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Insight into the vertical characteristics of dissolved organic matter in 5-m soil profiles under different land-use types on the Loess Plateau

机译:黄土高原不同土地利用类型下5 m土壤剖面可溶性有机物的垂直特征

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Dissolved organic matter (DOM) is a natural chemical component of all soils and influences soil organic pollutant migration, nutrient cycling, and global climate change. Previous field studies have focused on a single ecosystem. such as cropland, grassland, or forestland. However, the potential effect of different land-use types on the vertical distribution of soil DOM quantity and quality remains unclear. This study investigated the vertical characteristics of DOM in 5-m soil profiles under different land-use types (cropland, grassland, and forestland) on the Loess Plateau. The data from ultraviolet-visible spectral and parallel factor analysis of fluorescence excitation-emission matrix spectrophotometry were combined. These results indicated that the mean content of dissolved organic carbon (DOC) in the 30-yr forestland (203.33 mg kg(-1 )soil) was the highest, and the lowest was observed in the cropland (83.70 mg kg(-1) soil). Meanwhile, the mean DOC content of the forestland increased through time, particularly after 20 years. In other words, afforestation activities only significantly affected soil DOM after a long time (over 20 years). The DOC content of the cropland initially increased and then decreased with soil depth in the 1-m soil profiles, which may be related to agricultural activities. Three fluorescence components, including two humic acid-like substances (C1 and C3) and a tryptophan-like substance (C2), were identified from all samples. The humic acid-like components significantly decreased by 51% with soil depth, while the tryptophan-like component increased by 49%. particularly in the cropland. The variation in ultraviolet-visible spectral and optical indexes also indicated that soil DOM was dominated by both microbial and terrestrial sources. These findings help to understand the dynamics of DOC in deep soil profiles and the biogeochemical effects of DOM in the natural environment. (C) 2019 Elsevier B.V. All rights reserved.
机译:溶解有机物(DOM)是所有土壤的天然化学成分,会影响土壤有机污染物的迁移,养分循环和全球气候变化。先前的现场研究仅关注单个生态系统。例如农田,草原或林地。但是,不同土地利用类型对土壤DOM数量和质量的垂直分布的潜在影响尚不清楚。这项研究调查了黄土高原不同土地利用类型(作物,草地和林地)下5米土壤剖面中DOM的垂直特征。结合了紫外可见光谱和荧光激发-发射矩阵分光光度法的平行因子分析数据。这些结果表明,30年林地中的溶解有机碳(DOC)的平均含量(203.33 mg kg(-1)土壤)最高,而在农田中最低(83.70 mg kg(-1))。泥)。同时,林地的平均DOC含量随时间增加,特别是在20年后。换句话说,造林活动在很长一段时间(超过20年)后仅对土壤DOM有显着影响。农田中DOC的含量最初随着土壤深度在1-m土壤剖面中增加然后减少,这可能与农业活动有关。从所有样品中鉴定出三个荧光成分,包括两种腐殖酸样物质(C1和C3)和色氨酸样物质(C2)。腐殖酸样组分随土壤深度的增加而显着减少51%,而色氨酸样组分则增加49%。特别是在农田上。紫外线-可见光谱和光学指数的变化还表明,土壤DOM主要由微生物和陆地来源控制。这些发现有助于理解土壤深层剖面中DOC的动态以及DOM在自然环境中的生物地球化学作用。 (C)2019 Elsevier B.V.保留所有权利。

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