东江湖流域水体耗氧污染演变与溶解有机碳输出通量研究

Evolution of oxygen-consuming pollution and dissolved organic carbon export in Dongjiang Lake Basin

  • 摘要: 水体耗氧污染危及水生态系统平衡,影响碳输移与区域碳循环。基于2015—2024年连续监测数据,采用Pearson相关系数法、Spearman秩相关系数法、Mann-Kendall趋势检验等方法,系统解析重要战略水源地东江湖流域入湖河流、湖区和出口断面近10年水体耗氧污染时空演变规律与影响因素;基于耗氧物质和呼吸熵估算溶解有机碳(DOC)浓度,进而定量评估流域DOC输出及其在区域碳收支中的作用。结果表明:东江湖流域5个入湖河流断面水体溶解氧(DO)、高锰酸盐指数(CODMn)、五日生化需氧量(BOD5)和氨氮(NH3-N)浓度分别为4.2~11.7、0.2~4.3、0.1~3.9和0.01~0.92 mg/L,而2个湖区断面相应指标浓度分别为6.2~11.5、0.3~2.0、0.1~2.4和0.02~0.42 mg/L,耗氧污染总体稳定,但均有部分月份超出GB 3838—2002《地表水环境质量标准》Ⅰ类(湖区)或Ⅱ类(入湖河流)水质目标。入湖河流耗氧物质含量高于湖区且总体呈降低趋势,但湖区CODMn未同步降低甚至呈上升趋势,提示湖区有内源潜在贡献。气温与多数断面DO浓度呈显著负相关,其主导水体DO季节变化,耗氧物质对DO浓度变化的影响在具体断面尺度上缺乏系统规律性。流域水体DOC浓度为0.10~0.31 mg/L(以C计),DOC单位面积输出量为0.098~0.292 t/(km2·a),处于长江流域低值水平;流域DOC总输出量为453.7~1 353.4 t/a,占流域净生态系统生产力的0.1%~0.3%,呈现“强陆地固碳-弱水体输出”特征。研究可为深化水体耗氧污染和区域碳收支协同管理提供依据。

     

    Abstract: Oxygen-consuming pollution in waters threatens the balance of aquatic ecosystems and affects aquatic carbon transport and regional carbon cycling. Based on continuous monitoring data from 2015 to 2024, this study employed the Pearson correlation coefficient method, Spearman rank correlation coefficient method, and Mann-Kendall trend test to systematically analyze the spatiotemporal evolution patterns and influencing factors of oxygen-consuming pollution in the inflow rivers, lake area, and outlet sections of the Dongjiang Lake Basin, a critical strategic drinking-water source, over the past decade. Oxygen-consuming indicators and the respiratory quotient were used to estimate dissolved organic carbon (DOC) concentration to further quantitatively assess its export flux and relative role in regional carbon budgets. The results showed that the ranges of dissolved oxygen (DO), permanganate index (CODMn), five-day biochemical oxygen demand (BOD5), and ammonia nitrogen (NH3-N) at the five river sections were 4.2-11.7, 0.2-4.3, 0.1-3.9, and 0.01-0.92 mg/L, respectively; while at the two lake sections, they were 6.2-11.5, 0.3-2.0, 0.1-2.4, and 0.02-0.42 mg/L, respectively. Although oxygen-consuming pollution remained generally stable, it occasionally exceeded Class Ⅰ (for lakes) or Class Ⅱ (for rivers) water quality targets of Environmental Quality Standards for Surface Water (GB 3838-2002) in some months. Oxygen-consuming substance content was higher in the rivers than in the lake and showed a decreasing trend; however, the CODMn content in the lake did not decrease synchronously and even increased, suggesting potential contributions from endogenous sources. Temperature was significantly and negatively correlated with DO at most sections, dominating the seasonal variation in DO, whereas the influence of oxygen-consuming substances on DO variations lacked systematic regularity at the specific section scale. DOC concentrations in the waters of the basin were 0.10-0.31 mg/L (calculated as carbon), with a unit DOC export of 0.098-0.292 t/(km2·a), which was relatively low in the Yangtze River basin. DOC export from the basin was estimated to be 453.7-1 353.4 t/a, accounting for 0.1%-0.3% of the net ecosystem productivity (NEP) of the basin, highlighting a characteristic of "strong terrestrial carbon sequestration-weak aquatic carbon export". This study provides a scientific basis for the integrated management of oxygen-consuming pollution and regional carbon budgets.

     

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