Alves RJE, Guggenberger G, Gentsch N, Hugelius G, Palmtag J, Mikutta R, et al. (2018). A plant-microbe interaction framework explaining nutrient effects on primary production. Nature Ecology & Evolution, 2, 1588-1596.
[7]	Chen H, Li D, Feng W, Niu S, Plante AF, Luo Y, Wang K (2018a). Different responses of soil organic carbon fractions to additions of nitrogen. European Journal of Soil Science, 69, 1098-1104. DOI URL
[8]	Chen J, Luo YQ, van Groenigen KJ, Hungate BA, Cao JJ, Zhou XH, Wang RW (2018b). A keystone microbial enzyme for nitrogen control of soil carbon storage. Science Advances, 4, eaaq1689. DOI: 10.1126/sciadv.aaq1689. DOI URL
[9]	Chen JG, Ji CJ, Fang JY, He HB, Zhu B (2020a). Dynamics of microbial residues control the responses of mineral- associated soil organic carbon to N addition in two temperate forests. Science of the Total Environment, 748, 141318. DOI: 10.1016/j.scitotenv.2020.141318. DOI URL
[10]	Chen JG, Xiao W, Zheng CY, Zhu B (2020b). Nitrogen addition has contrasting effects on particulate and mineral- associated soil organic carbon in a subtropical forest. Soil Biology & Biochemistry, 142, 107708. DOI: 10.1016/j.soilbio.2020.107708. DOI URL
[11]	Chen ST, Zou JW, Hu ZH, Chen HS, Lu YY (2014). Global annual soil respiration in relation to climate, soil properties and vegetation characteristics: summary of available data. Agricultural and Forest Meteorology, 198-199, 335-346.
[12]	Chen Y, Liu X, Hou YH, Zhou SR, Zhu B (2021). Particulate organic carbon is more vulnerable to nitrogen addition than mineral-associated organic carbon in soil of an alpine meadow. Plant and Soil, 458, 93-103. DOI URL
[13]	Cheng SL, He S, Fang HJ, Xia JZ, Tian J, Yu GR, Geng J, Yu GX (2017). Contrasting effects of NH₄⁺ and NO₃^- amendments on amount and chemical characteristics of different density organic matter fractions in a boreal forest soil. Geoderma, 293, 1-9. DOI URL
[14]	Cleveland CC, Townsend AR, Schmidt SK (2002). Phosphorus limitation of microbial processes in moist tropical forests: evidence from short-term laboratory incubations and field studies. Ecosystems, 5, 680-691. DOI URL
[15]	Cotrufo MF, Ranalli MG, Haddix ML, Six J, Lugato E (2019). Soil carbon storage informed by particulate and mineral- associated organic matter. Nature Geoscience, 12, 989-994. DOI URL
[16]	Cotrufo MF, Soong JL, Horton AJ, Campbell EE, Haddix ML, Wall DH, Parton WJ (2015). Formation of soil organic matter via biochemical and physical pathways of litter mass loss. Nature Geoscience, 8, 776-779. DOI
[17]	Cotrufo MF, Wallenstein MD, Boot CM, Denef K, Paul E (2013). The Microbial Efficiency-Matrix Stabilization (MEMS) framework integrates plant litter decomposition with soil organic matter stabilization: Do labile plant inputs form stable soil organic matter? Global Change Biology, 19, 988-995. DOI PMID
[18]	Crow SE, Lajtha K, Filley TR, Swanston CW, Bowden RD, Caldwell BA (2009). Sources of plant-derived carbon and stability of organic matter in soil: implications for global change. Global Change Biology, 15, 2003-2019. DOI URL
[19]	Crowther TW, Riggs C, Lind EM, Borer ET, Seabloom EW, Hobbie SE, Wubs J, Adler PB, Firn J, Gherardi L, Hagenah N, Hofmockel KS, Knops JMH, McCulley RL, MacDougall AS, et al. (2019). Sensitivity of global soil carbon stocks to combined nutrient enrichment. Ecology Letters, 22, 936-945. DOI PMID
[20]	Cusack DF, Silver WL, Torn MS, Burton SD, Firestone MK (2011a). Changes in microbial community characteristics and soil organic matter with nitrogen additions in two tropical forests. Ecology, 92, 621-632. DOI URL
[21]	Cusack DF, Silver WL, Torn MS, McDowell WH (2011b). Effects of nitrogen additions on above- and belowground carbon dynamics in two tropical forests. Biogeochemistry, 104, 203-225. DOI URL
[22]	Demyan MS, Rasche F, Schulz E, Breulmann M, Müeller T, Cadisch G (2012). Use of specific peaks obtained by diffuse reflectance Fourier transform mid-infrared spectroscopy to study the composition of organic matter in a Haplic Chernozem. European Journal of Soil Science, 63, 189-199. DOI URL
[23]	Du EZ, Terrer C, Pellegrini AFA, Ahlström A, van Lissa CJ, Zhao X, Xia N, Wu XH, Jackson RB (2020). Global patterns of terrestrial nitrogen and phosphorus limitation. Nature Geoscience, 13, 221-226. DOI URL
[24]	Elser JJ, Bracken MES, Cleland EE, Gruner DS, Harpole WS, Hillebrand H, Ngai JT, Seabloom EW, Shurin JB, Smith JE (2007). Global analysis of nitrogen and phosphorus limitation of primary producers in freshwater marine and terrestrial ecosystems. Ecology Letters, 10, 1135-1142. DOI URL
[25]	Fan ZZ, Wang X, Wang C, Bai E (2018). Effect of nitrogen and phosphorus addition on soil enzyme activities: a meta-analysis. Chinese Journal of Applied Ecology, 29, 1266-1272. DOI
	[范珍珍, 王鑫, 王超, 白娥 (2018). 整合分析氮磷添加对土壤酶活性的影响. 应用生态学报, 29, 1266-1272.] DOI
[26]	Feng J, Zhu B (2021). Global patterns and associated drivers of priming effect in response to nutrient addition. Soil Biology & Biochemistry, 153, 108118. DOI: 10.1016/j.soilbio.2020.108118. DOI URL
[27]	Feng JG, He KY, Zhang QF, Han MG, Zhu B (2022). Changes in plant inputs alter soil carbon and microbial communities in forest ecosystems. Global Change Biology, 28, 3426-3440. DOI URL
[28]	Feng JG, Zhu B (2019). A global meta-analysis of soil respiration and its components in response to phosphorus addition. Soil Biology & Biochemistry, 135, 38-47. DOI URL
[29]	Feng JG, Zhu B (2020). A review on the effects of nitrogen and phosphorus addition on tree growth and productivity in forest ecosystems. Chinese Journal of Plant Ecology, 44, 583-597. DOI URL
	[冯继广, 朱彪 (2020). 氮磷添加对树木生长和森林生产力影响的研究进展. 植物生态学报, 44, 583-597.] DOI
[30]	Fog K (1988). The effect of added nitrogen on the rate of decomposition of organic matter. Biological Reviews, 63, 433-462. DOI URL
[31]	Frey SD, Knorr M, Parrent JL, Simpson RT (2004). Chronic nitrogen enrichment affects the structure and function of the soil microbial community in temperate hardwood and pine forests. Forest Ecology and Management, 196, 159-171. DOI URL
[32]	Galloway JN, Dentener FJ, Capone DG, Boyer EW, Howarth RW, Seitzinger SP, Asner GP, Cleveland CC, Green PA, Holland EA, Karl DM, Michaels AF, Porter JH, Townsend AR, Vörosmarty CJ (2004). Nitrogen cycles: past present and future. Biogeochemistry, 70, 153-226. DOI URL
[33]	Guo H, Ye CL, Zhang H, Pan S, Ji YG, Li Z, Liu MQ, Zhou XH, Du GZ, Hu F, Hu SJ (2017). Long-term nitrogen & phosphorus additions reduce soil microbial respiration but increase its temperature sensitivity in a Tibetan alpine meadow. Soil Biology & Biochemistry, 113, 26-34. DOI URL
[34]	Harpole WS, Ngai JT, Cleland EE, Seabloom EW, Borer ET, Bracken MES, Elser JJ, Gruner DS, Hillebrand H, Shurin JB, Smith JE (2011). Nutrient co-limitation of primary producer communities. Ecology Letters, 14, 852-862. DOI PMID
[35]	Hou EQ, Luo YQ, Kuang YW, Chen CR, Lu XK, Jiang LF, Luo XZ, Wen DZ (2020). Global meta-analysis shows pervasive phosphorus limitation of aboveground plant production in natural terrestrial ecosystems. Nature Communications, 11, 637. DOI: 10.1038/s41467-020-14492-w. DOI PMID
[36]	Hou EQ, Wen DZ, Jiang LF, Luo XZ, Kuang YW, Lu XK, Chen CR, Allen KT, He XJ, Huang XZ, Luo YQ (2021). Latitudinal patterns of terrestrial phosphorus limitation over the globe. Ecology Letters, 24, 1420-1431. DOI URL
[37]	Hou Y, Chen Y, Chen X, He K, Zhu B (2019). Changes in soil organic matter stability with depth in two alpine ecosystems on the Tibetan Plateau. Geoderma, 351, 153-162. DOI URL
[38]	Huang JS, Liu LL, Qi KB, Yang TH, Yang B, Bao WK, Pang XY (2019). Differential mechanisms drive changes in soil C pools under N and P enrichment in a subalpine spruce plantation. Geoderma, 340, 213-223. DOI URL
[39]	Hui D, Porter W, Phillips JR, Aidar MPM, Lebreux SJ, Schadt CW, Mayes MA (2020). Phosphorus rather than nitrogen enhances CO₂ emissions in tropical forest soils: evidence from a laboratory incubation study. European Journal of Soil Science, 71, 495-510. DOI URL
[40]	Hursh A, Ballantyne A, Cooper L, Maneta M, Kimball J, Watts J (2017). The sensitivity of soil respiration to soil temperature, moisture, and carbon supply at the global scale. Global Change Biology, 23, 2090-2103. DOI PMID
[41]	Jackson RB, Lajtha K, Crow SE, Hugelius G, Kramer MG, Piñeiro G (2017). The ecology of soil carbon: pools, vulnerabilities, and biotic and abiotic controls. Annual Review of Ecology, Evolution, and Systematics, 48, 419-445. DOI URL
[42]	Janssens IA, Dieleman W, Luyssaert S, Subke JA, Reichstein M, Ceulemans R, Ciais P, Dolman AJ, Grace J, Matteucci G, Papale D, Piao SL, Schulze ED, Tang J, Law BE (2010). Reduction of forest soil respiration in response to nitrogen deposition. Nature Geoscience, 3, 315-322. DOI URL
[43]	Jiang J, Wang YP, Liu F, Du Y, Zhuang W, Chang Z, Yu M, Yan J (2021). Antagonistic and additive interactions dominate the responses of belowground carbon-cycling processes to nitrogen and phosphorus additions. Soil Biology & Biochemistry, 156, 108216. DOI: 10.1016/j.soilbio.2021.108216. DOI URL
[44]	Jiang J, Wang YP, Yang Y, Yu M, Wang C, Yan J (2019). Interactive effects of nitrogen and phosphorus additions on plant growth vary with ecosystem type. Plant and Soil, 440, 523-537. DOI
[45]	John B, Yamashita T, Ludwig B, Flessa H (2005). Storage of organic carbon in aggregate and density fractions of silty soils under different types of land use. Geoderma, 128, 63-79. DOI URL
[46]	Johnston ER, Kim M, Hatt JK, Phillips JR, Yao Q, Song Y, Hazen TC, Mayes MA, Konstantinidis KT (2019). Phosphate addition increases tropical forest soil respiration primarily by deconstraining microbial population growth. Soil Biology & Biochemistry, 130, 43-54. DOI URL
[47]	Kamble PN, Rousk J, Frey SD, Bååth E (2013). Bacterial growth and growth-limiting nutrients following chronic nitrogen additions to a hardwood forest soil. Soil Biology & Biochemistry, 59, 32-37. DOI URL
[48]	Keeler BL, Hobbie SE, Kellogg LE (2009). Effects of long- term nitrogen addition on microbial enzyme activity in eight forested and grassland sites: implications for litter and soil organic matter decomposition. Ecosystems, 12, 1-15. DOI URL
[49]	Keller AB, Borer ET, Collins SL, DeLancey LC, Fay PA, Hofmockel KS, Leakey ADB, Mayes MA, Seabloom EW, Walter CA, Wang Y, Zhao Q, Hobbie SE (2022). Soil carbon stocks in temperate grasslands differ strongly across sites but are insensitive to decade-long fertilization. Global Change Biology, 28, 1659-1677. DOI URL
[50]	Kögel-Knabner I (2002). The macromolecular organic composition of plant and microbial residues as inputs to soil organic matter. Soil Biology & Biochemistry, 34, 139-162. DOI URL
[51]	Lajtha K, Bowden RD, Crow S, Fekete I, Kotroczó Z, Plante A, Simpson MJ, Nadelhoffer KJ (2018). The detrital input and removal treatment (DIRT) network: insights into soil carbon stabilization. Science of the Total Environment, 640-641, 1112-1120.
[52]	Lal R (2004). Soil carbon sequestration impacts on global climate change and food security. Science, 304, 1623-1627. DOI PMID
[53]	Lavallee JM, Soong JL, Cotrufo MF (2020). Conceptualizing soil organic matter into particulate and mineral-associated forms to address global change in the 21st century. Global Change Biology, 26, 261-273. DOI PMID
[54]	Lehmann J, Kleber M (2015). The contentious nature of soil organic matter. Nature, 528, 60-68. DOI URL
[55]	Li DD, Zhao BZ, Zhang JB, Liu KL, Huang QH (2021). Different traits from the paddy soil and upland soil regulate bacterial community and molecular composition under long-term fertilization regimes. Applied Soil Ecology, 165, 103982. DOI: 10.1016/j.apsoil.2021.103982. DOI URL
[56]	Li N, Sheng M, You MY, Han XZ (2019). Advancement in research on application of ¹³C NMR techniques to exploration of chemical structure of soil organic matter. Acta Pedologica Sinica, 56, 796-812.
	[李娜, 盛明, 尤孟阳, 韩晓增 (2019). 应用¹³C核磁共振技术研究土壤有机质化学结构进展. 土壤学报, 56, 796-812.]
[57]	Li R, Chang RY (2015). Effects of external nitrogen additions on soil organic carbon dynamics and the mechanism. Chinese Journal of Plant Ecology, 39, 1012-1020. DOI
	[李嵘, 常瑞英 (2015). 土壤有机碳对外源氮添加的响应及其机制. 植物生态学报, 39, 1012-1020.] DOI
[58]	Li Y, Nie C, Liu YH, Du W, He P (2019). Soil microbial community composition closely associates with specific enzyme activities and soil carbon chemistry in a long-term nitrogen fertilized grassland. Science of the Total Environment, 654, 264-274. DOI URL
[59]	Li Y, Niu SL, Yu GR (2016). Aggravated phosphorus limitation on biomass production under increasing nitrogen loading: a meta-analysis. Global Change Biology, 22, 934-943. DOI PMID
[60]	Liang C, Schimel JP, Jastrow JD (2017). The importance of anabolism in microbial control over soil carbon storage. Nature Microbiology, 2, 17105. DOI: 10.1038/nmicrobiol.2017.105. DOI PMID
[61]	Liu L, Zhang T, Gilliam FS, Gundersen P, Zhang W, Chen H, Mo JM (2013). Interactive effects of nitrogen and phosphorus on soil microbial communities in a tropical forest. PLOS ONE, 8, e61188. DOI: 10.1371/journal.pone.0061188. DOI URL
[62]	Liu LL, Greaver TL (2010). A global perspective on belowground carbon dynamics under nitrogen enrichment. Ecology Letters, 13, 819-828. DOI PMID
[63]	Liu WX, Qiao CL, Yang S, Bai WM, Liu LL (2018). Microbial carbon use efficiency and priming effect regulate soil carbon storage under nitrogen deposition by slowing soil organic matter decomposition. Geoderma, 332, 37-44. DOI URL
[64]	Lu M, Zhou XH, Luo YQ, Yang YH, Fang CM, Chen JK, Li B (2011). Minor stimulation of soil carbon storage by nitrogen addition: a meta-analysis. Agriculture Ecosystems & Environment, 140, 234-244. DOI URL
[65]	Lu X, Gilliam FS, Guo J, Hou E, Kuang Y (2022). Decrease in soil pH has greater effects than increase in above-ground carbon inputs on soil organic carbon in terrestrial ecosystems of China under nitrogen enrichment. Journal of Applied Ecology, 59, 768-778. DOI URL
[66]	Lu X, Hou E, Guo J, Gilliam FS, Li J, Tang S, Kuang Y (2021a). Nitrogen addition stimulates soil aggregation and enhances carbon storage in terrestrial ecosystems of China: a meta-analysis. Global Change Biology, 27, 2780-2792. DOI URL
[67]	Lu X, Vitousek PM, Mao Q, Gilliam FS, Luo Y, Turner BL, Zhou G, Mo J (2021b). Nitrogen deposition accelerates soil carbon sequestration in tropical forests. Proceedings of the National Academy of Sciences of the United States of America, 118, e2020790118. DOI: 10.1073/pnas.2020790118. DOI
[68]	Luo R, Fan J, Wang W, Luo J, Kuzyakov Y, He JS, Chu H, Ding W (2019). Nitrogen and phosphorus enrichment accelerates soil organic carbon loss in alpine grassland on the Qinghai-Tibetan Plateau. Science of the Total Environment, 650, 303-312. DOI URL
[69]	Luo R, Kuzyakov Y, Liu D, Fan J, Luo J, Lindsey S, He JS, Ding W (2020). Nutrient addition reduces carbon sequestration in a Tibetan grassland soil: disentangling microbial and physical controls. Soil Biology & Biochemistry, 144, 107764. DOI: 10.1016/j.soilbio.2020.107764. DOI URL
[70]	Ma SH, Chen GP, Du EZ, Tian D, Xing AJ, Shen HH, Ji CJ, Zheng CY, Zhu JX, Zhu JL, Huang HY, He HB, Zhu B, Fang JY (2021). Effects of nitrogen addition on microbial residues and their contribution to soil organic carbon in Chinaʼs forests from tropical to boreal zone. Environmental Pollution, 268, 115941. DOI: 10.1016/j.envpol.2020.115941. DOI URL
[71]	Man M, Deen B, Dunfield KE, Wagner-Riddle C, Simpson MJ (2021). Altered soil organic matter composition and degradation after a decade of nitrogen fertilization in a temperate agroecosystem. Agriculture, Ecosystems & Environment, 310, 107305. DOI: 10.1016/j.agee.2021.107305. DOI URL
[72]	Manzoni S, Taylor P, Richter A, Porporato A, Ågren GI (2012). Environmental and stoichiometric controls on microbial carbon-use efficiency in soils. New Phytologist, 196, 79-91. DOI PMID
[73]	Marín-Spiotta E, Swanston CW, Torn MS, Silver WL, Burton SD (2008). Chemical and mineral control of soil carbon turnover in abandoned tropical pastures. Geoderma, 143, 49-62. DOI URL
[74]	Moran KK, Six J, Horwath WR, van Kessel C (2005). Role of mineral-nitrogen in residue decomposition and stable soil organic matter formation. Soil Science Society of America Journal, 69, 1730-1736. DOI URL
[75]	Mori T, Ishizuka S, Konda R, Wicaksono A, Heriyanto J, Hardjono A, Ohta S (2015). Phosphorus addition reduced microbial respiration during the decomposition of Acacia mangium litter in South Sumatra, Indonesia. Tropics, 24, 113-118. DOI URL
[76]	Mori T, Lu XK, Aoyagi R, Mo J (2018). Reconsidering the phosphorus limitation of soil microbial activity in tropical forests. Functional Ecology, 32, 1145-1154. DOI URL
[77]	Neff JC, Townsend AR, Gleixner G, Lehman SJ, Turnbull J, Bowman WD (2002). Variable effects of nitrogen additions on the stability and turnover of soil carbon. Nature, 419, 915-917. DOI URL
[78]	Ning Q, Hättenschwiler S, Lü X, Kardol P, Zhang Y, Wei C, Xu C, Huang J, Li A, Yang J, Wang J, Peng Y, Peñuelas J, Sardans J, He J, et al. (2021). Carbon limitation overrides acidification in mediating soil microbial activity to nitrogen enrichment in a temperate grassland. Global Change Biology, 27, 5976-5988. DOI PMID
[79]	Norby RJ, de Kauwe MG, Domingues TF, Duursma RA, Ellsworth DS, Goll DS, Lapola DM, Luus KA, MacKenzie AR, Medlyn BE, Pavlick R, Rammig A, Smith B, Thomas R, Thonicke K, et al. (2016). Model-data synthesis for the next generation of forest free-air CO₂ enrichment (FACE) experiments. New Phytologist, 209, 17-28. DOI URL
[80]	Pan Y, Birdsey RA, Fang J, Houghton R, Kauppi PE, Kurz WA, Phillips OL, Shvidenko A, Lewis SL, Canadell JG, Ciais P, Jackson RB, Pacala SW, McGuire AD, Piao S, et al. (2011). A large and persistent carbon sink in the worldʼs forests. Science, 333, 988-993. DOI URL
[81]	Peng YF, Guo DL, Yang YH (2017). Global patterns of root dynamics under nitrogen enrichment. Global Ecology and Biogeography, 26, 102-114. DOI URL
[82]	Peñuelas J, Poulter B, Sardans J, Ciais P, van der Velde M, Bopp L, Boucher O, Godderis Y, Hinsinger P, Llusia J, Nardin E, Vicca S, Obersteiner M, Janssens IA (2013). Human-induced nitrogen-phosphorus imbalances alter natural and managed ecosystems across the globe. Nature Communications, 4, 2934. DOI: 10.1038/ncomms3934. DOI PMID
[83]	Peñuelas J, Sardans J, Rivas-Ubach A, Janssens IA (2012). The human-induced imbalance between C, N and P in earthʼs life system. Global Change Biology, 18, 3-6. DOI URL
[84]	Ramirez KS, Craine JM, Fierer N (2012). Consistent effects of nitrogen amendments on soil microbial communities and processes across biomes. Global Change Biology, 18, 1918-1927. DOI URL
[85]	Rasse DP, Rumpel C, Dignac MF (2005). Is soil carbon mostly root carbon? Mechanisms for a specific stabilisation. Plant and Soil, 269, 341-356. DOI URL
[86]	Riggs CE, Hobbie SE (2016). Mechanisms driving the soil organic matter decomposition response to nitrogen enrichment in grassland soils. Soil Biology & Biochemistry, 99, 54-65. DOI URL
[87]	Rocci KS, Lavallee JM, Stewart CE, Cotrufo MF (2021). Soil organic carbon response to global environmental change depends on its distribution between mineral-associated and particulate organic matter: a meta-analysis. Science of the Total Environment, 793, 148569. DOI: 10.1016/j.scitotenv.2021.148569. DOI URL
[88]	Schulte-Uebbing L, de Vries W (2018). Global-scale impacts of nitrogen deposition on tree carbon sequestration in tropical, temperate, and boreal forests: a meta-analysis. Global Change Biology, 24, e416-e431.
[89]	Six J, Conant RT, Paul EA, Paustian K (2002). Stabilization mechanisms of soil organic matter: implications for C- saturation of soils. Plant and Soil, 241, 155-176. DOI URL
[90]	Six J, Elliott ET, Paustian K (2000). Soil macroaggregate turnover and microaggregate formation: a mechanism for C sequestration under no-tillage agriculture. Soil Biology & Biochemistry, 32, 2099-2103. DOI URL
[91]	Sokol NW, Bradford MA (2019). Microbial formation of stable soil carbon is more efficient from belowground than aboveground input. Nature Geoscience, 12, 46-53. DOI
[92]	Sokol NW, Kuebbing SE, Karlsen-Ayala E, Bradford MA (2019). Evidence for the primacy of living root inputs, not root or shoot litter, in forming soil organic carbon. New Phytologist, 221, 233-246. DOI PMID
[93]	Song CC, Liu DY, Song YY, Mao R (2013). Effect of nitrogen addition on soil organic carbon in freshwater marsh of Northeast China. Environmental Earth Sciences, 70, 1653-1659. DOI URL
[94]	Spohn M, Diáková K, Aburto F, Doetterl S, Borovec J (2022). Sorption and desorption of organic matter in soils as affected by phosphate. Geoderma, 405, 115377. DOI: 10.1016/j.geoderma.2021.115377. DOI URL
[95]	Spohn M, Pötsch EM, Eichorst SA, Woebken D, Wanek W, Richter A (2016). Soil microbial carbon use efficiency and biomass turnover in a long-term fertilization experiment in a temperate grassland. Soil Biology & Biochemistry, 97, 168-175. DOI URL
[96]	Spohn M, Schleuss PM (2019). Addition of inorganic phosphorus to soil leads to desorption of organic compounds and thus to increased soil respiration. Soil Biology & Biochemistry, 130, 220-226. DOI URL
[97]	Sundqvist MK, Liu Z, Giesler R, Wardle DA (2014). Plant and microbial responses to nitrogen and phosphorus addition across an elevational gradient in subarctic tundra. Ecology, 95, 1819-1835. PMID
[98]	Tian DS, Niu SL (2015). A global analysis of soil acidification caused by nitrogen addition. Environmental Research Letters, 10, 024019. DOI: 10.1088/1748-9326/10/2/024019. DOI URL
[99]	Townsend AR, Cleveland CC, Houlton BZ, Alden CB, White JWC (2011). Multi-element regulation of the tropical forest carbon cycle. Frontiers in Ecology and the Environment, 9, 9-17. DOI URL
[100]	Treseder KK (2008). Nitrogen additions and microbial biomass: a meta-analysis of ecosystem studies. Ecology Letters, 11, 1111-1120. DOI PMID
[101]	Trumbore SE (1993). Comparison of carbon dynamics in tropical and temperate soils using radiocarbon measurements. Global Biogeochemical Cycles, 7, 275-290. DOI URL
[102]	van den Enden L, Anthony MA, Frey SD, Simpson MJ (2021). Biogeochemical evolution of soil organic matter composition after a decade of warming and nitrogen addition. Biogeochemistry, 156, 161-175. DOI URL
[103]	Villarino SH, Pinto P, Jackson RB, Piñeiro G (2021). Plant rhizodeposition: a key factor for soil organic matter formation in stable fractions. Science Advances, 7, eabd3176. DOI: 10.1126/sciadv.abd3176. DOI URL
[104]	Vitousek PM (1984). Litterfall, nutrient cycling, and nutrient limitation in tropical forests. Ecology, 65, 285-298. DOI URL
[105]	Vitousek PM, Porder S, Houlton BZ, Chadwick OA (2010). Terrestrial phosphorus limitation: mechanisms, implications, and nitrogen-phosphorus interactions. Ecological Applications, 20, 5-15. DOI URL
[106]	von Lützow M, Kögel-Knabner I, Ekschmitt K, Flessa H, Guggenberger G, Matzner E, Marschner B (2007). SOM fractionation methods: relevance to functional pools and to stabilization mechanisms. Soil Biology & Biochemistry, 39, 2183-2207. DOI URL
[107]	Wagai R, Kishimoto-Mo AW, Yonemura S, Shirato Y, Hiradate S, Yagasaki Y (2013). Linking temperature sensitivity of soil organic matter decomposition to its molecular structure, accessibility, and microbial physiology. Global Change Biology, 19, 1114-1125. DOI PMID
[108]	Waldrop MP, Zak DR, Sinsabaugh RL, Gallo M, Lauber C (2004). Nitrogen deposition modifies soil carbon storage through changes in microbial enzymatic activity. Ecological Applications, 14, 1172-1177. DOI URL
[109]	Wang B, An S, Liang C, Liu Y, Kuzyakov Y (2021). Microbial necromass as the source of soil organic carbon in global ecosystems. Soil Biology & Biochemistry, 162, 108422. DOI: 10.1016/j.soilbio.2021.108422. DOI URL
[110]	Wang JJ, Bowden RD, Lajtha K, Washko SE, Wurzbacher SJ, Simpson MJ (2019). Long-term nitrogen addition suppresses microbial degradation, enhances soil carbon storage, and alters the molecular composition of soil organic matter. Biogeochemistry, 142, 299-313. DOI URL
[111]	Wang QK, Zhang WD, Sun T, Chen LC, Pang XY, Wang YP, Xiao FM (2017). N and P fertilization reduced soil autotrophic and heterotrophic respiration in a young Cunninghamia lanceolata forest. Agricultural and Forest Meteorology, 232, 66-73. DOI URL
[112]	Wright SJ (2019). Plant responses to nutrient addition experiments conducted in tropical forests. Ecological Monographs, 89, e01382. DOI: 10.1002/ecm.1382. DOI
[113]	Wright SJ, Turner BL, Yavitt JB, Harms KE, Kaspari M, Tanner EVJ, Bujan J, Griffin EA, Mayor JR, Pasquini SC, Sheldrake M, Garcia MN (2018). Plant responses to fertilization experiments in lowland, species-rich, tropical forests. Ecology, 99, 1129-1138. DOI PMID
[114]	Xiao W, Chen X, Jing X, Zhu B (2018). A meta-analysis of soil extracellular enzyme activities in response to global change. Soil Biology & Biochemistry, 123, 21-32. DOI URL
[115]	Xing A, Du E, Shen H, Xu L, de Vries W, Zhao M, Liu X, Fang J (2022a). Nonlinear responses of ecosystem carbon fluxes to nitrogen deposition in an old-growth boreal forest. Ecology Letters, 25, 77-88. DOI URL
[116]	Xing W, Lu XM, Ying JY, Lan ZC, Chen DM, Bai YF (2022b). Disentangling the effects of nitrogen availability and soil acidification on microbial taxa and soil carbon dynamics in natural grasslands. Soil Biology & Biochemistry, 164, 108495. DOI: 10.1016/j.soilbio.2021.108495. DOI URL
[117]	Xu C, Xu X, Ju C, Chen HYH, Wilsey BJ, Luo Y, Fan W (2021a). Long-term, amplified responses of soil organic carbon to nitrogen addition worldwide. Global Change Biology, 27, 1170-1180. DOI URL
[118]	Xu S, Sayer EJ, Eisenhauer N, Lu X, Wang J, Liu C (2021b). Aboveground litter inputs determine carbon storage across soil profiles: a meta-analysis. Plant and Soil, 462, 429-444. DOI URL
[119]	Yang LM, Lyu MK, Li XJ, Xiong XL, Lin WS, Yang YS, Xie JS (2020). Decline in the contribution of microbial residues to soil organic carbon along a subtropical elevation gradient. Science of the Total Environment, 749, 141583. DOI: 10.1016/j.scitotenv.2020.141583. DOI URL
[120]	Ye C, Chen D, Hall SJ, Pan S, Yan X, Bai T, Guo H, Zhang Y, Bai Y, Hu S (2018). Reconciling multiple impacts of nitrogen enrichment on soil carbon: plant microbial and geochemical controls. Ecology Letters, 21, 1162-1173. DOI URL
[121]	Ye CL, Zhang H, Zhou XL, Zhou XH, Guo H, Hu SJ (2018). Effects of nitrogen additions on soil microbial respiration and its temperature sensitivity in a Tibetan alpine meadow. Acta Ecologica Sinica, 38, 2279-2287.
	[叶成龙, 张浩, 周小龙, 周显辉, 郭辉, 胡水金 (2018). 氮添加对高寒草甸土壤微生物呼吸及其温度敏感性的影响. 生态学报, 38, 2279-2287.]
[122]	Yu M, Wang YP, Baldock JA, Jiang J, Mo J, Zhou G, Yan J (2020). Divergent responses of soil organic carbon accumulation to 14 years of nitrogen addition in two typical subtropical forests. Science of the Total Environment, 707, 136104. DOI: 10.1016/j.scitotenv.2019.136104. DOI URL
[123]	Yuan X, Qin WK, Xu H, Zhang ZH, Zhou HK, Zhu B (2020). Sensitivity of soil carbon dynamics to nitrogen and phosphorus enrichment in an alpine meadow. Soil Biology & Biochemistry, 150, 107984. DOI: 10.1016/j.soilbio.2020.107984. DOI URL
[124]	Yue K, Fornara DA, Yang W, Peng Y, Peng C, Liu Z, Wu F (2017). Influence of multiple global change drivers on terrestrial carbon storage: additive effects are common. Ecology Letters, 20, 663-672. DOI PMID
[125]	Zhang C, Niu D, Hall SJ, Wen H, Li X, Fu H, Wan C, Elser JJ (2014). Effects of simulated nitrogen deposition on soil respiration components and their temperature sensitivities in a semiarid grassland. Soil Biology & Biochemistry, 75, 113-123. DOI URL
[126]	Zhang G, Cao ZP, Hu CJ (2011). Soil organic carbon fractionation methods and their applications in farmland ecosystem research: a review. Chinese Journal of Applied Ecology, 22, 1921-1930. PMID
	[张国, 曹志平, 胡婵娟 (2011). 土壤有机碳分组方法及其在农田生态系统研究中的应用. 应用生态学报, 22, 1921-1930.] PMID
[127]	Zhang TA, Chen HYH, Ruan HH (2018). Global negative effects of nitrogen deposition on soil microbes. The ISME Journal, 12, 1817-1825. DOI URL
[128]	Zhang ZS, Li M, Song XL, Xue ZS, Lü XG, Jiang M, Wu HT, Wang XH (2018). Effects of climate change on molecular structure and stability of soil carbon pool: a general review. Acta Pedologica Sinica, 55, 273-282.
	[张仲胜, 李敏, 宋晓林, 薛振山, 吕宪国, 姜明, 武海涛, 王雪宏 (2018). 气候变化对土壤有机碳库分子结构特征与稳定性影响研究进展. 土壤学报, 55, 273-282.]
[129]	Zhong Y, Yan WM, Shangguan ZP (2016). The effects of nitrogen enrichment on soil CO₂ fluxes depending on temperature and soil properties. Global Ecology and Biogeography, 25, 475-488. DOI URL
[130]	Zhou LY, Zhou XH, Zhang BC, Lu M, Luo YQ, Liu LL, Li B (2014). Different responses of soil respiration and its components to nitrogen addition among biomes: a meta- analysis. Global Change Biology, 20, 2332-2343. DOI URL
[131]	Zhu JX, Wang QF, He NP, Smith MD, Elser JJ, Du JQ, Yuan GF, Yu GR, Yu Q (2016). Imbalanced atmospheric nitrogen and phosphorus depositions in China: implications for nutrient limitation. Journal of Geophysical Research, 121, 1605-1616.

粒径分组 Size fractionation	密度分组 Density fractionation	特性 Characteristic	文献 Reference
大团聚体有机碳 Macroaggregate OC (>250 μm)	游离态的轻组分有机碳 Free light-fraction OC	来源于新输入的植物残体, 最容易被微生物分解, 周转速率最快 Originated from newly-inputted plant residues, most easily to be decomposed by microbes, and with the fastest turnover rate	Six et al., 2002; Marín-Spiotta et al., 2008
微团聚体有机碳 Microaggregate OC (53-250 μm)	包裹态的轻组分有机碳 Occluded light-fraction OC	来源于半分解的植物残体, 但在团聚体内部受到了物理保护, 较易分解, 周转速率较快 Originated from partly-decomposed plant residues, but physically protected within aggregates, easier to be decomposed, and with a faster turnover rate	Trumbore, 1993; von Lützow et al., 2007
黏粉粒/矿物结合态有机碳 Silt-clay/mineral-associated OC (<53 μm)	重组分有机碳 Heavy-fraction OC	与土壤矿物紧密结合, 较难被分解, 周转速率较慢 Closely bound to soil minerals, difficult to be decomposed, and with a slow turnover rate	John et al., 2005; Lavallee et al., 2020

粒径分组 Size fractionation	密度分组 Density fractionation	特性 Characteristic	文献 Reference
大团聚体有机碳 Macroaggregate OC (>250 μm)	游离态的轻组分有机碳 Free light-fraction OC	来源于新输入的植物残体, 最容易被微生物分解, 周转速率最快 Originated from newly-inputted plant residues, most easily to be decomposed by microbes, and with the fastest turnover rate	Six et al., 2002; Marín-Spiotta et al., 2008
微团聚体有机碳 Microaggregate OC (53-250 μm)	包裹态的轻组分有机碳 Occluded light-fraction OC	来源于半分解的植物残体, 但在团聚体内部受到了物理保护, 较易分解, 周转速率较快 Originated from partly-decomposed plant residues, but physically protected within aggregates, easier to be decomposed, and with a faster turnover rate	Trumbore, 1993; von Lützow et al., 2007
黏粉粒/矿物结合态有机碳 Silt-clay/mineral-associated OC (<53 μm)	重组分有机碳 Heavy-fraction OC	与土壤矿物紧密结合, 较难被分解, 周转速率较慢 Closely bound to soil minerals, difficult to be decomposed, and with a slow turnover rate	John et al., 2005; Lavallee et al., 2020

碳功能团 Functional group	化学位移 Chemical shift (δ)	碳的主要形式 Dominant forms of carbon	特性 Characteristic
烷基碳 Alkyl C	0-45	主要为脂肪族化合物等, 来自于植物角质、蜡质、木栓质 Mainly aliphatic compounds, originating from plant cutin, waxes, suberin	较稳定, 不易被分解, 为难分解碳 Relatively stable, not easy to be decomposed, and categorized as the recalcitrant C
烷氧碳 O-alkyl C	45-110	主要为碳水化合物, 如纤维素、半纤维素等 Mainly carbohydrates, such as cellulose, hemicellulose, etc.	容易被分解, 为易分解碳 Easy to be decomposed, and categorized as the easily- decomposed C
芳香碳 Aromatic C	110-165	主要为单宁、木质素等 Mainly tannin, lignin, etc.	难以被分解, 为难分解碳 Difficult to be decomposed, and categorized as the recalcitrant C
羰基碳 Carbonyl C	165-210	大多为脂肪酸、氨基酸、酰胺、酯、酮醛类物质 Mostly fatty acids, amino acids, amide, esters, ketones and aldehydes	容易被分解, 为易分解碳 Easy to be decomposed, and categorized as the easily- decomposed C

碳功能团 Functional group	化学位移 Chemical shift (δ)	碳的主要形式 Dominant forms of carbon	特性 Characteristic
烷基碳 Alkyl C	0-45	主要为脂肪族化合物等, 来自于植物角质、蜡质、木栓质 Mainly aliphatic compounds, originating from plant cutin, waxes, suberin	较稳定, 不易被分解, 为难分解碳 Relatively stable, not easy to be decomposed, and categorized as the recalcitrant C
烷氧碳 O-alkyl C	45-110	主要为碳水化合物, 如纤维素、半纤维素等 Mainly carbohydrates, such as cellulose, hemicellulose, etc.	容易被分解, 为易分解碳 Easy to be decomposed, and categorized as the easily- decomposed C
芳香碳 Aromatic C	110-165	主要为单宁、木质素等 Mainly tannin, lignin, etc.	难以被分解, 为难分解碳 Difficult to be decomposed, and categorized as the recalcitrant C
羰基碳 Carbonyl C	165-210	大多为脂肪酸、氨基酸、酰胺、酯、酮醛类物质 Mostly fatty acids, amino acids, amide, esters, ketones and aldehydes	容易被分解, 为易分解碳 Easy to be decomposed, and categorized as the easily- decomposed C

氮磷添加对土壤有机碳的影响: 进展与展望

Effects of nitrogen and phosphorus addition on soil organic carbon: review and prospects

全文

PDF (PC)

可视化

被引次数

摘要/Abstract

引用本文

使用本文

图/表 4

参考文献 131

相关文章 15

编辑推荐

Metrics

本文评价

[1]	张英, 张常洪, 汪其同, 朱晓敏, 尹华军. 氮沉降下西南山地针叶林根际和非根际土壤固碳贡献差异[J]. 植物生态学报, 2023, 47(9): 1234-1244.
[2]	陈颖洁, 房凯, 秦书琪, 郭彦军, 杨元合. 内蒙古温带草地土壤有机碳组分含量和分解速率的空间格局及其影响因素[J]. 植物生态学报, 2023, 47(9): 1245-1255.
[3]	仲琦, 李曾燕, 马炜, 况雨潇, 邱岭军, 黎蕴洁, 涂利华. 氮添加和凋落物处理对华西雨屏区常绿阔叶林凋落叶分解的影响[J]. 植物生态学报, 2023, 47(5): 629-643.
[4]	甘子莹, 王浩, 丁驰, 雷梅, 杨晓刚, 蔡敬琰, 丘清燕, 胡亚林. 亚热带森林不同植物及器官来源的可溶性有机质输入对土壤激发效应的影响及其作用机理[J]. 植物生态学报, 2022, 46(7): 797-810.
[5]	张英, 张常洪, 汪其同, 朱晓敏, 尹华军. 氮沉降下西南山地针叶林根际和非根际土壤微生物养分限制特征差异[J]. 植物生态学报, 2022, 46(4): 473-483.
[6]	田磊, 朱毅, 李欣, 韩国栋, 任海燕. 不同降水条件下内蒙古荒漠草原主要植物物候对长期增温和氮添加的响应[J]. 植物生态学报, 2022, 46(3): 290-299.
[7]	谢欢, 张秋芳, 曾泉鑫, 周嘉聪, 马亚培, 吴玥, 刘苑苑, 林惠瑛, 尹云锋, 陈岳民. 氮添加对杉木苗期磷转化和分解类真菌的影响[J]. 植物生态学报, 2022, 46(2): 220-231.
[8]	聂秀青, 王冬, 周国英, 熊丰, 杜岩功. 三江源地区高寒湿地土壤微生物生物量碳氮磷及其化学计量特征[J]. 植物生态学报, 2021, 45(9): 996-1005.
[9]	孙建, 王毅, 刘国华. 青藏高原高寒草地地上植物碳积累速率对生态系统多功能性的影响机制[J]. 植物生态学报, 2021, 45(5): 496-506.
[10]	董利军, 李金花, 陈珊, 张瑞, 孙建, 马妙君. 若尔盖湿地高寒草甸退化过程中土壤有机碳含量变化及成因分析[J]. 植物生态学报, 2021, 45(5): 507-515.
[11]	王奕丹, 李亮, 刘琪璟, 马泽清. 亚热带6个典型树种吸收细根寿命与形态属性格局[J]. 植物生态学报, 2021, 45(4): 383-393.
[12]	朱湾湾, 王攀, 许艺馨, 李春环, 余海龙, 黄菊莹. 降水量变化与氮添加下荒漠草原土壤酶活性及其影响因素[J]. 植物生态学报, 2021, 45(3): 309-320.
[13]	张宏锦, 王娓. 生态系统多功能性对全球变化的响应: 进展、问题与展望[J]. 植物生态学报, 2021, 45(10): 1112-1126.
[14]	裴广廷, 孙建飞, 贺同鑫, 胡宝清. 长期人为干扰对桂西北喀斯特草地土壤微生物多样性及群落结构的影响[J]. 植物生态学报, 2021, 45(1): 74-84.
[15]	胡宗达, 刘世荣, 罗明霞, 胡璟, 刘兴良, 李亚非, 余昊, 欧定华. 川西亚高山不同演替阶段天然次生林土壤碳氮含量及酶活性特征[J]. 植物生态学报, 2020, 44(9): 973-985.