福建宁化蛟湖岩溶湖地质成因

    Geological genesis of Jiaohu karst lake in Ninghua of Fujian Province

    • 摘要: 蛟湖岩溶湖位于福建省宁化县湖村盆地,是一种特殊类型的喀斯特地貌,其形成与气候条件、水文条件及地质历史演化关系密切,研究其地质成因是探明闽西北地区构造抬升和岩溶区地下水系发育演化过程的重要依据。在分析研究区地质背景及岩溶发育特征的基础上,采用以高密度电法为主,无人船多波束测深为辅的综合物探方法进行探测。通过高密度电法探测出隐伏岩溶构造的发育位置、空间形态特征及深度信息,确定蛟湖岩溶湖导水通道的分布和延伸情况,推测出2条主要的隐伏岩溶地下水径流带。通过无人船多波束测深系统扫描获取水下地形数据,构建了岩溶湖水下三维形态模型,探测出岩溶湖2条漏斗形通道的形态和位置,实现了导水通道的准确追踪和定位。查明了研究区2条隐伏岩溶地下水径流带走向及其与蛟湖的关系,分析了蛟湖导水补给通道及补给源,印证了蛟湖岩溶区具有地下水力联系紧密、通道复杂的特点。伴随着更新世以来的间歇性构造隆升,蛟湖地下水系统向深部径流,造成侵蚀基准面不断降低,促进地下水渗流的侵蚀作用而形成岩溶塌陷。蛟湖深部导水通道与地下水系统连通,是一种由潜蚀-重力塌陷机制形成的特殊岩溶湖。对蛟湖形成影响因素和地质成因机理的研究成果可为特殊岩溶景观资源的保护与利用提供科学依据。

       

      Abstract: Jiaohu karst lake is located in Hucun Basin of Ninghua County in Fujian Province. It is a special type of karst landform, and the formation of karst lakes is closely related to its climatic conditions, hydrological conditions and geological history. The geological genesis of Jiaohu karst lake is an important basis for studying the tectonic uplift and the development and evolution of underground water systems in karst areas of the northwest Fujian Province. Through analyzing the geological background and karst development characteristics, the authors adopted a comprehensive geophysical exploration method based on high-density electrical method and multibeam bathymetry system for unmanned vessels. The tectonic development location, spatial morphological characteristics and depth information of hidden karst were detected by high-density electrical method. The distribution and extension of water flowing channel in Jiaohu karst lake were detected and two hidden karst groundwater run-off bands were presumed. The underwater terrain data was obtained by scanning the multibeam bathymetry system for unmanned vessels, and the underwater three-dimensional morphological model of the karst lake was constructed. The shape and position of two infundibula form channels in the karst lake were detected to realize the accurate tracking and positioning of the water flowing channels. The trend of two concealed karst groundwater runoff zones in the study area and their relationship with Jiao karst lake were identified, and the water supply channel and supply source of Jiao Lake were analyzed, indicating that the karst area of Jiao lake had close connection with groundwater system and the karst channels were complex. With the intermittent tectonic uplifting since Pleistocene, the groundwater system flowed to the deep, resulting in the reducing erosion base level. This would further cause karst collapse formed by the erosion of groundwater seepage. The deep water flowing channels were connected with underground water, which was a special karst lake formed by water-creep and gravitational-collapse mechanism. The research achievements about the infuencing factors of Jiaohu's formation and its geological genetic mechanism could provide scientific basis for the protection and utilization of special karst landscape resources.

       

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