首页 | 本学科首页   官方微博 | 高级检索  
     

灌丛化对干旱区草地土壤有机碳化学结构和热稳定性的影响
引用本文:张宇,刘耘华,滕俐闯,白崇皓,盛建东. 灌丛化对干旱区草地土壤有机碳化学结构和热稳定性的影响[J]. 土壤, 2022, 54(6): 1138-1148
作者姓名:张宇  刘耘华  滕俐闯  白崇皓  盛建东
作者单位:新疆土壤与植物生态过程重点实验室,新疆土壤与植物生态过程重点实验室,新疆土壤与植物生态过程重点实验室,新疆土壤与植物生态过程重点实验室,新疆土壤与植物生态过程重点实验室
基金项目:新疆土壤与植物生态过程重点实验室开放课题(2020D04004)
摘    要:在典型的干旱区新疆,选取沿海拔分布的4类草地,使用固态13C核磁共振技术与热分析技术研究了灌丛化对草地土壤有机碳(SOC)化学结构和热稳定性的影响。结果表明:灌丛间的芳香碳比例沿海拔从温性荒漠到山地草甸逐渐降低。在温性荒漠、温性草原化荒漠、温性荒漠草原和山地草甸,灌丛下烷基碳/烷氧碳的比值相对于灌丛间分别增加了0.10、0.09、0.03、0.21。低海拔的温性荒漠和温性草原化荒漠的热易分解SOC质量(较低温度下分解的SOC)与SOC总质量的比值(%Exo1)、SOC分解一半时的温度(TG-T50)和SOC在能量释放一半时对应的温度(DSC-T50)显著低于高海拔的温性荒漠草原和山地草甸。在草原化荒漠、荒漠草原和山地草甸中,灌丛下的%Exo1和DSC-T50均高于灌丛间,而TG-T50低于灌丛间。在温性荒漠,从灌丛间到灌丛下,低温时SOC燃烧释放出的能量占总燃烧能量(Q)的比例减小,而高温时SOC燃烧释放出的能量增加。本研究结果表明灌...

关 键 词:干旱区  草地  海拔  灌丛化  有机碳的稳定性  固态13C核磁共振技术  热分析技术
收稿时间:2022-02-23
修稿时间:2022-04-21

Effects of Woody Proliferation on Chemical Structure and Thermal Stability of Soil Organic Carbon in Arid Grasslands
ZHANG Yu,LIU Yunhu,TENG Lichuang,BAI Chonghao,SHENG Jiandong. Effects of Woody Proliferation on Chemical Structure and Thermal Stability of Soil Organic Carbon in Arid Grasslands[J]. Soils, 2022, 54(6): 1138-1148
Authors:ZHANG Yu  LIU Yunhu  TENG Lichuang  BAI Chonghao  SHENG Jiandong
Affiliation:Xinjiang Key Laboratory of soil and plant ecological process,College of resources and environment,Xinjiang Agricultural University,Xinjiang Key Laboratory of soil and plant ecological process,College of resources and environment,Xinjiang Agricultural University,Xinjiang Key Laboratory of soil and plant ecological process,College of resources and environment,Xinjiang Agricultural University,Xinjiang Key Laboratory of soil and plant ecological process,College of resources and environment,Xinjiang Agricultural University,Xinjiang Key Laboratory of soil and plant ecological process,College of resources and environment,Xinjiang Agricultural University
Abstract:The stability of soil organic carbon (SOC) refers to its ability to resist microbial degradation, which determines the C cycle and turnover. Shrubbery refers to the significant increase of shrub coverage, density and biomass in grassland, which is particularly common in arid grassland. The study of the impact of shrub on grassland SOC stability is of great significance for the study of global C cycle, climate change and the interaction between them.In this study, four types of grassland distributed along the altitude were selected in the typical arid area of Xinjiang, and the effects of shrub on the stability of grassland SOC were revealed indirectly and completely by using solid-state 13C nuclear magnetic resonance technology and thermal analysis technology. The results showed that the proportion of aromatic carbon among shrubs decreased gradually from temperate desert to mountain meadow along the altitude. In temperate desert, temperate grassland desertification, temperate desert grassland and mountain meadow, the alkyl C/O-alkyl C value increased by 0.07, 0.12, 0.03 and 0.20 respectively. The index of low altitude temperate desert and temperate grassland desertification, the ratio of the mass of SOC easily decomposed by heat (SOC decomposed at lower temperature) to the total mass of SOC (% Exo1), the temperature at half of SOC decomposition (TG-T50) and the corresponding temperature at half of SOC energy release (DSC-T50) are significantly lower than those of high altitude temperate desert grassland and mountain meadow. In grassland desertification, desert grassland and mountain meadow, the% Exo1 and DSC-T50 under shrub were higher than those between shrubs, while TG-T50 was lower than that between shrubs. In temperate desert, from shrub to shrub, the proportion of energy released by SOC combustion in total combustion energy (Q) decreases at low temperature, while the energy released by SOC combustion increases at high temperature.The results showed that shrub increased the stability of SOC chemical structure and thermal stability in arid area.
Keywords:Arid areas   grassland   Altitude   Shrubbery   Organic carbon stability   Solid state 13C NMR technology   Thermal analysis technology
点击此处可从《土壤》浏览原始摘要信息
点击此处可从《土壤》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号