Yu-yan Yang , Hao Wang , Zi-xin Wang , Qing-wei Zhang , Ren Geng , Jian Wang , Ming Li
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Spatial heterogeneity and controlling factors of DOM characteristics in the slope-gully systems were identified systematically using the optical techniques and principal component analysis. Results indicated that the dissolved organic carbon (DOC) content in both SGS and NGS followed the modes of top horizon (261.39 mg kg<sup>−1</sup>, 347.31 mg kg<sup>−1</sup>) > middle horizon (178.47 mg kg<sup>−1</sup>, 164.83 mg kg<sup>−1</sup>) > bottom horizon (83.19 mg kg<sup>−1</sup>, 100.42 mg kg<sup>−1</sup>). Three fluorescence components (i.e., two humic-like substances and one protein-like substance) were identified from all soil samples. The proportion of protein-like component of the NGS was higher than that of the SGS for the bottom horizon. DOM of the top and middle horizons were mainly from plant source with high aromaticity and molecular weight, whereas DOM of the bottom horizon was mostly dominated by microbial source with low aromaticity and molecular weight. Landscape location significantly influenced the aromaticity, humification degree, and source of DOM in the top horizon. The variation in DOM characteristics of slope-gully system was primarily attributed to the difference in characteristics of biocrusts, roots, and litter driven by topographic conditions.</div></div>","PeriodicalId":9801,"journal":{"name":"Catena","volume":"248 ","pages":"Article 108567"},"PeriodicalIF":5.4000,"publicationDate":"2024-11-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Unraveling the spatial heterogeneity of dissolved organic matter characteristics from the optical level in slope-gully systems\",\"authors\":\"Yu-yan Yang , Hao Wang , Zi-xin Wang , Qing-wei Zhang , Ren Geng , Jian Wang , Ming Li\",\"doi\":\"10.1016/j.catena.2024.108567\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Dissolved organic matter (DOM) is a crucial component of soil organic matter, and it significantly affects a range of environmental processes. However, few studies have focused on the spatial heterogeneity of DOM characteristics in typical geomorphic units. Therefore, in this study, a southern slope-gully system (SGS) and a northern slope-gully system (NGS) widely distributed in semiarid regions were selected as the study objects. Soil samples were collected from the three soil horizons (i.e., top horizon (0–2 cm), middle horizon (3–20 cm), bottom horizon (21–50 cm)) at each landscape locations (i.e., summit (SU), middle ridge slope (MS), lower ridge slope (LS), loess shoulder-line (SL), gully slope (GS), and gully floor (GF)) of the SGS and NGS. Spatial heterogeneity and controlling factors of DOM characteristics in the slope-gully systems were identified systematically using the optical techniques and principal component analysis. Results indicated that the dissolved organic carbon (DOC) content in both SGS and NGS followed the modes of top horizon (261.39 mg kg<sup>−1</sup>, 347.31 mg kg<sup>−1</sup>) > middle horizon (178.47 mg kg<sup>−1</sup>, 164.83 mg kg<sup>−1</sup>) > bottom horizon (83.19 mg kg<sup>−1</sup>, 100.42 mg kg<sup>−1</sup>). Three fluorescence components (i.e., two humic-like substances and one protein-like substance) were identified from all soil samples. The proportion of protein-like component of the NGS was higher than that of the SGS for the bottom horizon. DOM of the top and middle horizons were mainly from plant source with high aromaticity and molecular weight, whereas DOM of the bottom horizon was mostly dominated by microbial source with low aromaticity and molecular weight. Landscape location significantly influenced the aromaticity, humification degree, and source of DOM in the top horizon. 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引用次数: 0
摘要
溶解有机质(DOM)是土壤有机质的重要组成部分,对一系列环境过程具有重要影响。然而,对典型地貌单元DOM特征的空间异质性研究较少。因此,本研究选择半干旱区广泛分布的南部坡沟系统(SGS)和北部坡沟系统(NGS)作为研究对象。在黄土高原和黄土高原各景观位置(即峰顶(SU)、中脊坡(MS)、下脊坡(LS)、黄土肩线(SL)、沟壑坡(GS)和沟壑底(GF))的3个土壤层(即顶层(0-2 cm)、中层(3-20 cm)、底层(21-50 cm)采集土壤样品。利用光学技术和主成分分析,系统地研究了坡沟系统DOM特征的空间异质性及其控制因素。结果表明:两种土壤中溶解有机碳(DOC)含量分别为顶层水平(261.39 mg kg - 1, 347.31 mg kg - 1)和顶层水平;中地平线(178.47 mg kg - 1, 164.83 mg kg - 1) >;底部水平(83.19 mg kg - 1, 100.42 mg kg - 1)。从所有土壤样品中鉴定出三种荧光成分(即两种腐殖质样物质和一种蛋白质样物质)。在底层,NGS蛋白样成分的比例高于SGS。上层和中层DOM主要来自植物源,芳香性和分子量较高,底层DOM主要来自微生物源,芳香性和分子量较低。景观位置对顶层DOM的芳香度、腐殖化程度和来源有显著影响。坡沟系统DOM特征的变化主要归因于地形条件驱动的生物结皮、根系和凋落物特征的差异。
Unraveling the spatial heterogeneity of dissolved organic matter characteristics from the optical level in slope-gully systems
Dissolved organic matter (DOM) is a crucial component of soil organic matter, and it significantly affects a range of environmental processes. However, few studies have focused on the spatial heterogeneity of DOM characteristics in typical geomorphic units. Therefore, in this study, a southern slope-gully system (SGS) and a northern slope-gully system (NGS) widely distributed in semiarid regions were selected as the study objects. Soil samples were collected from the three soil horizons (i.e., top horizon (0–2 cm), middle horizon (3–20 cm), bottom horizon (21–50 cm)) at each landscape locations (i.e., summit (SU), middle ridge slope (MS), lower ridge slope (LS), loess shoulder-line (SL), gully slope (GS), and gully floor (GF)) of the SGS and NGS. Spatial heterogeneity and controlling factors of DOM characteristics in the slope-gully systems were identified systematically using the optical techniques and principal component analysis. Results indicated that the dissolved organic carbon (DOC) content in both SGS and NGS followed the modes of top horizon (261.39 mg kg−1, 347.31 mg kg−1) > middle horizon (178.47 mg kg−1, 164.83 mg kg−1) > bottom horizon (83.19 mg kg−1, 100.42 mg kg−1). Three fluorescence components (i.e., two humic-like substances and one protein-like substance) were identified from all soil samples. The proportion of protein-like component of the NGS was higher than that of the SGS for the bottom horizon. DOM of the top and middle horizons were mainly from plant source with high aromaticity and molecular weight, whereas DOM of the bottom horizon was mostly dominated by microbial source with low aromaticity and molecular weight. Landscape location significantly influenced the aromaticity, humification degree, and source of DOM in the top horizon. The variation in DOM characteristics of slope-gully system was primarily attributed to the difference in characteristics of biocrusts, roots, and litter driven by topographic conditions.
期刊介绍:
Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment.
Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.