贵州纳朵洞滴水δ18O/δD的年际变化特征及其对ENSO的响应

王家录, 李维杰, 李廷勇. 贵州纳朵洞滴水δ18O/δD的年际变化特征及其对ENSO的响应[J]. 环境化学, 2020, (12): 3462-3470. doi: 10.7524/j.issn.0254-6108.2020071302
引用本文: 王家录, 李维杰, 李廷勇. 贵州纳朵洞滴水δ18O/δD的年际变化特征及其对ENSO的响应[J]. 环境化学, 2020, (12): 3462-3470. doi: 10.7524/j.issn.0254-6108.2020071302
WANG Jialu, LI Weijie, LI Tingyong. Interannual variations of drip water δ18O to δD Ratios in Naduo Cave of Guizhou and response to ENSO activities[J]. Environmental Chemistry, 2020, (12): 3462-3470. doi: 10.7524/j.issn.0254-6108.2020071302
Citation: WANG Jialu, LI Weijie, LI Tingyong. Interannual variations of drip water δ18O to δD Ratios in Naduo Cave of Guizhou and response to ENSO activities[J]. Environmental Chemistry, 2020, (12): 3462-3470. doi: 10.7524/j.issn.0254-6108.2020071302

贵州纳朵洞滴水δ18O/δD的年际变化特征及其对ENSO的响应

    通讯作者: 王家录, E-mail: lu226@163.com 李廷勇, E-mail: cdlity@163.com
  • 基金项目:

    贵州省科技合作计划项目(黔科合LH字[2016]7282号,黔科合LH字[2017]7059号)和贵州省科技计划院士工作站项目(黔科合平台人才[2016]5602)资助.

Interannual variations of drip water δ18O to δD Ratios in Naduo Cave of Guizhou and response to ENSO activities

    Corresponding authors: WANG Jialu, lu226@163.com ;  LI Tingyong, cdlity@163.com
  • Fund Project: Supported by the Science and Technology Cooperation Project (LH[2016]7282, LH[2017]7059) and the Academician Workstation of Science and Technology Plan (S&T Cooperation Platform Talents[2016]5602).
  • 摘要: 于2013年1月至2016年12月期间,对贵州纳朵洞洞内4处滴水和洞外降水的氢、氧稳定同位素(δ18O、δD)进行了4年的监测,发现滴水δ18O和δD都均匀地分布在当地大气降水线(LMWL)附近,说明大气降水是洞穴滴水的主要来源,且滴水δ18O和δD继承了当地大气降水δ18O和δD的信号.结合大气环流格局的分析,研究区大气降水δ18O和δD在监测时段内较好地响应了从El Niño向La Niña的转换.由于岩溶地下水的混合作用和包气带水的蒸发分馏,纳朵洞4处洞穴滴水δ18O和δD在雨季偏正,旱季偏负,与大气降水δ18O和δD旱季偏正,雨季偏负的特征相反;同时,滴水δ18O和δD在监测时段内对ENSO的响应,总体表现为在La Niña期间偏正,El Niño期间偏负,与大气降水δ18O和δD对La Niña和El Niño的响应情况也相反.因此,利用纳朵洞石笋δ18O记录研究古气候高分辨率的季节和年际变化,要充分考虑以上情况.
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  • 收稿日期:  2020-07-13
王家录, 李维杰, 李廷勇. 贵州纳朵洞滴水δ18O/δD的年际变化特征及其对ENSO的响应[J]. 环境化学, 2020, (12): 3462-3470. doi: 10.7524/j.issn.0254-6108.2020071302
引用本文: 王家录, 李维杰, 李廷勇. 贵州纳朵洞滴水δ18O/δD的年际变化特征及其对ENSO的响应[J]. 环境化学, 2020, (12): 3462-3470. doi: 10.7524/j.issn.0254-6108.2020071302
WANG Jialu, LI Weijie, LI Tingyong. Interannual variations of drip water δ18O to δD Ratios in Naduo Cave of Guizhou and response to ENSO activities[J]. Environmental Chemistry, 2020, (12): 3462-3470. doi: 10.7524/j.issn.0254-6108.2020071302
Citation: WANG Jialu, LI Weijie, LI Tingyong. Interannual variations of drip water δ18O to δD Ratios in Naduo Cave of Guizhou and response to ENSO activities[J]. Environmental Chemistry, 2020, (12): 3462-3470. doi: 10.7524/j.issn.0254-6108.2020071302

贵州纳朵洞滴水δ18O/δD的年际变化特征及其对ENSO的响应

    通讯作者: 王家录, E-mail: lu226@163.com ;  李廷勇, E-mail: cdlity@163.com
  • 1. 西南大学地理科学学院/岩溶环境重庆市重点实验室, 重庆, 400715;
  • 2. 安顺学院资源与环境工程学院, 安顺, 561000;
  • 3. 云南省高原地理过程与环境变化重点实验室, 云南师范大学地理学部, 昆明, 650500
基金项目:

贵州省科技合作计划项目(黔科合LH字[2016]7282号,黔科合LH字[2017]7059号)和贵州省科技计划院士工作站项目(黔科合平台人才[2016]5602)资助.

摘要: 于2013年1月至2016年12月期间,对贵州纳朵洞洞内4处滴水和洞外降水的氢、氧稳定同位素(δ18O、δD)进行了4年的监测,发现滴水δ18O和δD都均匀地分布在当地大气降水线(LMWL)附近,说明大气降水是洞穴滴水的主要来源,且滴水δ18O和δD继承了当地大气降水δ18O和δD的信号.结合大气环流格局的分析,研究区大气降水δ18O和δD在监测时段内较好地响应了从El Niño向La Niña的转换.由于岩溶地下水的混合作用和包气带水的蒸发分馏,纳朵洞4处洞穴滴水δ18O和δD在雨季偏正,旱季偏负,与大气降水δ18O和δD旱季偏正,雨季偏负的特征相反;同时,滴水δ18O和δD在监测时段内对ENSO的响应,总体表现为在La Niña期间偏正,El Niño期间偏负,与大气降水δ18O和δD对La Niña和El Niño的响应情况也相反.因此,利用纳朵洞石笋δ18O记录研究古气候高分辨率的季节和年际变化,要充分考虑以上情况.

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