ISSN 1000-3665 CN 11-2202/P

    微生物对海水入侵响应特征及指示意义的研究进展

    Research progress on the response characteristics and indicative significance of microorganisms to seawater intrusion

    • 摘要: 海水入侵是全球性环境地质问题,对沿海城市的供水安全及生态环境造成严重威胁。微生物对环境变化具有高度的敏感性,近年来许多学者开始关注微生物对海水入侵的响应特征,为海水入侵调查研究提供了新的思路与方法。为了充分认识该领域的研究进展,基于Web of Science 核心数据库,利用文献计量学可视化分析方法对海水入侵微生物响应特征研究现状、热点及趋势进行分析。文献分析结果表明:该新兴研究领域的成果集中出现在2011年以后,发文量和引文量呈现上升趋势;中国积极参与海水入侵微生物响应特征研究,其发文量及高引用指数均位居世界第二位,研究成果具有较高的学术影响力;由关键词聚类分析可知,该领域热门研究方向包括地下水微生物群落对海水入侵的响应研究、土壤微生物群落对海水入侵的响应研究、元素地球化学循环与微生物作用研究。研究结果表明:咸-淡水交互区微生物群落演替受盐度、溶解氧、温度、有机碳、pH值等多种因子的共同影响,其主控因子随水文地质条件的不同而变化;海水入侵会影响微生物介导的碳、氮、硫、铁等物质循环过程;在含水层中发现的典型海洋细菌及嗜盐古菌对海水入侵的识别具有重要指示意义,相关技术是海水入侵传统调查方法的有力补充,在古海水入侵、现代海水入侵的辨别应用中具有较大优势和潜力。

       

      Abstract: Seawater intrusion is a global environmental geological issue that poses a serious threat to the water supply security and ecological environment of coastal cities. Microorganisms exhibit a high sensitivity to environmental changes, and in recent years, numerous scholars have turned their attention to the response characteristics of microorganisms to seawater intrusion, offering new perspectives and methodologies for research in this field. To completely understand the research progress in this field, this study, based on the Web of Science core database, employed bibliometric visualization analysis methods to analyze the current status, hotspots, and trends of research on microbial response characteristics to seawater intrusion. The results indicate that significant developments in this emerging research area have mainly occurred after 2011, with a consistent increase in publication volume and citation counts. Chinese scholars actively engage in the research of microbial responses to seawater intrusion, ranking second in terms of both publication output and h-index, with a significant academic impact. Keyword cluster analysis reveals that popular research topics in this field encompass the response of groundwater microbial communities to seawater intrusion, investigations into soil microbial communities’ response to seawater intrusion, and the geochemical cycling of elements in conjunction with microbial processes. The study indicates that the succession of microbial communities in brackish-saline water transition zones is jointly influenced by factors such as salinity, dissolved oxygen, temperature, organic carbon, and pH. The primary controlling factors vary with hydrogeological conditions. The intrusion of seawater impacts microbial-mediated processes involved in the cycling of carbon, nitrogen, sulfur, iron, and other substances. The identification of typical marine bacteria and halophilic archaea found in aquifers holds significant indicative value concerning seawater intrusion. This serves as a potent complement to traditional investigative methods for seawater intrusion, offering substantial potential and advantages in distinguishing paleoseawater intrusion and seawater intrusion.

       

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