Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1007/s11104-023-06414-8 |
Evolving characteristics of dissolved organic matter in soil profiles during 56 years of revegetation in Mu Us Sandy Land | |
Wang, Yixiang; Hu, Hanzhe; Zhou, Yajie; Zhang, Buran; Li, Shuo; Liu, Jun; Tong, Xiaogang | |
通讯作者 | Tong, XG |
来源期刊 | PLANT AND SOIL
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ISSN | 0032-079X |
EISSN | 1573-5036 |
出版年 | 2024 |
卷号 | 497期号:1-2页码:567-584 |
英文摘要 | Background and aimsDissolved organic matter (DOM) is a vital bioactive component in soil nutrient cycling. However, the dynamics of its characteristics and composition along the soil profile during desertification reversal are poorly understood.MethodsSoil samples were gathered from shrub and arbor forests that have been established for 25, 35, 46, and 56 years on semifixed sand of Mu Us Sandy Land. The evolution of DOM composition and chemical properties were explored by ultraviolet-visible and fluorescence spectrophotometry.ResultsAfter 56 revegetation years, DOM increased significantly. In arbor lands, DOM was impacted mainly by dissolved organic carbon, with mean concentrations increasing from 58.89 mg center dot kg-1 to 131.95 mg center dot kg-1 in 0-100 cm soil profile. In the shrubland, changes in dissolved organic nitrogen were more remarkable, with mean concentrations increasing from 3.43 mg center dot kg-1 to 6.82 mg center dot kg-1 in 0-100 cm soil profile. Concurrently, as soil depth increased, noticeably decreased in the proportion of humic-like components within DOM, while protein-like components displayed an upward trend. The chemical properties of DOM in arbor lands display a higher proportion of hydrophobic substances along with an elevated aromaticity and humification degree. Conversely, in shrubland, the DOM composition exhibits a higher proportion of tryptophan components that are more available for microbial metabolism. Correlation analysis showed that DOM content and specific environmental factors (including soil depth, vegetation type, and afforestation age) profoundly affected soil DOM properties.ConclusionsThe DOM in arbor land and surface soil layer were more humified and relatively stable. Conversely, the DOM in shrubland and deeper soil layers contains more bioactive substances for microbial utilization. |
英文关键词 | Dissolved organic matter Soil profile EEM-PARAFAC Vegetation restoration Mu Us Sandy Land |
类型 | Article |
语种 | 英语 |
收录类别 | SCI-E |
WOS记录号 | WOS:001111261100001 |
WOS关键词 | PLANT LITTER DECOMPOSITION ; MICROBIAL COMMUNITY ; MOLECULAR-WEIGHT ; FOLIAR LITTER ; CARBON ; NITROGEN ; FLUORESCENCE ; DYNAMICS ; CLIMATE ; DEGRADABILITY |
WOS类目 | Agronomy ; Plant Sciences ; Soil Science |
WOS研究方向 | Agriculture ; Plant Sciences |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/405083 |
推荐引用方式 GB/T 7714 | Wang, Yixiang,Hu, Hanzhe,Zhou, Yajie,et al. Evolving characteristics of dissolved organic matter in soil profiles during 56 years of revegetation in Mu Us Sandy Land[J],2024,497(1-2):567-584. |
APA | Wang, Yixiang.,Hu, Hanzhe.,Zhou, Yajie.,Zhang, Buran.,Li, Shuo.,...&Tong, Xiaogang.(2024).Evolving characteristics of dissolved organic matter in soil profiles during 56 years of revegetation in Mu Us Sandy Land.PLANT AND SOIL,497(1-2),567-584. |
MLA | Wang, Yixiang,et al."Evolving characteristics of dissolved organic matter in soil profiles during 56 years of revegetation in Mu Us Sandy Land".PLANT AND SOIL 497.1-2(2024):567-584. |
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