Zhang Lian-Kai, Qin Xiao-Qun, Yang Hui, Huang Qi-Bo, Liu Peng-Yu
Karst Dynamics Laboratory, Ministry of Land and Resources & Guangxi Zhuang Autonomous Region, Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin 541004, China.
Huan Jing Ke Xue. 2013 Aug;34(8):3025-34.
The riverine carbon flux is a critical component of global carbon cycle. Riverine water samples were collected from eleven hydrometric stations in the main stream of Pearl River and its tributaries during April and July, 2012. The samples were analyzed for the space and seasonal distribution characteristics of the riverine suspended substance and carbon compositions. Carbon fluxes and erosion modulus of Pearl River basin were also estimated in Boluo, Shijiao, Gaoyao, namely Dongjiang, Beijiang, Xijiang, in these two hydrological seasons. The results showed that the total suspended substance (TSS) and organic carbon, including total particulate organic carbon (POC) and dissolved organic carbon (DOC) have higher concentration in the high-water season than that in the normal-water season. Dissolved inorganic carbon (DIC) has an overwhelming concentration compared to other carbon compositions in Pearl River basin. The DIC concentration shows an order of Xijiang, Beijiang and Dongjiang from high to low. The percentage of allogenic POC in Xijiang, Beijiang and Dongjiang are 78%, 72%, 26%, respectively, and C3 plants are the main sources of allogenic POC in those three tributaries. The transported fluxes of TSS, total carbon (TC), POC, particulate inorganic carbon (PIC), DOC, DIC, total particulate carbon (TPC) and total organic carbon (TOC) are 134 x 10(12),12.69 x 10(12), 2.50 x 10(12), 1.01 x 10(12), 1.13 x 10(12), 8.05 x 10(12), 3.51 x 10(12) and 3.65 x 10(12) g x a(-1), respectively, and the erosion modulus of those compositions are 309 x 10(6), 28.98 x 10(6), 5.75 x 10(6), 2.27 x 10(6), 2.56 x 10(6), 18.4 x 10(6), 8.02 x 10(6) and 8.31 x 10(6) g x (km2 x a)(-1), respectively. Compared with average values of global large rivers, the erosion modulus of DOC, POC, and TOC in Pearl River basin are higher than the corresponding values.
河流碳通量是全球碳循环的一个关键组成部分。2012年4月和7月期间,从珠江及其支流的11个水文站采集了河水样本。对样本进行了分析,以研究河流悬浮物和碳成分的空间和季节分布特征。在这两个水文季节,还估算了珠江流域在博罗、石角、高要(即东江、北江、西江)的碳通量和侵蚀模数。结果表明,总悬浮物(TSS)以及包括总颗粒有机碳(POC)和溶解有机碳(DOC)在内的有机碳在高水期的浓度高于平水期。与珠江流域的其他碳成分相比,溶解无机碳(DIC)的浓度占主导地位。DIC浓度呈现出西江、北江、东江从高到低的顺序。西江、北江和东江中异源POC的百分比分别为78%、72%、26%,这三条支流中C3植物是异源POC的主要来源。TSS、总碳(TC)、POC、颗粒无机碳(PIC)、DOC、DIC、总颗粒碳(TPC)和总有机碳(TOC)的输运通量分别为134×10¹²、12.69×10¹²、2.50×10¹²、1.01×10¹²、1.13×10¹²、8.05×10¹²、3.51×10¹²和3.65×10¹² g·a⁻¹,这些成分的侵蚀模数分别为³⁰⁹×¹⁰⁶、²⁸.⁹⁸×¹⁰⁶、⁵.⁷⁵×¹⁰⁶、².²⁷×¹⁰⁶、².⁵⁶×¹⁰⁶、¹⁸.⁴×¹⁰⁶、⁸.⁰²×¹⁰⁶和⁸.³¹×¹⁰⁶ g·(km²·a)⁻¹。与全球大型河流的平均值相比,珠江流域DOC、POC和TOC的侵蚀模数高于相应值。