Estimation of different source contributions to sediment organic matter in an agricultural-forested watershed using end member mixing analyses based on stable isotope ratios and fluorescence spectroscopy

被引:88
作者
Derrien, Morgane [1 ]
Kim, Min-Seob [2 ]
Ock, Giyoung [3 ]
Hong, Seongjin [4 ]
Cho, Jinwoo [1 ]
Shin, Kyung-Hoon [5 ]
Hur, Jin [1 ]
机构
[1] Sejong Univ, Dept Environm & Energy, Seoul 143747, South Korea
[2] Natl Inst Environm Res, Environm Measurement & Anal Ctr, Incheon 22689, South Korea
[3] Natl Inst Ecol, Seocheon 33657, South Korea
[4] Chungnam Natl Univ, Dept Ocean Environm Sci, Daejeon 34134, South Korea
[5] Hanyang Univ, Dept Marine Sci & Convergent Engn, Ansan 15588, Gyeonggi Do, South Korea
基金
新加坡国家研究基金会;
关键词
Sediment organic matter; EEM-PARAFAC; Stable isotope ratios; Source tracing; End-member mixing analysis; AQUATIC ENVIRONMENTS; SOURCE IDENTIFICATION; SPATIAL-DISTRIBUTION; SURFACE SEDIMENTS; LAND-USE; CARBON; NITROGEN; LAKE; INDICATORS; STREAM;
D O I
10.1016/j.scitotenv.2017.11.067
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The two popular source tracing tools of stable isotope ratios (delta C-13 and delta N-15) and fluorescence spectroscopy were used to estimate the relative source contributions to sediment organic matter (SeOM) at five different river sites in an agricultural-forested watershed (Soyang Lake watershed), and their capabilities for the source assignment were compared. Bulk sediments were used for the stable isotopes, while alkaline extractable organic matter (AEOM) from sediments was used to obtain fluorescent indices for SeOM. Several source discrimination indices were fully compiled for a range of the SeOM sources distributed in the catchments of the watershed, which included soils, forest leaves, crop (C3 and C4) and riparian plants, periphyton, and organic fertilizers. The relative source contributions to the river sediment samples were estimated via end member mixing analysis (EMMA) based on several selected discrimination indices. The EMMA based on the isotopes demonstrated that all sediments were characterized by a medium to a high contribution of periphyton ranging from similar to 30% to 70% except for one site heavily affected by forest and agricultural fields with relatively high contributions of terrestrial materials. The EMMA based on fluorescence parameters, however, did not show similar results with low contributions from forest leaf and periphyton. The characteristics of the studied watershed were more consistent with the source contributions determined by the isotope ratios. The discrepancy in the EMMA capability for source assignments between the two analytical tools can be explained by the limited analytical window of fluorescence spectroscopy for non-fluorescent dissolved organic matter (FDOM) and the inability of AEOM to represent original bulk particulate organic matter (POM). (c) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:569 / 578
页数:10
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