首页|高寒山区土壤溶解性有机质特征及其对河流溶解性有机质输出的影响

高寒山区土壤溶解性有机质特征及其对河流溶解性有机质输出的影响

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冻土区土壤中存储有大量有机碳.目前对高寒山区多年冻土区和季节冻土区土壤有机质特征及其差异研究较少,对土壤中溶解性有机质(dissolved organic matter,DOM)特征及其对河水中DOM输出的影响认识尚不明确.为了解高寒山区土壤中溶解性有机质的分布规律、成分特征及对水体中DOM输出特征的控制作用,本研究采集青藏高原东北部葫芦沟小流域中多年冻土区和季节冻土区不同深度(<1 m)土壤样品,对土壤中总有机碳(soil organic carbon,SOC)和溶解性有机碳(dissolved organic carbon,DOC)含量、DOM的光谱特征、DOC的生物可降解性(biodegradable dissolved organic matter,BDOC)进行分析,并将其与不同水体中DOM特征的季节性变化进行对比.研究发现:多年冻土区与季节冻土区土壤在DOC的生物可降解性及微生物活动方面存在明显差异;多年冻土区土壤中SOC含量较高,但DOC含量较低,DOM的腐殖化程度和芳香性低于季节冻土区;季节冻土区的土壤中BDOC占比高于多年冻土.研究表明:高寒山区土壤水文特性对土壤有机质含量和特征的显著影响,其中土壤含水率是重要影响因素;多年冻土区浅层土壤DOM对河水DOC浓度和成分变化起决定性作用;相比之下,季节冻土区土壤对河水DOC浓度和成分变化直接影响较小,水文条件影响着水体中DOM的输出特征.本研究成果对高寒山区冻土退化条件下的碳循环研究具有指导意义.
Characteristics of Dissolved Organic Matter in Alpine Mountain Soils and Its Effect on Riverine Dissolved Organic Matter Export
The soil layers in permafrost regions store a large amount of organic carbon.However,the understanding of the influence of dissolved organic matter(DOM)in permafrost and seasonally frozen ground on the DOM characteristics of riverine output is still unclear due to limited existing studies on the characteristics of soil organic matter in permafrost and seasonally frozen ground and their differences in alpine catchments.To understand the distributions,and controlling mechanisms of dissolved organic matter in the soil of alpine catchments on aquatic DOM,this study collected soil samples of permafrost and seasonally frozen ground in the Hulugou catchment in the northeastern part of the Tibetan plateau and analyzed the soil organic carbon(SOC),dissolved organic carbon(DOC)content,spectral characteristics of DOM,and its biodegradable dissolved organic carbon(BDOC).Then,DOM characteristics in soils were compared with those from different water bodies at different seasons.The study reveals significant differences between permafrost and seasonally frozen soils in terms of dissolved organic carbon(DOC)biodegradability and microbial activity.Permafrost soils have higher soil organic carbon(SOC)but lower DOC,and their dissolved organic matter(DOM)is less humified and aromatic compared to seasonally frozen soils,where biodegradable DOC(BDOC)proportions are higher.The findings indicate that soil hydrological traits in cold mountain areas significantly influence soil organic matter,highlighting soil moisture as a critical factor.In permafrost areas,shallow soil DOM crucially affects river water DOC concentrations and composition.In contrast,seasonal permafrost zone soils have less direct influence on changes in stream DOC concentration and composition,with hydrological conditions shaping DOM's output features in water bodies.This research is crucial for understanding carbon cycling under permafrost degradation in cold mountain regions,condensed into a comprehensive summary within the specified word limit.

alpine mountain areapermafrostseasonal freezing zonesoilsdissolved organic matterbiodegradable dissolved organic matterhydrogeology

熊净、孙自永、胡雅璐、马瑞

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中国地质大学环境学院,湖北武汉 430078

中国地质大学长江流域环境水科学湖北省重点实验室,湖北武汉 430078

中国地质大学水资源与环境学院,北京 100083

高寒山区 多年冻土 季节冻土 土壤 溶解性有机质 DOM生物可降解性 水文地质

2024

地球科学
中国地质大学

地球科学

CSTPCD北大核心
影响因子:1.447
ISSN:1000-2383
年,卷(期):2024.49(11)