Links

Tools

Export citation

Search in Google Scholar

Characterization of chromophoric dissolved organic matter in lakes on the Tibet Plateau, China, using spectroscopic analysis

Preprint published in 2018 by Kaishan Song, Sijia Li, Zhidan Wen, Lili Lyu, Yingxin Shang
This paper is available in a repository.
This paper is available in a repository.

Full text: Download

Question mark in circle
Preprint: policy unknown
Question mark in circle
Postprint: policy unknown
Question mark in circle
Published version: policy unknown

Abstract

Spatiotemporal variations in the characteristics of fluorescent dissolved organic matter (FDOM) components from 63 lakes across the Tibet Plateau, China, are examined using excitation-emission matrix spectra (EEM) and fluorescence regional integration (FRI) from 2014 to 2017. Freshwater ( N = 135) and brackish water ( N = 109) samples from 63 lakes were grouped according to salinity or electrical conductivity. In order to compare results between the lakes, cumulative volumes beneath the EEM values (φ i , i = I, II, III, IV, V) were normalized to a DOC concentration of 1 mg/L. EEM-FRI identified tyrosine-like (φ I ), tryptophan-like (φ II ), fulvic-like (φ III ), microbial protein-like (φ IV ), and humic-like (φ V ) fluorescence regions, as well as their proportions (P i ). Chromophoric dissolved organic matter (CDOM) absorption parameters, fluorescence indices, average fluorescence intensities of the five fluorescent components and total fluorescence intensities (φ T ) differed under spatial variation among brackish and freshwater lakes (ANOVA, p < 0.05). Principal component analysis (PCA) was used to assess and group five normalized FDOM components for all of the water samples. These results show that microbial protein-like (φ IV ), fulvic-like (φ III ) and humic-like (φ V ) have positive correlations (R 2 > 0.79, t -test, p < 0.01), indicating that these FDOM components may originate from similar sources. A correlation also exists between normalized φ i ( i = I, II, III, IV, V) and DOC concentrations with a salinity > 19 ‰ (averaged EC, 23 764 μs cm −1 ) ( t -test, p < 0.01), of which R 2 f regression analysis showed a decreasing tendency with EC. Similar correlations between a (254) and DOC concentrations ( t -test, p < 0.01) are also evident for sunshine hours > 2900 h. Redundancy analysis (RDA) indicates that a (254) and a (350) have a correlation with CDOM in brackish lakes. a (254), HIX and a (350) were also correlated with water quality. Strong evapoconcentration, intense ultraviolet irradiance and landscape features of the Tibet Plateau may be responsible for the FDOM characteristics identified in this study.

Beta version