中国地质学会岩矿测试技术专业委员会、国家地质实验测试中心主办

好氧不产氧光合细菌反馈作用下的五里峡水库坝前水体化学特征研究

宋昂, 彭文杰, 何若雪, 靳振江, 卢晓漩, 房君佳, 黄炳慧, 李强. 好氧不产氧光合细菌反馈作用下的五里峡水库坝前水体化学特征研究[J]. 岩矿测试, 2017, 36(2): 171-179. doi: 10.15898/j.cnki.11-2131/td.2017.02.011
引用本文: 宋昂, 彭文杰, 何若雪, 靳振江, 卢晓漩, 房君佳, 黄炳慧, 李强. 好氧不产氧光合细菌反馈作用下的五里峡水库坝前水体化学特征研究[J]. 岩矿测试, 2017, 36(2): 171-179. doi: 10.15898/j.cnki.11-2131/td.2017.02.011
Ang SONG, Wen-jie PENG, Ruo-xue HE, Zhen-jiang JIN, Xiao-xuan LU, Jun-jia FANG, Bing-hui HUANG, Qiang LI. Hydrochemistry Characteristics in front of the Wulixia Reservoir Dam Associated with Feedback from Aerobic Anoxygenic Phototrophic Bacteria[J]. Rock and Mineral Analysis, 2017, 36(2): 171-179. doi: 10.15898/j.cnki.11-2131/td.2017.02.011
Citation: Ang SONG, Wen-jie PENG, Ruo-xue HE, Zhen-jiang JIN, Xiao-xuan LU, Jun-jia FANG, Bing-hui HUANG, Qiang LI. Hydrochemistry Characteristics in front of the Wulixia Reservoir Dam Associated with Feedback from Aerobic Anoxygenic Phototrophic Bacteria[J]. Rock and Mineral Analysis, 2017, 36(2): 171-179. doi: 10.15898/j.cnki.11-2131/td.2017.02.011

好氧不产氧光合细菌反馈作用下的五里峡水库坝前水体化学特征研究

  • 基金项目:
    广西自然科学基金杰出青年基项目金(2015GXNSFGA139010);广西自然科学基金回国基金项目(2014GXNSFCA118012);中国地质科学院基本业务费项目(YYWF201505)
详细信息
    作者简介: 宋昂, 硕士研究生, 研究方向为岩溶生物地球化学。E-mail:2001140311@cugb.edu.cn
    通讯作者: 李强, 研究员, 主要从事岩溶生物地球化学研究。E-mail: glqiangli@163.com
  • 中图分类号: P641

Hydrochemistry Characteristics in front of the Wulixia Reservoir Dam Associated with Feedback from Aerobic Anoxygenic Phototrophic Bacteria

More Information
  • 微生物是水体生物地球化学循环的主要驱动者,也是能量代谢的主要参与者,在水体生态系统多样性与稳定性方面发挥着举足轻重的作用。好氧不产氧光合细菌(AAPB)是水体中一类分布广泛的重要功能类群,它们可利用光能补充自身能量代谢,并影响水体化学组分,其重要性被人们广泛认可并深入研究。为探讨岩溶区AAPB反馈作用下的五里峡水库坝前水体化学特征,本文对坝前不同层位水体进行实地监测,在获得不同层位水体溶解有机碳和颗粒有机碳稳定碳同位素特征的基础上,采用荧光定量PCR技术检测、研究了坝前水体不同层位AAPB分布规律。结果表明:取样期五里峡水库坝前水体为HCO3--Ca2+-Mg2+贫-中营养型;通过水体溶解氧、δ13CPOCδ13CDOC和碳氮比综合分析得出,坝前水体有机碳主要由微型生物产生;AAPB占总浮游细菌的相对丰度范围在1.33%~1.60%,且AAPB在不同层位的丰度变化强度要高于总浮游细菌的丰度变化强度,表明相较于总浮游细菌,AAPB对水化学特征的反馈作用更加敏感;使用典范对应分析可揭示水体理化性质与AAPB的内在联系,结果显示AAPB和总浮游细菌均受浊度的影响较大,故基于颗粒沉降的海洋微生物泵作用也适用于陆地岩溶水库。因而,AAPB反馈作用下的水化学特征对揭示CO2-水-碳酸盐岩-微生物代谢体系具有重要的启示意义。
  • 加载中
  • 图 1  五里峡水库坝前水体水化学Piper图

    Figure 1. 

    图 2  五里峡水库坝前水体环境指标与微生物丰度的典范对应分析

    Figure 2. 

    表 1  五里峡水库坝前水体的物理化学特征

    Table 1.  The physicochemical characterisitics of water sample in front of Wulixia Reservoir dam

    环境因子 层位 (m)
    0 2 4 6 8
    水温 (℃) 13.36 13.34 13.38 13.39 13.39
    Chla (μg/L) 0.87 3.02 2.66 3.20 4.59
    pH 7.97 7.88 7.83 7.82 7.79
    电导率 (μS/cm) 90.70 90.70 90.70 90.65 90.68
    DO (mg/L) 9.45 9.36 9.34 9.31 9.28
    浊度 (FNU) 4.58 4.34 4.65 4.30 6.23
    ORP (mV) 139.40 141.75 150.03 160.55 166.76
    TSI 23.08 36.64 35.29 37.29 41.22
    TDS (mg/L) 36.64 36.64 36.64 36.64 36.64
    硬度 (mg/L) 35.29 35.29 35.29 35.29 35.29
    DOC (mg/L) 1.22 1.13 1.16 0.98 0.98
    TOC (mg/L) 1.40 1.08 1.24 1.05 1.05
    TN (mg/L) 1.21 1.11 1.03 0.98 0.93
    K+ (mg/L) 0.63 0.65 0.62 0.67 0.65
    Na+(mg/L) 0.45 0.46 0.49 0.46 0.44
    Ca2+(mg/L) 14.78 15.80 14.60 12.89 12.58
    Mg2+(mg/L) 2.74 2.73 2.75 2.77 2.76
    Cl-(mg/L) 1.31 1.31 1.34 1.30 1.31
    SO4-(mg/L) 3.01 2.99 3.00 2.98 2.97
    HCO3-(mg/L) 51.55 51.55 51.55 44.68 44.68
    SIc -0.70 -0.73 -0.82 -0.93 -0.98
    SId -1.97 -2.07 -2.20 -2.38 -2.46
    pCO2(×10-6 Pa) 3.29 3.22 3.17 3.22 3.19
    注:pH、TSI、SIc和SId均为无量纲指标。
    下载: 导出CSV

    表 2  五里峡水库坝前水体碳同位素和C/N值

    Table 2.  Carbon isotope and C/N values of water sample in front of the Wulixia Reservoir dam

    层位 (m) δ13CPOC(‰) δ13CDOC(‰) C/N
    0 -29.65 -25.41 1.16
    2 -27.77 -24.08 0.97
    4 -29.09 -24.41 1.21
    6 -29.19 -25.48 1.08
    8 -29.79 -25.20 1.14
    下载: 导出CSV

    表 3  五里峡水库坝前水体16S rRNA与pufM基因归一化拷贝数

    Table 3.  The CNV of 16S rRNA and pufM genefrom water sample in front of the Wulixia Reservoir dam

    层位 (m) 16S rRNA总拷贝数×1010(拷贝/mL) 16S rRNA归一化拷贝数 pufM基因总拷贝数×108(拷贝/mL) pufM基因归一化拷贝数 p(AAPB)(%)
    0 6.50 0.20 10.40 0.22 1.60
    2 4.76 0.15 6.32 0.13 1.33
    4 7.55 0.24 11.30 0.24 1.50
    6 5.28 0.17 8.16 0.17 1.54
    8 7.69 0.24 11.50 0.24 1.49
    注:16S rRNA归一化拷贝数、pufM基因归一化拷贝数均为无量纲指标。
    下载: 导出CSV
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出版历程
收稿日期:  2016-12-16
修回日期:  2017-03-01
录用日期:  2017-03-25

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