上海大学学报(自然科学版) ›› 2021, Vol. 27 ›› Issue (2): 271-279.doi: 10.12066/j.issn.1007-2861.2280

• 中国西南地区河流拦截对物质循环的影响及生态意义 • 上一篇    下一篇

乌江流域下游梯级水库沉积物中木质素的特征及有机碳来源辨析

黄佳琦, 林昕, 汪福顺, 马静()   

  1. 上海大学 环境与化学工程学院, 上海 200444
  • 收稿日期:2020-05-11 出版日期:2021-04-30 发布日期:2021-04-27
  • 通讯作者: 马静 E-mail:jingma@shu.edu.cn
  • 作者简介:马 静(1980—), 女, 副研究员, 博士, 研究方向为环境地球化学. E-mail:jingma@shu.edu.cn
  • 基金资助:
    国家重点研发计划资助项目(2016YFA0601003)

Characteristics of lignin in sediment cores from cascade reservoirs downstream of the Wujiang River and[1mm] source analysis of organic carbon

HUANG Jiaqi, LIN Xin, WANG Fushun, MA Jing()   

  1. School of Environmental and Chemical Engineering, Shanghai University, Shanghai 200444, China
  • Received:2020-05-11 Online:2021-04-30 Published:2021-04-27
  • Contact: MA Jing E-mail:jingma@shu.edu.cn

摘要:

以位于中国西南喀斯特地貌乌江流域下游的两座大型深水水库(思林水库、彭水水库)为研究对象, 利用木质素生物标志物技术对沉积柱中的陆源有机碳(organic carbon, OC)进行了定性分析和定量计算. 研究结果表明: 木质素含量指标$\Sigma 8$值在0.55$\sim$ 2.97 mg/10 g dw(dry weight, 干重)之间, $\Lambda 8$值在0.38$\sim$1.42 mg/100 mg OC之间; 木质素母源植被信息显示, 沉积柱中的木质素主要来源于被子植物的草本组织; 木质素受白腐菌和棕腐菌共同作用, 发生较低程度的去甲基/去甲氧基以及侧链氧化降解. 端元模型结果显示, 沉积柱中外源有机碳的贡献总体上略大于内源有机碳, 其中土壤有机碳贡献最大. 河流梯级筑坝作用对沉积物中有机碳的影响表现为外源有机碳的拦截和内源有机碳的积蓄两个方面, 并且内外源有机碳分布存在明显的空间异质性.

关键词: 梯级水库, 木质素, 陆源有机碳, 乌江流域

Abstract:

The terrestrial organic carbon (OC) in sediment cores from two large deep-water reservoirs (Silin and Pengshui) located in the lower reaches of the Wujiang River in the karst landscape of Southwest China were analysed and quantified using lignin biomarker technology. Qualitative analysis and quantitative calculations of terrestrial-derived organic carbon in sediment cores using the lignin biomarker technique showed that the lignin content index $\Sigma 8$ ranged from 0.55 to 2.97 mg/10 g dw (dry weight) and $\Lambda 8$ ranged from 0.38 to 1.42 mg/100 mg OC. The lignin in the sediment cores was derived mainly from the herbaceous tissues of angiosperms, and had been degraded via demethylation, demethoxylation, and oxidative degradation of the side chains by white rot and brown rot bacteria. The end-member model showed that the contribution of exogenous organic carbon to the sediment cores was slightly greater than that of endogenous organic carbon, with soil organic carbon contributing the most. The influence of river cascade damming on sedimentary organic carbon was manifested in the interception of exogenous organic carbon and the accmulation of endogenous organic carbon, and there was obvious spatial heterogeneity in the distribution of both types of organic carbon.

Key words: cascade reservoir, lignin, terrestrial organic carbon (OC), Wujiang River

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