Variability in spectral absorbance metrics across boreal lake waters

被引:49
作者
Erlandsson, Martin [1 ]
Futter, Martyn N. [1 ]
Kothawala, Dolly N. [2 ]
Kohler, Stephan J. [1 ]
机构
[1] Swedish Univ Agr Sci, Dept Aquat Sci & Assessment, S-75007 Uppsala, Sweden
[2] Uppsala Univ, Dept Limnol, Evolutionary Biol Ctr, S-75236 Uppsala, Sweden
来源
JOURNAL OF ENVIRONMENTAL MONITORING | 2012年 / 14卷 / 10期
基金
瑞典研究理事会;
关键词
DISSOLVED ORGANIC-MATTER; AQUATIC HUMIC SUBSTANCES; FULVIC-ACID; ULTRAVIOLET ABSORBENCY; OPTICAL-PROPERTIES; MOLECULAR-WEIGHT; CARBON; ABSORPTION; FLOCCULATION; ALUMINUM;
D O I
10.1039/c2em30266g
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
Ultraviolet/visible (UV/Vis) absorbance spectroscopy is a commonly used technique for characterizing dissolved organic matter (DOM). We present an analysis of UV/Vis absorbance spectra from 983 lakes throughout Sweden, sampled during autumn 2009. Metrics included both specific absorbances (i.e. absorbance per mass unit of organic carbon), and descriptions of spectral shape. Overall, we found three factors to which all spectral metrics were similarly related: acidity, retention-time, and latitude. In general, alkaline lakes with a long retention time in northern Sweden have lower specific absorbance and steeper spectral slope than acidic lakes with a short retention time in southern Sweden. Relative to the specific absorbance measured at 254 nm (SUVA), commonly used as a measure of DOM aromaticity, the specific absorbance at longer wavelengths and metrics of spectral shape were more sensitive to acidity and less sensitive to latitude. Although different spectral metrics are hypothesized to reflect different properties of DOM, UV/Vis absorbance spectroscopy may not be useful for more refined characterization of organic matter because of the strong inter-correlation between metrics. Nevertheless, it remains useful as a quick, cheap and reliable method of estimating DOM quantity and describing quality. We suggest that the most informative range to measure absorbance is between approximately 250 and 360 nm, where the between-lake variability is largest and absorbance can, in general, be precisely measured.
引用
收藏
页码:2643 / 2652
页数:10
相关论文
共 58 条
[1]  
Alexandersson H., 1991, 81 SMHI
[2]  
[Anonymous], WAT CHEM PHYS AN
[3]  
Berg Bjorn, 1997, Environmental Reviews, V5, P1, DOI 10.1139/er-5-1-1
[4]   Landscape regulation of bacterial growth efficiency in boreal freshwaters [J].
Berggren, Martin ;
Laudon, Hjalmar ;
Jansson, Mats .
GLOBAL BIOGEOCHEMICAL CYCLES, 2007, 21 (04)
[5]  
Bertills U, 2007, 5766 SWED ENV PROT A
[6]  
BRANDT M, 1994, 49 SMHI
[7]   MOLECULAR-WEIGHT, POLYDISPERSITY, AND SPECTROSCOPIC PROPERTIES OF AQUATIC HUMIC SUBSTANCES [J].
CHIN, YP ;
AIKEN, G ;
OLOUGHLIN, E .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1994, 28 (11) :1853-1858
[8]   Generation of humic and fulvic acid from Callovo- Oxfordian clay under high alkaline conditions [J].
Claret, F ;
Schäfer, T ;
Bauer, A ;
Buckau, G .
SCIENCE OF THE TOTAL ENVIRONMENT, 2003, 317 (1-3) :189-200
[9]   Hydrologic control of dissolved organic matter in low-order Precambrian Shield Lakes [J].
Curtis, PJ ;
Schindler, DW .
BIOGEOCHEMISTRY, 1997, 36 (01) :125-138
[10]  
DEHAAN H, 1987, FRESHWATER BIOL, V17, P453