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    白洋淀近70年生态环境演化过程及影响因素

    毛欣 刘林敬 宋磊 姜高磊 李峻峰 李长安

    毛欣, 刘林敬, 宋磊, 姜高磊, 李峻峰, 李长安, 2021. 白洋淀近70年生态环境演化过程及影响因素. 地球科学, 46(7): 2609-2620. doi: 10.3799/dqkx.2020.203
    引用本文: 毛欣, 刘林敬, 宋磊, 姜高磊, 李峻峰, 李长安, 2021. 白洋淀近70年生态环境演化过程及影响因素. 地球科学, 46(7): 2609-2620. doi: 10.3799/dqkx.2020.203
    Mao Xin, Liu Linjing, Song Lei, Jiang Gaolei, Li Junfeng, Li Chang'an, 2021. A 70 Year Sedimentary Record of Eco-Environment Changes in Baiyangdian Lake and Its Influencing Factors. Earth Science, 46(7): 2609-2620. doi: 10.3799/dqkx.2020.203
    Citation: Mao Xin, Liu Linjing, Song Lei, Jiang Gaolei, Li Junfeng, Li Chang'an, 2021. A 70 Year Sedimentary Record of Eco-Environment Changes in Baiyangdian Lake and Its Influencing Factors. Earth Science, 46(7): 2609-2620. doi: 10.3799/dqkx.2020.203

    白洋淀近70年生态环境演化过程及影响因素

    doi: 10.3799/dqkx.2020.203
    基金项目: 

    河北省自然科学基金项目 D2018504013

    中国地质科学院基本科研业务费专项 SK202007

    中国地质调查项目 G201801-7

    详细信息
      作者简介:

      毛欣(1989-), 男, 助理研究员, 主要从事湖泊古生态方面的研究.ORCID: 0000-0001-7384-590X.E-mail: maoxin.iheg@cnu.edu.com

      通讯作者:

      刘林敬, ORCID: 0000-0002-8711-9578.E-mail: liulj206@126.com

    • 中图分类号: P95

    A 70 Year Sedimentary Record of Eco-Environment Changes in Baiyangdian Lake and Its Influencing Factors

    • 摘要: 基于白洋淀北部沉积岩心210Pb和137Cs测年、重金属元素、营养元素、粒度和硅藻优势属种分析,结合水文、气候以及保定市和安新县社会经济统计资料,重建了白洋淀近70年以来的生态环境演化历史,并探讨了影响硅藻优势属种演替的主要驱动因素.结果表明:1960年之前,重金属和营养元素处于较低的水平,硅藻属种以Aulacoseira granulata为主,反映湖泊生态环境处于自然演化阶段;1960年前后,由于受到上游水文调控的影响,白洋淀TP和TN含量开始缓慢增加,富营养指示种Cyclotella meneghiniana明显增加;1960~1990年,TP和TN含量明显升高,反映快速农业化进程中营养物质输入增加,但重金属含量仍保持在较低的水平,硅藻属种以A.granulataC.meneghiniana为优势组合;1990年以来,流域工农业活动的快速发展导致重金属和营养盐富集,尤其是2000年以后,重金属和营养盐富集进一步加剧,此时硅藻组合也发生了重大转变,由1990年前的A.granulata优势种转变为1990年后的C.meneghiniana优势种,重金属耐受种Nitzschia palea也自2000年以来开始持续增加.冗余分析表明沉积物重金属、TP、TN、温度、风速、入淀水量和水位是影响白洋淀近70年以来3个硅藻优势属种演替的显著因子,其中重金属和营养是硅藻组合演替的主要驱动因素,水文过程、温度和风速是硅藻组合演替的重要诱因.

       

    • 图  1  白洋淀流域(a)、采样点位置图(b)以及月平均气温和降水量(c)

      Fig.  1.  Drainage area of Lake Baiyangdian (a), location of the core site (b) and variation of monthly temperature and precipitation (c)

      图  2  1950年以来保定市气象记录(a)、保定市和安新县主要经济指标(b)、白洋淀水文资料(c)和白洋淀湿地和非湿地面积(d)

      Fig.  2.  Climate data of Baoding City (a), main economic indicators of Baoding city and Anxin County (b), hydrology data of Baiyangdian Lake (c) and areas change of wetlands and non-wetlands (d) since 1950 AD

      图  3  白洋淀沉积岩心137Cs、210Pbex比活度的垂直变化

      Fig.  3.  Vertical profile of 137Cs and 210Pb in the core of Baiyangdian Lake

      图  4  白洋淀沉积岩心粒度(粘土、粉砂和砂)、重金属元素(Zn、Cu、Cd和Pb)、总磷、总氮和硅藻组合的沉积序列

      Fig.  4.  Sedimentary profiles of grain size (clay, silt and sand), heavy metals (Zn, Cu, Cd and Pb), total phosphorus, total nitrogen and diatom assemblages in Baiyangdian Lake

      图  5  重金属元素主成分分析图(a)和硅藻优势属种冗余分析图(b)

      Fig.  5.  Principal components analysis of heavy metals (a) and redundancy analysis of diatom dominant species (b)

      图  6  白洋淀沉积物重金属单因子潜在生态危害系数($ {E}_{r}^{i} $)和综合潜在生态风险指数(RI)的变化

      Fig.  6.  Potential pollution risk index of heavy metal ($ {E}_{r}^{i} $) and potential ecological risk index (RI)

      图  7  Aulacoseira granulata与风速的相关性分析

      Fig.  7.  Correlation analysis between Aulacoseira granulata and wind speed

      表  1  单因子及综合潜在生态风险评价指数与分级标准

      Table  1.   Individual indice and grades of potential ecological risk assessment

      $ {E}_{r}^{i} $ 风险等级 RI 生态风险等级
      $ {E}_{r}^{i} $ < 40 低等 RI < 150 低等
      40≤$ {E}_{r}^{i} $ < 80 中等 150≤RI < 300 中等
      80≤$ {E}_{r}^{i} $ < 160 较重 300≤RI < 600
      160≤$ {E}_{r}^{i} $ < 320 RI≥600 严重
      $ {E}_{r}^{i} $≥320 严重
      下载: 导出CSV
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