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松花湖沉积物溶解性有机质荧光光谱特性
摘要点击 1726  全文点击 867  投稿时间:2021-08-13  修订日期:2021-09-23
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中文关键词  松花湖  激发发射矩阵光谱-平行因子分析(EEM-PARAFAC)  沉积物  溶解性有机物(DOM)  富营养化
英文关键词  Songhua Lake  excitation emission matrix-parallel factor analysis (EEM-PARAFAC)  sediment  dissolved organic matter (DOM)  eutrophication
作者单位E-mail
程云轩 吉林建筑大学松辽流域水环境教育部重点实验室, 长春 130000
中国环境科学研究院, 环境基准与风险评估国家重点实验室, 北京 100012 
244937163@qq.com 
赵可 吉林建筑大学松辽流域水环境教育部重点实验室, 长春 130000  
张越 中国环境科学研究院, 环境基准与风险评估国家重点实验室, 北京 100012
中国环境科学研究院, 湖泊水污染治理与生态修复技术国家工程实验室, 北京 100012 
 
张渝婷 中国环境科学研究院, 环境基准与风险评估国家重点实验室, 北京 100012
中国环境科学研究院, 湖泊水污染治理与生态修复技术国家工程实验室, 北京 100012 
 
焦立新 中国环境科学研究院, 环境基准与风险评估国家重点实验室, 北京 100012
中国环境科学研究院, 湖泊水污染治理与生态修复技术国家工程实验室, 北京 100012 
jiaolx@craes.org.cn 
中文摘要
      溶解性有机质(DOM)对于湖泊的主要污染指标(如COD等)有着较大的影响,而沉积物亦是湖泊污染的主要来源,因此沉积物DOM荧光光谱特性的研究对进一步揭示湖泊污染本质有重要意义.采集了松花湖20个点位的沉积物,利用激发发射矩阵光谱-平行因子分析(EEM-PARAFAC)技术对沉积物中的DOM组分进行了解析,从光谱学角度明确沉积物DOM的特性,并对DOM与水体富营养化水平之间的关系进行了初步探索.结果表明,从松花湖沉积物DOM中分离出4个组分:类腐殖质C1(330/415 nm)、C2(255/440 nm)、C3(365/470 nm)和类蛋白C4(280/355 nm).较高的HIX和低BIX表明沉积物DOM的来源以陆源为主,包含一部分生物源.4个组分的荧光强度存在关联,空间分布较为相似,均表现为上游(S1~S7)荧光强度高于下游(S8~S20).而辉发河、松花江和蛟河这3条主要入湖河流携带的悬浮颗粒物(SPM)在入湖段大量沉积是导致这种空间分布的主要原因.松花湖水体中富营养化状况(上游富营养化水平高于下游)与沉积物DOM的荧光强度分布状况相似,同时松花湖下游水体富营养化水平与沉积物DOM荧光强度存在较强相关性.
英文摘要
      Dissolved organic matter (DOM) has a significant impact on the main pollution indicators of the lake (e.g., COD), and sediment is the main source of pollution in the lake. Research on the fluorescence spectral characteristics of DOM in sediments is important to reveal the mechanism of lake pollution. In this study, sediments were collected from 20 sites in Songhua Lake. The DOM components in the sediment were analyzed using the excitation emission matrix-parallel factor analysis (EEM-PARAFAC) technique, and the properties of the sediment DOM were clarified via spectroscopy. Additionally, the relationship between DOM and eutrophication of the water column was explored. The results showed that four components were identified from the sediment DOM of Songhua Lake:humic-like C1 (330/415 nm), C2 (255/440 nm), C3 (365/470 nm), and protein-like C4 (280/355 nm). The high HIX and low BIX indicated that the source of sediment DOM was mainly terrestrial and included some biological sources. The spatial distribution of the fluorescence intensity of the four components was relatively similar, showing that the fluorescence intensity was higher in the upstream (S1-S7) than that in the downstream (S8-S20). The massive deposition of suspended particulate matter (SPM) carried by the three rivers (Huifa River, Songhua River, and Jiao River) was the main reason for this spatial distribution. Eutrophication status in the water column of Songhua Lake was similar to the fluorescence intensity distribution of sediment DOM. Meanwhile, there was a strong correlation between eutrophication level and sediment DOM fluorescence intensity in the downstream water column of Songhua Lake.

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