Temporal and Spatial Changes in Black Carbon Sedimentary Processes in Wetlands of Songnen Plain, Northeast of China

被引:10
|
作者
He, Jiabao [1 ,2 ]
Gao, Chuanyu [1 ,2 ]
Lin, Qianxin [1 ,3 ]
Zhang, Shaoqing [1 ]
Zhao, Winston [4 ]
Lu, Xianguo [1 ]
Wang, Guoping [1 ]
机构
[1] Chinese Acad Sci, Key Lab Wetland Ecol & Environm, Northeast Inst Geog & Agroecol, Changchun, Peoples R China
[2] Univ Chinese Acad Sci, Beijing, Peoples R China
[3] Louisiana State Univ, Dept Oceanog & Coastal Sci, Sch Coast & Environm, Baton Rouge, LA 70803 USA
[4] Penn State Univ, Smeal Coll, University Pk, PA 16802 USA
来源
PLOS ONE | 2015年 / 10卷 / 10期
基金
中国国家自然科学基金;
关键词
ORGANIC-CARBON; HISTORICAL TRENDS; ELEMENTAL CARBON; SOIL-PHOSPHORUS; TIBETAN PLATEAU; SANJIANG PLAIN; MIXING STATE; DESERTIFICATION; STORAGE; RECORD;
D O I
10.1371/journal.pone.0140834
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Black carbon (BC), an important component of organic carbon (OC) produced from incomplete combustion of carbon compounds, is widespread and affects the global carbon storage. The objectives of this study were to analyze the BC contents and fluxes in the last 150 years to determine the causes of differences in the three profiles of the Songnen Plain of Northeast China and to estimate the BC storage in the wetlands of the Songnen Plain. In the three sampling sites, BC fluxes in the period between 1950 and the present time increased by the ratios of 1.3, 31.1 and 1.4, respectively, compared to their own baseline between 1850 and 1900. Furthermore, the BC fluxes varying from 0.76 to 5.63 g m(-2) y(-1) in the three profiles had an opposite trend with the sand percentages with mean values changing from 78.9% to 19.6%, suggesting that sand desertification might additionally affect the BC processes in the region.
引用
收藏
页数:14
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