Radiocarbon age of different photoreactive fractions of freshwater dissolved organic matter

被引:5
|
作者
Ishikawa, Naoto F. [1 ]
Butman, David [2 ]
Raymond, Peter A. [3 ]
机构
[1] Japan Agcy Marine Earth Sci & Technol, Biogeochem Program, 2-15 Natsushima Cho, Yokosuka, Kanagawa 2370061, Japan
[2] Univ Washington, Dept Civil & Environm Engn, Seattle, WA 98195 USA
[3] Yale Univ, Sch Forestry & Environm Studies, 195 Prospect St, New Haven, CT 06511 USA
基金
日本学术振兴会; 美国国家科学基金会;
关键词
Dissolved organic carbon; Delta C-14; UV irradiation; Oxidation time; Mixing model; INORGANIC CARBON; ESTUARINE; CYCLE; C-14; RADIATION; RIVERINE; DOC;
D O I
10.1016/j.orggeochem.2019.06.006
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Dissolved organic carbon (DOC) plays a major role in aquatic carbon cycling. In order to determine if DOC photolability was related to DOC age, we tested the effect of oxidation time using UV irradiation on natural radiocarbon concentrations (Delta C-14) of DOC in six US rivers. The most photo-labile DOC was C-14 youngest. After a 100 min UV irradiation, most DOC (>93%) was oxidized in two out of the six rivers studied. On the other hand, the other four rivers still had a considerable amount (>20%) of DOC resistant to UV oxidation, which showed lower Delta C-14 values than those of bulk DOC. We also found that the concentration and Delta C-14 value of bulk DOC are controlled by the photochemically intermediate fraction. The results suggest that C-14 age of organic matter is not homogeneous within DOC, the degree of which may depend on the characteristics unique to rivers. (C) 2019 Elsevier Ltd. All rights reserved.
引用
收藏
页码:11 / 15
页数:5
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